Water-Soluble Components in Soils of Heterolithic Conjugate Landscapes in the Southern Taiga Subzone

Bogatyrev, L.G.; Benediktova, A.I.; Karpukhin, M.M.; Telesnina, V.M.; Zhilin, N.I.; Vartanov, A.N.; Zemskov, P.I.; V, V.D.

Авторы: Bogatyrev L.G., Benediktova A.I., Karpukhin M.M., Telesnina V.M., Zhilin N.I., Vartanov A.N., Zemskov Ph I., V V.Demiv
Журнал: Moscow University Soil Science Bulletin
Номер: 1
Год издания: 2021
Издательство: Allerton Press Inc.
Местоположение издательства: United States
Первая страница: 1
Последняя страница: 13
Оригинальные версии: Водорастворимые компоненты почв гетеролитных сопряженных ландшафтов южнотаежной подзоны
DOI: 10.3103/S0147687421010026
Аннотация: This paper discusses the composition of soil–water extracts prepared from soils developing withina heterolithic geochemical landscape of the Klyazma River basin at the upper reaches of the river. The mainfactors determining the content of water-soluble components are the soil genesis and position in the series ofelementary landscapes. The content of water-soluble macro- and microelements in soil profiles not affectedby anthropogenic impacts is determined by the eluvial–illuvial structure of these soils. In a superaqual landscape withdrawn from the floodplain regime and featuring a complex soil cover, the distribution of water-soluble components in the soil profile is determined by calcareousness of soil–ground waters and their occurrence depth. Another factor affecting the soil solution composition is peat deposits underlying the soils. It isshown that calcium is one of the key elements determining the specificity of the studied heterolithic landscape. The performed cluster analysis confirms the identified differences in the composition of water-solublecomponents in each of the studied soils.
Добавил в систему: Телеснина Валерия Михайловна

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Water-Soluble Components in Soils of Heterolithic Conjugate Landscapes in the Southern Taiga Subzoneстатья

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