LOCATION WOODMANSIE              NJ

Established Series
CS/Rev. JAK
11/2015

WOODMANSIE SERIES


TAXONOMIC CLASS: Coarse-loamy, siliceous, semiactive, mesic Typic Hapludults
MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA
DEPTH CLASS: Very deep
DRAINAGE CLASS: Well drained
PERMEABILITY: Moderate or moderately rapid in the solum and moderate to rapid in the substratum
SURFACE RUNOFF: Slow
PARENT MATERIAL: Loamy siliceous marine sediments
SLOPE: 0 to 10 percent
MEAN ANNUAL AIR TEMPERATURE (type location): 55 degrees F.
MEAN ANNUAL PRECIPITATION (type location): 44 inches

TAXONOMIC CLASS: Coarse-loamy, siliceous, semiactive, mesic Typic Hapludults

TYPICAL PEDON: Woodmansie sand, wooded. (Colors are for moist soils.)

A--0 to 2 inches; dark gray (N 4/0) sand; single grain; loose; less than 1 percent, by volume fine rounded quartz pebbles; very strongly acid; abrupt smooth boundary. (0 to 4 inches thick)

E--2 to 8 inches; gray (10YR 6/1) sand; single grain; loose; 1 percent fine rounded quartzose pebbles; very strongly acid; clear wavy boundary. (6 to 12 inches thick)

BE--8 to 17 inches; light yellowish brown (10YR 6/4) sand; single grain; loose; 2 percent, by volume rounded quartzose pebbles; very strongly acid; abrupt smooth boundary. (3 to 13 inches thick)

Bt--17 to 30 inches; yellowish brown (10YR 5/6) sandy loam; weak fine and medium subangular blocky structure; very friable; slightly sticky, nonplastic; common clay and silt bridging of sand grains; 3 percent, by volume fine and coarse rounded quartzose pebbles; very strongly acid; gradual smooth boundary. (10 to 20 inches thick)

C1--30 to 45 inches; yellow (2.5Y 8/6) coarse sand; single grain; loose; 10 percent, by volume fine pebbles; very strongly acid; gradual smooth boundary.

C2--45 to 60 inches; reddish yellow (7.5YR 6/6) coarse sandy loam; massive; friable; all grains coated and bridged with clay; very strongly acid.

TYPE LOCATION: Burlington County, New Jersey, 0.2 mile west of Burlington County Line on New Jersey Highway 72; about 0.3 mile southwest at intersection of two sand roads, on eastern side of Coyle Airport.

RANGE IN CHARACTERISTICS:
Solum Thickness: 24 to 50 inches
Depth to Bedrock: Greater than 60 inches
Depth to Seasonal High Water Table: Greater than 72 inches
Rock Fragments: 0 to 15 percent, by volume in the A horizon, 0 to 30 percent in the upper part of the B horizon, and at higher elevations, 0 to 50 percent in the lower part of the B horizon and the C horizon, mostly quartz pebbles
Soil Reaction: Extremely acid to strongly acid, throughout the profile, unless limed
Other Features: Some pedons in wooded areas have a microsequence of an A, E, and Bh horizon (micro-podzol). Total thickness of the A, E, and Bh horizons is less than 6 inches and individual horizons are less than 2 inches thick.

RANGE OF INDIVIDUAL HORIZONS:
O horizon (if it occurs):
Color--hue of 7.5YR to 10YR, value of 2 or 3, chroma of 1 to 3
Texture--slightly decomposed to highly decomposed plant material

A horizon:
Color--hue of 10YR to 2.5Y, value of 2 to 4, chroma of 1 or 2, or is neutral with value of 2.5 to 4
Texture--sand or loamy sand

Ap horizon (if it occurs):
Color--hue of 10YR to 2.5Y, value of 3 to 5, chroma of 2 to 4
Texture--sand or loamy sand

E horizon:
Color--hue of 10YR to 2.5Y, value of 6 to 8, chroma of 1 or 2
Texture--sand or loamy sand

Bh horizon (if it occurs):
Color--hue of 5YR to 10YR, value of 3 or 4, chroma of 2 or 4
Texture--sand or loamy sand, and commonly contains iron concretions

BE horizon:
Color--hue of 7.5YR to 2.5Y, value of 5 to 8, chroma of 3 to 6
Texture--sand or loamy sand

Bt horizon:
Color--hue of 7.5YR to 2.5Y, value of 5 or 6, chroma of 4 to 8
Texture (fine-earth fraction)--dominantly sandy loam, and may contain thin layers of sandy clay loam or loamy sand

BC horizon (if it occurs):
Color--hue of 7.5YR to 2.5Y, value of 4 to 6, chroma of 4 to 8
Texture (fine-earth fraction)--sandy clay loam, fine sandy loam, sandy loam, loamy fine sand, or loamy sand

C horizon:
Color--hue of 7.5YR to 2.5Y. value of 4 to 8, chroma of 4 to 8
Texture (fine-earth fraction)--stratified sandy clay loam, fine sandy loam, sandy loam, loamy fine sand, loamy sand, fine sand, or sand

COMPETING SERIES:
Dennisville soils--have redoximorphic features above 72 inches, on similar landforms
Downer soils--have a sandy E horizon less than 6 inches thick and do not allow rock fragments of more than 15 percent, by volume above 40 inches, on slightly higher landforms
Ingleside soil--have redoximorphic features above 72 inches, on similar landforms
Massanutten soils--moderately deep to lithic contact and formed in residuum weathered from sandstone
Phalanx soils--have iron cemented sandstone rock fragments within 40 inches, on slightly higher landforms
Swainton soils--have E horizons that are less than 6 inches thick, on similar landforms
Zepp soils--formed in colluvium underlain by residuum weathered form sandstone and shale

GEOGRAPHIC SETTING:
Landscape: Coastal Plain
Landform: Uplands and interstream divides
Elevation: 100 to 250 feet
Parent Material: Loamy siliceous marine sediments
Mean Annual Air Temperature: 52 to 58 degrees F.
Mean Annual Precipitation: 42 to 48 inches
Frost Free Period: 190 to 210 days

GEOGRAPHICALLY ASSOCIATED SOILS:
Aura soils--have a fine-loamy particle-size control section and a fragipan, on similar landforms
Downer soils--have a sandy E horizon less than 6 inches thick and do not allow rock fragments of more than 15 percent, by volume above 40 inches, on slightly higher landforms
Evesboro soils--excessively drained with a sandy particle-size control section, on similar landforms
Fort Mott soils--have sandy surface layers more than 20 inches thick, on slightly higher landforms
Hammonton soils--moderately well drained with a seasonal high water table above 42 inches, on lower landscape positions
Lakehurst soils--moderately well drained with a spodic horizon and a seasonal high water table above 42 inches, on lower landscape positions
Lakewood soils--excessively drained with a spodic horizon, on slightly higher lying positions
Sassafras soils--have a fine-loamy particle-size control section, on similar landforms
Woodstown soils--have a fine-loamy particle-size control section and have a seasonal high water table above 42 inches, on lower landscape positions

USE: Nearly all areas are wooded.

VEGETATION: Native vegetation is influenced by the frequency of forest fires at each site. Where wildfires have been prevalent, the vegetation is scrub oak, pitch pine, and black jack oaks less than 5 feet tall. In other areas of less severe fires, the vegetation consists of black, white, and scarlet oaks; pitch, shortleaf, and Virginia pines, and an understory of ericaceous shrubs.

DISTRIBUTION: The eastern part of the Atlantic Coastal Plain in New Jersey

EXTENT: Moderate

SERIES ESTABLISHED: New Jersey, Burlington County, 1967

REMARKS: Diagnostic horizons and other diagnostic soil characteristics recognized in this pedon are:
Ochric epipedon--the zone from the soil surface to a depth of 17 inches (A, E, and BE horizons)
Albic horizon--the zone from 2 to 8 inches (E horizon)
Argillic horizon--the zone from 17 to 30 inches (Bt horizon)

SERIES INTERPRETATION RECORD(S): NJ0012, NJ0226 (FIRM SUBSTRATUNM), NJ0227 (LOAMY SUBSTRATUM)

TABULAR SERIES DATA:

SOI-5  Soil Name   Slope  Airtemp FrFr/Seas Precip  Elevation
NJ0012 WOODMANSIE  0- 10     -        -       -         -     
NJ0226 WOODMANSIE  0-  5     -        -       -         -     
NJ0227 WOODMANSIE  0-  5   50- 55  160-190  40- 48      -     

SOI-5  FloodL FloodH Watertable Kind   Months  Bedrock Hardness
NJ0012 NONE          6.0-6.0              -     >60        
NJ0226 NONE          6.0-6.0              -     >60        
NJ0227 NONE          6.0-6.0              -     >60        

SOI-5  Depth  Texture                3-Inch  No-10  Clay%   -CEC-
NJ0012  0-17  S LS                    0-  0  85-100  5-17    -   
NJ0012 17-30  SL GR-SL SCL            0-  0  60-100  5-17    -   
NJ0012 30-60  SR GR-S SCL             0-  0  40-100  1-25    -   
NJ0226  0-17  S LS                    0-  0  85-100  0- 5    -   
NJ0226 17-30  SL GR-SCL               0-  0  55-100 10-25    -   
NJ0226 30-60  SC GR-SCL               0-  0  50- 85 20-32    -   
NJ0227  0-17  S LS                    0-  0  85-100  2- 6   1-  6
NJ0227 17-30  SL GR-SL SCL            0-  0  60-100 10-25   3-  8
NJ0227 30-40  GRV-LS S SL             0-  2  40-100  2-10   1-  3
NJ0227 40-60  SCL SC C                0-  0  85-100 25-45   8- 14

SOI-5  Depth    -pH-     O.M.  Salin  Permeab   Shnk-Swll
NJ0012  0-17  3.6- 4.4    -    0- 0   6.0-  20  LOW      
NJ0012 17-30  3.6- 5.5    -    0- 0   0.6- 6.0  LOW      
NJ0012 30-60  3.6- 5.5    -    0- 0   0.6-  20  LOW      
NJ0226  0-17  3.6- 4.4  .5-1.  0- 0   6.0-  20  LOW      
NJ0226 17-30  3.6- 5.5    -    0- 0   2.0- 6.0  LOW      
NJ0226 30-60  3.6- 5.5    -    0- 0   0.2- 0.6  LOW      
NJ0227  0-17  3.6- 4.4  .5-2.  0- 0   6.0-  20  LOW      
NJ0227 17-30  3.6- 4.4  0.-.5  0- 0   2.0- 6.0  LOW      
NJ0227 30-40  3.6- 5.5  0.-.5  0- 0   2.0-  20  LOW      
NJ0227 40-60  3.6- 5.5  0.-.5  0- 0  0.06- 2.0  MODERATE 


National Cooperative Soil Survey
U.S.A.