Abstract
Long-term monitoring data on the ameliorative status of soils in the agrolandscape of a terminal moraine ridge are given. The effect of agroclimatic factors and specific features of the agrolandscape of the experimental station on groundwater level and moisture content in soil horizons are shown. The differentiation of agroameliorative measures for optimizing water–physical soil properties in different parts of the agrolandscape is substantiated.
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