Abstract
Method of allocation and analysis of mobile forms of chemical elements in soil are considered. Chemical characteristics of the extracted liquid phase of the soil reflect its water-soluble part properties. Two reference soil profiles on glaciolacustrine clays (soddy-eluvial-metamorphic soil) and sands (soddy podzol) were investigated on the Russian Plain. The comparison of the data obtained with the results of analysis for the whole soil allows assessment of a share of highly mobile and less mobile forms of chemical compounds. The behavior of macro- and microelements was studied in soils and their liquid phase. Mobile forms of chemical elements play the important role as the basis for the development of a model describing their migration on soil profile, used in prospecting geochemistry and in environmental geochemistry.
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Acknowledgments
Analytical work was done in Chemical Laboratory of Russian Geological Research Institute and in Research Centers of Saint Petersburg State University «Geomodel» and «Methods of chemical analysis».
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Panova, E.G., Bakhmatova, K.A., Matinian, N.N., Oleynikova, G.A. (2020). Determination of Water-Soluble Fraction in Soils. In: Frank-Kamenetskaya, O., Vlasov, D., Panova, E., Lessovaia, S. (eds) Processes and Phenomena on the Boundary Between Biogenic and Abiogenic Nature. Lecture Notes in Earth System Sciences. Springer, Cham. https://doi.org/10.1007/978-3-030-21614-6_9
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