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VNUHCM Journal of

Science and Technology Development

An official journal of Viet Nam National University Ho Chi Minh City, Viet Nam since 1997

ISSN: 1859-0128
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LAND SUBSIDENCE BY SOAKING IN PLEISTOCENE SEDIMENT OF THU DUC FORMATION, LINH TRUNG AREA, THU DUC - HCMC

Huynh Ngoc Sang 1

Volume & Issue: Vol. 8 No. 1 (2005) | Page No.: 54-61 | DOI: 10.32508/stdj.v8i1.2957
Published: 2005-01-31

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Copyright © 2005 by the author(s).

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

The cause of land subsidence in Linh Trung, Thu Duc, HoChi Minh City is soaking compaction - Lan subsidence without changing load pressure, occurs when interconnected pores of lvose materials decrease their space by soaking. This paper presents some soaking properties of Pleistocene sediment, Linh Trung ont crop, Thu Duc District, Hochiminh City.

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