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.
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.
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