Abstract
The regularities of water infiltration and evaporation of groundwater at different depths of the groundwater table were established for soddy-podzolic and dark gray forest soils. The recharge of the soils with moisture from the groundwater decreased with a lowering of its table, and the infiltration increased. At the high groundwater table (70 cm from the surface), the moisture recharge of the soddy-podzolic soil amounted to 86 mm and the infiltration amounted to 17 mm; at the groundwater table of 145 cm, these values were 13 and 51 mm, respectively. The concentrations of chemical elements in the lysimeters with the high groundwater table were 2–4 times greater than those in the lysimeters with the low groundwater table.
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