Petro-mineralogical and Solubility Characterization in Soluble Rocks

용해성 암석의 용식 진전에 대한 암석-광물학적 특성 연구

  • 정의진 (서울대학교 지구환경과학부) ;
  • 윤운상 (주식회사 넥스지오) ;
  • 여상진 (서울대학교 지구환경과학부) ;
  • 김정환 (서울대학교 지구환경과학부) ;
  • 이근병 ((주) 유신코어퍼레이션 지반공학부) ;
  • 노영욱 ((주) 유신코어퍼레이션 지반공학부)
  • Published : 2002.03.01

Abstract

Chemical weathering processes related with mineralogical characters and ground water condition are very essential engineering problems in soluble rock masses. Detailed geological mapping were performed and 8 samples were collected from the 2 formations including various rock faces to deduce the possibility of the limestone cavity formation and their mechanism. Petrological descriptions and various petro-mineralogical experiments such as XRD analysis, clay mineral analysis, absorptivity test, impurity analysis were conducted to evaluate the cavity making processes. Laboratory solubility test for rock specimen were also carried out under the strong acid (pH=1) condition. From the experimental data and geological mapping data, it is found that the formation of limestone cavities in limestones are strongly related with geological structures such as beddings, cleavages and the contents of impurities rather than CaCO$_3$contents. In case of dolomites, rock textures, grain size, amounts and types of clay minerals as well as geological structures are major controlling factors of cavity forming processes

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