水文地质模型 meaning in English
hydro-geologic model
Examples
- Water - bearing characteristics and hydro - geological models of karstic collapse columns in north china
北方岩溶陷落柱的充水特征及水文地质模型 - Base on studying the analyzed - approach of reservior - induced seimicity , writer bring forward the hydrogeological analyzed method for reservior - induced seimicity , and with that eatimated the reservior - induced seimicity of hydrogeological model model in dam - region . at the same time analyzed the reservior - induced seimicity danger of large - scale break in periphery of dam region
在对比研究水库诱发地震分析方法的基础上，作者提出水库诱发地震水文地质分析方法并利用该方法对坝区水文地质模型水库诱发地震作出评价，同时对坝区外围大型断裂的水库诱发地震进行了一定程度的分析。 - 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。 - By analyzing and studying the hydrogeology condition of the reservoir bank , typical zone is selected to build the realistic hydrogeology and mathematic model . the dynamic character of the groundwater seepage field of slopes in fengjie section during the present time , the initial process of storing water and operation of the reservoir , the late process of storing water and operation of the reservoir is imitated with 3d - modflow
通过分析岸坡的水文地质条件，选出典型的代表区域，建立较逼真的水文地质模型和计算模型，运用3d - modflow软件对库区岸坡内地下水渗流场在现库水条件下、水库首期蓄水及运行过程中、二期蓄水及运行过程中的动态变化特征进行了模拟研究。