The lateral or downward movement of dissolved or suspended material within soil when rainfall exceeds evaporation.
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The lateral or downward movement of dissolved or suspended material within soil when rainfall exceeds evaporation.
The lateral or downward movement in suspension of clay or other fine particles. The clay-depleted horizon thus formed is an eluvial horizon and is found either below or in place of the A horizon. The eluviated particles may accumulate in the B horizon to form a clay pan.
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