焦阳. 成庄井田地下水补径排特征及奥灰顶部隔水层特性研究[J]. 煤矿安全, 2014, 45(10): 24-27.
    引用本文: 焦阳. 成庄井田地下水补径排特征及奥灰顶部隔水层特性研究[J]. 煤矿安全, 2014, 45(10): 24-27.
    JIAO Yang. Underground Recharge Runoff Discharge Characteristics and Aquifuge Characteristics at Ordovician Limestone Top of Chengzhuang Mine Field[J]. Safety in Coal Mines, 2014, 45(10): 24-27.
    Citation: JIAO Yang. Underground Recharge Runoff Discharge Characteristics and Aquifuge Characteristics at Ordovician Limestone Top of Chengzhuang Mine Field[J]. Safety in Coal Mines, 2014, 45(10): 24-27.

    成庄井田地下水补径排特征及奥灰顶部隔水层特性研究

    Underground Recharge Runoff Discharge Characteristics and Aquifuge Characteristics at Ordovician Limestone Top of Chengzhuang Mine Field

    • 摘要: 为了给晋煤集团成庄煤矿带压煤层的回采提供依据和安全保障,特对其地下水补、径、排特征及奥灰顶部隔水层特性进行了深入研究,主要技术手段包括野外地质调查、工程试验和室内试验等,结果表明:成庄井田处于延河泉域主径流带,地下水由东北面接受补给,向西南方向排入延河泉,另外,在无地质构造影响下,其奥灰顶部约35 m岩层渗透性能差,可作为相对隔水层,最终,结合改良后的突水系数公式,对成庄井田带压煤层进行了开采安全性评价。

       

      Abstract: In order to provide the basis and safety assurance for the mining under pressure at Chengzhuang Coal Mine, we made a study of recharge runoff discharge and relative strata impermeability in Ordovician limestone top. The main technical means include field geological investigation, engineering test and laboratory test. The results show that Chengzhuang Mine Field is located in the main runoff zones, the groundwater flow from the northeast to the southwest and drain to the Yanhe spring finally. In addition, the rock stratum at Ordovician top about 35 meters has low penetrability, which could be seen as relative water-resisting layer. At last, we made a safety evaluation about the mining under pressure at Chengzhuang Coal Mine according to the water inrush coefficient formula after improved.

       

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