核桃峪井田华池-洛河组水文地质条件评价
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Evaluation on hydro-geological condition of Huachi-Luohe in the Hetaoyu mine field
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    摘要:

    通过分析核桃峪井田所在区域内煤层上覆华池、洛河组巨厚层状砂岩孔隙裂隙承压水的补给、径流、排泄条件以及水文地质边界,研究了华池、洛河组承压含水层的水文地质特征,计算了因煤炭开采引起的冒落带及导水裂隙带的发育高度。结果表明该承压含水层厚度大、胶结性较差、承压性强、水文地质结构特殊,在一些节理裂隙发育的局部地段,富水性强,成为主要的导水通道,对井筒的开凿和煤炭开采影响较大,是构成矿井充水的主要含水岩组。

    Abstract:

    The hydro-geological border recharge,runoff and excretion of the confined water in Hua-chi-Luohe formation in the Hetaoyu mine field were analyzed the hydro-geological characteristics of this confined water were studied,and the height of water flowing fractured zone and caving zone caused by coal exploitation were calculated. The results show that the confined aquifer group is with large thickness low cementation,huge hydraulic pressure and special hydro-geological characteris-tics; in some regions where the joints and cracks develop have large amount of water and become the main underground watercourse,which plays an important effect on the well digging and coal resources exploitation becoming the main source of mine water-filled for well construction and coal exploita-tron.

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牛永强,李世峰.核桃峪井田华池-洛河组水文地质条件评价[J].河北工程大学自然版,2012,29(1):62-65

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  • 收稿日期:2011-10-20
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  • 在线发布日期: 2015-01-12
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