TY - JOUR
T1 - Triaxial Deformation Rate Analysis (DRA)
AU - Wang, Hongyu
AU - Dyskin, Arcady
AU - Pasternak, Elena
AU - Dight, Phil
N1 - Funding Information:
This study was funded by MRIWA project (M0464) and National Natural Science Foundation of China (U1965204 and 52061160367).
Funding Information:
The authors acknowledge support from the Australian Centre for Geomechanics and the following sponsors of the MRIWA project M0464: Aeris Resources Limited, Tritton Gold Mine, Australia; Agnico Eagle Mines Limited, LaRonde Mine, Canada; AngloGold Ashanti Australia Ltd, Australia; Ernest Henry Mining, Australia; Glencore Sudbury Integrated Nickel Operations, Canada; Gold Fields Australia Pty Ltd, Granny Smith Mine, Australia; Gold Fields Australia Pty Ltd, St Ives and Agnew Mines, Australia; Luossavaara-Kiirunavaara AB (LKAB), Sweden; Navachab Gold mine, Namibia; Newcrest Mining Limited, Cadia Valley Operations, Australia; Northern Star Resources Limited, Australia; Iamgold Corporation, Westwood Mine, Canada; BHP Olympic Dam, Australia; BHP Nickel West, Australia; Minerals Research Institute of Western Australia, Australia. Hongyu Wang acknowledges the useful discussion with Dr. Lingwei Zhong and Dr. Yu Zhou and support from the National Natural Science Foundation of China through project U1965204 and project 52061160367. The authors acknowledge the help from the technicians in our group: Mr. Sheehan Gabriel, Mr. Hayden Reynolds-Collins and Mrs. Ai Li.
Publisher Copyright:
© The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature 2023.
PY - 2024/3
Y1 - 2024/3
N2 - Reliable and low-cost in situ stress measurement is important for design and operation of underground excavations. Deformation rate analysis (DRA) is a rock memory stress determination method based on carrying out cyclic, non-destructive uniaxial compression tests on rock cores in the laboratory. The DRA method may not be applicable to rock cores with low uniaxial compressive strength as fractures or failure may be induced during loading. A triaxial DRA test was proposed with the intention of increasing rock strength by confining stresses in the course of DRA testing. However, triaxial DRA tests overestimate the pre-stress (the maximum previous stress), with the error increasing as the confining stress increases. To solve this problem, we develop a simple DRA model and propose linear triaxial deformation rate analysis (LDRA) based on performing triaxial DRA tests with different confining stresses and reconstruction of the pre-stress using linear regression. The LDRA method is demonstrated to work well on determining the maximum previous stresses memorized in rocks.
AB - Reliable and low-cost in situ stress measurement is important for design and operation of underground excavations. Deformation rate analysis (DRA) is a rock memory stress determination method based on carrying out cyclic, non-destructive uniaxial compression tests on rock cores in the laboratory. The DRA method may not be applicable to rock cores with low uniaxial compressive strength as fractures or failure may be induced during loading. A triaxial DRA test was proposed with the intention of increasing rock strength by confining stresses in the course of DRA testing. However, triaxial DRA tests overestimate the pre-stress (the maximum previous stress), with the error increasing as the confining stress increases. To solve this problem, we develop a simple DRA model and propose linear triaxial deformation rate analysis (LDRA) based on performing triaxial DRA tests with different confining stresses and reconstruction of the pre-stress using linear regression. The LDRA method is demonstrated to work well on determining the maximum previous stresses memorized in rocks.
KW - Deformation rate analysis
KW - DRA
KW - In situ stress measurement
KW - Triaxial compression
UR - http://www.scopus.com/inward/record.url?scp=85178439868&partnerID=8YFLogxK
U2 - 10.1007/s00603-023-03658-9
DO - 10.1007/s00603-023-03658-9
M3 - Article
AN - SCOPUS:85178439868
SN - 0723-2632
VL - 57
SP - 1939
EP - 1962
JO - Rock Mechanics and Rock Engineering
JF - Rock Mechanics and Rock Engineering
IS - 3
ER -