浅部地下水主要由现代区内降水补给形成，而深部地下水则可能由地质历史时期降水补给形成。
The shallow groundwater is mainly recharged by modern and local precipitation, and the deep groundwater might be originated from infiltration recharge of ancient precipitation.
隐伏硫化物矿体在地下水的作用下，在其覆盖层浅部含铁锰氧化物和有机质的土壤中形成盐晕。
Saline Halos are often formed in the soil containing Fe and Mn oxides and organic material by a concealed sulfide ore body under the action of the ground water.
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.
岩溶地下水赋存于地表以下浅部岩溶带、构造控制的中部岩溶带和深部古溶蚀带。
The karst groundwater stores in the shallow karst zones below the surface, the middle karst zones controlled by geological structures and the deep zones of fossil karst.
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.
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.
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