Comparative assessment of the contents of magnetic spherules, 137Cs, and 210Pb in soils as applied for the estimation of soil erosion

The contents of magnetic spherules and ^sup 137^Cs and ^sup 210^Pb isotopes were determined in gray forest soils of the Novosil Agroforest Experimental Station in Orel oblast (central part of European Russia). The spatial variability in the contents of these substances was studied, and their distrib...

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Veröffentlicht in:Eurasian soil science 2006-10, Vol.39 (10), p.1100-1115
Hauptverfasser: Gennadiyev, A. N., Golosov, V. N., Chernyanskii, S. S., Markelov, M. V., Kovach, R. G., Belyaev, V. R., Ivanova, N. N.
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container_end_page 1115
container_issue 10
container_start_page 1100
container_title Eurasian soil science
container_volume 39
creator Gennadiyev, A. N.
Golosov, V. N.
Chernyanskii, S. S.
Markelov, M. V.
Kovach, R. G.
Belyaev, V. R.
Ivanova, N. N.
description The contents of magnetic spherules and ^sup 137^Cs and ^sup 210^Pb isotopes were determined in gray forest soils of the Novosil Agroforest Experimental Station in Orel oblast (central part of European Russia). The spatial variability in the contents of these substances was studied, and their distribution in the soil profiles and along soil transects within the afforested and cultivated slopes was analyzed. Factors and processes favoring the accumulation of magnetic spherules and ^sup 137^Cs and ^sup 210^Pb isotopes in the soils, as well as their removal from the soils, were revealed. Similarities and distinctions in the patterns of their behavior were interpreted. Prospects for the combined use of these three tracers to estimate the rates of soil erosion and sediment deposition on the soil surface were tested.[PUBLICATION ABSTRACT]
doi_str_mv 10.1134/S1064229306100085
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subjects Agroforestry
Cesium radioisotopes
Erosion rates
Forest soils
Isotopes
Soil erosion
Soil profiles
Soil surfaces
title Comparative assessment of the contents of magnetic spherules, 137Cs, and 210Pb in soils as applied for the estimation of soil erosion
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