According to the field data the conclusion is to take osmotic coefficient K=10~(-5)cm/s as the criterion of dissolution of gypsum closed in Neogene mud-stone.
英
美
- 结合现场资料,将渗透系数K=10-5cm s作为石膏在第三系红层泥岩封闭下发生溶蚀的判据。
