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Illuvium
Illuvium is material displaced across a soil profile, from one layer to another one, by the action of rainwater. The removal of material from a soil layer is called eluviation. The transport of the material may be either mechanical or chemical. The process of deposition of illuvium is termed illuviation.〔(Glossary of Terms: I )〕 It is a water-assisted transport in a basically vertical direction, as compared to alluviation, the horizontal running water transfer. The resulting deposits are called illuvial deposits. Cutans are a type of illuvial deposit.〔(【引用サイトリンク】 publisher = Soil Science Society of America )〕
Illuvium includes organic matter, silicate clay, and hydrous oxides of iron and aluminum.
Illuvial deposits of clays, oxides, and organics accumulate in subsoil as distinctive soil horizons classified as "B horizons" or "zones of illuviation".
==Mechanical illuviation==
When percolating rain water reaches a drier soil horizon, water from the suspension is removed by capillary action of microchannels, leaving fine deposits (cutans) oriented along percolation macrochannels.
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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