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INVESTIGATING THE THYXOTROPY OF SOIL CONCERNING THE SUBSIDENCE OF 1,200 TONE OF IRON SHEET AT BINH CHANH (STORE HOUSE, 548 HUNG VUONG)

Huynh Ngoc Sang 1
Volume & Issue: Vol. 7 No. 1 (2004) | Page No.: 50-58 | DOI: 10.32508/stdj.v7i1.3152
Published: 2004-01-31

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Copyright The Author(s) 2023. This article is published with open access by Vietnam National University, Ho Chi Minh city, Vietnam. This article is distributed under the terms of the Creative Commons Attribution License (CC-BY 4.0) which permits any use, distribution, and reproduction in any medium, provided the original author(s) and the source are credited. 

Abstract

Thyxotropy or soil liquefization a mecanical engineering geological propertig of soil, occurs imediately on saturated fine-grained soil when load impact force is over the rigid limit of soil. On the point of wiew of a theoretical engineering geologist, the auther observes problem of a subsidence of 1200 Tons of iron sheet which sink over 20m in Holocene sediments at Binh Chanh.

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