Consolidation of soil

Consolidation of soil

Consolidation is the process in which reduction in volume takes place by expulsion of water under long-term static loads. When stress is applied to a soil that causes the soil particles to pack together more tightly. When this occurs in a soil that is saturated with water, water will be squeezed out of the soil. Various theories have been proposed in the literature to predict the consolidation of soil. This includes Terzaghi’s consolidation theory (1943) and Mikasa’s finite strain consolidation theory (1963). The civil engineering lab in Kunsan National University can predict the consolidation of soil using these two theories.

Consolidation in layered clay soil under added stress Consolidation in layered clay soil under added stress

Excess pore water pressure isochrones Excess pore water pressure isochrones

Time factor (Tv) vs degree of consolidation (U) Time factor (Tv) vs degree of consolidation (U)

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군산대학교 에서 제작한 "Consolidation of soil" 저작물은 "공공누리 " 공공저작물 자유이용 허락표시 적용 안함 조건에 따라 이용 할 수 있습니다.
  • 담당부서 : 신재생에너지연구센터
  • 담당자 : 김형주
  • 연락처 : 063-469-4760
  • 최종수정일 : 2020-02-14
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