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

Huynh Ngoc Sang

doi:10.32508/stdj.v8i1.2957

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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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Huynh Ngoc Sang

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

Issue: Vol 8 No 1 (2005)

Page No.: 54-61

Published: Jan 31, 2005

Section: Article

DOI: https://doi.org/10.32508/stdj.v8i1.2957

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. (2005). LAND SUBSIDENCE BY SOAKING IN PLEISTOCENE SEDIMENT OF THU DUC FORMATION, LINH TRUNG AREA, THU DUC - HCMC. Science and Technology Development Journal, 8(1), 54-61. https://doi.org/https://doi.org/10.32508/stdj.v8i1.2957