Residual stress measurement and analysis of siliceous slate-containing quartz veins

Tao Wang; Weiwei Ye; Yemeng Tong; Naisheng Jiang; Liyuan Liu

doi:10.1007/s12613-023-2667-9

Volume 30 Issue 12

Dec. 2023

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Article Navigation > International Journal of Minerals, Metallurgy and Materials > 2023 > 30(12): 2310-2320

Tao Wang, Weiwei Ye, Yemeng Tong, Naisheng Jiang, and Liyuan Liu, Residual stress measurement and analysis of siliceous slate-containing quartz veins, Int. J. Miner. Metall. Mater., 30(2023), No. 12, pp. 2310-2320. https://doi.org/10.1007/s12613-023-2667-9

Cite this article as:

Tao Wang, Weiwei Ye, Yemeng Tong, Naisheng Jiang, and Liyuan Liu, Residual stress measurement and analysis of siliceous slate-containing quartz veins, Int. J. Miner. Metall. Mater., 30(2023), No. 12, pp. 2310-2320. https://doi.org/10.1007/s12613-023-2667-9

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Research Article

Residual stress measurement and analysis of siliceous slate-containing quartz veins

+ Author Affiliations

Corresponding authors:
Yemeng Tong E-mail: tongyemeng977@163.com

Liyuan Liu E-mail: liuliyuan@ustb.edu.cn
Received: 21 February 2023; Revised: 10 April 2023; Accepted: 27 April 2023; Available online: 29 April 2023

Abstract

Abstract

Engineering geological disasters such as rockburst have always been a critical factor affecting the safety of coal mine production. Thus, residual stress is considered a feasible method to explain these geomechanical phenomena. In this study, electron backscatter diffraction (EBSD) and optical microscopy were used to characterize the rock microcosm. A measuring area that met the requirements of X-ray diffraction (XRD) residual stress measurement was determined to account for the mechanism of rock residual stress. Then, the residual stress of a siliceous slate-containing quartz vein was measured and calculated using the sin²ϕ method equipped with an X-ray diffractometer. Analysis of microscopic test results showed homogeneous areas with small particles within the millimeter range, meeting the requirements of XRD stress measurement statistics. Quartz was determined as the calibration mineral for slate samples containing quartz veins. The diffraction patterns of the (324) crystal plane were obtained under different ϕ and φ. The deviation direction of the diffraction peaks was consistent, indicating that the sample tested had residual stress. In addition, the principal residual stress within the quartz vein measured by XRD was compressive, ranging from 10 to 33 MPa. The maximum principal stress was parallel to the vein trend, whereas the minimum principal stress was perpendicular to the vein trend. Furthermore, the content of the low-angle boundary and twin boundary in the quartz veins was relatively high, which enhances the resistance of the rock mass to deformation and promotes the easy formation of strain concentrations, thereby resulting in residual stress. The proposed method for measuring residual stress can serve as a reference for subsequent observation and related research on residual stress in different types of rocks.
- residual stress;
- siliceous sand;
- rock microstructure;
- X-ray diffraction;
- electron backscatter diffraction

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[1]	L.Y. Liu, H.G. Ji, X.F. Lü, et al., Mitigation of greenhouse gases released from mining activities: A review, Int. J. Miner. Metall. Mater., 28(2021), No. 4, p. 513. doi: 10.1007/s12613-020-2155-4
[2]	G.R. Holzhausen and A.M. Johnson, The concept of residual stress in rock, Tectonophysics, 58(1979), No. 3-4, p. 237. doi: 10.1016/0040-1951(79)90311-1
[3]	M. Friedman, Residual elastic strain in rocks, Tectonophysics, 15(1972), No. 4, p. 297. doi: 10.1016/0040-1951(72)90093-5
[4]	T.T. Kie, Rockbursts, case records, theory and control, [in] Proceedings of the International Symposium on Engineering in Complex Rock Formations, Pergamon, 1988, p. 32.
[5]	S.H. Tang, Z.J. Wu, and X.H. Chen, Approach to occurrence and mechanism of rockburst in deep underground mines, Chin. J. Rock Mech. Eng., 22(2003), No. 8, p. 1250.
[6]	H. Zhou, F.Z. Meng, C.Q. Zhang, D.W. Hu, F.J. Yang, and J.J. Lu, Analysis of rockburst mechanisms induced by structural planes in deep tunnels, Bull. Eng. Geol. Environ., 74(2015), No. 4, p. 1435. doi: 10.1007/s10064-014-0696-3
[7]	D.I. Varnes and F.T. Lee, Hypothesis of mobilization of residual stress in rock, Geol. Soc. Am. Bull., 83(1972), No. 9, art. No. 2863. doi: 10.1130/0016-7606(1972)83[2863:HOMORS]2.0.CO;2
[8]	L. Müller, Rock Mechanics, Springer-Verlag, Berlin, 1974.
[9]	T.K. Tan and W.F. Kang, Locked in stresses, creep and dilatancy of rocks, and constitutive equations, Rock Mech., 13(1980), No. 1, p. 5. doi: 10.1007/BF01257895
[10]	Z.Q. Yue, Expansion power of compressed micro fluid inclusions as the cause of rockburst, Mech. Eng., 37(2015), No. 3, p. 287.
[11]	O. An, Forecast method for risk area and risk time of large earthquake in the Xianshuihe Fault Zone by superimposing the residual and present stress field, Bull. Inst. Crustal Dynamics, 1(1996), No. 0, p. 59.
[12]	X. Liu, H.S. Geng, H.F. Xu, Y.H. Yang, L.J. Ma, and L. Dong, Experimental study on the influence of locked-in stress on the uniaxial compressive strength and elastic modulus of rocks, Sci. Rep., 10(2020), No. 1, art. No. 17441. doi: 10.1038/s41598-020-74556-1
[13]	W.C. Chen, S.J. Wang, and H.R. Fu, Study advance on basic characteristics and formation causes of rock inner stress, J. Eng. Geol., 26(2018), No. 1, p. 62.
[14]	K. Sekine and K. Hayashi, Residual stress measurements on a quartz vein: A constraint on paleostress magnitude, J. Geophys. Res., 114(2009), No. B1.
[15]	K. Chen, M. Kunz, N. Tamura, and H.R. Wenk, Residual stress preserved in quartz from the San Andreas Fault Observatory at Depth, Geology, 43(2015), No. 3, p. 219. doi: 10.1130/G36443.1
[16]	H.R. Wenk, B.C. Chandler, K. Chen, Y. Li, N. Tamura, and R. Yu, Residual lattice strain in quartzites as a potential palaeo-piezometer, Geophys. J. Int., 222(2020), No. 1, p. 1363.
[17]	R. Weinberger, Y. Eyal, and N. Mortimer, Formation of systematic joints in metamorphic rocks due to release of residual elastic strain energy, Otago Schist, New Zealand, J. Struct. Geol., 32(2010), No. 3, p. 288. doi: 10.1016/j.jsg.2009.12.003
[18]	L.Y. Liu, H.G. Ji, D. Elsworth, S. Zhi, X.F. Lv, and T. Wang, Dual-damage constitutive model to define thermal damage in rock, Int. J. Rock Mech. Min. Sci., 126(2020), art. No. 104185. doi: 10.1016/j.ijrmms.2019.104185
[19]	C. Lu, Y. Lu, X.H. Gou, Y. Zhong, C. Chen, and J.C. Guo, Influence factors of unpropped fracture conductivity of shale, Energy Sci. Eng., 8(2020), No. 6, p. 2024. doi: 10.1002/ese3.645
[20]	D.W. Gentry, Horizontal residual stresses in the vicinity of a Breccia Pipe, Int. J. Rock Mech. Min. Sci. Geomech. Abstr., 10(1973), No. 1, p. 19. doi: 10.1016/0148-9062(73)90057-0
[21]	A. De Noni, D. Hotza, V.C. Soler, and E.S. Vilches, Analysis of the development of microscopic residual stresses on quartz particles in porcelain tile, J. Eur. Ceram. Soc., 28(2008), No. 14, p. 2629. doi: 10.1016/j.jeurceramsoc.2008.04.009
[22]	S.R. Kiahosseini and H. Ahmadian, Effect of residual structural strain caused by the addition of Co₃O₄ nanoparticles on the structural, hardness and magnetic properties of an Al/Co₃O₄ nanocomposite produced by powder metallurgy, Int. J. Miner. Metall. Mater., 27(2020), No. 3, p. 384. doi: 10.1007/s12613-019-1917-3
[23]	T. Sarkar, A.K. Pramanick, T.K. Pal, and A.K. Pramanick, Development of a new coated electrode with low nickel content for welding ductile iron and its response to austempering, Int. J. Miner. Metall. Mater., 25(2018), No. 9, p. 1090. doi: 10.1007/s12613-018-1660-1
[24]	X.M. Yuan, J. Zhang, Y. Lian, et al., Research progress of residual stress determination in magnesium alloys, J. Magnesium Alloys, 6(2018), No. 3, p. 238. doi: 10.1016/j.jma.2018.06.002
[25]	Z.H. Tang, X. Dong, Y.X. Geng, et al., The effect of warm laser shock peening on the thermal stability of compressive residual stress and the hot corrosion resistance of Ni-based single-crystal superalloy, Opt. Laser Technol., 146(2022), art. No. 107556. doi: 10.1016/j.optlastec.2021.107556
[26]	M. Friedman, X-ray analysis of residual elastic strain in quartzose rocks, [in] The 10th U.S. Symposium on Rock Mechanics, Texas, 1968, p.68.
[27]	A. Frischbutter, D. Neov, C. Scheffzük, M. Vrána, and K. Walther, Lattice strain measurements on sandstones under load using neutron diffraction, J. Struct. Geol., 22(2000), No. 11-12, p. 1587. doi: 10.1016/S0191-8141(00)00110-3
[28]	W.C. Chen, S.D. Li, X. Li, S.J. Wang, L.H. He, and S.M. Li, A novel method for determination of rock inner stress based on X-ray and neutron scaterring, J. Eng. Geol., 30(2022), No. 1, p. 223.
[29]	C.Y. Liu, H.L. Luo, H.J. Li, and X.X. Zhang, Formation mechanism and control technology of vein rockburst - A case study of Uzbekistan Kamchik tunnel, Rock Soil Mech., 42(2021), No. 5, p. 1413.
[30]	W.L. Bragg, The structure of some crystals as indicated by their diffraction of X-rays, Proc. R. Soc. London Ser. A, 89(1913), No. 610, p. 248. doi: 10.1098/rspa.1913.0083
[31]	I.C. Noyan and J.B. Cohen, Residual Stress: Measurement by Diffraction and Interpretation, Springer-Verlag, Berlin, 1987.
[32]	C. Palache, J.D. Dana, E.S. Dana, H. Berman, and C. Frondel, The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana, John Wiley and Sons, New York, 1944.
[33]	C. Frondel, Secondary Dauphiné twinning in quartz produced by sawing, Am. Mineral., 31(1946), No. 1-2, p. 58.
[34]	C. McGinn, E.A. Miranda, and L.J. Hufford, The effects of quartz Dauphiné twinning on strain localization in a mid-crustal shear zone, J. Struct. Geol., 134(2020), art. No. 103980.
[35]	G.E. Lloyd, Microstructural evolution in a mylonitic quartz simple shear zone: The significant roles of dauphine twinning and misorientation, Flow Process. Faults Shear Zones, 224(2004), p. 39.