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Physical Process

Soil Leaching

Biogeochemical and Pedological Processes

The downward movement of dissolved nutrients and minerals out of the upper soil layers as water percolates through, carrying soluble material beyond the reach of plant roots and into deeper soil or groundwater. Leaching is especially pronounced in humid climates with high rainfall and can gradually deplete a soil's fertility if not offset by ongoing nutrient inputs.

Facts
Timescale
Timescale (category)
Years 1
Process Type
Biogeochemical or Pedological 2
Sources
1. Soil salinity control (Wikipedia)
Wikipedia infobox 'Lead section' = 'Soil salinity control refers to controlling the process and progres...' on 'Soil salinity control'View the Source
2. Soil Leaching (Wikipedia)
Wikimedia FoundationIntroduction
Quote, Introduction
Leaching is the process of a solute becoming detached or extracted from its carrier substance by way of a solvent.
View the Source
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