A Laboratory Test for Detecting the Infiltrating Characteristics of Unsaturated Soil in Soil Slide

흙사면 절개지 불포화토의 침투거동 특성에 관한 연구

  • Kim Man-Il (Korea Institute of Water and Environment, Korea Water Resources Corporation) ;
  • Chae Byung-Gon (Geological & Environmental Hazards Div., Korea Institute of Geoscience and Mineral Resources) ;
  • Jeong Gyo-Cheol (Dept. of Earth and Environmental Sciences, Andong National University)
  • 김만일 (한국수자원공사 수자원연구원) ;
  • 채병곤 (한국지질자원연구원 지질환경재해연구부) ;
  • 정교철 (안동대학교 지구환경과학과)
  • Published : 2005.12.01

Abstract

In order to estimated a reason of soil slope failure new measurement technology is demanded to measure a variation of volumetric water content which is a key physical parameter for understanding the slope failure in the field. In this study a laboratory soil tank test were conducted to use RDB and ADR measurement probes for measuring the variation of volumetric water content. These experiments were compared with two physical parameters as volumetric water content and pressure water head which are estimated to the compacted weathered granite soil under the artificial rainfall, 7.5mm/hour, in the whole of two stages. From the results the variation of volumetric water content and pressure water head is represented to nearly similar travel time.

흙 절개지 사면붕괴 원인은 대부분 강우에 의해 체적함수비의 증가에 따라 발생되기 때문에 체적함수비 변화를 측정할 수 있는 새로운 측정기 술이 요구된다. 본 연구에서는 체적함수비 변화를 정량적으로 측정하기 위하여 유전율 측정시스템인 FDR과 ADR 측정프로브를 사용하여 실내 토조시험을 수행하였다. 총 2단계 에 걸쳐 시간당 7.5mm/hour의 인공강우 조건하에서 압밀 화강풍화토 내 발생되는 체적 함수비와 간극수압 변화를 측정하여 비교하였다. 측정결과, 인공강우에 의한 체적 함수비와 간극수압 변화는 거의 동일한 시점에서 함께 파악되었다.

Keywords

References

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