Study of gypsum rock triaxial compression experiment and characteristic of high temperature phase transition
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Study of gypsum rock triaxial compression experiment and characteristic of high temperature phase transition
Vol. 33, Issue 11, (2012)
作者机构:
1. 中国石油化工股份有限公司 石油勘探开发研究院 无锡石油地质研究所,江苏,无锡,214151
2. 中国石油化工集团公司油气成藏重点实验室,江苏,无锡,214126
3. 中国矿业大学 煤炭资源与安全开采国家重点实验室,北京,100083
作者简介:
基金信息:
DOI:
CLC:TU452
Online First:14 November 2012,
Published:2012
稿件说明:
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YU Ling-jie, ZHANG Wen-tao, FAN Ming, et al. Study of gypsum rock triaxial compression experiment and characteristic of high temperature phase transition[J]. 2012, 33(11).
DOI:
YU Ling-jie, ZHANG Wen-tao, FAN Ming, et al. Study of gypsum rock triaxial compression experiment and characteristic of high temperature phase transition[J]. 2012, 33(11).DOI:
Study of gypsum rock triaxial compression experiment and characteristic of high temperature phase transition
Experiments are carried out to study the influences of temperature and confining pressure on natural gypsum rock strength and deformation properties under triaxial compression using servo-controlling testing machine. The results indicate that gypsum rock has obvious plastic flow property under different confining pressures. There is no obvious shear failure surface but lateral dilation is observed. Based on Coulomb-Mohr theory
the strength criterion and shear strength parameters of gypsum rock are obtained. With the increase of temperature
the strength of gypsum decreases. At high temperature
gypsum dehydration process takes place with result of transformation from gypsum to bassanite. Scanning electron microscope (SEM) and X-ray diffraction (XRD) methods are used to study the process. With the dehydration process
the pore pressure increases and the failure property becomes brittle. With load continuing
failure surface tends to heal. Obvious plastic flow characteristic and fast self-healing property of gypsum rock are fundamental to sealing stability of natural gas caprock.