soil profile
Cross-sectional view of the horizons in a soil. See soil horizon.
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Cross-sectional view of the horizons in a soil. See soil horizon.
See porosity.
Rate at which water and air move from upper to lower soil layers. Compare porosity.
Horizontal zones that make up a particular mature soil. Each horizon has a distinct texture and composition that vary with different types of soils. See soil profile.
Movement of soil components, especially topsoil, from one place to another, usually by wind, flowing water, or both. This natural process can be greatly accelerated by human activities that remove vegetation from soil.
Methods used to reduce soil erosion, prevent depletion of soil nutrients, and restore nutrients already lost by erosion, leaching, and excessive crop harvesting.
Complex mixture of inorganic minerals (clay, silt, pebbles, and sand), decaying organic matter, water, air, and living organisms.
See windbreak.
Rock that forms from the accumulated products of erosion and in some cases from the compacted shells, skeletons, and other remains of dead organisms. See rock cycle. Compare igneous rock, metamorphic rock.
Accumulation of salts in soil that can eventually make the soil unable to support plant growth.
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