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Soil Survey of Murray and Whitfield Counties, Georgia

Soil Survey of Murray and Whitfield Counties, Georgia

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24 <strong>Soil</strong> <strong>Survey</strong><br />

<strong>Soil</strong>s that have pr<strong>of</strong>iles that are almost alike make up a soil series. Except for<br />

differences in texture <strong>of</strong> the surface layer, all the soils <strong>of</strong> a series have major horizons<br />

that are similar in composition, thickness, <strong>and</strong> arrangement.<br />

<strong>Soil</strong>s <strong>of</strong> one series can differ in texture <strong>of</strong> the surface layer, slope, stoniness,<br />

salinity, degree <strong>of</strong> erosion, <strong>and</strong> other characteristics that affect their use. On the basis<br />

<strong>of</strong> such differences, a soil series is divided into soil phases. Most <strong>of</strong> the areas shown<br />

on the detailed soil maps are phases <strong>of</strong> soil series. The name <strong>of</strong> a soil phase<br />

commonly indicates a feature that affects use or management. For example, Fullerton<br />

gravelly silt loam, 6 to 15 percent slopes, is a phase <strong>of</strong> the Fullerton series.<br />

Some map units are made up <strong>of</strong> two or more major soils or miscellaneous areas.<br />

These map units are complexes. A complex consists <strong>of</strong> two or more soils or<br />

miscellaneous areas in such an intricate pattern or in such small areas that they<br />

cannot be shown separately on the maps. The pattern <strong>and</strong> proportion <strong>of</strong> the soils or<br />

miscellaneous areas are somewhat similar in all areas. Shack-Minvale-Bodine<br />

complex, 15 to 30 percent slopes, is an example.<br />

This survey includes miscellaneous areas. Such areas have little or no soil material<br />

<strong>and</strong> support little or no vegetation. Urban l<strong>and</strong>, 2 to 10 percent slopes, is an example.<br />

The table “Acreage <strong>and</strong> Proportionate Extent <strong>of</strong> the <strong>Soil</strong>s” lists the map units in this<br />

survey area. Other tables give properties <strong>of</strong> the soils <strong>and</strong> the limitations, capabilities,<br />

<strong>and</strong> potentials for many uses. The Glossary defines many <strong>of</strong> the terms used in<br />

describing the soils.<br />

AbB—Albertville silt loam, 2 to 6 percent slopes<br />

L<strong>and</strong>form: Hills<br />

L<strong>and</strong>form position: Footslopes<br />

Flooding: None<br />

Slope: Gently sloping<br />

Surface layer:<br />

0 to 6 inches—yellowish brown silt loam<br />

Setting<br />

Typical Pr<strong>of</strong>ile<br />

Subsoil:<br />

6 to 9 inches—brownish yellow silty clay loam that has pale yellow mottles<br />

9 to 24 inches—brownish yellow silty clay that has red <strong>and</strong> pale yellow mottles<br />

24 to 35 inches—brownish yellow silty clay that has red <strong>and</strong> strong brown mottles<br />

35 to 47 inches—brownish yellow silty clay that has red, very pale brown, <strong>and</strong> strong<br />

brown mottles<br />

Underlying material:<br />

47 to 60 inches—multicolored, rippable shale bedrock<br />

<strong>Soil</strong> Properties <strong>and</strong> Qualities<br />

Drainage class: Moderately well drained<br />

Seasonal high water table: Apparent; at a depth <strong>of</strong> 2.5 to 3.5 feet<br />

Permeability: Moderately slow<br />

Available water capacity: Moderate<br />

Root zone: Deep<br />

Minor Components<br />

Conasauga <strong>and</strong> Docena soils, which are in similar l<strong>and</strong>form positions<br />

Cunningham <strong>and</strong> Townley soils, which are in the higher l<strong>and</strong>form positions

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