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      익산 미륵사지석탑 화강암의 풍화에 의한 물리화학적 특성변화 = Physicochemical Variation by Weathering Degree of Granite from the Mireuksaji Temple Stone Pagoda, Iksan, Korea

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      다국어 초록 (Multilingual Abstract) kakao i 다국어 번역

      A physical characteristics and chemical compositions change by weathering on the granite were examined for the conservation treatment of the Mireuksaji temple stone pagoda. The natural weathered granite was collected from the Mt. Mireuk, and divided into the classification standards based on weathering degrees and strength measured by rock-test hammer. The results from comparison of the strength measured by undestructive rock-test hammer and the strength values converted from ultrasonic velocity showed that each strength measurement value was proportionate. The water absorption of the sample was 1.68 to 0.20%. The F-type of fresh rock was not naturally saturated and the WW-type was naturally saturated but took quite a long time. The water absorption was increased gradually in order of SW-type, the MW-type and the HW-type according to weathering condition. The CW-type samples showed the highest water absorption among the weathered classification samples. Through dyeing test, it was found out that only the feldspar was dyed out of the F-type and the WW-type. The SW-type and the MW-type were distinguished by the fact that plagioclase being dyed. And dyed area was expanded to quartz crack in HW-type and CW-type. Physical change by weathering of the rock-forming minerals could be classified with 3 grades. Through the XRD analysis, albite among the rock-forming mineral showed remarkable decrease. SEM-EDX analysis of the component change in the rock-forming minerals such as biotite, plagioclase, and orthoclase, showed that in case of highly-weathered grade samples compared with fresh samples, contents of the $Al_2O_3$, $K_2O$, $Na_2O$ increase and CaO, MgO decrease in the biotite, the CaO, $K_2O$ increase and $Na_2O$ decrease in the plagioclase, the $Al_2O_3$ a little increase and $K_2O$, $Na_2O$ decrease in the orthoclase. The results of extracted cation analysis using the powder samples of each weathering grade, the CaO, $Na_2O$, $K_2O$ and MgO are highly chemical variations in rock forming minerals and positive variation show high in the weathering grade of the WW-type and CW-type. This research will be used as an importance data to establish a plan for conservation treatment of composed stone in the Mireuksaji temple stone pagoda.
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      A physical characteristics and chemical compositions change by weathering on the granite were examined for the conservation treatment of the Mireuksaji temple stone pagoda. The natural weathered granite was collected from the Mt. Mireuk, and divided i...

      A physical characteristics and chemical compositions change by weathering on the granite were examined for the conservation treatment of the Mireuksaji temple stone pagoda. The natural weathered granite was collected from the Mt. Mireuk, and divided into the classification standards based on weathering degrees and strength measured by rock-test hammer. The results from comparison of the strength measured by undestructive rock-test hammer and the strength values converted from ultrasonic velocity showed that each strength measurement value was proportionate. The water absorption of the sample was 1.68 to 0.20%. The F-type of fresh rock was not naturally saturated and the WW-type was naturally saturated but took quite a long time. The water absorption was increased gradually in order of SW-type, the MW-type and the HW-type according to weathering condition. The CW-type samples showed the highest water absorption among the weathered classification samples. Through dyeing test, it was found out that only the feldspar was dyed out of the F-type and the WW-type. The SW-type and the MW-type were distinguished by the fact that plagioclase being dyed. And dyed area was expanded to quartz crack in HW-type and CW-type. Physical change by weathering of the rock-forming minerals could be classified with 3 grades. Through the XRD analysis, albite among the rock-forming mineral showed remarkable decrease. SEM-EDX analysis of the component change in the rock-forming minerals such as biotite, plagioclase, and orthoclase, showed that in case of highly-weathered grade samples compared with fresh samples, contents of the $Al_2O_3$, $K_2O$, $Na_2O$ increase and CaO, MgO decrease in the biotite, the CaO, $K_2O$ increase and $Na_2O$ decrease in the plagioclase, the $Al_2O_3$ a little increase and $K_2O$, $Na_2O$ decrease in the orthoclase. The results of extracted cation analysis using the powder samples of each weathering grade, the CaO, $Na_2O$, $K_2O$ and MgO are highly chemical variations in rock forming minerals and positive variation show high in the weathering grade of the WW-type and CW-type. This research will be used as an importance data to establish a plan for conservation treatment of composed stone in the Mireuksaji temple stone pagoda.

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      참고문헌 (Reference)

      1 김영화, "화강암의 풍화현상에 수반되는 물성변화의 특성" 2 : 36-46, 1992

      2 남기상, "화강암류 및 현무암류의 풍화에 있어서 화학조성의 변화와 주요원소의 상대적 이동" 7 : 277-290, 1971

      3 강승철, "풍화화강암의 물리적, 암석학적 지구화적 특성" 22 : 339-352, 1985

      4 김영화, "풍화현상에 수반되는 화강암의 물성 변화에 관한 연구" 23 : 221-232, 1990

      5 최석원, "충남지역석조문화재의 현황과 보존대책" 충청남도 425-, 1999

      6 양희제, "익산 미륵사지석탑 구성부재의 암석학적 특징과 석재의 원산지 해석" 대한지질학회 42 (42): 293-306, 2006

      7 이찬희, "영주 가흥리 마애삼존불상의 풍화특성과 불연속면의 안정성 해석" 대한지질학회 41 (41): 401-413, 2005

      8 문화재청, "암석의 풍화상태에 따른 분류기준" 114-, 2001

      9 서만철, "암석의 파괴 확률 분석을 통한 불국사 삼층석탑 구조 안전 진단" 10 : 57-69, 2001

      10 김사덕, "석조문화재 에폭시수지 개발 시험연구" 20 : 139-155, 1990

      1 김영화, "화강암의 풍화현상에 수반되는 물성변화의 특성" 2 : 36-46, 1992

      2 남기상, "화강암류 및 현무암류의 풍화에 있어서 화학조성의 변화와 주요원소의 상대적 이동" 7 : 277-290, 1971

      3 강승철, "풍화화강암의 물리적, 암석학적 지구화적 특성" 22 : 339-352, 1985

      4 김영화, "풍화현상에 수반되는 화강암의 물성 변화에 관한 연구" 23 : 221-232, 1990

      5 최석원, "충남지역석조문화재의 현황과 보존대책" 충청남도 425-, 1999

      6 양희제, "익산 미륵사지석탑 구성부재의 암석학적 특징과 석재의 원산지 해석" 대한지질학회 42 (42): 293-306, 2006

      7 이찬희, "영주 가흥리 마애삼존불상의 풍화특성과 불연속면의 안정성 해석" 대한지질학회 41 (41): 401-413, 2005

      8 문화재청, "암석의 풍화상태에 따른 분류기준" 114-, 2001

      9 서만철, "암석의 파괴 확률 분석을 통한 불국사 삼층석탑 구조 안전 진단" 10 : 57-69, 2001

      10 김사덕, "석조문화재 에폭시수지 개발 시험연구" 20 : 139-155, 1990

      11 엄두성, "석조문화재 발수경화제 시험연구(Ⅰ)" 20 : 155-173, 2006

      12 국립문화재연구소, "미륵사지석탑 해체조사보고서Ⅲ" 2005

      13 국립문화재연구소, "미륵사지석탑 해체조사보고서Ⅱ" 2004

      14 국립문화재연구소, "미륵사지석탑 해체조사보고서Ⅰ" 2003

      15 김수진, "광물학원론" 우성출판사 430-460, 1996

      16 국립문화재연구소, "감은사지삼층석탑(서탑) 강화처리제 선정 및 신석제작용 석재연구" 143-177, 2006

      17 안효수, "面 打擊 反撥度試驗器의 適用에 관한 實驗的 硏究" 대한건축학회 20 (20): 51-58, 2004

      18 C. A. Price, "“Stone conservation”, An over view of current research" The Gettty Conservation Institute 1996

      19 W.R., Dearm, "Weathering classification in the characterization of rock, a revision" 13 : 123-127, 1976

      20 C.H. Lee, "Weathering and deterioration of rock properties of the Dabotap pagoda (World Cultural Heritage), Republic of Korea" 47 : 547-557, 2005

      21 W. Chesworth, "The major element geochemistry and the minerlogical evolution of granic rocks during weathering”. In: Origin and distribution of elements" Pergamon Press 305-313, 1971

      22 Amoroso, "Stone decay and conservation In: Materials Science Monographs Ⅱ" elsevier 1983

      23 F. John, "Lime treatments" 2 : 19-28, 2002

      24 "KS F-2518, 흡수율시험, 한국산업규격"

      25 C.H. Lee, "Deterioration assessment and conservation of a heavily degraded Korean stone Buddha from the 9th Century" 51 : 305-316, 2006

      26 J.L. Drever, "Chemical weathering of silicate rocks as a function of elevation in the southern Swiss Alps" 3209-3216, 1992

      27 S.G. Lee, "A revision of the description and classification of weathered granite and its application to granites in Korea. Quater" 22 : 31-48, 1989

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