• Proceedings of the Korean Fiber Society Conference
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• 1997.04a
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• pp.56-61
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• 1997

• Proceedings of the Korean Fiber Society Conference
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• 1997.04a
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• pp.72-77
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• 1997

• Proceedings of the Korean Fiber Society Conference
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• 2001.04a
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• pp.313-316
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• 2001

• Proceedings of the Korean Fiber Society Conference
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• 1994.10a
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• pp.66-67
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• 1994

• Magazine of the Korea Concrete Institute
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• v.25 no.3
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• pp.39-42
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• 2013

• Proceedings of the Korean Fiber Society Conference
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• 1996.10a
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• pp.98-104
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• 1996

• Economic and Environmental Geology
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• v.49 no.1
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• pp.1-11
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• 2016

Chrysotile is well known as a fibrous mineral in serpentinite by the previous studies in S. Korea. Previous studies in other countries showed that antigorite also occurred as asbestiform and harmful to humans. Therefore, the objective of this study was to investigate types and characteristics of fibrous serpentine minerals occurred in serpentinite in Hongseong, Chungnam and Gapyeong, Gyeonggi in S. Korea. XRD, SEM-EDS, PLM and EPMA mapping analyses were used to examine the occurrence and formation mechanism of serpentine minerals. Serpentinization partially occurred in amphibole-schist and calc-schist at two study sites, Hongseong, Chungnam and Gapyeong, Gyeonggi, respectively. Both chrysotile and antigorite occurred as a fibrous mineral at Hongseong site, but chrysotile occurred as a fibrous mineral at Gapyeong site. Based on PLM analysis with dispersion staining, the chrysotile was observed horizontally magenta and vertically blue colors. The antigorite appeared as horizontally gold to golden magenta and vertically blue magenta colors under central stop dispersion staining objective(DSO). PLM and SEM analyses showed the fibrous minerals were formed from plate form of serpentine minerals or by hydrothermal alternation of primary minerals. The EPMA mapping showed that Mg contents in chrysotile is relatively higher than that in antigorite while Si and O contents in antigorite is higher than them in chrysotile. However, more studies are necessary to know the exact variation in chemical composition of chrysotile and antigorite. These results indicate that even though asbestiform antigorite found associated with asbestos chrysotile in serpentinites, the fibrous antigorite can be distinguished from chrysotile by different dispersion staining colors.

• Proceedings of the Korean Fiber Society Conference
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• 2002.04a
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• pp.147-150
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• 2002

PVC를 염색하는 방법에는 분산염료, vat 염료, 함금속염료, 산성염료 등이 보고되고 있다. 그러나 PVC는 의류용 사로 적용되는 예가 적기 때문에 이의 염색에 대한 연구 결과도 상대적으로 드물다. 가발용 사를 만드는 공정의 경우 PVC 방사 시 안료를 배합해 유색 PVC를 얻는 방법에 대한 문헌이 약간 있을 뿐 PVC의 염색에 관한 자료는 거의 찾아보기가 힘들다. 최근 PVC 사의 용도가 다양해지고 있고, 가발용 원사로 이용되는 경우 안료를 배합한 방사법만으로는 two tone colour 등 가발용 원사로서의 다양한 요구에 부합되지 못하므로 후염색에 의해 PVC를 염색하는 방법의 필요성이 요구된다. (중략)

• Proceedings of the Korean Fiber Society Conference
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• 2001.10a
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• pp.452-455
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• 2001

고분자/실리케이트 나노복합체란 고분자 매트릭스에 층상 구조의 점토 광물을 나노 스케일의 시트상의 기본 단위로 박리(exfoliation)ㆍ분산시켜 얻어진 복합체를 말한다. 실리케이트를 구성하는 두께 1nm 정도의 판으로 박리ㆍ분산시키기 때문에 5wt% 정도의 첨가량만으로도 고분자의 획기적인 물성 개선이 가능하다는 장점을 가지고 있다[1]. (중략)

• Proceedings of the Korea Concrete Institute Conference
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• 2009.05a
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• pp.491-492
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• 2009

This paper presents evaluation results of fiber dispersion, number of fibers in a unit area, fiber orientation according to the mix-proportion of ECC and bridging stress calculated on the basis of fiber distribution characteristics.