Modification of a content of mobile iron in the podzolic and sod-podzolic soils during growth season
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A content of mobile iron was determined in the forest podzolic and arable sod-podzolic soils. Quantity of the iron combination is changed essentially in the soil profile and during growth season. Correlation between the content of mobile iron and some soil factors: рНКСl, general and mobile carbon of humus, humidity of soil were revealed.
Keywords: soil, iron, season dynamics
