地下水循环方式的不同对围岩温度场产生的影响有很大差异。
Different ways of groundwater circulation exert different effects on wall_rock temperature field.
在地热资源开发利用中，对深部地下水循环模式进行研究具有实际意义。
In exploitation and utilization of geotherm resources, it is of practical significance to study cyclic pattern of deep Karst groundwater.
在山前地区，与山区常温地下水循环交替强烈，浅部地温梯度明显偏低。
In the front of the mountain area, circle alternate is intensive, the shallow geo-temperature gradient is on the low side.
大量的开矿过程对含水层中的地下水循环和化学成分都造成了可观的变化。
Extensive mining progress caused considerable changes in both groundwater circulation and groundwater chemical composition of the aquifer.
通过建立地下水流模拟模型，对傍河开采给黄河下游地下水循环、侧渗量及径流量带来的影响进行了分析。
It analyzes the influence of exploitation near the river to the phreatic cycle, lateral seepage and run-off amount of the lower Yellow river through establishing an under-flowing simulation model.
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.
大面积过度放牧扰乱了水循环、减少了地表和地下水资源的补充。
Widespread overgrazing disturbs water cycles, reducing replenishment of above and below ground water resources.
作为全球水循环的重要环节，地下水是全球环境变化的受体和信息载体。
As an important component of global water circulation, groundwater is a receptor and information carrier of global environmental changes.
本文侧重讨论岩溶水循环中产流与汇流、岩溶区流域面积确定、地表水与地下水划分、以及解决这些问题的技术方法。
In this paper, the mechanism of runoff-producing and flow confluence in karst area, the structure function of karst hydrological conceptual model, and the problem of modelling process are discussed.
由于岩溶地下水分布难以量测，岩溶水文系统多为黑箱或灰箱，采用岩溶水文模型量化其水循环过程常存在许多疑难问题。
There are some problems in modelling karst water circulation using hydrological model as lack of information of groundwater distribution in karst system (black box or grey box).
同位素研究表明，包头平原中山前倾斜平原和黄河冲积平原区地下水具有不同的水循环模式。
The isotopic evidence shows that the groundwater in the mountain apron and the Yellow River alluvial plain in Baotou plain has different groundwater circulation models.
该岩溶地下水年龄之所以偏大，主要是因为受制于其所处的地质环境的制约，水循环交替比较缓慢。
The major reason for the groundwater getting older is the water cycle becoming slower that is influenced by the geologic environment.
该岩溶地下水年龄之所以偏大，主要是因为受制于其所处的地质环境的制约，水循环交替比较缓慢。
The major reason for the groundwater getting older is the water cycle becoming slower that is influenced by the geologic environment.
应用推荐