The regularity of karst development in Jiangxi area is discussed, which indicates that it becomes less developed and the water inflow tends to decrease with the increase of the depth.
本文阐述了江西地区岩溶发育由浅到深逐渐减弱的规律，以及岩溶突水量随深度的增加而减小的趋势。
The regularity of karst development in Jiangxi area is discussed, which indicates that it becomes less developed and the water inflow tends to decrease with the increase of the depth.
本文阐述了江西地区岩溶发育由浅到深逐渐减弱的规律，以及岩溶突水量随深度的增加而减小的趋势。
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