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Paraskevopoulou, Chrysothemis; Perras, Matthew; Diederichs, Mark; Amann, Florian; Löw, Simon; Lam, Tom; Jensen, Mark
Engineering geology, 01/2017, Letnik: 216Journal Article
Underground openings can experience time-dependent deformations and stress changes. Studying time-dependent rock behaviour is commonly done with static load (creep) tests in the laboratory which typically exhibit three distinct stages of behaviour. In this study relaxation tests were conducted to examine if three stages also exist under constant strain boundary conditions and to understand how the relaxation behaviour changes as the driving stress to strength ratio is increased. Tests were conducted on two types of limestone. At different load levels similar stress-time responses were measured indicating three distinct stages of stress relaxation. The first stage of stress relaxation (RI) where the stress relaxes with a decreasing rate is followed by the second stage (RII) in which the stress decrease approaches a constant rate and in the third stage (RIII) no further stress relaxation takes place. In the first stage 55% to 95% of the total stress relaxation takes place. The test results are compared with literature data to understand the influence of the stiffness on the magnitude and time to reach the maximum stress relaxation. Relaxation tests could be used to derive numerical model inputs to describe the time-dependent behaviour in a manner similar to static load tests. •We give insight into the time-dependent behaviour of rock materials and the importance of performing laboratory testing.•The paper focuses on stress relaxation of brittle rocks, the time-dependent response under constant (controlled) strain.•We show that three distinct stages during stress relaxation take place.•A data set of stress relaxation test results is presented to estimate and predict the relaxation of different rock types.
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