电磁精细探测法在隐伏型导水地质裂缝勘探中的应用

针对传统隐伏型导水地质裂缝勘探方法存在勘测精度较差的问题,提出电磁精细探测法探析隐伏型导水地质裂缝。依照屏蔽系数、实测场强和理论场强数据绘制综合曲线图,通过该图获取隐伏型导水地质裂缝所处位置几何阴影范围,采用层析成像法得到网格化的工作面,获取隐伏型导水地质图像。通过图像直接观测隐伏型导水地质工作面裂缝所处位置,在此基础上,观测四个电磁场分量,采用正交电磁场分量计算介质视电阻率,依据计算视电阻率数值和视电阻率分布状态研究裂缝发育情况和裂缝富水程度。结果表明:采用该方法能较为精准地获取隐伏型导水地质裂缝位置。通过裂缝位置进一步检测出隐伏型导水地质裂缝最大发育高度为63.5 m。当视电阻数值不断增加时,隐伏型导水地质裂缝和裂缝富水性逐渐减小,与实际情况较为相符,说明该种方法探析效果较好。     

中关村中心区水文地质及工程地质特征

本文全面、系统地分析了北京市中关村中心区的水文地质及工程地质特征 ,为该地区的工程建设提供可靠的地质资料     

台缙高速公路苍岭隧道水文地质勘察与涌水量预测

以台缙高速公路苍岭隧道为例，通过水文地质综合勘探方法，查明隧道不同裂隙发育程度岩体的渗透系数K值。然后利用地下水动力学法、地下水径流模数法对隧道开挖涌水量进行了预测。通过施工检验发现，涌水段位置和涌水量总体较接近，说明预测工作对隧道的施工开挖和排水设计具有指导意义。     

勘测关键技术及其综合应用研究

勘测关键技术及其综合应用研究，系国家“八五”科技攻关２０８－０２－０５专题。该专题研究结合锦屏一、二级等工程，专业面广，应用性强，研究工作难度大，是当前水电工程地质勘探技术中的薄弱环节，是关系到前期工作进展和工程经济效益的重大课题。其研究内容包括：岩心定向技术、砂卵石层取心技术，地应力测试与分析新技术，岩体裂隙结构面的计算机处理系统、岩溶探测新技术、高分辨率工程地震勘探技术、３０００系列测井仪的改     

坝址区垂直温度场及其水文地质意义——以湖北溇水江坪河水电站为例

江坪河水电站坝址区钻孔内分层水温随埋深增大而上升,钻孔孔底水温17.16℃~19.83℃为所处河湾地块岩溶地下水代表性水温,钻孔顶面水温15.88℃~16.30℃与河水水温15.81℃相近,反映了坝址区河水位比下伏岩溶水位高,部分河水下渗补给下伏岩溶水。通过比较得出,左岸ZK17与右岸ZK19一线,河水对岩溶地下水下渗补给比下游ZK79、ZK36地段强烈。分层测温这种简单易行的研究分析方法对具有复杂水动力场的同类型岩溶峰丛峡谷建坝有一定参考意义。     

基于Aquifer Test的水文地质参数计算方法研究

根据抽水试验结果,常用人工求参的方法确定水文地质参数。人工求参方法计算结果较为可靠,但计算过程繁琐,并且结果因人而异,具有人为随意性。利用AquiferTest软件求参,计算方便快捷,与人工求参方法对比,具有计算精度较高,规范性好等优点。     

近松散层疏放开采的水文地质条件改造研究

阐述了水地质条件改造意义，结合太平煤矿近松散层疏放开采的实际水、地质条件，试验研究了矿井水地质条件，提出了地面供水井封堵和井下疏放结合的综合开采方案，阶段性地实现了第四系上组水的开采保护和井下安全生产，对进一步疏放开采亦具有重要的指导意义．     

Forecasting of Hydrographs to Simulate Long Term Recharge From Rivers in Numerical Models of Mining Reservoirs; Application to A Coal Mine in NW Spain

Although the natural permeability of rocks in the Asturian Central Coal Basin (NW Spain) is generally low, intensive mining activities over many decades has given rise to fracture flow paths that are far more permeable than those associated with the natural lithology. Abandoned and flooded mining works set up artificial ‘pseudo‐karst’ aquifers, which can act as underground reservoirs, with many potential applications. In particular, a mining reservoir shaped by two connected mining shafts within the River Turón basin has been studied. A runoff model was used to produce accurate simulations of streamflow in three different gauging stations during a monitored period of 2 years. The purpose was to use this model in the forecast situation, in order to predict long‐term situations in a hydrogeological FEFLOW model. It was necessary to develop depletion curves for each gauging station based on the available daily effective rainfall and measured flow data, as well as the knowledge of the basin characteristics. The resulting simulated hydrographs were very similar to the measured hydrographs during the monitored period, so the adequate adjusting allows input of the flow for forecast purposes. The model produced forecast hydrographs that had a r = 0.8 and difference in annual volume ranging from 1.6% to 5%. The defined model was applied to a rainfall data set of 30 years, and the average recharge from the river to the mining reservoir could be adequately estimated. The method developed needs to be refined and tested on additional years, but the approach appears to be applicable to operational runoff forecasting for numerical models input data. Copyright © 2015 John Wiley & Sons, Ltd.     

矿井水文地质工程钻探现状与发展方向

就水文地质钻探工作的必要性进行了说明,并对煤矿水文地质钻探现状进行了分析和总结,以此为基础对提升水文地质钻探工作质量的方法提出了几点见解,最后简述了水文地质钻探新技术和未来发展趋势。     

某客运专线花岗岩隧道水文地质条件分析及涌水量预测

采用综合勘探方法对某花岗岩隧道水文地质条件进行了分析,通过压水试验,获得隧道各段围岩体的渗透系数,利用地下水动力学方法及经验公式法对该隧道的涌水量进行了预测。经开挖验证实测涌水量与预测涌水量基本一致。