Труды сотрудников ИЛ им. В.Н. Сукачева СО РАН

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    Biogeochemical migration of calcophylic elements in the conditions of a deep-seated marsh in West Siberia
[Text] / T. T. Efremova [et al.] // J. Radioanal. Nucl. Chem. - 1999. - Vol. 241, Is. 2. - P355-360, DOI 10.1007/BF02347475. - Cited References: 17 . - 6. - ISSN 0236-5731
РУБ Chemistry, Analytical + Chemistry, Inorganic & Nuclear + Nuclear Science & Technology

Аннотация: An accumulation of Cu and As is found in the peat deposit of an eutrophic marsh together with anomalously high concentrations of Ga in some layers. The element dispersed in the peatbog depth in the greatest extent is Zn, and in equally small portions there is dispersed In and Au. The main factors of the biogeochemical migration of Cu, Zn, In, Au, As, Ga in peatbog formation are: the lithological peculiarities of the territory, the oxidation-reduction zonality of the deposit depth within the limits of oxidation and the reduction background, the quality of the humus sorbing barriers, the carbonate equilibrium of marsh waters, and anthropogenic factors. A tendency to accumulate Zn migration streams in the bedding of marsh forests in South West Siberian taiga is observed.

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Держатели документа:
RAS, Siberian Branch, Inst Forest, Krasnoyarsk 660036, Russia
SB RAS, Inst Chem Kinet & Combust, Novosibirsk 630090, Russia
Joint Inst Nucl Res, Neutron Phys Lab, Dubna 141980, Moscow Region, Russia

Доп.точки доступа:
Efremova, T.T.; Efremov, S.P.; Koutzenogii, K.P.; Peresedov, V.F.