吕东亮,李松营,张春光,杨培,张万鹏

• 1:义马煤业集团股份有限公司石壕煤矿
• 2:义马煤业集团股份有限公司地质研究所
• 3:河南理工大学资源环境学院

摘要(Abstract)：

为了准确把握新安煤田矿井充水条件的时空差异,制定有针对性、时效性的防治水措施,收集500余个井上下钻孔以及水库动态资料,分析了新安水文地质单元的补给、径流和排泄条件,研究了区域水文地质条件时空差异。研究表明:区域水文地质条件在小浪底水库蓄水前后以及前期后期与开采前后存在明显的时间性差异;煤田东部与西部、浅部与深部、不同含水层之间以及同一含水层的不同区段也存在明显的空间性差异;寒武系及奥陶系灰岩含水层是区域主要含水层,在平面上,可以划分为补给区、顺层径流区、折向汇流区、缓流滞流区和排泄区,强径流条带集中在折向汇流区。新安煤田区域水文地质条件的时空差异决定了区域内矿井充水条件的复杂性与差异性。

关键词(KeyWords)： 水文地质条件;时空差异;水文地质分区;大型地表水体

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金重点资助项目(41130419)

作者(Author): 吕东亮,李松营,张春光,杨培,张万鹏

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