HomeMy WebLinkAboutLucknow - Harnett County DRB Application (1)Lucknow Solar Project
Development Review Board Application
Prepared by:
Lucknow Solar, LLC
3400 W. Leigh Street
Richmond, VA 23230
November 12, 2025
c/o Jay Sikes, Manager of Planning Services
Harnett County Planning Department
420 McKinney Parkway,
Lillington, NC 27546
Re: Development Review Board Application – Lucknow Solar, LLC
Dear Mr. Sikes,
Please find enclosed the submittal of Lucknow Solar, LLC’s development review board
(DRB) application. Lucknow Solar is a 70 MWac solar energy system proposed in Harnett
County and the town of Erwin, North Carolina’s extraterritorial jurisdiction. Harnett County
issued a special use permit for the Lucknow Solar project on November 13, 2023.
To support a full review, this DRB application includes the following documents:
- Attachment A: Application Form
- Attachment B: Site Plan
- Attachment C: Stormwater Management Statement
- Attachment D: USGS Quadrangles Map
- Attachment E: NRCS Soil Report
- Attachment F: Site Zoning Map
- Attachment G: Deeds
- Attachment H: SUP Application (September 2023)
- Attachment I: SUP Approval (November 2023)
We look forward to the continued engagement with Harnett County to answer questions and
offer any needed clarity during the review process. The AES team is available to meet or talk
at your convenience.
Respectfully,
Anne Kelly
Senior Analyst - Permitting
anne.kelly@aes.com
Lucknow Solar DRB Application
ATTACHMENT A
Application Form
11/12/2025
Lucknow Solar DRB Application
ATTACHMENT B
Site Plan
BABABABABABABABABABABABABABABABABABABABABABABABABABABA BA
BABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABA BABABABABABABABABABABABABABABABA
BABABABABABABABABABA BABA
B
A
BABABABABABA
BABABABABABABABABABABABABA
BA
BA
BA
BA
BA
BA
BA
BA
BA
BA
BA
BA
BA
BA
BABABA
BABABABABABABABABABABABA
BA
BABABA
BABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABA
BABABABABABABABABABABABABA
BABA BA
BAB
A
B
A
BA
BA
BA
BA BABABA
BA
BA
B
ABA BABABABABABABABA BABABABABABABABABABABABABABABABABABA
BABABABA
BABA BABABABABA BA BA BA BABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABABA
BA
BABABABA
BABABA
BABABABABA BABABABABA BABABABABABA
BABABA
BA
BABA BABABA
BA
BA
BA
BA
BA
BA
BABABABA
BA
BABABABABABABABABABABABABABABABABABABABABABA BABABABABABAOHEOHEOHE OHE OHE
OHEOHEOHEOHEOHEOHE
OHEOHEOHEOHEOHEOHEOHEOHEOHEOHEOHEOHE
OHE
OHE
OHE
OHE
OHE
OHE
OHE
OHE
OHE
OHE
OHE OHE OHE OHE OHEOHEOHEOHEOHE OHEXXXXXXXXXXXX
X
X
X
X X XXXXXXXXX XXX XXXXX
X
X
X
XX
XXXXXXXXDMVMVMVMVMVMVMVMVMVMVMVMVMVMVMV
MVMVMVMVMVMVMVMVMVMVMVMVMVMV MV MV MV MV
MVMVXXXXX
X
X
X
X X XXXXXXXXXXXXXXXXXXXXXXXX
XXX
XX
XXX
X
X XXX
X
X
X
X
X
XXX
XX
XXX
XXX50' WATERBODYSETBACK (TYP.)50' WETLANDSETBACK (TYP.)50' STREAMSETBACK (TYP.)50' FRONT SETBACK35' FRONT SETBACK25' SIDE SETBACKTX 2.A.1TX 2.A.5TX 2.A.2TX 2.A.3TX 2.A.4TX 2.B.2TX 2.B.1TX 1.B.2TX 1.B.3TX 1.B.4TX 1.B.5TX 2.B.3TX 2.B.5TX 2.B.4155'152'155'164'170'175'180'180'170'1
5
8
'
165
'177'175'179'178'175'175'EEEEDATEPLOTTED: 9/15/2025 11:33 AMC:\AESCloud\Box\2. Projects\SERC - NC\Lucknow\4. Engineering\4. Design Sets\4.4.1 Dev Eng CAD\4.4.1.3 System Layout\Lucknow 10 Pcnt-PV-E.01.01-Overall Electrical Plan-Harnett County Side Only.dwg
2180 South 1300 East, Suite 600Salt Lake City, UT 84106-2749(801) 679 - 3500PROJECT TITLE:DESCRIPTIONXREFs: .\Lucknow 10 Pcnt-PV-Constraints Map.dwg; .\Lucknow-PV-Base-Delineation.dwg; .\Lucknow-PV-Base-ALTA.dwg; .\Lucknow-PV-Base-Hydrology.dwg
APV:PROJECT LOCATION:NO.KEY PLAN:PE STAMP:REVISIONS:SHEET NO:REV:SCALE AT 24" x 36":CHK:DWN:DES:DATE:PROJNUM:AES Titleblock 24X36 v210209
SHEET TITLE & DESCRIPTION:LUCKNOW791 DORMAN ROAD,DUNN, NC 2833435.2689, -78.6578OVERALL ELECTRICALPLAN70 MW AC28 MW / 4 HR BESSS. BARR ENGELA. CASABUENAC. SANCHEZ06/06/2024PV-E.01.012006/04/2023INITIAL 5% DESIGN109/05/2023REVISED 5% DESIGN206/06/2024INITIAL 10% DESIGNEXISTINGLEGENDGENERAL NOTESSHEET NOTESSITE ENTRANCE W/ 20' GATEEPV PANELSPROPOSEDXFMR SKIDSITE INPUT OR STUDYDESKTOPBASEDFIELDSTUDYDATEPROJECT BOUNDARYX02/09/2024TOPOGRAPHYX02/09/2024WETLAND DELINEATIONX07/25/2023FLOOD INUNDATION AREAX04/08/2024TREE HEIGHTSN/AN/AGEOTECHX05/01/2023EXISTING UTILITIES & EASEMENTSX02/09/2024HYDROLOGY**X04/08/2024T&E SPECIESX07/25/2023ARCHEOLOGICAL STUDYX07/17/2023CUP / SUP / AHJ REQUIREMENTSN/AN/ASTUDIES INCORPORATEDFOR ADDITIONAL INFORMATION, INCLUDING THE SOURCE OF STUDIES/INPUTS, REFER TO THE DUE DILIGENCE MEMO. STUDIES MARKED 'N/A' ARE NOT NEEDED FOR THIS PROJECT. STUDIES MARKED 'TBD' HAVE NOT BEEN INCORPORATED. WASH / DRAINAGEPOWER LINE ROWOVERHEAD TRANSMISSION LINEOHEOHEBABABABABABAINTERIOR ROADSLAYDOWN AREA5' MAJOR CONTOURSAPPROXIMATE WETLANDXXXXXBUILDABLE AREAADJACENT PARCELSYSTEM DETAILS1.THIS DRAWING IS PRELIMINARY AND FOR ESTIMATING PURPOSES ONLY.IT IS NOT FOR CONSTRUCTION.2.LOCATION OF ALL EXISTING ITEMS IS APPROXIMATE AND MUST BEVERIFIED IN THE FIELD PRIOR TO CONSTRUCTION.3.ALL SPECIFIED EQUIPMENT IS PRELIMINARY. FINAL EQUIPMENTSELECTION SHALL BE APPROVED BY OWNER.AES PARCEL SETBACKAES PARCEL BOUNDARY100-YEAR FLOOD (1.5' INUNDATION)SLOPE KEEPOUTWASH / DRAINAGE SETBACKWATERBODYWATERBODY SETBACKWETLAND SETBACKBUILDING1' MINOR CONTOURSAES SUBSTATIONMAJOR PUBLIC ROADROAD RIGHT-OF-WAYFENCEOVERHEAD GEN-TIE LINEPROVISIONS FOR 4' DEEPWATER QUALITY MANAGEMENTUTILITY SWITCHYARDBUILDING SETBACK0300'600'900'1,200'1" = 600'AC CAPACITY AT POI70.0 MWDC CAPACITY94.0 MWDC:AC RATIO AT POI1.34DESIGN TEMPERATURE36.1° CJINKO 590W MODULE COUNT159,327STRING SIZE27 MODULESPITCH22.00'INTER-ROW SPACING (MODULE TO MODULE)14.54'GCR34.0%SUNGROW SG4400UD PCS COUNT19PCS NAMEPLATE RATING4.4 MVADERATED PCS CAPACITY4.154 MVARACKING TYPENEXTRACKER 1PTRACKER MOTOR COUNT1,8802 STRING TRACKER ROWS5763 STRING TRACKER ROWS4674 STRING TRACKER ROWS837BESS CAPACITY AT POI28.0 MWBESS DURATION4 HRBESS INSTALLED ENERGY, BOL156.4 MWhBESS INSTALLED ENERGY, EOL120.7 MWhBATTERY MODULE (MANUF - MODEL)SAMSUNG SDI E5SBATTERY STRING LENGTH (# OF MODULES)12STRINGS PER CONTAINER15 - 16CONTAINER TYPECEN 40'CONTAINER COUNT26BESS PCS SUNGROW SG3450UD COUNT13BESS PCS NAMEPLATE RATING3.45 MVATOTAL PARCEL ACREAGE963.6LINEAR FEET OF FENCE69,161'FENCED ACREAGE480.8NUMBER OF SITE ENTRANCES11NUMBER OF DIRECTION BORINGS2LINEAR FEET OF INTERIOR ROADS17,450'LINEAR FEET OF MV CIRCUIT/TRENCH28,471'LAYDOWN AREA (ACRES)20.8WATER QUALITY MANAGEMENT TOTAL AREA(ACRES)15.0PRELIMINARYNOT FOR CONSTRUCTIONNDBDIRECTIONAL BORINGTREELINEHARNETT COUNTY BOUNDARY30' LANDSCAPE BUFFER
Lucknow Solar DRB Application
ATTACHMENT C
Stormwater Management Statement
Stormwater Management Statement
Project Overview
Lucknow Solar, LLC, a subsidiary of AES Clean Energy (“AES”) is proposing the ‘Lucknow Solar’ energy
project at 791 Dorman Road (State Highway 177) in both Harnett County and the southeastern portion
of the Town of Erwin’s ETJ, North Carolina. Lucknow Solar is centered along Doorman Road between
Middle Road and Arrowhead Road, with the extents of the project shown on the provided “Overall
Electrical Plan” Drawn by AES last revised June 6, 2024.
Existing Site Conditions
The 962-acre development area is primarily used for agricultural purposes today. Ground cover
consists of mainly agricultural fields, with portions of the development area being wooded, wetlands or
existing farm access roads.
The topography of the site is generally flat with stormwater draining to the east directly to the Black
River or draining southeast to unnamed tributaries and roadside ditches ultimately leading to the Black
River. (Refer to Attachment D for USGS Quadrangles Map)
Existing onsite soils within the development area are primarily well or moderately well drained made up
of sandy or silty loams. Outside of the development area, within the site boundaries, soil conditions vary
from well-draining soils to poorly drained soils in areas of avoided onsite wetlands and flood plains.
(Refer to Attachment E for NRCS soil report)
Wetlands located within the site are primarily freshwater forested/ shrub wetlands and Palustrine
Forested wetlands adjacent to the Black River and along its unnamed tributaries. Within the
northeastern portion of the site there exist freshwater ponds, Palustrine Emergent wetlands along with
ephemeral and intermittent streams. These features have been identified on the “Overall Electrical
Plan” and maintain a 50 foot buffer from any proposed disturbance. Stormwater runoff reaches these
features today via overland and shallow concentrated flow
The eastern boundary of the site along the Black River is within the Conservation Zoning district. No
improvements or development associated with this project are proposed for the area within the
Conservation Zoning District. (Refer to Attachment F for the Site Zoning Map)
Proposed Site Conditions
The proposed development will be designed to mimic the existing drainage patterns and reduce or
maintain the discharge from existing to post development conditions. This will primarily be achieved
through the reduction of stormwater runoff from the change in site use. Comparing similar soil types and
conditions from agricultural to meadow land use will reduce the runoff coefficient allowing more
stormwater to permeate into the soils and maintain overland and shallow concentrated flow to wetlands
and site boundaries.
The guidance outlined in NCDEQ section E-6 will be applied to the project allowing the solar panels to
be considered pervious.
Impervious areas from the proposed site development will primarily consist of gravel access roads,
concrete invertor pads along with temporary and permanent laydown yards. Currently the development
proposes approximately 30 acres of impervious cover, approximately 6.3%, of the total site development.
This number may vary slightly as site engineering progresses.
Based on the reduction in runoff from change in land use no negative downstream or offsite impacts are
anticipated. Currently the design proposes onsite infiltration basins, as shown on the “Overall Electric
Plan”; these basins may change in size or be removed as the stormwater design evolves to ensure the
required treatment and storage volumes are achieved prior to final permit issuance.
Due to the general “uphill” nature of the site stormwater run-on is anticipated to be minimal. No diversion
swales are anticipated or proposed at this time.
Lucknow Solar DRB Application
ATTACHMENT D
USGS Quadrangles Map
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│―│―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│
―│―│
―│
―│
―│―│―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│―│
―│
―│―│―│―│―│
―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│
―│
―│―│
―│―│
―│
―│―│
―│
―│
―│
―│―│―│―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│―│―│
―│
―│―│―│―│―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│―│―│―│―│
―│―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│―│―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│―│
―│―│
―│
―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│―│―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│―│―│―│
―│
―│―│―│―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│
―│
―│
―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│―│
―│
―│
―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│―│―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│―│―│―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│―│―│
―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│
―│―│
―│
―│
―│―│―│―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│―│―│
―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│―│―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│―│―│―│―│―│
―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│
―│―│―│―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│―│―│―│―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│―│―│―│―│
―│―│
―│―│
―│
―│―│
―│―│
―│
―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│―│
―│―│
―│
―│
―│
―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│―│
―│―│―│―│
―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│―│
―│―│―│―│―│―│―│
―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│―│―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│―│
―│―│
―│―│
―│
―│
―│
―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│―│
―│―│―│
―│
―│―│
―│―│
―│
―│
&PO
&PO
!"
!"
^;▄n▄n ▄n
▄n ▄n
▄n▄n
F
F
H100200200200
200
200200100100100100150150150
150200
15
0
1
5
0
75200
200200200
200100
10020
0
200
2
0
0
150150
150
15015
0
100100
10
0 1001001
0
0
200200
15015
0 2502
5
0
2002002002002
0
0
200200
20
0
20020015
0
150
150
150
150100100100100
100
150150
20020020
0
200200200200200
200
200
200 25020
0
200
200200 2
0
0
200
150
150150150150200200250200250100100 100100
100100 100100
100100 150150150
150150
150100100
1
0
0
100
100100100100100COVINGTONRDHORSESHOE B
E
N
D
R
DROSSRD
CLERVIE DR
HOLIDAY
RD
BALL PARK L
N
LOOP RDMILL RD£¤421
DUKE RD
CO
U
N
T
R
Y
S
P
R
I
N
G
L
N
HALL RD
GREENFORES
T
CIRCRAWFORDRDMONROELN
PROSPECTCHURCHRD
DRY FAR
M
L
N
NTWHITTINGTONLANEERWIN CHAP
E
L
R
D
§¨¦95
£¤301
¬«82
¬«1860
¬«217
¬«55
¬«1779
¬«217
¬«217
THREE BRIDGE RD
W PO
P
E
S
T
A N T IO C H C H URCHRDERWIN RD
SU
SAN
TART
RD
E K ST
S 14TH STS
1
2
TH
S
T
R
I
V
E
RBLUFFDRNOLD POST RD RED HILL CHURCH RDBEAVER DAM RD
B
E
A
V
E
R
D
A
M
R
D WARRENRDDENIMDRN 12TH STN 10TH STGLENEAGLESAVE
LUCASRD
E J ST
E D STW D ST
W K ST
E H S
T
W C STJERRY LNS POWELL AVEW
ONDERTO
W
N
DR
E I ST
TILGHMANDRARMSTRONG STDYNASTYLN N POWELL AVEBUTCH STNORRIS RD
S
A
I
N
T
M
A
T
T
H
E
W
S
R
D
PORTER DRWIL
S
O
N
L
U
C
A
S
R
D
BUNNLEVEL ERWIN RD
CHICKEN FARM RDERWINACCESSRD
HOG HEAVEN LNALPHIN
RD
W THORNTON RD
MACGRUDER RD
ANT
I
O
C
H
C
H
U
R
C
H
R
D
NC 82N
C
8
2NC 55 EBURNETT RDW CUMBE
R
L
A
N
D
S
T
EJACKSONBLVD
£¤301
£¤421
WOOD RDNEW PATH RDW BLACKMAN RDG LENEAGLERDMAIN ST NC 217£¤421 NTW HITTINGT ON LA N EPUMPSTATIO
N
R
DRAYMOND AV
E
RYRDC
HI
C
OR
ARDWARRENBAITFARMRDCOVINGTON RDASHEAVEGLENNRUTHLN
S 8TH STN 11TH STN 14TH STBRYA NT RDW
J
S
T
W A ST
W E ST
BRIDGEWA
T
E
R
D
R BUTLER DR
R
O
S
S
RDW F ST
PECA
N
L
NBRUCE DRTURLINGTONRD
HOMERS LN OL
D
H
AM
I
L
TO
N
R
D
BUMPAS CR E E K A C C
BUNNLEVEL ERWIN RD
JOHN
L
E
E
R
D
TH
R
E
E
B
R
I
D
G
E
R
D
MIDDLE
RDS13THSTNC 217¬«82
¬«82
¬«55217
¬«55
¬«217
¬«55
TITAN ROBER
T
S
R
D
TITAN
R
O
B
E
R
T
S
RDW AYNELN
AVERY RD
AS
H
E
A
V
E
SU
G
G
S
R
D
W B ST
BAIT R DBYRDSMILLRDBYR
D
S
M
I
L
L
R
D MAYNARD LAKE RDGENTRY RDARROWHEAD RDCADE STEVENS
O
N
L
N
OLD SILO LN
M C IN T Y R E LN
CRAB APPLE LN
L
E
A
N
N
A
L
N
PRVT
D
RI
V
E
WAYO
L
D
ST
A
G
E
R
D
S DANIELS RDDORMA
N
R
DN 13TH STKINGSW
AYDRBUDHAWKINSRDFRIE
N
D
L
Y
R
D
JWEDWARDSLNHARNETT COCUMBERLAND CO
HARNETT COCUMBERLAND COHARNETTCOCUMBERLANDCO
J u n ip e r C r BlackRiverLittleR iv e r StewartCreekCape Fear
R
iver
C
a
p
e
F
e
a
r
R
i
v
e
r
BlackRive
r
Ste
wartCrJuniper CrCapeFearRiver
Ca
p
e
F
e
a
r
R
iv
er
T h o rn ton sCrBeaverdamSw
a
mp
CanalU p p e r L itt le R i v e r
Black RiverJernigansPond
LittleRiver
BlackRiverGreenwoodCem
AverasboroCem
Linden
DUNN
Turlington
Erwin
05
06
07
08
09
10
11
12
13
14
15
04
3916000mN
05
06
07
08
09
10
11
12
13
14
15
16
3904000mN
17
06 07 08 09 10 11 12 13 14 1505 716000mE
06 07 08 09 10 11 12 13 14705000mE 15
35.2500°
35.3750°-78.7500°-78.6250°35.3750°
35.2500°-78.6250°-78.7500°NSN.NGA REF NO.*7643016378723*U S G S X 2 4 K 1 4 5 1 97 6 4 3 0 1 6 3 7 8 7 2 3
NORTHCAROLINA
8
5
7
4
6
321
QUADRANGLE LOCATION
ERWIN QUADRANGLENORTH CAROLINA7.5-MINUTE SERIES
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY
×
Ø GN
MN
1°20´24 MILS
9°7´162 MILS
UTM GRID AND 2019 MAGNETIC NORTHDECLINATION AT CENTER OF SHEET
QV
Grid Zone Designation17S
U.S. National Grid100,000 - m Square ID
1 Lillington
8 Mingo
2 Coats3 Benson4 Bunnlevel5 Dunn6 Slocomb7 Wade
ADJOINING QUADRANGLES
Imagery.....................................................NAIP, September 2020 - September 2020Roads......................................... U.S. Census Bureau, 2016Names............................................................................GNIS, 1980 - 2022Hydrography...............................National Hydrography Dataset, 2005 - 2018Contours............................................National Elevation Dataset, 2008Boundaries..............Multiple sources; see metadata file 2019 - 2021
Wetlands.................FWS National Wetlands Inventory Not Available
North American Datum of 1983 (NAD83)World Geodetic System of 1984 (WGS84). Projection and1 000-meter grid:Universal Transverse Mercator, Zone 17S
Produced by the United States Geological Survey
This map is not a legal document. Boundaries may begeneralized for this map scale. Private lands within governmentreservations may not be shown. Obtain permission beforeentering private lands.
This map was produced to conform with the National Geospatial Program US Topo Product Standard.
CONTOUR INTERVAL 10 FEETNORTH AMERICAN VERTICAL DATUM OF 1988
SCALE 1:24 000
1000 500 0 METERS 1000 2000
21KILOMETERS00.51
1 0.5 0
MILES
1
1000 0 1000 2000 3000 4000 5000 6000 7000 8000 9000 10000
FEET
ERWIN, NC
2022
Expressway Local Connector
ROAD CLASSIFICATION
Ramp 4WDSecondary Hwy Local Road
Interstate Route State RouteUS RouteWX./
Approximate Project
Boundary
Lucknow Solar DRB Application
ATTACHMENT E
NRCS Soil Report
United States
Department of
Agriculture
A product of the National
Cooperative Soil Survey,
a joint effort of the United
States Department of
Agriculture and other
Federal agencies, State
agencies including the
Agricultural Experiment
Stations, and local
participants
Custom Soil Resource
Report for
Harnett County,
North CarolinaNatural
Resources
Conservation
Service
October 9, 2025
Preface
Soil surveys contain information that affects land use planning in survey areas.
They highlight soil limitations that affect various land uses and provide information
about the properties of the soils in the survey areas. Soil surveys are designed for
many different users, including farmers, ranchers, foresters, agronomists, urban
planners, community officials, engineers, developers, builders, and home buyers.
Also, conservationists, teachers, students, and specialists in recreation, waste
disposal, and pollution control can use the surveys to help them understand,
protect, or enhance the environment.
Various land use regulations of Federal, State, and local governments may impose
special restrictions on land use or land treatment. Soil surveys identify soil
properties that are used in making various land use or land treatment decisions.
The information is intended to help the land users identify and reduce the effects of
soil limitations on various land uses. The landowner or user is responsible for
identifying and complying with existing laws and regulations.
Although soil survey information can be used for general farm, local, and wider area
planning, onsite investigation is needed to supplement this information in some
cases. Examples include soil quality assessments (http://www.nrcs.usda.gov/wps/
portal/nrcs/main/soils/health/) and certain conservation and engineering
applications. For more detailed information, contact your local USDA Service Center
(https://offices.sc.egov.usda.gov/locator/app?agency=nrcs) or your NRCS State Soil
Scientist (http://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/contactus/?
cid=nrcs142p2_053951).
Great differences in soil properties can occur within short distances. Some soils are
seasonally wet or subject to flooding. Some are too unstable to be used as a
foundation for buildings or roads. Clayey or wet soils are poorly suited to use as
septic tank absorption fields. A high water table makes a soil poorly suited to
basements or underground installations.
The National Cooperative Soil Survey is a joint effort of the United States
Department of Agriculture and other Federal agencies, State agencies including the
Agricultural Experiment Stations, and local agencies. The Natural Resources
Conservation Service (NRCS) has leadership for the Federal part of the National
Cooperative Soil Survey.
Information about soils is updated periodically. Updated information is available
through the NRCS Web Soil Survey, the site for official soil survey information.
The U.S. Department of Agriculture (USDA) prohibits discrimination in all its
programs and activities on the basis of race, color, national origin, age, disability,
and where applicable, sex, marital status, familial status, parental status, religion,
sexual orientation, genetic information, political beliefs, reprisal, or because all or a
part of an individual's income is derived from any public assistance program. (Not
all prohibited bases apply to all programs.) Persons with disabilities who require
2
alternative means for communication of program information (Braille, large print,
audiotape, etc.) should contact USDA's TARGET Center at (202) 720-2600 (voice
and TDD). To file a complaint of discrimination, write to USDA, Director, Office of
Civil Rights, 1400 Independence Avenue, S.W., Washington, D.C. 20250-9410 or
call (800) 795-3272 (voice) or (202) 720-6382 (TDD). USDA is an equal opportunity
provider and employer.
3
Contents
Preface....................................................................................................................2
How Soil Surveys Are Made..................................................................................5
Soil Map..................................................................................................................8
Soil Map................................................................................................................9
Legend................................................................................................................10
Map Unit Legend................................................................................................11
Map Unit Descriptions........................................................................................12
Harnett County, North Carolina.......................................................................14
AtA—Altavista fine sandy loam, 0 to 3 percent slopes, rarely flooded,
Southern Coastal Plain.........................................................................14
Au—Augusta fine sandy loam, rarely flooded.............................................15
AyA—Aycock silt loam, 0 to 2 percent slopes.............................................16
AyB—Aycock silt loam, 2 to 6 percent slopes.............................................17
Bb—Bibb soils, frequently flooded..............................................................18
Co—Coxville loam.......................................................................................20
ExA—Exum very fine sandy loam, 0 to 2 percent slopes............................21
GoA—Goldsboro loamy sand, 0 to 2 percent slopes, Southern Coastal
Plain......................................................................................................23
Gr—Grantham loam....................................................................................24
Ly—Lynchburg sandy loam, 0 to 2 percent slopes......................................26
MaA—Marlboro sandy loam, 0 to 2 percent slopes....................................27
MaB—Marlboro sandy loam, 2 to 6 percent slopes....................................28
Na—Nahunta loam......................................................................................29
NoA—Norfolk loamy sand, 0 to 2 percent slopes........................................31
NoB—Norfolk loamy sand, 2 to 6 percent slopes........................................32
OrB—Orangeburg loamy sand, 2 to 6 percent slopes................................34
Pd—Pits-Dumps complex...........................................................................35
Ps—Portsmouth loam, rarely flooded..........................................................36
Ra—Rains sandy loam, 0 to 2 percent slopes............................................37
StA—State fine sandy loam, 0 to 3 percent slopes, rarely flooded.............39
To—Toisnot loam.........................................................................................40
W—Water....................................................................................................42
References............................................................................................................43
4
How Soil Surveys Are Made
Soil surveys are made to provide information about the soils and miscellaneous
areas in a specific area. They include a description of the soils and miscellaneous
areas and their location on the landscape and tables that show soil properties and
limitations affecting various uses. Soil scientists observed the steepness, length,
and shape of the slopes; the general pattern of drainage; the kinds of crops and
native plants; and the kinds of bedrock. They observed and described many soil
profiles. A soil profile is the sequence of natural layers, or horizons, in a soil. The
profile extends from the surface down into the unconsolidated material in which the
soil formed or from the surface down to bedrock. The unconsolidated material is
devoid of roots and other living organisms and has not been changed by other
biological activity.
Currently, soils are mapped according to the boundaries of major land resource
areas (MLRAs). MLRAs are geographically associated land resource units that
share common characteristics related to physiography, geology, climate, water
resources, soils, biological resources, and land uses (USDA, 2006). Soil survey
areas typically consist of parts of one or more MLRA.
The soils and miscellaneous areas in a survey area occur in an orderly pattern that
is related to the geology, landforms, relief, climate, and natural vegetation of the
area. Each kind of soil and miscellaneous area is associated with a particular kind
of landform or with a segment of the landform. By observing the soils and
miscellaneous areas in the survey area and relating their position to specific
segments of the landform, a soil scientist develops a concept, or model, of how they
were formed. Thus, during mapping, this model enables the soil scientist to predict
with a considerable degree of accuracy the kind of soil or miscellaneous area at a
specific location on the landscape.
Commonly, individual soils on the landscape merge into one another as their
characteristics gradually change. To construct an accurate soil map, however, soil
scientists must determine the boundaries between the soils. They can observe only
a limited number of soil profiles. Nevertheless, these observations, supplemented
by an understanding of the soil-vegetation-landscape relationship, are sufficient to
verify predictions of the kinds of soil in an area and to determine the boundaries.
Soil scientists recorded the characteristics of the soil profiles that they studied. They
noted soil color, texture, size and shape of soil aggregates, kind and amount of rock
fragments, distribution of plant roots, reaction, and other features that enable them
to identify soils. After describing the soils in the survey area and determining their
properties, the soil scientists assigned the soils to taxonomic classes (units).
Taxonomic classes are concepts. Each taxonomic class has a set of soil
characteristics with precisely defined limits. The classes are used as a basis for
comparison to classify soils systematically. Soil taxonomy, the system of taxonomic
classification used in the United States, is based mainly on the kind and character
of soil properties and the arrangement of horizons within the profile. After the soil
5
scientists classified and named the soils in the survey area, they compared the
individual soils with similar soils in the same taxonomic class in other areas so that
they could confirm data and assemble additional data based on experience and
research.
The objective of soil mapping is not to delineate pure map unit components; the
objective is to separate the landscape into landforms or landform segments that
have similar use and management requirements. Each map unit is defined by a
unique combination of soil components and/or miscellaneous areas in predictable
proportions. Some components may be highly contrasting to the other components
of the map unit. The presence of minor components in a map unit in no way
diminishes the usefulness or accuracy of the data. The delineation of such
landforms and landform segments on the map provides sufficient information for the
development of resource plans. If intensive use of small areas is planned, onsite
investigation is needed to define and locate the soils and miscellaneous areas.
Soil scientists make many field observations in the process of producing a soil map.
The frequency of observation is dependent upon several factors, including scale of
mapping, intensity of mapping, design of map units, complexity of the landscape,
and experience of the soil scientist. Observations are made to test and refine the
soil-landscape model and predictions and to verify the classification of the soils at
specific locations. Once the soil-landscape model is refined, a significantly smaller
number of measurements of individual soil properties are made and recorded.
These measurements may include field measurements, such as those for color,
depth to bedrock, and texture, and laboratory measurements, such as those for
content of sand, silt, clay, salt, and other components. Properties of each soil
typically vary from one point to another across the landscape.
Observations for map unit components are aggregated to develop ranges of
characteristics for the components. The aggregated values are presented. Direct
measurements do not exist for every property presented for every map unit
component. Values for some properties are estimated from combinations of other
properties.
While a soil survey is in progress, samples of some of the soils in the area generally
are collected for laboratory analyses and for engineering tests. Soil scientists
interpret the data from these analyses and tests as well as the field-observed
characteristics and the soil properties to determine the expected behavior of the
soils under different uses. Interpretations for all of the soils are field tested through
observation of the soils in different uses and under different levels of management.
Some interpretations are modified to fit local conditions, and some new
interpretations are developed to meet local needs. Data are assembled from other
sources, such as research information, production records, and field experience of
specialists. For example, data on crop yields under defined levels of management
are assembled from farm records and from field or plot experiments on the same
kinds of soil.
Predictions about soil behavior are based not only on soil properties but also on
such variables as climate and biological activity. Soil conditions are predictable over
long periods of time, but they are not predictable from year to year. For example,
soil scientists can predict with a fairly high degree of accuracy that a given soil will
have a high water table within certain depths in most years, but they cannot predict
that a high water table will always be at a specific level in the soil on a specific date.
After soil scientists located and identified the significant natural bodies of soil in the
survey area, they drew the boundaries of these bodies on aerial photographs and
Custom Soil Resource Report
6
identified each as a specific map unit. Aerial photographs show trees, buildings,
fields, roads, and rivers, all of which help in locating boundaries accurately.
Custom Soil Resource Report
7
Soil Map
The soil map section includes the soil map for the defined area of interest, a list of
soil map units on the map and extent of each map unit, and cartographic symbols
displayed on the map. Also presented are various metadata about data used to
produce the map, and a description of each soil map unit.
8
9
Custom Soil Resource Report
Soil Map
3906700390710039075003907900390830039087003909100390710039075003907900390830039087003909100711800 712200 712600 713000 713400 713800 714200 714600 715000 715400
711800 712200 712600 713000 713400 713800 714200 714600 715000 715400
35° 18' 12'' N 78° 40' 22'' W35° 18' 12'' N78° 37' 46'' W35° 16' 49'' N
78° 40' 22'' W35° 16' 49'' N
78° 37' 46'' WN
Map projection: Web Mercator Corner coordinates: WGS84 Edge tics: UTM Zone 17N WGS84
0 500 1000 2000 3000
Feet
0 250 500 1000 1500
Meters
Map Scale: 1:18,000 if printed on A landscape (11" x 8.5") sheet.
MAP LEGEND MAP INFORMATION
Area of Interest (AOI)
Area of Interest (AOI)
Soils
Soil Map Unit Polygons
Soil Map Unit Lines
Soil Map Unit Points
Special Point Features
Blowout
Borrow Pit
Clay Spot
Closed Depression
Gravel Pit
Gravelly Spot
Landfill
Lava Flow
Marsh or swamp
Mine or Quarry
Miscellaneous Water
Perennial Water
Rock Outcrop
Saline Spot
Sandy Spot
Severely Eroded Spot
Sinkhole
Slide or Slip
Sodic Spot
Spoil Area
Stony Spot
Very Stony Spot
Wet Spot
Other
Special Line Features
Water Features
Streams and Canals
Transportation
Rails
Interstate Highways
US Routes
Major Roads
Local Roads
Background
Aerial Photography
The soil surveys that comprise your AOI were mapped at
1:24,000.
Please rely on the bar scale on each map sheet for map
measurements.
Source of Map: Natural Resources Conservation Service
Web Soil Survey URL:
Coordinate System: Web Mercator (EPSG:3857)
Maps from the Web Soil Survey are based on the Web Mercator
projection, which preserves direction and shape but distorts
distance and area. A projection that preserves area, such as the
Albers equal-area conic projection, should be used if more
accurate calculations of distance or area are required.
This product is generated from the USDA-NRCS certified data as
of the version date(s) listed below.
Soil Survey Area: Harnett County, North Carolina
Survey Area Data: Version 23, Sep 2, 2025
Soil map units are labeled (as space allows) for map scales
1:50,000 or larger.
Date(s) aerial images were photographed: Apr 24, 2022—May
9, 2022
The orthophoto or other base map on which the soil lines were
compiled and digitized probably differs from the background
imagery displayed on these maps. As a result, some minor
shifting of map unit boundaries may be evident.
Custom Soil Resource Report
10
Map Unit Legend
Map Unit Symbol Map Unit Name Acres in AOI Percent of AOI
AtA Altavista fine sandy loam, 0 to 3
percent slopes, rarely
flooded, Southern Coastal
Plain
56.9 7.1%
Au Augusta fine sandy loam, rarely
flooded
61.5 7.7%
AyA Aycock silt loam, 0 to 2 percent
slopes
22.7 2.8%
AyB Aycock silt loam, 2 to 6 percent
slopes
0.8 0.1%
Bb Bibb soils, frequently flooded 92.7 11.6%
Co Coxville loam 62.1 7.8%
ExA Exum very fine sandy loam, 0 to
2 percent slopes
9.2 1.2%
GoA Goldsboro loamy sand, 0 to 2
percent slopes, Southern
Coastal Plain
19.2 2.4%
Gr Grantham loam 0.1 0.0%
Ly Lynchburg sandy loam, 0 to 2
percent slopes
5.2 0.7%
MaA Marlboro sandy loam, 0 to 2
percent slopes
96.4 12.1%
MaB Marlboro sandy loam, 2 to 6
percent slopes
8.8 1.1%
Na Nahunta loam 14.1 1.8%
NoA Norfolk loamy sand, 0 to 2
percent slopes
59.3 7.4%
NoB Norfolk loamy sand, 2 to 6
percent slopes
63.3 7.9%
OrB Orangeburg loamy sand, 2 to 6
percent slopes
9.4 1.2%
Pd Pits-Dumps complex 88.8 11.1%
Ps Portsmouth loam, rarely flooded 17.5 2.2%
Ra Rains sandy loam, 0 to 2
percent slopes
40.2 5.0%
StA State fine sandy loam, 0 to 3
percent slopes, rarely flooded
17.5 2.2%
To Toisnot loam 32.0 4.0%
W Water 20.0 2.5%
Totals for Area of Interest 797.8 100.0%
Custom Soil Resource Report
11
Map Unit Descriptions
The map units delineated on the detailed soil maps in a soil survey represent the
soils or miscellaneous areas in the survey area. The map unit descriptions, along
with the maps, can be used to determine the composition and properties of a unit.
A map unit delineation on a soil map represents an area dominated by one or more
major kinds of soil or miscellaneous areas. A map unit is identified and named
according to the taxonomic classification of the dominant soils. Within a taxonomic
class there are precisely defined limits for the properties of the soils. On the
landscape, however, the soils are natural phenomena, and they have the
characteristic variability of all natural phenomena. Thus, the range of some
observed properties may extend beyond the limits defined for a taxonomic class.
Areas of soils of a single taxonomic class rarely, if ever, can be mapped without
including areas of other taxonomic classes. Consequently, every map unit is made
up of the soils or miscellaneous areas for which it is named and some minor
components that belong to taxonomic classes other than those of the major soils.
Most minor soils have properties similar to those of the dominant soil or soils in the
map unit, and thus they do not affect use and management. These are called
noncontrasting, or similar, components. They may or may not be mentioned in a
particular map unit description. Other minor components, however, have properties
and behavioral characteristics divergent enough to affect use or to require different
management. These are called contrasting, or dissimilar, components. They
generally are in small areas and could not be mapped separately because of the
scale used. Some small areas of strongly contrasting soils or miscellaneous areas
are identified by a special symbol on the maps. If included in the database for a
given area, the contrasting minor components are identified in the map unit
descriptions along with some characteristics of each. A few areas of minor
components may not have been observed, and consequently they are not
mentioned in the descriptions, especially where the pattern was so complex that it
was impractical to make enough observations to identify all the soils and
miscellaneous areas on the landscape.
The presence of minor components in a map unit in no way diminishes the
usefulness or accuracy of the data. The objective of mapping is not to delineate
pure taxonomic classes but rather to separate the landscape into landforms or
landform segments that have similar use and management requirements. The
delineation of such segments on the map provides sufficient information for the
development of resource plans. If intensive use of small areas is planned, however,
onsite investigation is needed to define and locate the soils and miscellaneous
areas.
An identifying symbol precedes the map unit name in the map unit descriptions.
Each description includes general facts about the unit and gives important soil
properties and qualities.
Soils that have profiles that are almost alike make up a soil series. Except for
differences in texture of the surface layer, all the soils of a series have major
horizons that are similar in composition, thickness, and arrangement.
Soils of one series can differ in texture of the surface layer, slope, stoniness,
salinity, degree of erosion, and other characteristics that affect their use. On the
basis of such differences, a soil series is divided into soil phases. Most of the areas
Custom Soil Resource Report
12
shown on the detailed soil maps are phases of soil series. The name of a soil phase
commonly indicates a feature that affects use or management. For example, Alpha
silt loam, 0 to 2 percent slopes, is a phase of the Alpha series.
Some map units are made up of two or more major soils or miscellaneous areas.
These map units are complexes, associations, or undifferentiated groups.
A complex consists of two or more soils or miscellaneous areas in such an intricate
pattern or in such small areas that they cannot be shown separately on the maps.
The pattern and proportion of the soils or miscellaneous areas are somewhat similar
in all areas. Alpha-Beta complex, 0 to 6 percent slopes, is an example.
An association is made up of two or more geographically associated soils or
miscellaneous areas that are shown as one unit on the maps. Because of present
or anticipated uses of the map units in the survey area, it was not considered
practical or necessary to map the soils or miscellaneous areas separately. The
pattern and relative proportion of the soils or miscellaneous areas are somewhat
similar. Alpha-Beta association, 0 to 2 percent slopes, is an example.
An undifferentiated group is made up of two or more soils or miscellaneous areas
that could be mapped individually but are mapped as one unit because similar
interpretations can be made for use and management. The pattern and proportion
of the soils or miscellaneous areas in a mapped area are not uniform. An area can
be made up of only one of the major soils or miscellaneous areas, or it can be made
up of all of them. Alpha and Beta soils, 0 to 2 percent slopes, is an example.
Some surveys include miscellaneous areas. Such areas have little or no soil
material and support little or no vegetation. Rock outcrop is an example.
Custom Soil Resource Report
13
Harnett County, North Carolina
AtA—Altavista fine sandy loam, 0 to 3 percent slopes, rarely flooded,
Southern Coastal Plain
Map Unit Setting
National map unit symbol: 2vx8w
Elevation: 0 to 520 feet
Mean annual precipitation: 39 to 61 inches
Mean annual air temperature: 47 to 74 degrees F
Frost-free period: 175 to 280 days
Farmland classification: All areas are prime farmland
Map Unit Composition
Altavista, rarely flooded, and similar soils:80 percent
Minor components:20 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Altavista, Rarely Flooded
Setting
Landform:Ridges, stream terraces
Landform position (three-dimensional):Tread, riser
Down-slope shape:Linear, convex
Across-slope shape:Linear
Parent material:Loamy alluvium derived from igneous and metamorphic rock
Typical profile
Ap - 0 to 7 inches: fine sandy loam
E - 7 to 11 inches: fine sandy loam
Bt - 11 to 37 inches: sandy clay loam
BC - 37 to 54 inches: sandy loam
C - 54 to 80 inches: sandy loam
Properties and qualities
Slope:0 to 3 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Moderately well drained
Capacity of the most limiting layer to transmit water (Ksat):Moderately low to
moderately high (0.14 to 1.42 in/hr)
Depth to water table:About 18 to 30 inches
Frequency of flooding:Rare
Frequency of ponding:None
Maximum salinity:Nonsaline to very slightly saline (0.0 to 2.0 mmhos/cm)
Available water supply, 0 to 60 inches: Moderate (about 8.4 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 2w
Hydrologic Soil Group: C
Ecological site: F133AY220NC - Stream Terraces, Moist
Hydric soil rating: No
Custom Soil Resource Report
14
Minor Components
Augusta, rarely flooded
Percent of map unit:8 percent
Landform:Stream terraces
Landform position (three-dimensional):Tread
Down-slope shape:Concave
Across-slope shape:Linear
Ecological site:F133AY220NC - Stream Terraces, Moist
Hydric soil rating: No
State, undrained
Percent of map unit:8 percent
Landform:Stream terraces
Landform position (three-dimensional):Riser, tread
Down-slope shape:Concave
Across-slope shape:Linear
Ecological site:F133AY220NC - Stream Terraces, Moist
Hydric soil rating: No
Wickham, rarely flooded
Percent of map unit:4 percent
Landform:Stream terraces
Landform position (three-dimensional):Riser, tread
Down-slope shape:Convex
Across-slope shape:Linear
Ecological site:F133AY220NC - Stream Terraces, Moist
Hydric soil rating: No
Au—Augusta fine sandy loam, rarely flooded
Map Unit Setting
National map unit symbol: 3sns
Elevation: 80 to 330 feet
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 210 to 265 days
Farmland classification: Prime farmland if drained
Map Unit Composition
Augusta and similar soils:85 percent
Minor components:5 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Augusta
Setting
Landform:Stream terraces
Down-slope shape:Concave
Across-slope shape:Linear
Custom Soil Resource Report
15
Parent material:Old loamy alluvium derived from igneous and metamorphic rock
Typical profile
A - 0 to 9 inches: fine sandy loam
Bt - 9 to 19 inches: clay loam
Btg - 19 to 60 inches: clay loam
Cg - 60 to 80 inches: coarse sandy loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Somewhat poorly drained
Runoff class: Very high
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.57 to 1.98 in/hr)
Depth to water table:About 12 to 24 inches
Frequency of flooding:Rare
Frequency of ponding:None
Available water supply, 0 to 60 inches: Moderate (about 8.7 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 3w
Hydrologic Soil Group: B/D
Ecological site: F133AY220NC - Stream Terraces, Moist
Hydric soil rating: No
Minor Components
Roanoke, undrained
Percent of map unit:3 percent
Landform:Depressions on stream terraces, backswamps on stream terraces
Landform position (three-dimensional):Flat
Down-slope shape:Concave
Across-slope shape:Linear
Ecological site:F133AY210NC - Stream Terraces, Wet
Hydric soil rating: Yes
Wehadkee, undrained
Percent of map unit:2 percent
Landform:Depressions on flood plains
Down-slope shape:Concave
Across-slope shape:Linear
Ecological site:F133AY120NC - Large River Flood Plains, Piedmont Source, Wet
Hydric soil rating: Yes
AyA—Aycock silt loam, 0 to 2 percent slopes
Map Unit Setting
National map unit symbol: 3snt
Elevation: 80 to 330 feet
Custom Soil Resource Report
16
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 210 to 265 days
Farmland classification: All areas are prime farmland
Map Unit Composition
Aycock and similar soils:90 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Aycock
Setting
Landform:Broad interstream divides on marine terraces, flats on marine terraces
Down-slope shape:Linear
Across-slope shape:Linear
Parent material:Loamy and silty marine deposits
Typical profile
Ap - 0 to 7 inches: silt loam
E - 7 to 12 inches: silt loam
Bt - 12 to 90 inches: clay loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Well drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.20 to 1.98 in/hr)
Depth to water table:About 48 to 72 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: High (about 10.8 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 2e
Hydrologic Soil Group: B
Ecological site: F133AY420NC - Summits, Loamy and Clayey, Moist
Hydric soil rating: No
AyB—Aycock silt loam, 2 to 6 percent slopes
Map Unit Setting
National map unit symbol: 3snv
Elevation: 80 to 330 feet
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 210 to 265 days
Farmland classification: All areas are prime farmland
Custom Soil Resource Report
17
Map Unit Composition
Aycock and similar soils:85 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Aycock
Setting
Landform:Broad interstream divides on marine terraces, ridges on marine
terraces
Landform position (two-dimensional):Summit, shoulder
Landform position (three-dimensional):Crest
Down-slope shape:Convex
Across-slope shape:Linear, convex
Parent material:Loamy and silty marine deposits
Typical profile
Ap - 0 to 7 inches: silt loam
E - 7 to 12 inches: silt loam
Bt - 12 to 90 inches: clay loam
Properties and qualities
Slope:2 to 6 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Well drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.20 to 1.98 in/hr)
Depth to water table:About 48 to 72 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: High (about 10.8 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 3e
Hydrologic Soil Group: B
Ecological site: F133AY420NC - Summits, Loamy and Clayey, Moist
Hydric soil rating: No
Bb—Bibb soils, frequently flooded
Map Unit Setting
National map unit symbol: 3snw
Elevation: 80 to 330 feet
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 210 to 265 days
Farmland classification: Not prime farmland
Map Unit Composition
Bibb, undrained, and similar soils:80 percent
Custom Soil Resource Report
18
Johnston, undrained, and similar soils:10 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Bibb, Undrained
Setting
Landform:Flood plains
Landform position (two-dimensional):Toeslope
Down-slope shape:Concave
Across-slope shape:Linear
Parent material:Sandy and loamy alluvium
Typical profile
A - 0 to 6 inches: sandy loam
Cg1 - 6 to 60 inches: sandy loam
Cg2 - 60 to 80 inches: loamy sand
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Poorly drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):High (1.98 to 5.95
in/hr)
Depth to water table:About 0 to 12 inches
Frequency of flooding:Frequent
Frequency of ponding:None
Available water supply, 0 to 60 inches: Moderate (about 7.2 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 5w
Hydrologic Soil Group: A/D
Ecological site: F133AY140NC - Small Stream Flood Plains, Wet
Hydric soil rating: Yes
Description of Johnston, Undrained
Setting
Landform:Flood plains
Down-slope shape:Concave
Across-slope shape:Linear
Parent material:Sandy and loamy alluvium
Typical profile
A - 0 to 30 inches: mucky loam
Cg1 - 30 to 34 inches: loamy fine sand
Cg2 - 34 to 80 inches: fine sandy loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Very poorly drained
Runoff class: Ponded
Capacity of the most limiting layer to transmit water (Ksat):High (1.98 to 5.95
in/hr)
Depth to water table:About 0 inches
Frequency of flooding:Frequent
Custom Soil Resource Report
19
Frequency of ponding:Frequent
Available water supply, 0 to 60 inches: High (about 9.4 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 7w
Hydrologic Soil Group: A/D
Ecological site: F133AY140NC - Small Stream Flood Plains, Wet
Hydric soil rating: Yes
Co—Coxville loam
Map Unit Setting
National map unit symbol: 3sp4
Elevation: 80 to 330 feet
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 210 to 265 days
Farmland classification: Farmland of statewide importance
Map Unit Composition
Coxville, drained, and similar soils:85 percent
Coxville, undrained, and similar soils:10 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Coxville, Drained
Setting
Landform:Depressions, carolina bays
Landform position (two-dimensional):Summit
Down-slope shape:Concave
Across-slope shape:Concave
Parent material:Clayey marine deposits
Typical profile
Ap - 0 to 9 inches: loam
Eg - 9 to 11 inches: loam
Btg - 11 to 72 inches: sandy clay
Cg - 72 to 80 inches: sandy clay loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Poorly drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately high (0.20
to 0.57 in/hr)
Depth to water table:About 0 to 12 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: Moderate (about 7.6 inches)
Custom Soil Resource Report
20
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 3w
Hydrologic Soil Group: C/D
Ecological site: F153AY065NC - Wet Clay Flats and Depressions, F133AY320NC
- Upland Depressions, Flats, and Carolina Bays
Hydric soil rating: Yes
Description of Coxville, Undrained
Setting
Landform:Depressions, carolina bays
Landform position (two-dimensional):Summit
Down-slope shape:Concave
Across-slope shape:Concave
Parent material:Clayey marine deposits
Typical profile
A - 0 to 9 inches: loam
Eg - 9 to 11 inches: loam
Btg - 11 to 72 inches: sandy clay
Cg - 72 to 80 inches: sandy clay loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Poorly drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately high (0.20
to 0.57 in/hr)
Depth to water table:About 0 to 12 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: Moderate (about 7.6 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 4w
Hydrologic Soil Group: C/D
Ecological site: F153AY065NC - Wet Clay Flats and Depressions, F133AY320NC
- Upland Depressions, Flats, and Carolina Bays
Hydric soil rating: Yes
ExA—Exum very fine sandy loam, 0 to 2 percent slopes
Map Unit Setting
National map unit symbol: 3spc
Elevation: 80 to 330 feet
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Custom Soil Resource Report
21
Frost-free period: 210 to 265 days
Farmland classification: All areas are prime farmland
Map Unit Composition
Exum and similar soils:90 percent
Minor components:5 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Exum
Setting
Landform:Flats on marine terraces, broad interstream divides on marine terraces
Down-slope shape:Concave
Across-slope shape:Linear
Parent material:Loamy and silty marine deposits
Typical profile
Ap - 0 to 8 inches: very fine sandy loam
E - 8 to 12 inches: silt loam
Bt - 12 to 70 inches: clay loam
C - 70 to 100 inches: loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Moderately well drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately high (0.20
to 0.57 in/hr)
Depth to water table:About 24 to 36 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: High (about 10.8 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 2w
Hydrologic Soil Group: C
Ecological site: F153AY040NC - Moist Loamy Rises and Flats, F133AY410NC -
Summits, Loamy and Clayey, Seasonally Wet
Hydric soil rating: No
Minor Components
Grantham, undrained
Percent of map unit:5 percent
Landform:Broad interstream divides on depressions, broad interstream divides on
flats
Down-slope shape:Concave
Across-slope shape:Concave, linear
Ecological site:F153AY065NC - Wet Clay Flats and Depressions, F133AY320NC -
Upland Depressions, Flats, and Carolina Bays
Hydric soil rating: Yes
Custom Soil Resource Report
22
GoA—Goldsboro loamy sand, 0 to 2 percent slopes, Southern Coastal
Plain
Map Unit Setting
National map unit symbol: 2v750
Elevation: 110 to 300 feet
Mean annual precipitation: 40 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 200 to 280 days
Farmland classification: All areas are prime farmland
Map Unit Composition
Goldsboro and similar soils:85 percent
Minor components:15 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Goldsboro
Setting
Landform:Flats on marine terraces, broad interstream divides on marine terraces
Landform position (three-dimensional):Talf
Down-slope shape:Linear
Across-slope shape:Linear
Parent material:Loamy marine deposits
Typical profile
Ap - 0 to 9 inches: loamy sand
E - 9 to 12 inches: loamy sand
Bt - 12 to 62 inches: sandy clay loam
Btg - 62 to 80 inches: sandy clay loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Moderately well drained
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.57 to 1.98 in/hr)
Depth to water table:About 24 to 36 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: Moderate (about 8.1 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 2w
Hydrologic Soil Group: B
Ecological site: F153AY040NC - Moist Loamy Rises and Flats, F133AY410NC -
Summits, Loamy and Clayey, Seasonally Wet
Hydric soil rating: No
Custom Soil Resource Report
23
Minor Components
Norfolk
Percent of map unit:8 percent
Landform:Broad interstream divides on marine terraces, flats on marine terraces
Landform position (three-dimensional):Talf
Down-slope shape:Convex, linear
Across-slope shape:Convex, linear
Ecological site:F153AY030NC - Dry Loamy Rises and Flats, F133AY420NC -
Summits, Loamy and Clayey, Moist
Hydric soil rating: No
Lynchburg
Percent of map unit:7 percent
Landform:Flats on marine terraces, broad interstream divides on marine terraces
Landform position (three-dimensional):Talf
Down-slope shape:Linear
Across-slope shape:Linear
Ecological site:F153AY040NC - Moist Loamy Rises and Flats, F133AY410NC -
Summits, Loamy and Clayey, Seasonally Wet
Hydric soil rating: No
Gr—Grantham loam
Map Unit Setting
National map unit symbol: 3spl
Elevation: 80 to 330 feet
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 210 to 265 days
Farmland classification: Prime farmland if drained
Map Unit Composition
Grantham, drained, and similar soils:80 percent
Grantham, undrained, and similar soils:10 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Grantham, Drained
Setting
Landform:Broad interstream divides on depressions, broad interstream divides on
flats
Down-slope shape:Concave
Across-slope shape:Concave, linear
Parent material:Loamy and silty marine deposits
Typical profile
A - 0 to 6 inches: loam
Eg - 6 to 11 inches: loam
Btg - 11 to 77 inches: loam
Custom Soil Resource Report
24
Cg - 77 to 110 inches: loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Poorly drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately high (0.20
to 0.57 in/hr)
Depth to water table:About 0 to 12 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: High (about 10.7 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 3w
Hydrologic Soil Group: C/D
Ecological site: F153AY065NC - Wet Clay Flats and Depressions, F133AY320NC
- Upland Depressions, Flats, and Carolina Bays
Hydric soil rating: Yes
Description of Grantham, Undrained
Setting
Landform:Broad interstream divides on depressions, broad interstream divides on
flats
Down-slope shape:Concave
Across-slope shape:Concave, linear
Parent material:Loamy and silty marine deposits
Typical profile
A - 0 to 6 inches: loam
Eg - 6 to 11 inches: loam
Btg - 11 to 77 inches: loam
Cg - 77 to 110 inches: loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Poorly drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately high (0.20
to 0.57 in/hr)
Depth to water table:About 0 to 12 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: High (about 10.7 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 6w
Hydrologic Soil Group: C/D
Ecological site: F153AY065NC - Wet Clay Flats and Depressions, F133AY320NC
- Upland Depressions, Flats, and Carolina Bays
Hydric soil rating: Yes
Custom Soil Resource Report
25
Ly—Lynchburg sandy loam, 0 to 2 percent slopes
Map Unit Setting
National map unit symbol: 2vx8p
Elevation: 10 to 330 feet
Mean annual precipitation: 40 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 200 to 280 days
Farmland classification: Prime farmland if drained
Map Unit Composition
Lynchburg and similar soils:84 percent
Minor components:16 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Lynchburg
Setting
Landform:Flats on marine terraces, broad interstream divides on marine terraces
Landform position (three-dimensional):Talf
Down-slope shape:Linear
Across-slope shape:Linear
Parent material:Loamy marine deposits
Typical profile
Ap - 0 to 8 inches: sandy loam
E - 8 to 11 inches: sandy loam
Bt - 11 to 21 inches: sandy clay loam
Btg - 21 to 65 inches: sandy clay loam
BCg - 65 to 85 inches: sandy clay loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Somewhat poorly drained
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.57 to 1.98 in/hr)
Depth to water table:About 6 to 18 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: Moderate (about 6.6 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 2w
Hydrologic Soil Group: B/D
Ecological site: F153AY040NC - Moist Loamy Rises and Flats, F133AY410NC -
Summits, Loamy and Clayey, Seasonally Wet
Hydric soil rating: No
Custom Soil Resource Report
26
Minor Components
Goldsboro
Percent of map unit:8 percent
Landform:Flats on marine terraces, broad interstream divides on marine terraces
Landform position (three-dimensional):Talf
Down-slope shape:Linear
Across-slope shape:Linear
Ecological site:F153AY040NC - Moist Loamy Rises and Flats, F133AY410NC -
Summits, Loamy and Clayey, Seasonally Wet
Hydric soil rating: No
Rains
Percent of map unit:8 percent
Landform:Flats on marine terraces, broad interstream divides on marine terraces
Landform position (three-dimensional):Dip, talf
Down-slope shape:Linear
Across-slope shape:Linear
Ecological site:F153AY060NC - Wet Loamy Flats and Depressions,
F133AY320NC - Upland Depressions, Flats, and Carolina Bays
Hydric soil rating: Yes
MaA—Marlboro sandy loam, 0 to 2 percent slopes
Map Unit Setting
National map unit symbol: 3spv
Elevation: 80 to 330 feet
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 210 to 265 days
Farmland classification: All areas are prime farmland
Map Unit Composition
Marlboro and similar soils:90 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Marlboro
Setting
Landform:Broad interstream divides on marine terraces, ridges on marine
terraces
Down-slope shape:Convex
Across-slope shape:Linear
Parent material:Clayey marine deposits
Typical profile
Ap - 0 to 10 inches: sandy loam
Bt1 - 10 to 71 inches: sandy clay
Bt2 - 71 to 80 inches: sandy clay
Custom Soil Resource Report
27
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Well drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.57 to 1.98 in/hr)
Depth to water table:About 48 to 72 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: High (about 9.2 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 1
Hydrologic Soil Group: B
Ecological site: F133AY420NC - Summits, Loamy and Clayey, Moist
Hydric soil rating: No
MaB—Marlboro sandy loam, 2 to 6 percent slopes
Map Unit Setting
National map unit symbol: 3spw
Elevation: 80 to 330 feet
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 210 to 265 days
Farmland classification: All areas are prime farmland
Map Unit Composition
Marlboro and similar soils:90 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Marlboro
Setting
Landform:Broad interstream divides on marine terraces, ridges on marine
terraces
Landform position (two-dimensional):Summit, shoulder
Landform position (three-dimensional):Crest
Down-slope shape:Convex
Across-slope shape:Convex
Parent material:Clayey marine deposits
Typical profile
Ap - 0 to 10 inches: sandy loam
Bt1 - 10 to 71 inches: sandy clay
Bt2 - 71 to 80 inches: sandy clay
Properties and qualities
Slope:2 to 6 percent
Depth to restrictive feature:More than 80 inches
Custom Soil Resource Report
28
Drainage class:Well drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.57 to 1.98 in/hr)
Depth to water table:About 48 to 72 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: High (about 9.2 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 2e
Hydrologic Soil Group: B
Ecological site: F133AY420NC - Summits, Loamy and Clayey, Moist
Hydric soil rating: No
Na—Nahunta loam
Map Unit Setting
National map unit symbol: 3spx
Elevation: 80 to 330 feet
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 210 to 265 days
Farmland classification: Prime farmland if drained
Map Unit Composition
Nahunta, drained, and similar soils:80 percent
Nahunta, undrained, and similar soils:10 percent
Minor components:7 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Nahunta, Drained
Setting
Landform:Flats on marine terraces, broad interstream divides on marine terraces
Down-slope shape:Concave
Across-slope shape:Linear
Parent material:Loamy and silty marine deposits
Typical profile
Ap - 0 to 8 inches: loam
E - 8 to 12 inches: loam
Btg - 12 to 79 inches: clay loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Somewhat poorly drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately high (0.20
to 0.57 in/hr)
Custom Soil Resource Report
29
Depth to water table:About 12 to 18 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: High (about 10.8 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 2w
Hydrologic Soil Group: C/D
Ecological site: F153AY040NC - Moist Loamy Rises and Flats, F133AY410NC -
Summits, Loamy and Clayey, Seasonally Wet
Hydric soil rating: No
Description of Nahunta, Undrained
Setting
Landform:Flats on marine terraces, broad interstream divides on marine terraces
Down-slope shape:Concave
Across-slope shape:Linear
Parent material:Loamy and silty marine deposits
Typical profile
A - 0 to 8 inches: loam
E - 8 to 12 inches: loam
Btg - 12 to 79 inches: clay loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Somewhat poorly drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately high (0.20
to 0.57 in/hr)
Depth to water table:About 12 to 18 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: High (about 10.8 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 3w
Hydrologic Soil Group: C/D
Ecological site: F153AY040NC - Moist Loamy Rises and Flats, F133AY410NC -
Summits, Loamy and Clayey, Seasonally Wet
Hydric soil rating: No
Minor Components
Grantham, undrained
Percent of map unit:5 percent
Landform:Broad interstream divides on depressions, broad interstream divides on
flats
Down-slope shape:Concave
Across-slope shape:Concave, linear
Ecological site:F153AY065NC - Wet Clay Flats and Depressions, F133AY320NC -
Upland Depressions, Flats, and Carolina Bays
Hydric soil rating: Yes
Custom Soil Resource Report
30
Rains, undrained
Percent of map unit:2 percent
Landform:Flats on marine terraces, carolina bays on marine terraces, broad
interstream divides on marine terraces
Landform position (two-dimensional):Summit
Down-slope shape:Linear
Across-slope shape:Linear
Ecological site:F153AY060NC - Wet Loamy Flats and Depressions,
F133AY320NC - Upland Depressions, Flats, and Carolina Bays
Hydric soil rating: Yes
NoA—Norfolk loamy sand, 0 to 2 percent slopes
Map Unit Setting
National map unit symbol: 2v75w
Elevation: 10 to 330 feet
Mean annual precipitation: 40 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 200 to 280 days
Farmland classification: All areas are prime farmland
Map Unit Composition
Norfolk and similar soils:83 percent
Minor components:17 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Norfolk
Setting
Landform:Broad interstream divides on marine terraces, flats on marine terraces
Landform position (three-dimensional):Talf
Down-slope shape:Convex, linear
Across-slope shape:Convex, linear
Parent material:Loamy marine deposits
Typical profile
Ap - 0 to 8 inches: loamy sand
E - 8 to 14 inches: loamy sand
Bt - 14 to 65 inches: sandy clay loam
BC - 65 to 80 inches: sandy clay loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Well drained
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.57 to 1.98 in/hr)
Depth to water table:About 40 to 72 inches
Frequency of flooding:None
Custom Soil Resource Report
31
Frequency of ponding:None
Available water supply, 0 to 60 inches: Moderate (about 6.9 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 1
Hydrologic Soil Group: A
Ecological site: F153AY030NC - Dry Loamy Rises and Flats, F133AY420NC -
Summits, Loamy and Clayey, Moist
Hydric soil rating: No
Minor Components
Goldsboro
Percent of map unit:9 percent
Landform:Flats on marine terraces, broad interstream divides on marine terraces
Landform position (three-dimensional):Talf
Down-slope shape:Linear
Across-slope shape:Linear
Ecological site:F153AY040NC - Moist Loamy Rises and Flats, F133AY410NC -
Summits, Loamy and Clayey, Seasonally Wet
Hydric soil rating: No
Wagram
Percent of map unit:8 percent
Landform:Broad interstream divides on marine terraces, ridges on marine
terraces
Landform position (two-dimensional):Summit, shoulder
Landform position (three-dimensional):Crest, talf
Down-slope shape:Convex
Across-slope shape:Convex
Ecological site:F153AY030NC - Dry Loamy Rises and Flats, F133AY430NC -
Summits, Loamy, Thick Sandy Surface
Hydric soil rating: No
NoB—Norfolk loamy sand, 2 to 6 percent slopes
Map Unit Setting
National map unit symbol: 2v75y
Elevation: 30 to 450 feet
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 200 to 280 days
Farmland classification: All areas are prime farmland
Map Unit Composition
Norfolk and similar soils:83 percent
Minor components:17 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Custom Soil Resource Report
32
Description of Norfolk
Setting
Landform:Broad interstream divides on marine terraces, flats on marine terraces
Landform position (three-dimensional):Talf
Down-slope shape:Convex, linear
Across-slope shape:Convex, linear
Parent material:Loamy marine deposits
Typical profile
Ap - 0 to 8 inches: loamy sand
E - 8 to 14 inches: loamy sand
Bt - 14 to 65 inches: sandy clay loam
BC - 65 to 80 inches: sandy clay loam
Properties and qualities
Slope:2 to 6 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Well drained
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.57 to 1.98 in/hr)
Depth to water table:About 40 to 72 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: Moderate (about 6.9 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 2e
Hydrologic Soil Group: A
Ecological site: F153AY030NC - Dry Loamy Rises and Flats, F133AY420NC -
Summits, Loamy and Clayey, Moist
Hydric soil rating: No
Minor Components
Wagram
Percent of map unit:10 percent
Landform:Broad interstream divides on marine terraces, ridges on marine
terraces
Landform position (two-dimensional):Summit, shoulder
Landform position (three-dimensional):Riser, rise
Down-slope shape:Convex, linear
Across-slope shape:Convex
Ecological site:F153AY030NC - Dry Loamy Rises and Flats, F133AY430NC -
Summits, Loamy, Thick Sandy Surface
Hydric soil rating: No
Goldsboro
Percent of map unit:7 percent
Landform:Flats on marine terraces, broad interstream divides on marine terraces
Landform position (three-dimensional):Talf
Down-slope shape:Linear
Across-slope shape:Linear
Ecological site:F153AY040NC - Moist Loamy Rises and Flats, F133AY410NC -
Summits, Loamy and Clayey, Seasonally Wet
Custom Soil Resource Report
33
Hydric soil rating: No
OrB—Orangeburg loamy sand, 2 to 6 percent slopes
Map Unit Setting
National map unit symbol: 3sq4
Elevation: 80 to 330 feet
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 210 to 265 days
Farmland classification: All areas are prime farmland
Map Unit Composition
Orangeburg and similar soils:90 percent
Minor components:5 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Orangeburg
Setting
Landform:Broad interstream divides on marine terraces, ridges on marine
terraces
Landform position (two-dimensional):Summit, shoulder
Landform position (three-dimensional):Crest
Down-slope shape:Convex
Across-slope shape:Convex
Parent material:Loamy marine deposits
Typical profile
Ap - 0 to 7 inches: loamy sand
BA - 7 to 12 inches: sandy loam
Bt1 - 12 to 54 inches: sandy clay loam
Bt2 - 54 to 80 inches: sandy clay loam
Properties and qualities
Slope:2 to 6 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Well drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.57 to 1.98 in/hr)
Depth to water table:More than 80 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: Moderate (about 7.3 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 2e
Hydrologic Soil Group: A
Custom Soil Resource Report
34
Ecological site: F153AY030NC - Dry Loamy Rises and Flats, F133AY420NC -
Summits, Loamy and Clayey, Moist
Hydric soil rating: No
Minor Components
Bibb, undrained
Percent of map unit:3 percent
Landform:Flood plains
Landform position (two-dimensional):Toeslope
Down-slope shape:Concave
Across-slope shape:Linear
Ecological site:F153AY090NC - Flooded Mineral Soil Flood Plains and Terraces,
F133AY140NC - Small Stream Flood Plains, Wet
Hydric soil rating: Yes
Johnston, undrained
Percent of map unit:2 percent
Landform:Flood plains
Down-slope shape:Concave
Across-slope shape:Linear
Ecological site:F153AY090NC - Flooded Mineral Soil Flood Plains and Terraces,
F133AY140NC - Small Stream Flood Plains, Wet
Hydric soil rating: Yes
Pd—Pits-Dumps complex
Map Unit Composition
Pits:50 percent
Dumps:30 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Pits
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 8s
Hydric soil rating: No
Description of Dumps
Setting
Parent material:Loamy mine spoil or earthy fill
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 8s
Hydric soil rating: No
Custom Soil Resource Report
35
Ps—Portsmouth loam, rarely flooded
Map Unit Setting
National map unit symbol: 3sqb
Elevation: 20 to 160 feet
Mean annual precipitation: 40 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 200 to 280 days
Farmland classification: Prime farmland if drained
Map Unit Composition
Portsmouth, drained, and similar soils:80 percent
Portsmouth, undrained, and similar soils:10 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Portsmouth, Drained
Setting
Landform:Depressions on stream terraces, flats on marine terraces
Down-slope shape:Linear
Across-slope shape:Linear
Parent material:Loamy fluviomarine deposits over sandy fluviomarine deposits
Typical profile
Ap - 0 to 12 inches: loam
Eg - 12 to 19 inches: loam
BEg - 19 to 23 inches: loam
Btg - 23 to 35 inches: sandy clay loam
BCg - 35 to 38 inches: sandy loam
2Cg1 - 38 to 48 inches: sand
2Cg2 - 48 to 80 inches: sand
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:20 to 40 inches to strongly contrasting textural
stratification
Drainage class:Very poorly drained
Runoff class: Very high
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.57 to 1.98 in/hr)
Depth to water table:About 0 to 12 inches
Frequency of flooding:Rare
Frequency of ponding:None
Available water supply, 0 to 60 inches: Low (about 5.8 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 3w
Hydrologic Soil Group: B/D
Ecological site: F153AY060NC - Wet Loamy Flats and Depressions,
F133AY210NC - Stream Terraces, Wet
Custom Soil Resource Report
36
Hydric soil rating: Yes
Description of Portsmouth, Undrained
Setting
Landform:Flats on marine terraces, depressions on stream terraces
Down-slope shape:Linear
Across-slope shape:Linear
Parent material:Loamy fluviomarine deposits over sandy fluviomarine deposits
Typical profile
A - 0 to 12 inches: loam
Eg - 12 to 19 inches: loam
BEg - 19 to 23 inches: loam
Btg - 23 to 35 inches: sandy clay loam
BCg - 35 to 38 inches: sandy loam
2Cg1 - 38 to 48 inches: sand
2Cg2 - 48 to 80 inches: sand
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:20 to 40 inches to strongly contrasting textural
stratification
Drainage class:Very poorly drained
Runoff class: Very high
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.57 to 1.98 in/hr)
Depth to water table:About 0 to 12 inches
Frequency of flooding:Rare
Frequency of ponding:Rare
Available water supply, 0 to 60 inches: Low (about 5.8 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 6w
Hydrologic Soil Group: B/D
Ecological site: F153AY060NC - Wet Loamy Flats and Depressions,
F133AY210NC - Stream Terraces, Wet
Hydric soil rating: Yes
Ra—Rains sandy loam, 0 to 2 percent slopes
Map Unit Setting
National map unit symbol: 2v760
Elevation: 30 to 330 feet
Mean annual precipitation: 40 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 200 to 280 days
Farmland classification: Prime farmland if drained
Custom Soil Resource Report
37
Map Unit Composition
Rains, undrained, and similar soils:58 percent
Rains, drained, and similar soils:24 percent
Minor components:18 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Rains, Undrained
Setting
Landform:Carolina bays on marine terraces, broad interstream divides on marine
terraces, flats on marine terraces
Landform position (three-dimensional):Dip, talf
Down-slope shape:Linear
Across-slope shape:Linear
Parent material:Loamy marine deposits
Typical profile
A - 0 to 6 inches: sandy loam
Eg - 6 to 12 inches: sandy loam
Btg - 12 to 65 inches: sandy clay loam
BCg - 65 to 80 inches: sandy clay loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Poorly drained
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.20 to 1.98 in/hr)
Depth to water table:About 0 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: Moderate (about 7.9 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 4w
Hydrologic Soil Group: A/D
Ecological site: F153AY060NC - Wet Loamy Flats and Depressions,
F133AY320NC - Upland Depressions, Flats, and Carolina Bays
Hydric soil rating: Yes
Description of Rains, Drained
Setting
Landform:Carolina bays on marine terraces, broad interstream divides on marine
terraces, flats on marine terraces
Landform position (three-dimensional):Dip, talf
Down-slope shape:Linear
Across-slope shape:Linear
Parent material:Loamy marine deposits
Typical profile
Ap - 0 to 6 inches: sandy loam
Eg - 6 to 12 inches: sandy loam
Btg - 12 to 65 inches: sandy clay loam
BCg - 65 to 80 inches: sandy clay loam
Custom Soil Resource Report
38
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Poorly drained
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.20 to 1.98 in/hr)
Depth to water table:About 12 to 36 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: Moderate (about 7.9 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 3w
Hydrologic Soil Group: B
Ecological site: F153AY060NC - Wet Loamy Flats and Depressions,
F133AY320NC - Upland Depressions, Flats, and Carolina Bays
Hydric soil rating: Yes
Minor Components
Lynchburg
Percent of map unit:10 percent
Landform:Flats on marine terraces, broad interstream divides on marine terraces
Landform position (three-dimensional):Talf
Down-slope shape:Linear
Across-slope shape:Linear
Ecological site:F153AY040NC - Moist Loamy Rises and Flats, F133AY410NC -
Summits, Loamy and Clayey, Seasonally Wet
Hydric soil rating: No
Pantego, undrained
Percent of map unit:8 percent
Landform:Stream terraces, flats, broad interstream divides
Landform position (three-dimensional):Tread, talf
Down-slope shape:Linear
Across-slope shape:Concave
Ecological site:F153AY060NC - Wet Loamy Flats and Depressions,
F133AY320NC - Upland Depressions, Flats, and Carolina Bays
Hydric soil rating: Yes
StA—State fine sandy loam, 0 to 3 percent slopes, rarely flooded
Map Unit Setting
National map unit symbol: 3sqg
Elevation: 80 to 330 feet
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 210 to 265 days
Custom Soil Resource Report
39
Farmland classification: All areas are prime farmland
Map Unit Composition
State and similar soils:95 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of State
Setting
Landform:Stream terraces
Landform position (three-dimensional):Tread
Down-slope shape:Convex
Across-slope shape:Linear
Parent material:Old loamy alluvium derived from igneous and metamorphic rock
Typical profile
Ap - 0 to 6 inches: fine sandy loam
E - 6 to 13 inches: fine sandy loam
Bt1 - 13 to 38 inches: sandy clay loam
Bt2 - 38 to 42 inches: fine sandy loam
C - 42 to 80 inches: fine sandy loam
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:More than 80 inches
Drainage class:Well drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high
(0.57 to 1.98 in/hr)
Depth to water table:About 48 to 72 inches
Frequency of flooding:Rare
Frequency of ponding:None
Available water supply, 0 to 60 inches: Moderate (about 7.1 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 1
Hydrologic Soil Group: B
Ecological site: F133AY220NC - Stream Terraces, Moist
Hydric soil rating: No
To—Toisnot loam
Map Unit Setting
National map unit symbol: 3sqh
Elevation: 80 to 330 feet
Mean annual precipitation: 38 to 55 inches
Mean annual air temperature: 59 to 70 degrees F
Frost-free period: 210 to 265 days
Farmland classification: Not prime farmland
Custom Soil Resource Report
40
Map Unit Composition
Toisnot, undrained, and similar soils:80 percent
Toisnot, drained, and similar soils:10 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Toisnot, Undrained
Setting
Landform:Flats on marine terraces, broad interstream divides on marine terraces,
carolina bays on marine terraces
Landform position (two-dimensional):Summit
Down-slope shape:Linear
Across-slope shape:Linear
Parent material:Loamy fluviomarine deposits
Typical profile
A - 0 to 6 inches: loam
Eg - 6 to 13 inches: sandy loam
E/Btg - 13 to 28 inches: sandy loam
Ex - 28 to 45 inches: sandy loam
Btg - 45 to 61 inches: sandy clay loam
2Cg - 61 to 90 inches: sandy clay
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:20 to 40 inches to fragipan
Drainage class:Poorly drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately low to
moderately high (0.06 to 0.20 in/hr)
Depth to water table:About 0 to 12 inches
Frequency of flooding:None
Frequency of ponding:Frequent
Available water supply, 0 to 60 inches: Low (about 3.7 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 5w
Hydrologic Soil Group: C/D
Ecological site: F153AY060NC - Wet Loamy Flats and Depressions,
F133AY320NC - Upland Depressions, Flats, and Carolina Bays
Hydric soil rating: Yes
Description of Toisnot, Drained
Setting
Landform:Flats on marine terraces, broad interstream divides on marine terraces,
carolina bays on marine terraces
Landform position (two-dimensional):Summit
Down-slope shape:Linear
Across-slope shape:Linear
Parent material:Loamy fluviomarine deposits
Typical profile
Ap - 0 to 6 inches: loam
Eg - 6 to 13 inches: sandy loam
Custom Soil Resource Report
41
E/Btg - 13 to 28 inches: sandy loam
Ex - 28 to 45 inches: sandy loam
Btg - 45 to 61 inches: sandy clay loam
2Cg - 61 to 90 inches: sandy clay
Properties and qualities
Slope:0 to 2 percent
Depth to restrictive feature:20 to 40 inches to fragipan
Drainage class:Poorly drained
Runoff class: Low
Capacity of the most limiting layer to transmit water (Ksat):Moderately low to
moderately high (0.06 to 0.20 in/hr)
Depth to water table:About 0 to 12 inches
Frequency of flooding:None
Frequency of ponding:None
Available water supply, 0 to 60 inches: Low (about 3.7 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 4w
Hydrologic Soil Group: C/D
Ecological site: F153AY060NC - Wet Loamy Flats and Depressions,
F133AY320NC - Upland Depressions, Flats, and Carolina Bays
Hydric soil rating: Yes
W—Water
Map Unit Composition
Water:100 percent
Estimates are based on observations, descriptions, and transects of the mapunit.
Description of Water
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 8
Hydric soil rating: No
Custom Soil Resource Report
42
References
American Association of State Highway and Transportation Officials (AASHTO).
2004. Standard specifications for transportation materials and methods of sampling
and testing. 24th edition.
American Society for Testing and Materials (ASTM). 2005. Standard classification of
soils for engineering purposes. ASTM Standard D2487-00.
Cowardin, L.M., V. Carter, F.C. Golet, and E.T. LaRoe. 1979. Classification of
wetlands and deep-water habitats of the United States. U.S. Fish and Wildlife
Service FWS/OBS-79/31.
Federal Register. July 13, 1994. Changes in hydric soils of the United States.
Federal Register. September 18, 2002. Hydric soils of the United States.
Hurt, G.W., and L.M. Vasilas, editors. Version 6.0, 2006. Field indicators of hydric
soils in the United States.
National Research Council. 1995. Wetlands: Characteristics and boundaries.
Soil Survey Division Staff. 1993. Soil survey manual. Soil Conservation Service.
U.S. Department of Agriculture Handbook 18. http://www.nrcs.usda.gov/wps/portal/
nrcs/detail/national/soils/?cid=nrcs142p2_054262
Soil Survey Staff. 1999. Soil taxonomy: A basic system of soil classification for
making and interpreting soil surveys. 2nd edition. Natural Resources Conservation
Service, U.S. Department of Agriculture Handbook 436. http://
www.nrcs.usda.gov/wps/portal/nrcs/detail/national/soils/?cid=nrcs142p2_053577
Soil Survey Staff. 2010. Keys to soil taxonomy. 11th edition. U.S. Department of
Agriculture, Natural Resources Conservation Service. http://
www.nrcs.usda.gov/wps/portal/nrcs/detail/national/soils/?cid=nrcs142p2_053580
Tiner, R.W., Jr. 1985. Wetlands of Delaware. U.S. Fish and Wildlife Service and
Delaware Department of Natural Resources and Environmental Control, Wetlands
Section.
United States Army Corps of Engineers, Environmental Laboratory. 1987. Corps of
Engineers wetlands delineation manual. Waterways Experiment Station Technical
Report Y-87-1.
United States Department of Agriculture, Natural Resources Conservation Service.
National forestry manual. http://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/
home/?cid=nrcs142p2_053374
United States Department of Agriculture, Natural Resources Conservation Service.
National range and pasture handbook. http://www.nrcs.usda.gov/wps/portal/nrcs/
detail/national/landuse/rangepasture/?cid=stelprdb1043084
43
United States Department of Agriculture, Natural Resources Conservation Service.
National soil survey handbook, title 430-VI. http://www.nrcs.usda.gov/wps/portal/
nrcs/detail/soils/scientists/?cid=nrcs142p2_054242
United States Department of Agriculture, Natural Resources Conservation Service.
2006. Land resource regions and major land resource areas of the United States,
the Caribbean, and the Pacific Basin. U.S. Department of Agriculture Handbook
296. http://www.nrcs.usda.gov/wps/portal/nrcs/detail/national/soils/?
cid=nrcs142p2_053624
United States Department of Agriculture, Soil Conservation Service. 1961. Land
capability classification. U.S. Department of Agriculture Handbook 210. http://
www.nrcs.usda.gov/Internet/FSE_DOCUMENTS/nrcs142p2_052290.pdf
Custom Soil Resource Report
44
Lucknow Solar DRB Application
ATTACHMENT F
Site Zoning Map
²Harnett.org/GIS
October 24, 2025
Harnett County GIS NOT FOR LEGAL USE
0 2,600
Feet
County Boundary
City Limits
Railroad
Road Centerlines
Interstate
NC
US
Parcels
Cape Fear River
B1
C-3
COMM
CONS
CV
I-10
I-100
IND
OI
R-10
R-20
R-7
R10
R15
RA-30
RA-40
RD
RM
Z
R-7 CZDPUD
MXU-CZD
ETJ
Lucknow Solar Zoning Map
Lucknow Solar DRB Application
ATTACHMENT G
Deeds
Lucknow Solar DRB Application
ATTACHMENT H
SUP Application (September 2023)
NON-RESIDENTIAL SPECIAL USE PERMIT APPLICATION
Signatures
I, as the landowner, hereby CERTIFY that the information contained herein is true to the best of my knowledge; and by accepting this Permit (if approved) shall in every respect conform to the terms of this application and to the provisions of the Statutes and Ordinances regulating development in Harnett
County. Any VIOLATION of the terms above stated immediately REVOKES this Permit. I further
understand this structure is not to be occupied until a CERTIFICATE OF OCCUPANCY is issued. This Permit
expires 24 months (2 years) after the date the Permit is granted by the Harnett County Board of
Adjustment.
Property Owner(s) Signature Date Written Statement
** Applicant is required to answer the following questions under oath at the Board of Adjustment Meeting – Please print answers **
Public Convenience & Welfare
*Please see supplemental narrative and Exhibits A - C for responses to questions 1 – 13.
1. Why are you requesting this use?
2. How will this use benefit the citizens of Harnett County?
On-site & Surrounding Land Uses
3. How will the use you are requesting affect the surrounding properties, residents and businesses in the
area? Describe in detail why and how it will or will not affect the surrounding areas?
Utilities, Access Roads, Drainage, etc…
4. Describe the driveway (width and surface) that you will be using to enter and exit the property.
5. Describe the drainage of this property.
.
6. How is your trash and garbage going to get to the landfill?
Traffic
7. Describe the traffic conditions and sight distances at the State Road that serves the property.
8. What is the approximate distance between your driveway and the next nearest driveway or
intersection?
General
9. How many employees will this development employ?
10. What is the estimated investment of the development?
11. What experience do you have in the proposed field?
Conditions
Lucknow Solar DRB Application
ATTACHMENT I
SUP Approval (November 2023)