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.
我国西南喀斯特岩溶区石漠化与当地长期以来的贫困问题没有得到恰当解决有着直接关系。
The rocky desertification in the karst areas of southwest China is a serious environmental problem at present.
两座公园特有的被称为喀斯特——即岩溶——地貌的景致，由相同的化学作用形成。
Similar chemical processes form the distinct landscapes, known as karst topography, of the two parks.
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