자원환경지질 (Economic and Environmental Geology)

  • 제45권2호
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  • Pages.157-167
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  • 2012
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  • 1225-7281(pISSN)
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  • 2288-7962(eISSN)
대한자원환경지질학회 (The Korean Society of Economic and Environmental Geology)
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광주 치평동 유적 출토 철기시대 토기의 제작특성과 매장환경 연구

Production Characteristics and Post-depositional Influence of Iron Age Pottery from Chipyeongdong Site in Gwangju, Korea

  • 장성윤 (국립문화재연구소 복원기술연구실) ;
  • 문은정 (공주대학교 문화재보존과학과) ;
  • 이찬희 (공주대학교 문화재보존과학과) ;
  • 이기길 (조선대학교 사학과)
  • Jang, Sung-Yoon (Restoration Technology Division, National Research Institute of Cultural Heritage) ;
  • Moon, Eun-Jung (Department of Cultural Heritage Conservation Sciences, Kongju National University) ;
  • Lee, Chan-Hee (Department of Cultural Heritage Conservation Sciences, Kongju National University) ;
  • Lee, Gi-Gil (Department of History, Chosun University)
  • 투고 : 2012.03.26
  • 심사 : 2012.04.17
  • 발행 : 2012.04.28
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초록

이 연구에서는 광주 치평동 유적에서 출토된 토기의 태토산지와 소성온도를 광물학적 및 지구화학적 연구방법으로 해석하고 매장환경 하에서 토기의 변질을 조사하였다. 토기와 토양시료는 유사한 광물조성과 지구화학적 진화경향을 갖는 것으로 보아 재료로서의 유사성이 인정되며 토기는 유적의 인근 지역 토양을 이용하여 제작된 것으로 해석된다. 광물학적 분석결과를 근거로, 토기는 크게 $1,000{\sim}1,100^{\circ}C$에서 고온 소성된 그룹과 $700{\sim}1,000^{\circ}C$에서 저온 소성된 그룹으로 나눌 수 있다. 또한 고온 소성된 시료에서는 거정질 입자를 제거하는 수비과정을 거쳤을 것으로 보이는데 저온 소성된 시료들과는 다른 시기 또는 용도의 차이를 보이는 것으로 판단된다. 저온 소성된 토기에서 매장환경 동안 P이 토기 내 Al, Fe 등과 반응하여 비결정질의 침전물을 형성하는 것이 관찰되었으며, 이는 환경에 의한 토기의 변질 현상으로 해석된다.

This study aimed to interpret the provenance and firing temperature of pottery from Chipyeongdong site in Gwangju, Korea though mineralogical and geochemical methods and also investigated the post-depositional alteration of pottery in burial environments. It is also presumed that they were made of soils near the site because they have similar mineralogical composition and same geochemical evolution path. Based on the results of mineralogical analysis, the pottery samples are largely divided into 2 groups; $700^{\circ}C$ to $1,000^{\circ}C$ and 1,000 to $1,100^{\circ}C$. At some pottery fired at over $1,000^{\circ}C$, it is thought that the refinement of raw materials were processed to remove macrocrystalline fragments. However, it was found that phosphate in soil environments formed amorphous aggregates with Al and Fe within the pores and voids on pottery fired at the low temperature. It indicates the contamination of pottery after burial.

키워드

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피인용 문헌

  1. Petrological and Mineralogical Characteristics and Firing Temperature of Pottery in the 5-6th Century from Changnyeong, Gyeongsangnamdo vol.27, pp.2, 2014, https://doi.org/10.9727/jmsk.2014.27.2.63