水文地质单元

旱平川断陷盆地受南北两区域大断裂控制，形成走向南东&北西向、倾向东北的条带状水文地质单元。

The Hanpingchuan fault basin is controlled by two regional major faults on both north and south , and formed a SE-NW strike , dip NE striped hydrogeological unit .

徐州市水文地质单元岩溶地下水循环系统分析

Analyses of Circulation System of Karst Water in Xuzhou Hydrogeological Unit

研究了地下水空间信息系统方法在一个较小的水文地质单元中的应用。

Groundwater Spacial Information System for a small hydrogeologic unit is established .

从整个地下水文地质单元特征来看，有其独特的发育形成条件。

From groundwater hydrological geological unit , it had a unique formation conditions of the development .

在深埋隧道中，隧道通过的地质条件复杂，揭示的水文地质单元较多。

In deeply buried tunnel , geology condition is complex . Many geological units are opened out .

水文地质单元内水化学类型形成某些机制问题的探讨&以辛安泉域潞安矿区为例

Some mechanisms for hydrochemical reaction model within hydrogeology unit : an example of Lu'an mine , Xin'an springs

结果表明：徐州市水文地质单元岩溶地下水循环系统是一个复杂的循环系统，整个系统既有畅流型，又有汇流型和散流型。

The result shows that the karst water circulation system in Xuzhou is complicated with different flowing patterns of fluent flow , converging flow , and dispersing flow .

根据水均衡原理，分析了该区水文地质单元岩溶地下水循环系统，揭示了该区岩溶地下水在不同的自然地理及地质条件下的循环规律；

According to the principle of water balance , the karst water circulation system was analyzed , the circulation law under different geographical and geological conditions was studied .

本文分析了临汾市地下水开发现状以及人类活动对地下水的影响，以水资源的可持续利用为出发点，针对不同的水文地质单元，提出了临汾市地下水的开发规划。

This article analysis the exploitation situation and the influence of the groundwater , on the basis of sustainable exploitation and utilization of the groundwater , aim directly at the different hydrology geology unit , this article raised the exploitation and utilization planning of the groundwater of Linfen city .

该文在唐山中西部地区水文地质调查基础上，分析了不同水文地质单元的地下水动态特征。

On the basis of hydrogeological investigation in the middle west of Tangshan city , the characteristics of groundwater regime for different groundwater system are analyzed .

由于平原区特有的水文地质条件，在平原区地下取水建设项目水资源论证中，单纯以完整和独立的水文地质单元来确定论证范围，往往不易做到。

It is very difficult to take a closed and independent hydro-geologic area as a range of water resources demonstration for underground water intake projects in plain areas due to the specific hydro-geologic features of plain areas .