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Soil Survey of Murray and Whitfield Counties, Georgia

Soil Survey of Murray and Whitfield Counties, Georgia

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138 <strong>Soil</strong> <strong>Survey</strong><br />

on the use <strong>and</strong> the point at which the soil feature is not a limitation. The limitations<br />

appear in order from the most limiting to the least limiting. Thus, if more than one<br />

limitation is identified, the most severe limitation is listed first <strong>and</strong> the least severe one<br />

is listed last.<br />

Crops <strong>and</strong> Pasture<br />

James E. Dean, conservation agronomist, Natural Resources Conservation Service, helped prepare<br />

this section.<br />

General management needed for crops <strong>and</strong> pasture is suggested in this section.<br />

The estimated yields <strong>of</strong> the main crops <strong>and</strong> pasture plants are listed, <strong>and</strong> the system<br />

<strong>of</strong> l<strong>and</strong> capability classification used by the Natural Resources Conservation Service is<br />

explained.<br />

Planners <strong>of</strong> management systems for individual fields or farms should consider the<br />

detailed information given in the description <strong>of</strong> each soil under the heading “Detailed<br />

<strong>Soil</strong> Map Units.” Specific information can be obtained from the local <strong>of</strong>fice <strong>of</strong> the<br />

Natural Resources Conservation Service or the Cooperative Extension Service.<br />

The most important management needs on most <strong>of</strong> the soils used for farming in<br />

<strong>Murray</strong> <strong>and</strong> <strong>Whitfield</strong> <strong>Counties</strong> are controlling water erosion, removing excess water,<br />

<strong>and</strong> maintaining good tilth <strong>and</strong> productivity. Most <strong>of</strong> the soils in the survey area are<br />

susceptible to erosion. The degree <strong>of</strong> erosion depends on the erodibility <strong>of</strong> the soil, the<br />

frequency <strong>and</strong> intensity <strong>of</strong> rainfall, the steepness <strong>and</strong> length <strong>of</strong> slopes, the kinds <strong>of</strong><br />

crops grown, <strong>and</strong> the tillage system used.<br />

Loss <strong>of</strong> the surface layer through erosion is damaging for two major reasons. First,<br />

productivity is reduced as the surface layer is lost <strong>and</strong> part <strong>of</strong> the subsoil is<br />

incorporated into the plow layer. Loss <strong>of</strong> the surface layer is especially damaging on<br />

soils that have a clayey subsoil, such as the Capshaw, Cunningham, Dewey, Enders,<br />

Fullerton, <strong>and</strong> Townley soils. Second, soil erosion on farml<strong>and</strong> results in the<br />

sedimentation <strong>of</strong> streams. Control <strong>of</strong> erosion minimizes this pollution <strong>and</strong> improves the<br />

quality <strong>of</strong> water for municipal use, for recreation, <strong>and</strong> for fish <strong>and</strong> wildlife.<br />

Erosion-control practices provide a protective surface cover, help to control run<strong>of</strong>f,<br />

<strong>and</strong> increase the rate <strong>of</strong> water infiltration. A cropping system that keeps a plant cover<br />

on the surface for extended periods helps to maintain the productive capacity <strong>of</strong> the<br />

soil. On livestock farms, which require pasture <strong>and</strong> hay, including forage crops in the<br />

cropping system reduces the hazard <strong>of</strong> erosion on sloping l<strong>and</strong> <strong>and</strong> improves tilth for<br />

the crops that follow in the rotation.<br />

Applying conservation tillage systems that leave adequate amounts <strong>of</strong> crop residue<br />

on the surface increases the rate <strong>of</strong> water infiltration, helps to control run<strong>of</strong>f, <strong>and</strong><br />

reduces the hazard <strong>of</strong> erosion. This practice can be used on most <strong>of</strong> the soils in<br />

<strong>Murray</strong> <strong>and</strong> <strong>Whitfield</strong> <strong>Counties</strong>. No-till planting is an example <strong>of</strong> a conservation practice<br />

that can be used on most <strong>of</strong> the soils in the survey area.<br />

Terraces <strong>and</strong> diversions reduce the length <strong>of</strong> a slope <strong>and</strong> help to control run<strong>of</strong>f <strong>and</strong><br />

the concentrated flow <strong>of</strong> water on the soil. They are most practical on soils that have<br />

smooth <strong>and</strong> convex slopes, such as the Cunningham, Enders, Dewey, <strong>and</strong> Fullerton soils.<br />

Information about erosion-control <strong>and</strong> drainage practices for each kind <strong>of</strong> soil is<br />

available at the local <strong>of</strong>fice <strong>of</strong> the Natural Resources Conservation Service.<br />

Excess water is a limitation on some soils in the survey area. The type <strong>of</strong> drainage<br />

system needed depends on the soil <strong>and</strong> the kinds <strong>of</strong> crops grown. Arkabutla,<br />

Chenneby, <strong>and</strong> Ketona soils are examples <strong>of</strong> poorly drained or somewhat poorly<br />

drained soils in the county where flooding <strong>and</strong> wetness are management concerns.<br />

Management <strong>of</strong> drainage in conformance with regulations influencing wetl<strong>and</strong>s may<br />

require special permits <strong>and</strong> extra planning.<br />

Natural fertility is low in most <strong>of</strong> the soils in the survey area. The soils in the survey<br />

area are naturally acid. Applications <strong>of</strong> agricultural limestone are needed in order to

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