The migration and interception of the released clay particles such as illite, kaolinite and chlorite were changed due to salinity changes.

 
  • 另外,本區滲透性發(fā)生變化主要是由伊利石、高嶺石和綠泥石這些非膨脹性粘粒在滲流柱內遷移和沉積引起的。
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