王冬青, 许肖锋, 闫长红, 孔雪, 赵振华, 程琦, 石强. 2018: 基于多源水文地质信息的裂隙岩体地下水来源分析. 工程地质学报, 26(s1): 587-593. DOI: 10.13544/j.cnki.jeg.2018145
    引用本文: 王冬青, 许肖锋, 闫长红, 孔雪, 赵振华, 程琦, 石强. 2018: 基于多源水文地质信息的裂隙岩体地下水来源分析. 工程地质学报, 26(s1): 587-593. DOI: 10.13544/j.cnki.jeg.2018145
    WANG Dongqing, XU Xiaofeng, YAN Changhong, KONG Xue, ZHAO Zhenhua, CHENG Qi, SHI Qiang. 2018: FRACTURED ROCK MASS GROUNDWATER SOURCE ANALYSIS BASED ON MULTI-SOURCE HYDROGEOLOGY INFORMATION. JOURNAL OF ENGINEERING GEOLOGY, 26(s1): 587-593. DOI: 10.13544/j.cnki.jeg.2018145
    Citation: WANG Dongqing, XU Xiaofeng, YAN Changhong, KONG Xue, ZHAO Zhenhua, CHENG Qi, SHI Qiang. 2018: FRACTURED ROCK MASS GROUNDWATER SOURCE ANALYSIS BASED ON MULTI-SOURCE HYDROGEOLOGY INFORMATION. JOURNAL OF ENGINEERING GEOLOGY, 26(s1): 587-593. DOI: 10.13544/j.cnki.jeg.2018145

    基于多源水文地质信息的裂隙岩体地下水来源分析

    FRACTURED ROCK MASS GROUNDWATER SOURCE ANALYSIS BASED ON MULTI-SOURCE HYDROGEOLOGY INFORMATION

    • 摘要: 地下水补给是地下水循环中重要的环节之一,查明其来源对于认识地下水循环过程具有重要意义。基岩地区地下水由于受构造影响,分布较为复杂,因此对其补给来源的研究是水文地质研究中的一个难点。通过分析基于遥感信息建立的富水带模型,结合地下水动态、主要离子浓度、地下水流速流向、水源地抽水量与水位数据的分析,本文研究了库如塔格山前的巴拉干水源地地下水补给来源问题,分析了造成水源地总出水量和水位降深异常变化的原因。结果表明,水源地地下水来自于其西北约6.5km的砂石料场方向,砂石料场取水是造成水源地总出水量和水位降深异常变化的原因,基于此提出了保护水源地安全的措施。

       

      Abstract: Groundwater recharge is an important part of groundwater circulation, and it is important to study its source for understanding the groundwater circulation process. Controlled by geological structures, the distribution of groundwater in bedrock area is complicated, and therefore the study of its source is a difficult work in hydrogeology research. By analyzing the model of water-rich zone based on remote sensing information, and according to the groundwater dynamics, major ion concentration, velocity and direction of groundwater flow, pumping and water level data of water source site, this article studies the source of groundwater recharge of Barakan Water Source Site(BWSS)in front of Kuruktag, northwest of China, and analyses the reasons for the abnormal change of the total water yield and the drawdown of the well. The results show that the groundwater of the water source site comes from the Aggregate Reclaiming Plant(ARP)about 6.5 kilometers northwest of BWSS. The ARP water pumping is the main reason of the abnormal change of the total water yield and the drawdown of the well of BWSS. Based on this conclusions, the methods to protect the water source site safety are put forward.

       

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