Analysis of ground subsidence induced by gobs of salt caverns in Zhangshu based on improved Mogi mode
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Analysis of ground subsidence induced by gobs of salt caverns in Zhangshu based on improved Mogi mode
Vol. 35, Issue 10, (2014)
作者机构:
1. 中国科学院武汉岩土力学研究所 岩土力学与工程国家重点实验室,武汉,430071
2. 上海光华勘测设计院有限公司,上海,200050
作者简介:
基金信息:
DOI:
CLC:TU196.2
Online First:27 October 2014,
Published:2014
稿件说明:
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XU Yu-long, YANG Chun-he, LI Yin-ping, et al. Analysis of ground subsidence induced by gobs of salt caverns in Zhangshu based on improved Mogi mode[J]. 2014, 35(10).
DOI:
XU Yu-long, YANG Chun-he, LI Yin-ping, et al. Analysis of ground subsidence induced by gobs of salt caverns in Zhangshu based on improved Mogi mode[J]. 2014, 35(10).DOI:
Analysis of ground subsidence induced by gobs of salt caverns in Zhangshu based on improved Mogi mode
Ground subsidence induced by salt cavern gobs under the planned Zhangshu Modern Pharmaceutical Logistic Center determines the feasibility of the project. Mogi model is a ground movement prediction model based on the principle of semi-infinite elasticity
which has been widely used in the modeling of the deformation of volcanoes caused by pressure changes in their magma chambers. With the consideration that the main cause of salt cavern-induced subsidence is the volume shrinkage of caverns
the analytical solution of the salt cavern in steady state creep is introduced to improve the Mogi model and the improved model is used to predict the subsidence of Pharmaceutical Logistic Center. The superposition method is cited to gain the subsidence of the cavern group. The results show that: the ground subsidence and tilt induced by cavern groups are within the scope of building foundation settlement rule
and along with the increase of the distance to cavern groups
the ground tilt firstly increases
and then decreases. What else
the results by Mogi model are in accordance with the numerical simulation. The improved Mogi model provides an accurate and fast method for the ground subsidence analysis of salt cavern groups.