4.6 Article

Creep crack energy dissipation and instability prediction in micritic bioclastic limestone

Journal

FRONTIERS IN EARTH SCIENCE
Volume 11, Issue -, Pages -

Publisher

FRONTIERS MEDIA SA
DOI: 10.3389/feart.2023.1138302

Keywords

micritic bioclastic limestone; crack strain; energy dissipation; rock instability prediction; creep-sensitive stress

Ask authors/readers for more resources

The time-dependent deformation and long-term stability of rocks are important considerations in water conservancy and geotechnical engineering. Current theoretical criteria for predicting stability and damage considering time-dependent deformation are lacking. In this study, multi-level creep experiments were conducted on micritic bioclastic limestone obtained from a continuously deforming tunnel in Xinjiang, China. The evolution characteristics of axial crack strain and crack dissipation energy density were investigated, and an instability index based on creep crack dissipation energy density was proposed. The study also established an evolutionary model for the instability index and defined a stress threshold for creep sensitivity. The time-dependent instability index surface was divided into different zones, providing a criterion for evaluating and predicting rock instability and lifespan under specific stress conditions.
Time-dependent deformation and long-term stability of rocks are important issues in water conservancy and geotechnical engineering. Currently, there are no well-accepted theoretical criteria with which to predict stability and damage considering time-dependent deformation. In-depth research is still needed. Multilevel creep experiments were performed on micritic bioclastic limestone obtained from a continuously deforming tunnel in Xinjiang, China. Based on crack strain theory, the axial crack strain evolution characteristics during loading and creep processes were investigated. The evolutionary characteristics of the crack dissipation energy density, which was obtained via integration of the crack strain during loading and creep, were revealed. The energy dissipation leading to rock fracture in each multilevel creep experiment was identified and used to calculate the total energy dissipated at the point at which the rock loses strength. A rock instability index based on the creep crack dissipation energy density was proposed. An instability index evolution model was proposed, expressed as a surface for the change in instability index with the bearing state (R-d ) and time. Based on the instability index surface, the stress threshold creep-sensitive stress sigma(cs ) was defined. The time-dependent instability index surface was divided into a long-term stability zone (Z(1)), an initial time-dependent instability zone (Z(2)), a time-dependent instability stable evolution zone (Z(3)) and a time-dependent instability sensitive zone (Z(4)) by the crack initial stress, crack damage stress, and creep sensitive stress. The instability index model was established as an energy instability evolution criterion to evaluate and predict the rock instability and lifespan under specific stress states.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.6
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available