보존과학회지 (Journal of Conservation Science)

  • 제35권6호
  • /
  • Pages.600-611
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  • 2019
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  • 1225-5459(pISSN)
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  • 2287-9781(eISSN)
한국문화재보존과학회 (The Korean Society Of Conservation Science For Cultural Heritage)
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국내 산출되는 황토의 특징에 따른 천연(제조)안료 특성연구

A Study on the Making Properties of Natural Pigments based on Substance Characteristics for Hwangto in Korea

  • 문성우 (국립문화재연구소 복원기술연구실) ;
  • 강영석 (국립문화재연구소 복원기술연구실) ;
  • 박주현 (국립문화재연구소 복원기술연구실) ;
  • 한민수 (한국전통문화대학교 문화유산전문대학원 문화재수리기술학과) ;
  • 정혜영 (국립문화재연구소 복원기술연구실)
  • Mun, Seong Woo (Restoration Technology Division, National Research Institute of Cultural Heritage) ;
  • Kang, Yeong Seok (Restoration Technology Division, National Research Institute of Cultural Heritage) ;
  • Park, Ju Hyun (Restoration Technology Division, National Research Institute of Cultural Heritage) ;
  • Han, Min Su (Department of Heritage Conservation and Restoration, Graduate School of Cultural Heritage, Korea National University of Cultural Heritage) ;
  • Jeong, Hye Young (Restoration Technology Division, National Research Institute of Cultural Heritage)
  • 투고 : 2019.10.07
  • 심사 : 2019.11.27
  • 발행 : 2019.12.20
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초록

국내에서 황색 내지 적갈색 토양을 일반적으로 황토라 지칭하며 산업 곳곳에서 황토가 활용되고 있다. 그 중 단청에 무기안료로서 황토가 이용되고 있음에도 불구하고 황토에 대한 토양학적 및 광물학적 특징과 연계된 안료의 특성연구는 미비하다. 이번 연구에서 황토의 토양학적 및 광물학적 특징이 안료 특성에 어떠한 영향을 미치는지 고찰하였다. 연구결과 적색계열의 황토와 황색계열의 황토는 토성, 구성광물, 흡유량, 안정성에서 차이를 보였다. 대부분 적색계열 황토는 clay가 우세한 영역에 도시되나 울릉도 황토는 loam 영역에 도시된다. 황색계열 황토는 대부분 clay loam~loam 영역에 도시되지만 해남 황토는 sandy clay loam 영역에 도시된다. 광물학적 분석결과 적색계열의 황토는 장석질, 점토질 토양으로 구분되며 황색계열의 황토는 대부분 주구성광물이 유사하지만 점토광물의 구성에 차이를 확인 할 수 있었다. 수비법으로 제조된 안료의 특성 분석결과 평균 10~20 ㎛ 이내의 평균입도를 보이며, 흡유량은 적색계열의 황토가 황색계열의 황토보다 평균 20 ml/100 g 높은 값을 가진다. 또한 황색계열의 황토는 적색계열의 황토보다 빛에 의한 변색 및 변질에 대해 보다 안정하다. 본 연구는 황토의 토양학적 및 광물학적 특징은 제조된 안료의 물성 및 안정성에 영향을 미친다는 것을 확인 할 수 있었으며 앞으로 황토를 이용한 천연 무기 안료의 사용에 대한 기초자료로 활용하고자 한다.

Yellow to reddish brown soil is generally referred to as hwangto and is used in various industries in Korea. Despite the fact that it is used as an inorganic pigment in dancheong, limited studies have been conducted on the properties of pigments associated with soil and on the mineralogical characteristics of hwangto. This study examines how the pedological and mineralogical features of hwangto affect pigment properties. Results indicate that reddish and yellowish soils have differences in terms of soil texture, mineral composition, oil absorption and stability under light. Reddish soil is mostly found in clay regions, whereas Ulleungdo hwangto is found in loam regions. Yellowish soil is mostly present in the clay loam to loam zones. whereas Haenam hwangto exists in the sandy clay loam zone. As a result of a mineralogical analysis, reddish soil is classified into the feldspar group and clay soil. The major minerals in the yellowish soils are similar however these soils differ in terms of clay mineral compositions. results of the characteristics of pigments prepared by the traditional method revealed that the average particle size is in the range of 10-20 ㎛, reddish soil has an average of 20 ml/100 g higher oil absorption than yellowish soil. In addition, reddish soil is more susceptible to discoloration and deterioration under light than yellowish soil. This study confirms that the soil and mineral characteristics of hwangto affect the physical properties and stability of produced pigments. These result can be used as basic data in future studies natural inorganic pigments using hwangto.

키워드

참고문헌

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