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Soil Survey of Lincoln County, West Virginia - Soil Data Mart - US ...

Soil Survey of Lincoln County, West Virginia - Soil Data Mart - US ...

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<strong>Soil</strong> <strong>Survey</strong> <strong>of</strong> <strong>Lincoln</strong> <strong>County</strong>, <strong>West</strong> <strong>Virginia</strong><br />

manure, returning crop residue to the soil, and growing sod crops, cover crops, and<br />

green manure crops.<br />

Tilth is an important factor affecting the germination <strong>of</strong> seeds and the infiltration <strong>of</strong><br />

water into the soil. <strong>Soil</strong>s that have good tilth have a surface layer that is granular and<br />

porous and have a moderate or high organic matter content. <strong>Soil</strong>s that have poor tilth<br />

have structure that is weak and generally have low organic matter content. In areas<br />

with poor soil tilth, a surface crust generally forms during periods <strong>of</strong> heavy rainfall.<br />

Since the crust is hard when dry and nearly impervious to water, it reduces the rate <strong>of</strong><br />

water infiltration and increases the rate <strong>of</strong> run<strong>of</strong>f and the hazard <strong>of</strong> erosion. Tillage<br />

tends to break down soil structure, especially during periods <strong>of</strong> wetness. As a result, it<br />

should be kept to the minimum necessary to prepare a seedbed and help control<br />

weeds. Continuously cropping the same field for a long period <strong>of</strong> time lowers the<br />

organic matter content and reduces tilth, the rate <strong>of</strong> permeability, and, ultimately,<br />

yields. Maintaining the content <strong>of</strong> organic matter in the plow layer helps to maintain<br />

soil structure. Including grasses and legumes in the cropping sequence and adding<br />

manure or other organic material to the soil help to maintain the organic matter<br />

content.<br />

Many small areas in <strong>Lincoln</strong> <strong>County</strong> are used for home gardens. The soils that are<br />

best suited to garden crops are nearly level or gently sloping, loamy, moderately<br />

permeable, and well drained; have a high available water capacity; and have less than<br />

15 percent rock fragments in the surface layer. Examples are the Kanawha,<br />

Moshannon, and Chagrin soils. The soil pH, or the degree <strong>of</strong> acidity or alkalinity as<br />

determined by means <strong>of</strong> a glass, quinhydrone, or other suitable electrode or indicator<br />

at a specified moisture content or soil-water ratio, should be between 6.0 and 7.0 for<br />

most garden plants.<br />

The suitability <strong>of</strong> the soils in the county to produce grasses and legumes varies<br />

widely because <strong>of</strong> differences in the depth to bedrock or other root-limiting layers,<br />

drainage, the ability to supply moisture, and many other properties. The selection <strong>of</strong><br />

forage species is important, and the species that are selected should be those that<br />

are suited to the different kinds <strong>of</strong> soils. Nearly level and gently sloping, well drained<br />

soils should be used for the most productive crops, such as corn silage, alfalfa, and a<br />

mixture <strong>of</strong> alfalfa and orchardgrass or alfalfa and timothy. Alfalfa should be grown with<br />

cool-season grasses in areas where the soil is at least 2 feet deep over bedrock and<br />

is well drained. The more poorly drained soils, the soils that are less 40 inches deep<br />

over a seasonal high water table, and the soils that are less than 2 feet deep over<br />

bedrock are suited to clover-grass mixtures or to pure stands <strong>of</strong> clover or grasses. In<br />

pastured areas with steeper slopes, sod-forming grasses, such as tall fescue and<br />

bluegrass, minimize erosion. For critical areas, or areas that are bare and undergoing<br />

severe erosion, a grass-legume mixture, such as tall fescue and crownvetch, helps to<br />

control erosion if the ground cover is properly established.<br />

Yields per Acre<br />

The average yields per acre that can be expected <strong>of</strong> the principal crops under a<br />

high level <strong>of</strong> management are shown in table 5. In any given year, yields may be<br />

higher or lower than those indicated in the table because <strong>of</strong> variations in rainfall and<br />

other climatic factors. The land capability classification <strong>of</strong> map units in the survey area<br />

also is shown in the table.<br />

The yields are based mainly on the experience and records <strong>of</strong> farmers,<br />

conservationists, and extension agents. Available yield data from nearby counties and<br />

results <strong>of</strong> field trials and demonstrations also are considered.<br />

The management needed to obtain the indicated yields <strong>of</strong> the various crops<br />

depends on the kind <strong>of</strong> soil and the crop. Management can include drainage, erosion<br />

control, and protection from flooding; the proper planting and seeding rates; suitable<br />

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