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

doi:10.32508/stdj.v7i1.3152

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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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Huynh Ngoc Sang

Faculty of Geology, University of Natural Sciences, VNU-HCM
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Article Details

Issue: Vol 7 No 1 (2004)

Page No.: 50-58

Published: Jan 31, 2004

Section: Article

DOI: https://doi.org/10.32508/stdj.v7i1.3152

Copyright: The Authors. This is an open access article distributed under the terms of the Creative Commons Attribution License CC-BY 4.0., which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

How to Cite

Sang, H. (2004). INVESTIGATING THE THYXOTROPY OF SOIL CONCERNING THE SUBSIDENCE OF 1,200 TONE OF IRON SHEET AT BINH CHANH (STORE HOUSE, 548 HUNG VUONG). Science and Technology Development Journal, 7(1), 50-58. https://doi.org/https://doi.org/10.32508/stdj.v7i1.3152