ground water system meaning in Chinese
地下水系统
Examples
- The analyzed result are : ( 1 ) the f1 fault and f15 fault ground water system ' s dangerous of reservior - induced seimicity is lower ; the f5 fault f7 fault ground water system and the intersected segment of f5 f7 and f2 fault are the dangerous part of reservior - induced seimicity
分析结果认为： ( 1 )坝区f1断层及fl5断层地下水系诱发地震危险性较小， f5 、 f7断层地下水系及其与f2交汇部位是水库诱发地震的危险部位。 - Yellow river replenish to shallow layer ground water system from side . this system is regional shallow layer ground water of hydrological cycle and this system is one of subsystem which belong to groundwater system of north china yellow river flood plain
黄河水侧渗补给浅层地下水系统，是水文循环中一个局部性的浅层地下水系统，是属华北黄河冲积平原地下水系统的一个子系统，包括黄河水系统和由它演化形成的地下水系统两个部分。 - Because there are several periods of tectonic movement and several tectonic zones " development and complex superposition at da gangshan hydropower staion , geological structure in dam area is great complex and water - bearing media has the characteristic if inhomogeneity , which make it difficult to further clarify the burial condition of different bearing aqueous structure and the development of ground water system at the dam area
由于大岗山水电站坝区存在多期次的构造运动以及多个构造带的共同发育、复合叠加，使得坝区地质构造显得错综复杂以及含水介质的不均一性，使得进一步阐明坝区不同承压储水构造埋藏条件和坝区地下水系的发育特点变得很困难。 - The embed feature of ground water is flaw - water with the special trait of rock - conformation . sorted macro - ammount element in earthe ' s surface water and underground water with categorical - analyzed method , analyzed the trait of rare earth c - o isotop in water pattern and the runoff mode number of earth ' s surface ; with the dynamic variational characteristic of ground water , the text divided ground water system and build the hydrogeological model in dam - region
大岗山电站位于大渡河断裂带、磨西断裂带和龙门山断裂带的交汇部位，新生代以来构造活动、地震活动和水热活动均较强烈。大岗山电站坝区岩体为花岗岩及辉绿岩脉，断裂和裂隙相当发育；其特殊的岩性构造特征决定坝区地下水埋藏特征为裂隙水。 - Through field investigation and analysis indoor , with studying all hydrochemistry data in detail , including macro components and micro components , the author finds out the hydrochemistry feature of ground water . for further specifying the ground water system , with cluster analysis of macro components of surface water and ground water in total 147 samples and the analysis of micro components , including ree , the main ground water systems are distinguished by and large , especially the ground water system main of fault no . 7 and fault no . 15 water bearing belts which have differences at macro and micro components between the two ground water systems , moreover , the main hydrogeochemistry effects are established such as lixiviation , oxidization , precipitation and mixing effect , especially the mixing effect which result in the complexit y of the hydrochemistry of deep bearing tectonic fracture water . based on them , the hydro geological model of upper dam base is established , meanwhile the author summarizes the hydrochemistry feature of weathering crevice water , surface tectonic crevice water and deep tectonic crevice water
为此，本文以大岗山坝区水文地球化学问题为研究对象，通过野外调查和室内分析，详细的研究了坝区水化学资料，包括宏量组分、微量组分，查明了坝区地下水水化学特征，对采集的147个地表及地下水样的宏量组分进行聚类分析，结合微量元素，稀土元素的研究，并应用二氧化硅地热温标确定了深部构造裂隙水的热源深度，基本区分了坝区各个主要地下水水系，特别是以f7 、 f15断裂含水带为主的地下水系，它们的宏量组分、微量组分以及稀土等方面均存在差异，以此为基础，结合坝区水文地质条件，建立了坝区的上坝址的水文地质模型，同时通过分析了坝区花岗岩区的水化学资料，确立了坝区主要的水文地球化学作用，分别为：溶滤作用、氧化作用、沉淀作用、以及混合作用，混合作用是导致深部承压裂隙水水化学复杂的主要原因，并总结了坝区风化裂隙水、浅部构造裂隙水、深部构造裂隙水的水化学特征。