Abstract

This research reports the laboratory relaxation tests investigating the time-dependent behavior of intact and failed sandstone specimens under unconfined condition. The results indicate that the stress relaxation curves show smooth relaxation behavior in the pre-failure region and show staircase type relaxation behavior in the post-failure region. The failed specimens experienced sudden and large stress drops after a stage of smooth relaxation and as a result, more stress is relaxed from the failed specimens than the intact ones. In addition, the radial-strain-time curve during a relaxation test shows similar trend as creep. No third stage was observed for the relaxation test in the pre-failure region while in the post-failure region, the radial strain accelerates to failure in a short time after a few cycles of jump and stabilization. The sudden changes in the radial strain are likely induced by the failure propagation or shear-off of asperities along the major shear failure plane. The radial strain is much larger than the inelastic axial strain, especially in the post-failure region, demonstrating that the time-dependent deformation concentrates in radial direction once the specimen fails. Furthermore, any change in the radial strain curve coincides with the change in the stress curve during a relaxation test, and the regression analyses show that they are linearly correlated. The sensitivity of stress to radial strain depends on the failure condition of the specimens.

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.