1. Specific Features of the Elemental Composition of Alluvial Soils in the Middle Reaches of the Bolshaya Kokshaga River.
- Author
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Isaev, A. V., Demakov, Y. P., and Sharafutdinov, R. N.
- Subjects
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FLUVISOLS , *SOIL composition , *TRACE elements , *PEAT soils , *COMPOSITION of sediments , *SOIL classification , *SHORELINES , *TRACE metals - Abstract
The contents of chemical elements in the alluvial soils (Fluvisols) in the middle reaches of the Bolshaya Kokshaga River have been studied, The parent material of these soils inherits its composition from sediments of the Central Russian and Cisuralian mineralogical and geochemical provinces. Limits of the bulk contents of elements and their background concentrations have been established, which forms the basis for the environmental monitoring in the Bolshaya Kokshaga Nature Reserve. In total, 34 elements have been determined in the alluvial soils and sands of shoreline shoals; the most abundant elements with concentrations above 1 g/kg are Si, Al, Fe, Ca, K, Mg, Na, Ti, Mn, P, and S. Element concentrations in different types of soils differ in a statistically significant manner. The highest similarity in the elemental composition is observed for meadow and mucky gley soils. As compared with the alluvial soils, the sands of shoreline shoals display the maximum content of Si and the minimum contents of other elements. Soddy soils are characterized by the low content of all elements, except for Si. Meadow and mucky gley soils accumulate larger amounts of Al, Fe, K, Na, Mg, Ti, Mn, Ba, Cr, Zn, Ni, V and As, while eutrophic peat soils (highly mineralized peat deposits) accumulate more Ca, S, P, Sr, Cl, and Rb. Concentrations of As, Cu, V, P, Zr, Ni, and Zn in the alluvial soils exceed their natural abundance in the Earth crust (clarke values) by 1.5–2 times (Kc = 1.5–2), while concentrations of Al, K, Mg, Ti, Sr, Rb, Na, Cl, and Ca are below their clarke values (Kc < 1); concentrations of other elements are comparable to clarke values. [ABSTRACT FROM AUTHOR]
- Published
- 2023
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