岩溶作用是水对可溶岩的破坏和改造作用。由于条件不同,岩溶作用的方式和所形成的岩溶现象千差万别。决定碳酸盐岩中岩溶发育特征的最重要的因素是含有侵蚀性CO_2,的地下水的运动与交替条件。 在已有研究中对扩散溶蚀作用及凝结溶蚀作用尚未引起足够重视,而这两种作用在岩溶化作用中是不 Karstification is the effect of water on the destruction and remodeling of soluble rocks. Due to different conditions, the way of karstification and the formation of karst phenomenon vary widely. The most important factor that determines the karst development in carbonate rocks is the movement and alternation of groundwater containing aggressive CO2. In the previous studies, attention has not been given to diffusion and dissolution and condensation and erosion, and neither of these two roles is relevant to karstification