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Geochemistry Characteristics of Limestone Groundwater and Formation Mechanism of H2S in Sanjiao

机译:三交石灰岩地下水地球化学特征及硫化氢形成机理

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摘要

In order to observe the content of H2S in Sanjiao and its distribution characteristics,hydrogeology conditions of limestone aquifers were analyzed,and some water samples of Taiyuan formation and Shanxi formation were collected and tested,and geochemical characteristics of limestone groundwater were analyzed.Base on the above research,two mechanical models are provided,namely bacterial sulfate reduction and thermochemical sulfate reduction,which could explain genesis of H2S and its heterogeneous distribution.
机译:为了观察三交中H2S的含量及其分布特征,分析了石灰岩含水层的水文地质条件,并收集和测试了太原组和​​山西组的一些水样,并分析了石灰石地下水的地球化学特征。上述研究提供了两种力学模型,即细菌硫酸盐还原和热化学硫酸盐还原,可以解释硫化氢的成因及其异质分布。

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