23-04-2012, 05:06 PM
Soil formation
Soil is a natural body consisting of layers (soil horizons) of mineral constituents of variable thicknesses, which differ from the parent materials in their morphological, physical, chemical, and mineralogical characteristics.[1] Strictly speaking, soil is the depth of regolith that influence and have been influenced by plant roots.
Soil is composed of particles of broken rock that have been altered by chemical and mechanical processes that include weathering and erosion. Soil differs from its parent rock due to interactions between the lithosphere, hydrosphere, atmosphere, and the biosphere.[2] It is a mixture of mineral and organic constituents that are in solid, gaseous and aqueous states.[3][4] Soil is commonly referred to as earth or dirt; technically, the term dirt should be restricted to displaced soil. [5]
Soil forms a structure that is filled with pore spaces, and can be thought of as a mixture of solids, water and air (gas).[6] Accordingly, soils are often treated as a three state system.[7] Most soils have a density between 1 and 2 g/cm³.[8] Little of the soil composition of planet Earth is older than the Tertiary and most no older than the Pleistocene.[9] In engineering, soil is referred to as regolith, or loose rock material.
Soil formation, or pedogenesis, is the combined effect of physical, chemical, biological, and anthropogenic processes on soil parent material. Soil genesis involves processes that develop layers or horizons in the soil profile. These processes involve additions, losses, transformations and translocations of material that compose the soil. Minerals derived from weathered rocks undergo changes that cause the formation of secondary minerals and other compounds that are variably soluble in water. These constituents are moved (translocated) from one area of the soil to other areas by water and animal activity. The alteration and movement of materials within soil causes the formation of distinctive soil horizons.
The weathering of bedrock produces the purely mineral based parent material from which soils form. An example of soil development from bare rock occurs on recent lava flows in warm regions under heavy and very frequent rainfall. In such climates, plants become established very quickly on basaltic lava, even though there is very little organic material. The plants are supported by the porous rock as it is filled with nutrient-bearing water which carries dissolved minerals from rocks and guano. The developing plant roots, themselves are associated with mycorrhizal fungi[12] that gradually break up the porous lava, and by these means organic matter and a finer mineral soil soon accumulates.
But even before it does, the predominantly porous broken lava in which the plant roots grow can be considered a soil. How the soil "life" cycle proceeds is influenced by at least five classic soil forming factors that are dynamically intertwined in shaping the way soil is developed, they include: parent material, regional climate, topography, biotic potential and the passage of time.[13]