陕北榆神府矿区浅部煤层开采导水裂隙带高度的研究及其环境生态意义

    STUDY ON THE HEIGHT OF WATER FLOWING FRACTURED ZONE FORMED BY SHALLOW COAL MINING IN YU-SHEN-FU MINE AREA OF NORTH SHAANXI PROVINCE AND ITS ENVIRONMENT-ECOLOGY SIG-NIFICANCE

    • 摘要: 在研究陕北榆神府矿区浅部煤层顶板工程地质性质和覆岩结构类型分区基础上,采用经验公式和有限元法,结合GIS空间数字化技术,预测了研究区浅部煤炭资源开采导水裂隙带发育高度及其空间变化分布.分析了采煤失水区及其环境生态效应.该研究对西北部干早半干早区煤炭资源开发有普遍指导意义.

       

      Abstract: Based on the study of the overlying strata engineering geological properties and structure types of shallow buried opal in Yu-Shen-Fu mine area of north Shaanxi province, with empirical formula and FEM, as well as GIS technology, the height of the water flowing fractured zone formed by the shallow buried coal mining in the studied area is predicted. The losing water area and environment-ecology effected by the coal mining is analyzed. This research result has a general significance to guide the coal resource exploitation in the arid-semiarid area of northwest China.

       

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