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How soils
are classified


Pedologists classify soils according to the characteristics of a polypedon. The Soil Survey Staff of the United States Department of Agriculture uses a system that consists of 10 orders (groups) of soils. They are (1) alfisols, (2) aridisols, (3) entisols, (4) histosols, (5) inceptisols, (6) mollisols, (7) oxisols, (8) spodosols, (9) ultisols, and (10) vertisols.

Alfisols develop under forests and grasslands in humid climates. Some agricultural soils are alfisols.

Aridisols occur in dry regions and contain small amounts of organic matter. Desert soils are aridisols.

SOILS ARE CLASSIFIED

Composition of soils

How Soil is Formed

Characteristics of soils

How soils are classified

Soil conservation

Entisols show little development. They resemble the parent material and occur in many climates.

Histosols are organic soils. They form in water-saturated environments, including swamps and bogs.

Inceptisols are only slightly developed. They are more common in subhumid and humid climates, but also occur in most other kinds of climates.

Mollisols develop in prairie regions. They have thick, organically rich topsoils.

Oxisols are the most chemically weathered soils. They have a reddish color and occur in tropical regions.

Spodosols contain iron, aluminum, and organic matter in their B horizons. They form in humid climates.

Ultisols occur in warm, humid climates. They are moist, well-developed, acid soils.

Vertisols form in subhumid and arid warm climates. They develop wide, deep cracks during dry seasons.

Soil conservation

The soils of farmlands, grazing lands, and forestlands provide many products and recreational areas. Soil conservationists work to ensure the wise use of these soils.

Wise use of farmlands involves maintaining a high level of nutrients and organic matter in cultivated soils. Farmers add organic matter to the soil by plowing under certain green plants. They also add fertilizers and rotate crops to replace nutrients that leaching and growing plants remove. In addition, farmers plow and plant their fields in ways that control erosion.

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Grazing lands that have been overgrazed also suffer from erosion. Overgrazing decreases the amounts of plant life and organic matter in the soil, and the soil erodes easily. Ranchers conserve grazing lands by limiting the time that their herds graze in one area.

Forestlands also must be protected from erosion. In some cases, foresters leave unusable branches and other parts of trees on the forest floor to add organic matter to the soil. They also develop large groups of trees whose roots protect the soil by holding it in place against wind and water erosion.

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Contributor: Taylor J. Johnston, Ph.D., Interim Chair, Department of Crop and Soil Sciences, Michigan State University.
Additional resources
Bochnek, Jonathan. The Science of Soil. Gareth Stevens, 1999. Younger readers.
Gerrard, John. Fundamentals of Soils. Routledge, 2000.
Miller, Raymond W., and Gardiner, D. T.Soils in Our Environment. 9th ed. Prentice Hall, 2001.
Singer, Michael J., and Munns, D. N. Soils. 4th ed. Prentice Hall, 1999. -
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