Micromechanics of rock damage and its recovery in cyclic loading conditions

TL;DR

This study investigates rock damage and recovery under cyclic loading, revealing that slip dominates hysteresis, tensile cracks influence elastic properties, and friction controls crack closure and rheology in brittle rocks.

Contribution

It provides new insights into the micromechanical processes of rock damage and recovery, emphasizing the role of slip, tensile cracks, and friction in cyclic loading conditions.

Findings

Hysteresis in stress-strain is explained by slip.

Elastic wave velocity changes are linked to tensile cracks.

Friction controls crack closure and elastic property recovery.

Abstract

Under compressive stress, rock ``damage'' in the form of tensile microcracks is coupled to internal slip on microscopic interfaces, such as preexisting cracks and grain boundaries. In order to characterise the contribution of slip to the overall damage process, we conduct triaxial cyclic loading experiments on Westerly granite, and monitor volumetric strain and elastic wave velocity and anisotropy. Cyclic loading tests show large hysteresis in axial stress-strain behaviour that can be explained entirely by slip. Elastic wave velocity variations are observed only past a yield point, and show hysteresis with incomplete reversibility upon unloading. Irrecoverable volumetric strain and elastic wave velocity drop and anisotropy increase with increasing maximum stress, are amplified during hydrostatic decompression, and decrease logarithmically with time during hydrostatic hold periods after deformation cycles. The mechanical data and change in elastic properties are used to determine the proportion of mechanical work required to generate tensile cracks, which increases as the rock approaches failure but remains small, up to around 10\% of the net dissipated work per cycle. The pre-rupture deformation behaviour of rocks is qualitatively compatible with the mechanics of wing cracks. While tensile cracks are the source of large changes in rock physical properties, they are not systematically associated with significant energy dissipation and their aperture and growth is primarily controlled by friction, which exerts a dominant control on rock rheology in the brittle regime. Time-dependent friction along preexisting shear interfaces explains how tensile cracks can close under static conditions and produce recovery of elastic wave velocities over time.