E horizon
Quick Summary
The E horizon is a distinct soil layer characterized by a lighter color and a significant loss of clay and humus. This depletion, known as eluviation, gives the E horizon a bleached appearance. This process occurs as percolating water washes these materials downward from the surface layers. The development of E horizons is more common in areas with high rainfall and sandy soil, which facilitate extensive water percolation.12
Soil horizons are layers within the soil profile, formed by the combined actions of living organisms and percolating water. From top to bottom, the main horizons are O, A, E, B, C, and R. The E horizon lies below the A horizon and above the B horizon, which accumulates the leached materials.231
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