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초기함수비, 비표면적, 풍건 및 동결.융해작용이 흙의 액성한계에 미치는 영향
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  • 초기함수비, 비표면적, 풍건 및 동결.융해작용이 흙의 액성한계에 미치는 영향
  • Influence of Initial Water Content, Specific Surface, Air Drying and Freezing-thawing Action on the Liquid Limit of Soils
저자명
류능환
간행물명
한국농공학회지
권/호정보
1996년|38권 5호|pp.116-124 (9 pages)
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한국농공학회
파일정보
정기간행물|
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이 논문은 한국과학기술정보연구원과 논문 연계를 통해 무료로 제공되는 원문입니다.
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기타언어초록

The purpose of The work described in this paper is to clear up the initial moisture content, specific surface, air drying and freezing-thawing process on liquid limit of clayey soils distributed widely at estuary of three main rivers in the west coast. To this end, a series of tests were conducted on clayey soils samples with natural state and treated state. From the test results, the liquid limit was decreased with decrement of initial moisture content, air drying process, and freezing-thawing cycles and increased with increment of specific surface. The specific surface which influenced on the liquid limit is over $25 m^2$m$^2$/g, and their relationships are well formulated. Air drying process is expected to improve the engineering properties of the soils such the pro-water properties were changed to anti-water proper-ties through lowering of water holding as resulted to incline from A-7-5 to A-5 on the soil classificaction plastic chart. The freezing-thawing process decreased 20% of liquid limit, especially under the first cycle of the behavious, as a result of above mentioned reasons, phase change of soil-water system brought the decrement of specific surface and affected to the liquid limit.