Abstract:In the early 50s the increase of magnetic susceptibility in head horizons of soils has been observed. The reason was accepted to be forest and steppe fire. Later we discovered that the increasing of susceptibility and magnetic saturation was observed more clearly in the soils developed on weak magnetic native rock (loam, carbonate) and the magnetic fraction was separated from these soils in a more simple fashion. An abnormal increase in magnetic parameters is observed in primitive soils and the debris layer of… Show more
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