Salt composition of groundwater and reclaimed solonetzes in the Baraba Lowland


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Solonetzes of experimental trials established in 1981 and 1986 in the Baraba Lowland were examined. It was found that gypsum-based ameliorants improve the soil and lead to a decrease in the content of soluble salts in the soil profile. Exchange processes between cations of the soil adsorption complex and calcium of gypsum were particularly intensive in the first years after gypsum application. This resulted in a sharp rise in the content of soluble salts that migrated down the soil profile to the groundwater. In the following years, the reclaimed solonetzes were desalinized under the conditions of relatively stable groundwater level. On the 30th year after single gypsum application, the groundwater level sharply rose (to 50 cm), and the soil was subjected to the secondary salinization; the contents of bicarbonates, carbonates, and sodium in the soils increased. Spring leaching caused some desalinization, but the content of soluble salts in the upper soil meter increased again in the fall. A close correlation between the salt compositions of the groundwater and the reclaimed solonetzes was revealed.

作者简介

N. Semendyaeva

Novosibirsk State Agrarian University; Siberian Research Institute of Farming and Chemization of Agriculture, Siberian Federal Scientific Center of Agrobiotechnologies

编辑信件的主要联系方式.
Email: semendyeva@ngs.ru
俄罗斯联邦, Novosibirsk, 630039; Novosibirsk, 630501

N. Elizarov

Institute of Soil Science and Agrochemistry

Email: semendyeva@ngs.ru
俄罗斯联邦, Novosibirsk, 630090


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