Analysis of deformation and fracture characteristics of wall rock interface of underground storage caverns in salt rock formation
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Analysis of deformation and fracture characteristics of wall rock interface of underground storage caverns in salt rock formation
Vol. 34, Issue 6, (2013)
作者机构:
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
作者简介:
基金信息:
DOI:
CLC:TU452
Online First:14 June 2013,
Published:2013
稿件说明:
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LIU Wei、 LI Yin-ping、 HUO Yong-sheng、 SHI Xi-lin、 XU Bao-cai、 YANG Chun-he、 LIN Yong-jie、. Analysis of deformation and fracture characteristics of wall rock interface of underground storage caverns in salt rock formation[J]. 2013, 34(6).
DOI:
LIU Wei、 LI Yin-ping、 HUO Yong-sheng、 SHI Xi-lin、 XU Bao-cai、 YANG Chun-he、 LIN Yong-jie、. Analysis of deformation and fracture characteristics of wall rock interface of underground storage caverns in salt rock formation[J]. 2013, 34(6).DOI:
Analysis of deformation and fracture characteristics of wall rock interface of underground storage caverns in salt rock formation
For the significant influence of the interface between salt rock and interlayer on the stability and tightness of gas (oil) storage caverns in bedded salt rock
related research of meso and macro-aspects on the fracture properties of the interface has been launched. On meso-aspects
scanning electron microscope(SEM) has been carried out; and the results reveal that the grains embedded with each other very tightly so the cementation near the interface is good; it supplies advantageous guarantee for the tightness of the caverns. On macro-aspect
based on the mechanical theory of composite laminated rocks
the expressions of stresses near the interface of bedded salt rock have been established; and the characteristics of deformation and fracture of interlayer have also been analyzed. The research above indicates that the stress state of the interface is very complex. The anchoring effect of hard interlayer exerting to salt rock has been indicated; and the research also reveals that the stress concentration tends to occur near the interface between hard interlayer and salt rock. Combining the aspects of meso and macro together
the research shows that the mechanism of fracture initiation and propagation
and the formation of percolation paths
are induced by both the meso-structure properties and the macro stress state of the interface. The analysis provides some references for further study of the stability and tightness of storage caverns in bedded rock salt.