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Podzel is a type of soil horizon characterized by a distinct layer of leached, light-colored material, typically found beneath the surface layer. It is formed through the process of podzolization, which occurs in cool, humid climates where acidic conditions promote the leaching of minerals and organic matter. This soil type is often associated with coniferous forests and is typically low in nutrients, making it less suitable for agriculture. Podzols are important for understanding soil formation and ecosystem dynamics in specific regions.

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