Biogeochemical conversion of sulfur species in saline lakes of Steppe Altai

Svetlana V. BORZENKO; Marina N. KOLPAKOVA; Stepan L. SHVARTSEV; Vitaly P. ISUPOV

doi:10.1007/s00343-018-6293-8

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Biogeochemical conversion of sulfur species in saline lakes of Steppe Altai

Geology | Updated：2023-05-19

- Biogeochemical conversion of sulfur species in saline lakes of Steppe Altai
- Biogeochemical conversion of sulfur species in saline lakes of Steppe Altai
- 海洋湖沼学报（英文） 2018年36卷第3期页码：676-686
- Affiliations：
  
  1.Institute of Natural Resources, Ecology and Cryology, Siberian Branch of Russian Academy of Sciences, Chita 672049, Russia
  2.Sobolev Institute of Geology and Mineralogy, Siberian Branch of Russian Academy of Sciences, Novosibirsk 630090, Russia
  3.National Research Tomsk Polytechnic University, Tomsk 634050, Russia
  4.Tomsk Department of the Trofimuk Institute of Petroleum-Gas Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, Tomsk 634050, Russia
  5.Institute of Solid State Chemistry and Mechanochemistry, Siberian Branch of Russian Academy of Sciences, Novosibirsk 630090, Russia
- Author bio：
  
  BORZENKO Svetlana V., svb-64@yandex.ru
- Funds：
  
  the Russian Science Foundation(15-17-10003)
- DOI：10.1007/s00343-018-6293-8
  中图分类号：
- 收稿：2016-11-01，
  
  录用：2017-2-3，
  
  网络首发：2017-04-06，
  
  纸质出版：2018-05
- Accepted：
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Biogeochemical conversion of sulfur species in saline lakes of Steppe Altai[J]. 海洋湖沼学报（英文）, 2018,36(3):676-686.

Svetlana V. BORZENKO, Marina N. KOLPAKOVA, Stepan L. SHVARTSEV, et al. Biogeochemical conversion of sulfur species in saline lakes of Steppe Altai[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(3): 676-686.
Biogeochemical conversion of sulfur species in saline lakes of Steppe Altai[J]. 海洋湖沼学报（英文）, 2018,36(3):676-686. DOI： 10.1007/s00343-018-6293-8.

Svetlana V. BORZENKO, Marina N. KOLPAKOVA, Stepan L. SHVARTSEV, et al. Biogeochemical conversion of sulfur species in saline lakes of Steppe Altai[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(3): 676-686. DOI： 10.1007/s00343-018-6293-8.

摘要

Abstract

The aim of the present research is to identify the main mechanisms of sulfur behavior in saline lakes in the course of time and followed transformations in their chemical composition. The influence of water on chemical composition of biochemical processes involved in decomposition of organic matter was determined by the study of behavior of reduced forms of sulfur in lakes. The determination of reduced forms of sulfur was carried out by successive transfer of each form of sulfur to hydrogen sulfide followed by photometric measurements. The other chemical components were determined by standard methods (atomic absorption

potentiometric method

titration method and others). The salt lakes of the Altai steppe were studied in summer season 2013-2015. Analysis of the chemical composition of the saline lakes of Altai Krai has shown that carbonate-

hydrocarbonate-and chloride ions dominate among anions; sodium is main cation; sulfates are found in subordinate amounts. Reduced forms of sulfur occur everywhere:hydrogen and hydrosulfide sulfur S

prevail in the bottom sediments; its derivative-elemental S

-prevails in the lakes water. The second important species in water of soda lakes is hydrosulfide sulfur S

and in chloride lakes is thiosulfate sulfur S

. The lag in the accumulation of sulfates in soda lakes in comparison to chloride lakes can be explained by their bacterial reduction

followed by the formation and deposition of iron sulfides in sediments. In chloride lakes gypsum is a predominantly barrier for sulfates.

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