WINTER INTRASOIL MOISTURE MIGRATION AND SALT TRANSPORT IN SALINE SOIL OF BARABA
We present quantitative data of transfer and removal of soluble salts on the soil surface with saline soils in the forest-steppe zone of Baraba plain as an example. In the control the content of salt ions in the snow-water in the bottom layer of snow by the end of winter is higher than in the initial period of the winter. It is clearly seen for the sodium and sulfate ions and it is less pronounced for the hydrocarbonate ions. The content of calcium and magnesium ions decreases, probably due to the precipitation of carbonate ions to the surface during recrystallization of snow.