Claypan is a dense, compact, slowly permeable layer in the subsoil.[1] It has a much higher clay content than the overlying material, from which it is separated by a sharply defined boundary. The dense structure restricts root growth and water infiltration. Therefore, a perched water table might form on top of the claypan.[2] In the Canadian classification system, claypan is defined as a clay-enriched illuvial B (Bt) horizon.[3]
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