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An albic horizon can be formed either as a result of lessivage, podzolisation, or reductomorphic processes. Lessivage (argilluviation) is accompanied by the formation of an argic and/or cambi-argic horizon below the clay-translocative horizon. The spodic humus-illuvial or Al-Fe-illuvial horizon is diagnostic for podzolisation in various sands. Noncalcareous(More)
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