Illuviation is the accumulation, in a lower soil horizon, of clay particles, organic matter, iron and aluminium oxides or dissolved minerals that percolating water has carried down from the horizons above. It is the paired counterpart to eluviation, the leaching that removes the same material from the upper horizon, and the two together are the mechanism that builds the layered profile, an organic-poor, leached upper horizon over a clay-enriched or iron-stained lower one, used to classify and identify soil types in the field. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
Facts
Timescale
Timescale (category) Timescale (category) Process TypeBiogeochemical or Pedological 1 TimescaleYears to centuries, over the course of soil profile development. 1 Connections
Associated With
Source Illuviation (Wikipedia)
Sources
1. Illuviation (Wikipedia)
Wikimedia FoundationIntroduction
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.
- In Category: Physical Processes
- Associated With: Pedogenesis
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