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Correlations between Mercury in Soils and Bottom Deposits of Bol'shoye Yarovoye Lake. / Malikova, I. N.; Strakhovenko, V. D.
в: Chemistry for Sustainable Development, Том 25, № 2, 2017, стр. 191-198.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Correlations between Mercury in Soils and Bottom Deposits of Bol'shoye Yarovoye Lake
AU - Malikova, I. N.
AU - Strakhovenko, V. D.
PY - 2017
Y1 - 2017
N2 - It was found that mercury contents in saline soils of Bol'shoye Yarovoye Lake met the average content in solonetz soils of the steppe zone of Altai Territory. Differences between types of soils are explained by the peculiarities of solonetz and solonchak processes. The distribution of mercury in bottom deposits is uneven both along cores on depth of individual wells, and in different wells. The average content of mercury and the value of the Hg/Al ratio in bottom deposits are significantly higher than their values in soils because of local pollution. Low mercury contents and Hg/Al ratios were found in coastal wells only. Factor analysis and pair correlation method detected differences in correlations of mercury between soils and bottom sediments both in granulometric fractions, and the initial samples. Correlation analysis results in the initial samples of soils and bottom sediments give the overall picture of mercury distribution in the sedimentation process. Mercury in soils has positive correlations with the terrigenous component that is its major natural source. A negative correlation with the "carbonate group" (N a, Mg, Sr) and antimony is typical. Mercury in bottom deposits has positive correlations with antimony and manganese, and is bound with the major composition of precipitates indirectly only. These results argue of a change in the deportment of mercury in the sedimentation process, which confirms its local entrance into precipitation from a technogenic source that is accompanied by antimony.
AB - It was found that mercury contents in saline soils of Bol'shoye Yarovoye Lake met the average content in solonetz soils of the steppe zone of Altai Territory. Differences between types of soils are explained by the peculiarities of solonetz and solonchak processes. The distribution of mercury in bottom deposits is uneven both along cores on depth of individual wells, and in different wells. The average content of mercury and the value of the Hg/Al ratio in bottom deposits are significantly higher than their values in soils because of local pollution. Low mercury contents and Hg/Al ratios were found in coastal wells only. Factor analysis and pair correlation method detected differences in correlations of mercury between soils and bottom sediments both in granulometric fractions, and the initial samples. Correlation analysis results in the initial samples of soils and bottom sediments give the overall picture of mercury distribution in the sedimentation process. Mercury in soils has positive correlations with the terrigenous component that is its major natural source. A negative correlation with the "carbonate group" (N a, Mg, Sr) and antimony is typical. Mercury in bottom deposits has positive correlations with antimony and manganese, and is bound with the major composition of precipitates indirectly only. These results argue of a change in the deportment of mercury in the sedimentation process, which confirms its local entrance into precipitation from a technogenic source that is accompanied by antimony.
KW - mercury
KW - Altai Territory
KW - Bol'shoye Yarovoye Lake
KW - soils
KW - bottom deposits
KW - factor analysis
M3 - Article
VL - 25
SP - 191
EP - 198
JO - Chemistry for Sustainable Development
JF - Chemistry for Sustainable Development
SN - 1817-1818
IS - 2
ER -
ID: 25765328