典型中深埋煤层覆岩结构特征与风化基岩富水性研究

Structural characteristics of the overburden and water yield property of weathered bedrock aquifer in a representative medium-deep coal seam

  • 摘要:
    背景 风化基岩含水层是陕北侏罗纪煤田煤炭开采的主要充水含水层,风化基岩含水层富水性评价是顶板水害防治的关键。
    方法 以陕西曹家滩煤矿12盘区为研究区,分析2−2煤层上覆地层结构与覆岩岩性结构类型,确定风化基岩层为煤层上覆主要充水含水层。选取砂地比、砂岩厚度、风化影响指数、风化基岩埋深、单位涌水量、渗透系数、RQD及视电阻率作为评价风化基岩含水层富水性指标,将层次分析法(AHP)、变异系数法(CV)、灰色关联分析法(GRA)进行耦合,构建含水层富水性综合评价模型(AHP-CV-GRA),计算各个富水性指标的权重,对各个指标进行叠加分析,得到风化基岩含水层富水性分区预测结果。
    结果和结论 2−2煤层富水性分为相对强、中等和相对弱3类富水区,并结合瞬变电磁富水异常区探测结果进行验证,富水性分区结果中相对强富水性区域大部分对应风化基岩底界低阻异常区域;为了更加准确地验证AHP-CV-GRA组合方法评价的富水性结果,根据122104工作面井下疏放水量结果对该富水性分区结果进行验证,井下疏放水量大的区域富水性相对较强,发现该富水性分区评价结果与实际情况吻合较好,AHP-CV-GRA方法能够相对科学地评价含水层的富水性。

     

    Abstract:
    Background  The weathered bedrock aquifer represents a major water-filled aquifer encountered during coal mining in the Jurassic coalfield in northern Shaanxi Province. Therefore, evaluating the water yield property of the weathered bedrock aquifer is the key to the prevention and control of water hazards in coal seam roofs.
    Methods  This study investigated panel 12 of the Caojiatan Coal Mine, Shaanxi Province. Analysis of the stratigraphic and lithological structure types of the overburden of coal seam 2−2 identified the weathered bedrock as the primary overlying water-bearing aquifer of the coal seam. Using net-to-gross (NTG) ratio, sandstone thickness, weathering influence index, burial depth of weathered bedrock, specific yield, permeability coefficient, rock quality designation (RQD), and apparent resistivity as evaluation indicators and based on the coupling of analytic hierarchy process (AHP), coefficient of variation (CV), and grey relational analysis (GRA), this study constructed a comprehensive AHP-CV-GRA evaluation model for the water yield property of the weathered bedrock aquifer. By calculating the weights and performing spatial overlay analysis for these indicators, this study predicted the zoning of the water yield property of the weathered bedrock aquifer.
    Results and Conclusions  The water yield property of coal seam 2−2 can be categorized into three types: strong, moderate, and weak. The detection results of the anomaly areas of water yield property obtained using the transient electromagnetic method demonstrated that most of zones with strong water yield property in the study area corresponded to the low-resistance anomaly areas near the bottom boundary of the weathered bedrock. To further validate the evaluation results obtained using the AHP-CV-GRA model more accurately, the underground drainage volumes of mining face 122104 were adopted for validation. The results indicated that zones with large drainage volume featured strong water yield property, revealing a good agreement between the evaluation results and the actual conditions. Therefore, the proposed AHP-CV-GRA method enables the scientifically robust elevation of the water yield property of aquifers.

     

/

返回文章
返回