岩溶水（Karst Water）： 赋存或运移于岩溶化岩层中的地下水。由于岩溶水在运移过程中仍不断进行溶蚀，改造其赋存和运移空间，构成岩溶水独特的性质，因...
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The model forecasted that the maximum additional drawdown caused by exploiting of the karst water was lower than 2 meters, having little effect on the agricultural use.
经模型预测，岩溶水开发后引起孔隙水的最大附加降深小于2.0m，对当地农业用水影响较小。
参考来源 - 山东济宁北部岩溶地下水资源勘察与评价研究·2,447,543篇论文数据，部分数据来源于NoteExpress
山西省延河泉岩溶水系统是我国北方岩溶大泉之一。
Yanhe spring karst water system is one of the famous springs in North China.
在此基础上，对西部子系统岩溶水径流特征提出了新的见解。
On this basis, a new understanding of western subsystem karst water runoff features was advanced.
结果表明，本区地下水有三个来源：深部喀斯特岩溶水、浅部孔隙水和地表水。
These results show that the underground water has three sources, namely deep karst, shallow porous and surface waters.
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