Experimental Study on the Mechanical Properties of Deep Granite under Gradient-Confining Pressure
Source abstract
Abstract
In deep layers, the complex geological environment is characterized by high temperature and high stress which causes marked differences in the mechanical properties of granite compared to those of granite in shallow areas. To investigate the mechanical properties of deep granite, this paper utilizes conventional triaxial compression tests to determine the various mechanical properties and failure modes of deep granite under different confining pressures. The findings indicate that the elastic modulus, Poisson’s ratio, and peak strength of deep granite display greater dispersion than those of shallow granite under the influence of confining pressure. Based on the stress-strain curve, various characteristic stresses of deep granite under different confining pressures are calculated, and a distinct exponential function relationship exists between the characteristic stresses and the confining pressure. Furthermore, the finite element numerical simulation software Abaqus is employed to simulate the conventional triaxial compression of granite under different confining pressures, thereby revealing the stress and deformation evolution process of granite during the compression process. This research unveils the mechanical properties of deep granite under gradient-confining pressure, which can offer crucial theoretical evidence and data to support engineering applications in relevant fields.
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Research context
OpenAlex topics: Rock Mechanics and Modeling · Geotechnical and Geomechanical Engineering · Drilling and Well Engineering
SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.
Affiliations
Key Laboratory of Ground Control Management Plan in Deep Metal Mines, National Mine Safety Administration, Northeastern University, Shenyang 110819, China
Funding
Key Projects of the National Natural Science Foundation of China · Ministry of Education’s Major Needs Program for Basic Research Operating Expenses
References (28)
Show source-provided references
1. Crack Initiation, Propagation, and Failure Characteristics of Jointed Rock or Rock-Like Specimens: A Review10.1155/2019/6975751 ↗
2. A review of the New Geophysics: A new understanding of pre-fracturing deformation in the crack-critical crust with implications for hydrocarbon production10.1007/s12182-008-0001-9 ↗
3. Time-dependent cracking and brittle creep in crustal rocks: A review10.1016/j.jsg.2013.03.007 ↗
4. Long-term creep behavior of deep-buried marble under different confining pressures10.2298/TSCI180615078Z ↗
5. Numerical simulation of rock fragmentation during cutting by conical picks under confining pressure10.1016/j.crme.2017.09.004 ↗
6. Experimental study on the mechanical and failure behaviors of deep rock subjected to true triaxial stress: A review10.1016/j.ijmst.2022.05.006 ↗
7. Ultra-deep level mining—Future requirements
8. Geotechnical classification of deep and ultra-deep Witwatersrand mining areas, South Africa10.1007/s001260050100 ↗
9. Petrogenesis of Archaean granites in the Barberton region of South Africa as a guide to early crustal evolution10.25131/sajg.124.0021 ↗
10. Geology and geochemistry of Archaean granites in the Kalgoorlie region of the eastern goldfields, Western Australia: A syn-collisional tectonic setting?10.1016/S0301-9268(97)00008-9 ↗
11. Fluid-rock interaction in the Qitianling granite and associated tin deposits, South China: Evidence from boron and oxygen isotopes10.1016/j.oregeorev.2011.07.002 ↗
12. Mineralogical and geochemical constraints on the genesis of the granite-hosted Huangao uranium deposit, SE China10.1016/S0169-1368(98)00020-1 ↗
13. Zhang, S.S., Yang, X.Y., and Liu, L. (2023). Evolution, Magmatic Source and Metallogenesis of A-Type Granites in the Fanchang Volcanic Basin, Middle and Lower Yangtze Metallogenic Belt: A Review. Minerals, 13.10.3390/min13040571 ↗
14. Episodes of fast crystal growth in pegmatites10.1038/s41467-020-18806-w ↗
15. Mechanical properties and fracturing of rock-backfill composite specimens under triaxial compression10.1016/j.conbuildmat.2021.124577 ↗
16. Advances in stress-strain constitutive models for rock failure: Review and new dynamic constitutive failure (DCF) model using core data from the Tarim Basin (China)10.1016/j.earscirev.2023.104473 ↗
17. Analytical solutions for characteristic radii of circular roadway surrounding rock plastic zone and their application10.1016/j.ijmst.2018.10.002 ↗
18. Experiment investigation of granite damage under the high-temperature and high-pressure supercritical water condition10.1016/j.petrol.2019.05.031 ↗
19. Effect of Grain Size on the Mechanical Behaviour of Granite Under High Temperature and Triaxial Stresses10.1007/s00603-020-02303-z ↗
20. The effect of rapid cooling on the thermal diffusivity of granite10.1016/j.jappgeo.2019.06.002 ↗
21. Effect of Anisotropy on the Long-Term Strength of Granite10.1007/s00603-014-0634-5 ↗
22. Fracture Mechanics Behavior of Jointed Granite Exposed to High Temperatures10.1007/s00603-021-02393-3 ↗
23. Experimental investigation on mechanical behaviors of Nanan granite after thermal treatment under conventional triaxial compression10.1007/s12665-020-09326-3 ↗
24. Analysis of dynamic fracture of granite after uniaxial recompression predamaged by high confining pressure cyclic loading based on acoustic emission10.1016/j.engfracmech.2022.108414 ↗
25. Evolutionary characteristics of mode-I fracture toughness and fracture energy in granite from different burial depths under high-temperature effect10.1016/j.engfracmech.2020.107306 ↗
26. Creep characteristics and fractional rheological model of granite under temperature and disturbance load coupling10.1007/s11043-023-09618-8 ↗
27. Dynamic cumulative damage characteristics of deep-buried granite from Shuangjiangkou hydropower station under true triaxial constraint10.1016/j.ijimpeng.2022.104215 ↗
28. A novel observation method for determining the crack stress thresholds of rock based on Hooke’s law10.1111/ffe.13306 ↗