• Title/Summary/Keyword: Marine deposited soil

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Engineering Characteristics of Soil-Lime or Cement Mixtures on the Curing Conditions (양생조건에 따른 생석회 혼합토의 공학적 특성)

  • 민덕기;황광모;이완진;최영철
    • Proceedings of the Korean Geotechical Society Conference
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    • 2002.03a
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    • pp.305-312
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    • 2002
  • To estimate the effects of lime and cement on the surplus soil, the engineering properties of the marine deposited clay and the fresh water clay were analyzed. The specimen were prepared under several curing conditions, namely, underwater curing, wet condition curing and underwater curing after heating. Unconfined compression strength were estimated after 7, 14, 28 and 60 days, respectively. The strength were steeply increased with time until first 14 days. Specially the increase of the strength of the heated soil were large.

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Chemical and Mineralogical Properties on the Ulsan Marine Deposited Clay (울산 퇴적 점토의 화학적, 광물학적 특성)

  • 민덕기;황광모;강문기
    • Journal of the Korean Geotechnical Society
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    • v.16 no.6
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    • pp.51-58
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    • 2000
  • 울산지역에 널리 분포하고 있는 해성 퇴적토에 대하여 깊이별로 물리, 화학 그리고 광물학적 특성을 파악하였으며, 이 지역에서 채취된 시료에 대하여 깊이별로 퓨준압말시험을 실시하였다. 본 논문을 위하여 울산 해성 퇴적토의 생성과정을 추정하고, X-선 회절 분석, X-선 형광분석 및 에너지분산분광분석을 실시하여 깊이에 따른 변화를 비교하였다. 울산 해성 퇴적토의 점토광물에 대한 정량분석결과, 일라이트, 카올리나이트, 녹니석, 스멕타이트 순으로 많게 나타났음, 화학성분 분석결과, SiO$_2$, $Al_2$O$_3$그리고 Fe$_2$O$_3$가 대부분을 차지하는 것으로 나타났다. 주사전자현미경 관찰결과, 유공충과 규조류가 관찰되었다. 표준압밀시험 결과, 울산지역의 해성 퇴적 점토는 깊이에 따른 변형거동이 화학적, 광물학적 분석결과와 마찬가지로 깊이에 따른 변화를 보이지 않아 같은 시디에 퇴적인 것으로 판단된다.

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Geoarchaeology of the Piseo-ri Paleolithic site, Muan (무안 피서리구석기유적의 지질.고고학적 특성)

  • Lee, Heon-Jong;Chung, Chull-Hwan;Park, Sung-Tan
    • The Korean Journal of Quaternary Research
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    • v.24 no.2
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    • pp.13-21
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    • 2010
  • The Piseo-ri site in Muan provides significant data in investigation on the Paleolithic sites in the southwest coast of Korea. Stratigraphic and geological analysis indicates that the characteristic of soil wedge can vary in accordance with soil property and relief of paleo-surface. Considering that the cultural layer was deposited after the Last Glacial Maximum, co-occurrence of the late Middle to early Upper Paleolithic stone tools suggests a possibility of redeposition of different ages resulted from active erosion. The result shows that the distribution of the Paleolithic tools and the property of soil wedge could be controlled by environmental conditions such as relief of paleo-surface and climate.

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