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贵州小河口煤矿水文地质特征分析

nalysis of Hydrogeological Characteristics in Xiaohekou Coalmine, Guizhou Province

中文摘要英文摘要

基于小河口煤矿地质勘探资料,结合区域水文地质特征,探讨了该井田的水文地质特征。结果表明:小河口煤矿水文地质条件中等偏简单,主要含水层为新生界松散岩类孔隙水和中生界碎屑岩基岩裂隙水两大类,地下水补给主要来源于大气降水,由南西向北东方向径流,最终汇入乌江;井田的充水水源为地表水、地下水、老煤窑积水等,充水通道为断裂节理裂隙、开采冒落带裂隙和老窑采空区。

Based on geological exploration data of Xiaohekou coalmine, combined with the regional hydrogeological characteristics, this paper explored the hydrogeological characteristics of the Minefield. The Result Indicates: Xiaohekou coalmine hydrogeological condition is medium close to simple, and the main aquifers are Mesozoic and Cenozoic Ida loose rock pore water and Mesozoic clastic bedrock fissure water. Groundwater recharge and spring mainly from atmospheric precipitation, runoff from the southwest to the northeast, eventually import the Wujiang River. The water-filled sources of the Minefield are surface water, groundwater, water of old coal mines and so on, and water-filled channel have broken joints cracks, mining caving zones and goaf fissures.

李明、姜波、虞青松、杨帆

矿山地质、矿山测量

含水层水文地质充水因素充水通道小河口煤矿

aquiferhydrogeologywater filling factorwater-filled channelXiaohekou coalmine

李明,姜波,虞青松,杨帆.贵州小河口煤矿水文地质特征分析[EB/OL].(2013-04-01)[2025-08-16].http://www.paper.edu.cn/releasepaper/content/201304-28.点此复制

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