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Soil Survey of
Nantucket County Massachusetts
The following map unit description is from the
published "Soil Survey of Nantucket County, Massachusetts"

KaA-Katama sandy loam, 0 to 3 percent slopes. This nearly level,
well drained soil is in smooth areas that are irregular in shape and range from
20 to 200 acres.
Typically, the surface layer is black and reddish brown sandy loam 16 inches
thick (fig. 7). The subsoil is about 18 inches thick. The upper 4 inches of the
subsoil is dark yellowish brown, friable gravelly sandy loam; the lower 14
inches is olive brown, loose sand. The substratum is light yellowish brown sand
to a depth of 60 inches or more.
Included with this soil in mapping are small areas of Riverhead and Evesboro
soils and Udipsamments, rolling. Also included are areas of wind-deposited sand
from nearby sand dunes. Included soils make up about 15 percent of this unit.
The permeability of this soil is moderately rapid in the surface layer and
subsoil and moderately rapid or rapid in the substratum. Available water
capacity is moderate.
Most areas of this soil are in idle farmland or grassland. The soil is well
suited to openland wildlife habitat and most other nonfarm uses.
This soil is suitable for crops, hay, and pasture, but drought in summer
limits the soil for these uses. Irrigation helps overcome the drought
limitation.
This Katama soil has essentially no limitations as a site for buildings or
for local roads and streets; however, the sides of excavations in this soil are
unstable and steep excavations commonly collapse. The soil has few limitations
for septic tank absorption fields, but seepage of the effluent through the
substratum causes a hazard of ground-water contamination.
Capability subclass IIs.
KaB-Katama sandy loam, 3 to 8 percent slopes. This
gently sloping, well drained soil is on the sides of old drainageways. Slopes
are smooth or undulating and mainly are 10 to 100 feet long.
Typically, the surface layer is black and dark reddish brown sandy loam 10
inches thick. The subsoil is 18 inches thick. The upper 4 inches of the subsoil
is dark yellowish brown, friable gravelly sandy loam; the lower 14 inches is
olive brown, loose sand. The substratum is light yellowish brown sand to a depth
of 60 inches or more.
Included with this soil in Mapping are small areas of Riverhead and Evesboro
soils and Udipsamments, rolling. Also included are areas of wind-deposited sand
from nearby sand dunes. Included soils make up about 15 percent of this unit.
The permeability of this soil is moderately rapid in the surface layer and
subsoil and moderately rapid or rapid in the substratum. Available water
capacity is moderate.
Most areas of this soil are in idle farmland or grassland. The soil is well
suited to openland wildlife habitat and most other nonfarm uses.
This soil is suitable for crops, hay, and pasture. Drought in summer is the
main limitation for these uses, and erosion is a hazard. Irrigation helps
overcome the drought limitation. Maintaining a plant cover and using crop
residue and contour farming help to reduce erosion.
This Katama soil has essentially no limitations as a site for buildings or
for local roads and streets; however, the sides of excavations in this soil are
unstable and steep excavations commonly collapse. The soil has few limitations
for septic tank absorption fields, but seepage of the effluent through the
substratum causes a hazard of ground-water contamination.
Capability subclass IIs.
More information on Berryland Soils
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