段玉成, 黑磊, 解克新. 古汉山井田地下水同位素组成特征研究[J]. 煤田地质与勘探, 1992, 20(6): 47-50.
引用本文: 段玉成, 黑磊, 解克新. 古汉山井田地下水同位素组成特征研究[J]. 煤田地质与勘探, 1992, 20(6): 47-50.
Duan Yucheng, Hei Lei, Jie Kexin. THE RESEARCH ON THE ISOTOPE COMPOSITION FEATURES OF THE UNDERGROUND WATER IN GUHANSHAN COAL MINE FIELD[J]. COAL GEOLOGY & EXPLORATION, 1992, 20(6): 47-50.
Citation: Duan Yucheng, Hei Lei, Jie Kexin. THE RESEARCH ON THE ISOTOPE COMPOSITION FEATURES OF THE UNDERGROUND WATER IN GUHANSHAN COAL MINE FIELD[J]. COAL GEOLOGY & EXPLORATION, 1992, 20(6): 47-50.

古汉山井田地下水同位素组成特征研究

THE RESEARCH ON THE ISOTOPE COMPOSITION FEATURES OF THE UNDERGROUND WATER IN GUHANSHAN COAL MINE FIELD

  • 摘要: 根据古汉山井田地下水中3H、D、18O和13C等资料,建立了该井田鉴别主要含水层地下水的同位素标志,并对冲积层水、奥陶纪石灰岩水和煤系薄层石灰岩水之间的关系,以及矿井充水条件,做出了判断,为今后矿井基建、采矿中判别突水来源,提供了依据。

     

    Abstract: By means of the study of T、D、18O and 13 C in the underground water in Guhanshan coal mine field, the criterions to indentify the recharge source of the underground water of the main aquifers in this field are set up in this paper, which will be coefficiently used for ascertaining where the mine water comesfrom, alluvial aquifer, Ordovician Karst aquifer, and the thin limestone aquifel, in coalbearing strata, and will provide with the basis for identifying the recharge source of inrushing water during coal mine construction and exploitation.

     

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