The Sulfur Cycle

STEFAN M. SIEVERT; RONALD P. KIENE; HEIDE N. SCHULZ-VOGT

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The Sulfur Cycle

机译：硫循环

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The ocean represents a major reservoir of sulfur on Earth, with large quantities in the form of dissolved sulfate and sedimentary minerals (e.g., gypsum and pyrite). Sulfur occurs in a variety of valence states, ranging from -2 (as in sulfide and reduced organic sulfur) to +6 (as in sulfate). Sulfate is the most stable form of sulfur on today's oxic Earth; weathering and leaching of rocks and sediments are its main sources to the ocean.

机译：海洋代表着地球上主要的硫磺储集层，以溶解的硫酸盐和沉积性矿物质（例如石膏和黄铁矿）的形式大量存在。硫以多种价态存在，范围从-2（如在硫化物和还原的有机硫中）到+6（如在硫酸盐中）。硫酸盐是当今有氧地球上最稳定的硫形式。岩石和沉积物的风化和浸出是其向海洋的主要来源。

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来源
《Oceanography》 |2007年第2期|117-123|共7页
作者
STEFAN M. SIEVERT; RONALD P. KIENE; HEIDE N. SCHULZ-VOGT;
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作者单位

Biology Department, Woods Hole Oceanographic Institution, Woods Hole, MA, USA;

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正文语种 eng
中图分类海洋学;
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The Sulfur Cycle

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