1) underground karst
地下岩溶
2) karst groundwater
岩溶地下水
1.
Characteristics of karst groundwater system at Baiquan of Xingtai City and its reasonable development and utilization;
邢台百泉岩溶地下水系统特征分析与开发利用研究
2.
Duality method for assessing karst groundwater vulnerability and its application in Jinfo mountain of Chongqing;
岩溶地下水脆弱性评价“二元法”及其在重庆金佛山的应用
3.
Hydrochemical study of karst groundwater in the Jinan spring catchment;
济南泉域排泄区岩溶地下水水化学特征
3) karst ground water
岩溶地下水
1.
On the basis of discussion into the hydrogeological Features of Karst ground water system in Longzici spring, preliminary probe into the prospects of exploitation and application of the karst ground water.
在讨论龙子祠泉岩溶水系统岩溶地下水水文地质特征的基础上，岩溶地下水对开发利用前景进行了初步探讨。
2.
Karst ground water is widely dispersed in China.
岩溶地下水资源的准确评价是一个重要而又难以解决的问题 。
3.
The paper researches intensively the effect to water environmentbeing produced by mass exploiting the karst ground water in largepower plant taking HANFENG power plant for example.
本文以邯峰火电厂为例研究了大型火电厂集中开采岩溶地下水所造成的水环境影响。
4) karst water
岩溶地下水
1.
the constantly increasing mining of karst water, decreasing of precipitation, and coal mining induced water discharge.
从自然因素和人为因素两方面分析了郭庄泉流量衰减的主要原因是岩溶地下水开采量不断增大 ,降雨量减小 ,以及由于开采下组煤 ,大量抽排岩溶地下水。
2.
In this paper the character istics of karst water flow are expounded and the features of karst water movement in South China and in North China are discussed respectively.
阐述岩溶地下水运动特点，分别讨论南方岩溶地下水与北方岩溶地下水运动特征，在此基础上建立了概念性模型。
3.
This paper focuses on karst water resource and its recharge and discharge properties in Xuzhou.
研究了徐州市岩溶地下水资源及补排关系 。
5) underground karat water
地下岩溶水
6) karstic groundwater
岩溶地下水
1.
This paper introduces the general situation of Yanhe Spring Area,studies the data of the karstic groundwater level in Yanhe Spring Area,and analyzes the dynamic characteristics and influencing factors of karstic groundwater.
介绍了延河泉泉域概况,研究了泉域岩溶地下水水位资料,分析了岩溶地下水动态特征及其影响因素。
2.
After the impounding of the reservoir,the karstic hydrogeological condition in the mining area has changed obviously: the first is general rising of karstic groundwater table,upswing range is declinin.
万家寨水库蓄水后,准格尔矿区岩溶地下水文地质条件发生了明显改变:一是岩溶地下水位的普遍升高,由黄河岸边至矿区西部升幅逐渐变小;二是岩溶地下水位与黄河水位间具有较大的高差,且近岸入渗区水力坡降变陡;三是岩溶地下水位与库水位具有同步大变幅,且同步升降;四是矿区岩溶地下水接受黄河地表水的侧向渗漏补给比例增大,侧向渗漏补给增量在1。
补充资料：岩溶地貌
即“喀斯特地貌”(461页)。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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