How Soil is DefinedSoil is the surface of the earth that is not water, air, or rock. More precise definitions diverge in the direction of interest and need. Interest in soil is primarily for agricultural or engineering purposes and this bias is reflected in soil definitions, classification systems, and research. An agricultural definition of soil is "a dynamic natural body on the surface of the earth in which plants grow, composed of mineral and organic materials and living forms" (Brady, 1974, p. 617). The USDA Soil Taxonomy definition is:
An engineering definition of soil is "all the fragmented mineral material at or near the surface of the earth, the moon, or other planetary body, plus the air, water, organic matter, and other substances which may be included therein" (Spangler and Handy, 1982, p. 67). This is the same definition for regolith. Geological definitions of soil depend on the interest of the geologist. "Hard rock" geologists tend to view soil as regolith, employing the engineering definition. Geomorphologists, however, are interested in soil forming processes and adopt definitions and classification systems developed primarily for agriculturists. ReferencesBrady, N.C. (1974). The Nature and Properties of Soils. New York: MacMillan. 639 pp. Buol, S.W., F.D. Hole, and R.J. McCracken (1973). Soil Genesis and Classification. Ames, Iowa: The Iowa State University Press. 360 pp. Soil Survey Staff (1975). Soil Taxonomy. USDA Agriculture Handbook No. 436. Washington, D.C.: U.S. Government Printing Office. 754 pp. Soil Survey Staff (1993). Soil Survey Manual. USDA Handbook No. 18. Washington, D.C.: U.S. Government Printing Office. 437 pp. Spangler, M.G. and R.L. Handy (1982). Soil Engineering. New York: Harper & Row. 819 pp. Text by Joe Tabor |
URL:http://cals.arizona.edu/OALS/soils/defined.html
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