Article
Article
Soil
Article By:
Peterson, G. A. Department of Soil and Crop Sciences, Colorado State University, Fort Collins, Colorado.
Last reviewed:April 2019
DOI:https://doi.org/10.1036/1097-8542.631500
Show previous versions
- Soil, published June 2014:Download PDF Get Adobe Acrobat Reader
- Origin and formation
- Classification
- Soil surveys
- Physical properties
- Plant growth and biological activity
- Management
- Related Primary Literature
- Additional Reading
Finely divided rock-derived material containing an admixture of organic matter and capable of supporting vegetation. Soils are independent natural bodies, each with a unique morphology resulting from a particular combination of climate, living plants and animals inhabiting it, parent rock materials, relief, groundwaters, and age. Soils support plants (Fig. 1), occupy large portions of the Earth's surface, and have shape, area, breadth, width, and depth. Note that the term soil, as used here, differs in meaning from the term as used by engineers, where the meaning is unconsolidated rock material. See also: Forest soil; Pedology; Soil chemistry; Soil conservation; Soil ecology; Soil fertility; Soil mechanics; Soil microbiology
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