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LOCATION BARN ISLAND CT | ||
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Tentative Series | ||
BEF-CEP-DCP | ||
03/2024 | ||
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BARN ISLAND SERIES | ||
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MLRA(s)--144A, 145 | ||
Depth class--Very deep | ||
Drainage Class--Very poorly drained | ||
Saturated Hydraulic Conductivity--low to high | ||
Surface Runoff--negligible | ||
Parent material--Sapric herbaceous organic deposits over loamy alluvium, estuarine or glacial deposits | ||
Slope range for series--0 to 2 percent | ||
Mean annual air temperature--10 degrees C (50 degrees F) | ||
Mean annual precipitation--1295 millimeters (51 inches) | ||
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TAXONOMIC CLASS: Loamy, mixed, euic, mesic Terric Sulfisaprists | ||
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TYPICAL PEDON: Barn island mucky peat on a linear, zero percent slope in a tidal marsh. (Colors are for moist soil unless otherwise noted). | ||
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Oese--0 to 32 centimeters (0.0 to 12.6 inches); very dark brown (10YR 2/2) mucky peat; many very fine to medium roots throughout; 80 percent unrubbed plant fiber, 40 percent rubbed plant fiber; H5 von Post humification scale; slight sulfurous odor; neutral (xxx); xxx acid (xxx) oxidized pH; clear boundary. (10 to 50 centimeters thick) | ||
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Oase--32 to 96 centimeters (12.6 to 37.8 inches); very dark brown (10YR 2/2) muck; common very fine to medium roots throughout; 25 percent unrubbed plant fiber, 12 percent rubbed plant fiber fragments; H8 von Post humification scale slight sulfurous odor; neutral (xxx); xxx acid (xxx) oxidized pH; gradual boundary. (hemic material is 20 to 90 centimeters thick, combined thickness of organic horizons is 40 to 130 centimeters) | ||
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Aseg--96 to 112 centimeters (37.8 to 44.1 inches); black (N 2.5/), silt loam; structureless, massive; nonsticky, nonplastic; very fluid; few very fine roots throughout; slight sulfurous odor; neutral (xxx); xxx acid (xxx) oxidized pH; clear boundary. | ||
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ACseg--112 to 129 centimeters (44.1 to 50.8 inches); 90 percent very dark gray (5Y 3/1) and 10 percent greenish gray (10Y 5/1) fine sandy loam; structureless, massive; nonsticky, nonplastic; slightly fluid; slight sulfurous odor; neutral (xxx); xxx acid (xxx) oxidized pH; clear boundary. | ||
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2Cg--129 to 200 centimeters (50.8 to 72.0 inches); greenish gray (10Y 5/1) fine sand; structureless, single grain; nonsticky, nonplastic, nonfluid; neutral (xxx); xxx acid (xxx) oxidized pH. | ||
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TYPE LOCATION: New London County, Town of Stonington, Connecticut; Barn Island Wildlife Management Area, approximately 2,100 feet north of Barn Island Boat Ramp, and 450 feet East of Palmer Neck Road in a tidal marsh. USGS topographic quadrangle: Mystic, CT. | ||
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Latitude--41.3433330 | ||
Longitude-- -71.8765420 | ||
Datum--WGS84 | ||
Coordinates source--from hand-held GPS | ||
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RANGE IN CHARACTERISTICS: | ||
Depth to bedrock--Greater than 200 centimeters | ||
Soil moisture--Saturated; peraquic moisture regime | ||
Reaction throughout--Slightly acid to moderately alkaline | ||
Oxidized reaction--Ultra acid or extremely acid in the organic horizons, and extremely acid to moderately acid in the mineral substrate | ||
Electrical Conductivity (EC 1:5 water)--Greater than 0.6 dS/m throughout | ||
Depth to hypersulfidic materials (incubated pH 4.0 or less)--0 to 50 centimeters | ||
Coarse fragments--0 to 50 percent fine and medium gravels, and/or 0 to 10 percent fine and medium shells in the underlying mineral horizons | ||
Coastal Blue Carbon density range--from XXXX in the organic horizons to XXXX in the mineral substrate. Barn island soils can often average XXXX mega grams of coastal blue carbon per hectare to a 2 meter depth. | ||
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Oa, Oase, Oe, Oese, Oi, or Oise horizons (Oase horizons often dominate the surface and subsurface tiers, other types of O horizons are thin or absent) | ||
Hue--7.5YR, 10YR, 2.5Y, 5Y, or N | ||
Value--2 to 4 | ||
Chroma--0 to 3 | ||
Texture--muck, mucky peat, or peat | ||
Organic matter content--20 percent or more | ||
Von Post Scale of Humification - typically ranges from H7 to H10 | ||
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Aseg or ACseg horizon (where present) | ||
Hue--7.5YR, 10YR, 2.5Y, 5Y, 10Y or N | ||
Value--2 to 3 | ||
Chroma--0 to 2 | ||
Texture--Silt loam, very fine sandy loam, fine sandy loam, sandy loam, coarse sandy loam including mucky analogues. | ||
Manner of failure/fluidity class--slightly fluid to moderately fluid | ||
Organic matter content--less than 20 percent | ||
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2Cseg or 2Cg horizon (where present) | ||
Hue--2.5Y, 5Y, 10Y, or N | ||
Value--2.5 to 5 | ||
Chroma--0 to 3 | ||
Texture--ranges from coarse sand to silty clay loam, coarser textures are typically below 130 centimeters in glacial deposits. | ||
Organic matter content--less than 20 percent | ||
Clay content--5 to 25 percent | ||
Manner of failure / fluidity class--nonfluid to very fluid | ||
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COMPETING SERIES: | ||
There are no competing series in the same family. | ||
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GEOGRAPHIC SETTING: | ||
Parent material--Sapric herbaceous organic material over estuarine, alluvial or glacial deposits | ||
Landscape--Estuaries, coastal lowlands, and tidal rivers | ||
Landform--Tidal marshes | ||
Slope--0 to 2 percent | ||
Mean annual precipitation--1023 to 1320 millimeters (40 to 52 inches) | ||
Mean annual air temperature--4 to 13 degrees C (39.2 to 55.4 degrees F) | ||
Frost-free period--180 to 225 days | ||
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GEOGRAPHICALLY ASSOCIATED SOILS: | ||
These are the Hammonasset, Ipswich, Oyster River, Pawcatuck, Quinnipiac, and Westbrook soils. | ||
Hammonasset soils--formed in thick deposits (greater than 130 centimeters) of sapric dominated organic soil materials. | ||
Ipswich soils--formed in thick deposits of hemic dominated organic soil materials. | ||
Oyster River soils--formed coarse-loamy mineral soil materials with buried organic soil materials 40 centimeters thick within 200 centimeters of the mineral soil surface. | ||
Pawcatuck soils--formed in hemic organic soil materials over sandy mineral soil materials. | ||
Quinnipiac soils--formed in loamy alluvium and do not have histic epipedons. | ||
Westbrook soils--formed in hemic dominated organic soil materials over loamy mineral soil materials | ||
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DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: | ||
Drainage class--Very poorly drained | ||
Saturated hydraulic conductivity--Low to High | ||
Soil moisture regime--Peraquic | ||
Flooded twice daily by tides in addition to periodic riverine flooding at times. | ||
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USE AND VEGETATION: | ||
Major uses--Most areas are in salt marsh and provide food and habitat for fish, shellfish and wildfowl. | ||
Vegetation--Phragmites australis, Spartina alterniflora, Spartina patens, and Salicornia spp. may occur on these soils. | ||
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DISTRIBUTION AND EXTENT: | ||
General area--These soils are located along the Connecticut coast. | ||
Land Resource Regions--R - Northeastern Forage and Forest Region | ||
MLRA(s)--144A, 145 | ||
Extent--Small | ||
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SOIL SURVEY REGIONAL OFFICE (SSRO) RESPONSIBLE: Amherst, Massachusetts | ||
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SERIES ESTABLISHED: New London County, Connecticut, 2024. | ||
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REMARKS: | ||
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Diagnostic horizons and features in this pedon include-- | ||
Peraquic feature--Zero or positive soil water potential at the soil surface. | ||
Particle-size control section--The zone from 0 to 130 centimeters. | ||
Organic soil materials--0 to 96 centimeters | ||
Sapric soil materials--The zone from 32 to 96 centimeters (Oase horizon). | ||
Hypersulfidic materials--The zone from 0 to 129 centimeters (Oese, Oase, 2Aseg, and 2ACseg horizons) have oxidized reactions with pH values less than 4 after 16 weeks. | ||
Lithologic Discontinuity--129 to 200 centimeters. | ||
Taxonomic version--Keys to Soil Taxonomy, 13th edition (2022) | ||
Series Name - Named for the Barn island River, a tidal tributary of the Connecticut River in Old Lyme, CT. | ||
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ADDITIONAL DATA: Type location taken from S2023CT011317 in Barn Island Wildlife Management area, Stonington, CT. | ||
________________________________________ | ||
National Cooperative Soil Survey | ||
U.S.A. |
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LOCATION HAMMONASSET CT | ||
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Tentative Series | ||
Revised DCP-BEF-CEP | ||
03/2024 | ||
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HAMMONASSET SERIES | ||
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MLRA(s)--144A, 145 | ||
Depth class--Very deep | ||
Drainage Class--Very poorly drained | ||
Saturated Hydraulic Conductivity--Low to high | ||
Surface Runoff--Negligible | ||
Parent material--Herbaceous organic material | ||
Slope range for series--0 to 2 percent | ||
Mean annual air temperature--10 degrees C (50 degrees F) | ||
Mean annual precipitation--1295 millimeters (51 inches) | ||
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TAXONOMIC CLASS: Euic, mesic Typic Sulfisaprists | ||
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TYPICAL PEDON: Hammonasset mucky peat on a linear, zero percent slope in a tidal marsh. Tidal range is 194 centimeters. (Colors are for moist soil unless otherwise stated). | ||
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Oese--0 to 33 centimeters (0 to 13 inches); very dark brown (10YR 2/2) mucky peat, very dark gray (2.5Y 3/1) rubbed; 50 percent unrubbed fibers, 30 percent rubbed fibers; H3 von Post humification; many very fine, fine, and medium, few coarse roots throughout; 10 percent mineral soil material; negative color change with 3% hydrogen peroxide; slight effervescence with 30% hydrogen peroxide; moderately saline; neutral (xxx); xxx acid (xxx) oxidized pH; clear boundary. (0 to 56 centimeters thick.) | ||
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Oase1--33 to 108 centimeters (13 to 43 inches); very dark gray (10YR 3/1) muck, black (10YR 2/1) rubbed; 25 percent unrubbed fibers, 12 percent rubbed fibers; H8 von Post humification; common very fine and fine roots throughout; 5 percent mineral soil material; slight sulfurous odor; negative color change with 3% hydrogen peroxide; slight effervescence with 30% hydrogen peroxide; moderately saline; neutral (xxx); xxx acid (xxx) oxidized pH; gradual boundary. | ||
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Oase2--108 to 200 centimeters (43 to 79 inches); very dark gray (2.5Y 3/1) muck; 10 percent unrubbed fibers, 3 percent rubbed fibers; H9 von Post humification; few fine roots throughout; 40 percent mineral soil material; slight sulfurous odor; negative color change with 3% hydrogen peroxide; slight effervescence with 30% hydrogen peroxide; moderately saline; neutral (xxx); xxx acid (xxx) oxidized pH. (Combined thickness of Oase horizons is 132 to 200 centimeters thick.). | ||
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TYPE LOCATION: Middlesex County, Connecticut; Hammock River Marsh Wildlife Area, approximately 540 feet northeast (73 degree bearing) of intersection of E Main Street and Meadow Road in Clinton, CT. USGS topographic quadrangle: Clinton, CT. | ||
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Latitude--41.2716020 | ||
Longitude-- -72.5003911 | ||
Datum--WGS84 | ||
Coordinates source--from hand-held GPS | ||
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RANGE IN CHARACTERISTICS: | ||
Depth to bedrock--Greater than 200 centimeters | ||
Soil moisture--Saturated; peraquic moisture regime | ||
Reaction throughout--Slightly acid to moderately alkaline | ||
Oxidized reaction--Ultra acid or extremely acid | ||
Electrical Conductivity (EC 1:5 water)--Greater than 0.6 dS/m throughout | ||
Depth to hypersulfidic materials (incubated pH 4.0 or less)--0 to 100 centimeters | ||
Coastal Blue Carbon density range--from XXXX in the organic horizons to XXXX in the mineral substrate, if present. Hammonasset soils can often average XXXX mega grams of coastal blue carbon per hectare to a 2-meter depth. | ||
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Oase horizon | ||
Hue--2.5YR, 5YR, 7.5YR, 10YR, or 2.5Y | ||
Value--2 to 3 | ||
Chroma--1 or 2 | ||
Texture--Muck | ||
Organic matter content--30 to 100 percent | ||
Rubbed fiber content--1 to 15 percent | ||
Von Post humification--H7to H10 | ||
Mineral soil content--0 to 70 percent | ||
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Oese (where present) | ||
Hue--10YR, 2.5Y, or 5Y | ||
Value--2 to 3 | ||
Chroma--1 or 2 | ||
Texture--Mucky peat | ||
Organic matter content--50 to 92 percent | ||
Rubbed fiber content--18 to 38 percent | ||
Von Post humification scale-H4 to H6 | ||
Mineral soil content--8 to 50 percent | ||
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Oise horizon (where present) | ||
Hue--7.5YR, 10YR, 2.5Y, 5Y, or 10Y | ||
Value--2 to 3 | ||
Chroma--1 to 3 | ||
Texture--Peat | ||
Organic matter content--90 to 95 percent | ||
Rubbed fiber content--40 to 75 percent | ||
Von Post humification scale--H1 to H3 | ||
Mineral soil content--5 to 10 percent | ||
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Aseg horizon (where present) | ||
Hue--N | ||
Value--2.5 | ||
Chroma--0 | ||
Texture--mucky silt loam | ||
Clay content-- | ||
Manner of failure / fluidity class--moderately fluid | ||
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2Cseg or 2Cse (where present) | ||
Hue--10YR, 2.5Y, 5Y, 10Y, 5GY, or 10BG | ||
Value--2 to 4 | ||
Chroma--1 to 3 | ||
Texture--fine sand, loamy fine sand, sandy loam, very fine sandy loam, silt loam, or silty clay loam and their mucky analogs | ||
Unrubbed fiber content--0 to 35 percent | ||
Clay content-- | ||
Manner of failure / fluidity class--nonfluid to moderately fluid | ||
Coarse fragments--0 to 12 percent, by volume, fine and medium gravels | ||
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COMPETING SERIES: | ||
There are no competing series in the same family. | ||
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GEOGRAPHIC SETTING: | ||
Parent material--herbaceous organic material sometimes underlain by coarse-loamy estuarine deposits | ||
Landscape--Coastal estuaries, coastal lowlands, and tidal rivers | ||
Landform--Tidal marshes | ||
Slope--0 to 2 percent | ||
Mean annual precipitation--754 to 1826 millimeters (40 to 52 inches) | ||
Mean annual air temperature-6.4to 16.2 degrees C (39.2 to 55.4 degrees F) | ||
Water salinity range--18 to 30 parts per thousand | ||
Frost-free period--180 to 204 days | ||
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GEOGRAPHICALLY ASSOCIATED SOILS: | ||
These are the Barn Island, Calves, Ipswich, Pawcatuck, Quinnipiac, and Westbrook soils. | ||
Barn Island soils--formed in sapric dominated organic soil materials over loamy mineral soil materials. | ||
Calves soils--formed in loamy estuarine deposits overlying loamy or sandy alluvium and have a histic epipedon | ||
Ipswich soils--formed in thick deposits of hemic dominated organic soil materials. | ||
Pawcatuck soils--formed in hemic organic soil materials over sandy mineral soil materials. | ||
Quinnipiac soils--formed in loamy alluvium and do not have thick organic soil materials. | ||
Westbrook soils--formed in hemic dominated organic soil materials over loamy mineral soil materials. | ||
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DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: | ||
Drainage class--Very poorly drained | ||
Saturated hydraulic conductivity--Low to high | ||
Soil moisture regime--Peraquic | ||
Flooded twice daily by tides in addition to periodic riverine flooding at times. | ||
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USE AND VEGETATION: | ||
Major uses--Most areas are in salt marsh and provide food and habitat for fish, shellfish and wildfowl. | ||
Vegetation--Phragmites australis, Spartina alterniflora, Spartina patens, and Salicornia spp. may occur on these soils. | ||
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DISTRIBUTION AND EXTENT: | ||
General area--These soils are located along the Connecticut coast. | ||
Land Resource Regions--R - Northeastern Forage and Forest Region | ||
MLRA(s)--144A, 145 | ||
Extent--Small | ||
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SOIL SURVEY REGIONAL OFFICE (SSRO) RESPONSIBLE: Amherst, Massachusetts | ||
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SERIES ESTABLISHED: Middlesex County, Connecticut, 2024. | ||
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REMARKS: | ||
Diagnostic horizons and features in this pedon include-- | ||
Peraquic feature--Zero or positive soil water potential at the soil surface. | ||
Particle-size control section--The zone from 0 to 130 centimeters. | ||
Hemic soil materials--The zone from 0 to 33 centimeters (Oese horizon). | ||
Sapric soil materials--The zone from 33 to 200 centimeters (Oase horizons). | ||
Hypersulfidic materials--The zone from 0 to 200 centimeters (Oese and Oase horizons) have oxidized reactions with pH values less than 4.0 after 16 weeks. | ||
Taxonomic version--Keys to Soil Taxonomy, 13th edition (2022) | ||
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ADDITIONAL DATA: Type location taken from S2023CT007348 in Hammock River Marsh Wildlife Area, Clinton, CT. | ||
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Additional support pedons used to develop this series include S2023CT007220, S2023CT007228, S2023CT007243, S2023CT007340, S2023CT007356, S2023CT009243, S2023CT009248, S2023CT011201, S2023CT011226, and S2023CT011279. | ||
________________________________________ | ||
National Cooperative Soil Survey | ||
U.S.A. |
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