Fractionation of stable sulfur isotopes in hydromorphic saline soils and its role as an indicator of reducing processes

被引：0

作者：

Oleinik, SA ^{[1
]}

Ryskov, YG ^{[1
]}

Morgun, EG ^{[1
]}

机构：

[1] Russian Acad Sci, Inst Physicochem & Biol Problems Soil Sci, Pushchino 142290, Moscow Oblast, Russia

来源：

GEOCHEMISTRY INTERNATIONAL | 2003年 / 41卷 / 12期

关键词：

D O I：

暂无

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

The distribution of stable sulfur isotopes in various hydromorphic soil profiles has been studied. The reduction in the soil profile is expressed as an appreciable enrichment of reduced sulfide of the light S-32 isotope and concomitant enrichment of residual sulfate of the heavy S-32 isotope. The distribution of stable sulfur isotopes is characterized by a specific structure that bears information on the direction of motion and transformation of sulfur compounds.

引用

页码：1207 / 1213

页数：7

共 47 条

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