马培智, 郑士田, 黄贤瑞. 范各庄井田奥灰水NO3-离子形成机理及在水源判别中的应用[J]. 煤田地质与勘探, 1998, 26(1): 48-50.
引用本文: 马培智, 郑士田, 黄贤瑞. 范各庄井田奥灰水NO3-离子形成机理及在水源判别中的应用[J]. 煤田地质与勘探, 1998, 26(1): 48-50.
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Ma Peizhi, Zheng Shitian, Huang Xianrui. THE FORMATION REASON OF NO3- IN ORDOVICIAN LIMESTONE WATER AND THE APPLICATION OF DISTINGUISHING WATER RESOURCE IN FANGEZHANG COAL MINE[J]. COAL GEOLOGY & EXPLORATION, 1998, 26(1): 48-50.
Citation: Ma Peizhi, Zheng Shitian, Huang Xianrui. THE FORMATION REASON OF NO3- IN ORDOVICIAN LIMESTONE WATER AND THE APPLICATION OF DISTINGUISHING WATER RESOURCE IN FANGEZHANG COAL MINE[J]. COAL GEOLOGY & EXPLORATION, 1998, 26(1): 48-50.
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范各庄井田奥灰水NO3-离子形成机理及在水源判别中的应用

THE FORMATION REASON OF NO3- IN ORDOVICIAN LIMESTONE WATER AND THE APPLICATION OF DISTINGUISHING WATER RESOURCE IN FANGEZHANG COAL MINE

    摘要
  • 摘要: 在分析范各庄井田水文地质特征的基础上,利用水文地球化学理论初步探讨了奥陶系灰岩含水层地下水中赋存高含量NO3-离子的形成机理,介绍了应用这一水化学特征分析矿井充水条件的方法。

     

    Abstract: On the base of analysis of hydrogeological condition in Fan Gezhuang Coal Mine,using hydrogeochemical theory the paper discusses the formation reason of high contention NO3- in Ordovician limestone water.The analysis method of coal mine water inrush conditions,using hydrogeochemical characteristics,were introduced.

     

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