埋藏环境硫酸盐岩岩溶发育的微生物机理

张凤娥; 张胜; 齐继祥; 张云; 宋淑红

doi:10.3799/dqkx.2010.015

Volume 35 Issue 1

Jan. 2010

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Article Navigation > Earth Science > 2010 > 35(1): 146-154

ZHANG Feng-e, ZHANG Sheng, QI Ji-xiang, ZHANG Yun, SONG Shu-hong, 2010. Bacterial Mechanism of the Development of Sulfate Karst in Burial Environment. Earth Science, 35(1): 146-154. doi: 10.3799/dqkx.2010.015

Citation:

ZHANG Feng-e, ZHANG Sheng, QI Ji-xiang, ZHANG Yun, SONG Shu-hong, 2010. Bacterial Mechanism of the Development of Sulfate Karst in Burial Environment. Earth Science, 35(1): 146-154. doi: 10.3799/dqkx.2010.015

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Bacterial Mechanism of the Development of Sulfate Karst in Burial Environment

doi: 10.3799/dqkx.2010.015

Institute of Hydrogeology & Engineering Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China

Received Date: 2009-06-13
Publish Date: 2010-01-01

Abstract

Abstract

The present work is designed to simulate the dissolution of sulphate rock under various conditions of different bacterial cell numbers, temperatures and reaction times both in water-rock and water-rock-bacteria systems by laboratory experiment. The results show that chemical dissolution of sulphate rock is dominated in water-rock system, while bacterial sulphate reduction process and the dissolution of sulphate rock driven by bacterial sulphate reduction are dominated in water-rock-bacteria system. The dissolution of sulphate rock driven by bacterial sulphate reduction resultes in the formation of sulphate karst, which enhances the permeability of carbonate rock coexisted with sulphate rock. The research is an insight into biokarst, which provides a new perspective for the field of petroleum geology.
- sulfate karst,
- sulfate-reducing bacteria (SRB),
- bacterial sulfate reduction,
- water-rock-bacteria system,
- burial environment,
- hydrogeology

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References(44)

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Bacterial Mechanism of the Development of Sulfate Karst in Burial Environment

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