Water Extracts as Criterion of Assessment of Geochemical Conditions on a Monolithic Soil–Geochemical Catena in the Upper Reaches of the ... View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2020-10

AUTHORS

L. G. Bogatyrev, A. I. Benediktova, V. M. Telesnina, M. M. Karpukhin, N. I. Zhilin, Ph. I. Zemskov, V. V. Demin

ABSTRACT

The composition of water-soluble macro- and microelements and anions has been studied in soils formed within a monolithic soil–geochemical catena. It has been shown that the carbon and nitrogen contents regularly increase from eluvial to accumulative landscapes parallel to their hydromorphism. The distribution of water-soluble forms of macro- and microelements is related to bioaccumulative processes and features of eluvial–illuvial differentiation of soils. The margins of the watershed depression are characterized by the combination of eluvial–illuvial differentiation and intensive lateral removal of elements in spring, which determines the maximal leaching of the top soil horizons. The data of the cluster analysis confirm that there is a correlation of soil genesis and location in the system of geochemical catena with the composition of water extracts. More... »

PAGES

159-167

Identifiers

URI

http://scigraph.springernature.com/pub.10.3103/s014768742004002x

DOI

http://dx.doi.org/10.3103/s014768742004002x

DIMENSIONS

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