Abstract
This study focuses on the transport properties and permeability evolution characteristics of fluid flow through thermally treated rock samples containing single fractures. First, splitting fractures were generated in cylindrical granite samples after high-temperature exposure (25–800 °C). Then a series of water flow tests through both intact and fractured samples were conducted in a triaxial cell under different confining pressures (10–30 MPa) and varying inlet hydraulic pressures (0.4–6 MPa). The results show that as the temperature increases from 25 to 800 °C, the standard deviations of the 3D spatial distribution parameters, including the asperity height, slope angle, and aspect direction of the fracture surface mesh element planes, all increase, indicating gradually increasing fracture surface roughness. The relationships between the pressure gradient and flow rate of intact samples, fractured rock samples, and the fractures themselves can all be well fitted using the Forchheimer’s law. Both linear and nonlinear coefficients in the Forchheimer’s law increase with increasing confining pressure. An exponential function is used to evaluate the equivalent permeability of intact samples based on temperature levels. The permeability undergoes an increasing trend as the temperature increases due to thermally induced defects, but undergoes a decreasing trend as the confining pressure increases due to defect closure. Two representative types of flow characteristics through the fractured rock samples, dominated by either the rock matrix or fracture flow, are identified. In the temperature range of 25–800 °C, the critical Reynolds number of the fractures declines, which first remains generally constant for temperatures of 25–400 °C and then experiences a dramatic decrease for temperatures of 400–800 °C. The nonlinear coefficient bf in Forchheimer’s law versus the hydraulic aperture eh curves displays a decreasing trend following a power-law relationship. The Forchheimer’s law results are evaluated by plotting the normalized transmissivity against the pressure gradient. An increase in the confining pressure shifts the fitted curves downward. As the temperature increases, the contribution of the matrix to the overall discharge capacity of the fractured rock samples gradually enhances, while that for the fractures weakens. The reduction extent in permeability of the rough-walled fractures is more remarkable than that of the matrix under an applied confining pressure.
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References
Babadagli T, Ren X, Develi K (2015) Effects of fractal surface roughness and lithology on single and multiphase flow in a single fracture: an experimental investigation. Int J Multiph Flow 68:40–58
Bandis SC, Lumsden AC, Barton NR (1983) Fundamentals of rock joint deformation. Int J Rock Mech Min Sci Geomech Abstr 20(6):249–268
Barton N, Choubey V (1977) The shear strength of rock joints in theory and practice. Rock Mech Felsmechanik Mecanique Des Roches 10(1–2):1–54
Barton N, Bandis S, Bakhtar K (1985) Strength, deformation and conductivity coupling of rock joints. Int J Rock Mech Min Sci Geomech Abstr 22(3):121–140
Brush DJ, Thomson NR (2003) Fluid flow in synthetic rough-walled fractures: Navier–Stokes, Stokes, and local cubic law simulations. Water Resour Res 39(4):1037–1041
Chen YF, Zhou JQ, Hu SH, Hu R, Zhou CB (2015) Evaluation of Forchheimer equation coefficients for non-Darcy flow in deformable rough-walled fractures. J Hydrol 529:993–1006
Chen SW, Yang CH, Wang GB (2017) Evolution of thermal damage and permeability of Beishan granite. Appl Therm Eng 110:1533–1542
Cherubini C, Giasi CI, Pastore N (2012) Bench scale laboratory tests to analyze non-linear flow in fractured media. Hydrol Earth Syst Sci Discuss 9(4):2511–2522
Durham WB, Bonner BP (1994) Self-propping and fluid flow in slightly offset joints at high effective pressures. J Geophys Res 99(B5):9391–9399
Huang N, Liu R, Jiang Y, Li B, Yu L (2018) Effects of fracture surface roughness and shear displacement on geometrical and hydraulic properties of three-dimensional crossed rock fracture models. Adv Water Resour 113:30–41
ISRM (1981) Rock characterization, testing and monitoring—ISRM suggested methods. In: Brown ET (ed) Suggested methods for the quantitative description of discontinuities in rock masses. Pergamon, Oxford, pp 3–52
Javadi M, Sharifzadeh M, Shahriar K, Mitani Y (2014) Critical Reynolds number for nonlinear flow through rough-walled fractures: the role of shear processes. Water Resour Res 50(2):1789–1804
Kong B, Wang E, Li Z, Wang X, Niu Y, Kong X (2017) Acoustic emission signals frequency-amplitude characteristics of sandstone after thermal treated under uniaxial compression. J Appl Geophys 136:190–197
Kristinsdóttir LH, Flóvenz ÓG, Árnason K, Bruhn D, Milsch H, Spangenberg E, Kulenkampff J (2010) Electrical conductivity and P-wave velocity in rock samples from high-temperature Icelandic geothermal fields. Geothermics 39(1):94–105
Kumari WGP, Ranjith PG, Perera MSA, Chen BK, Abdulagatov IM (2017) Temperature-dependent mechanical behaviour of Australian strathbogie granite with different cooling treatments. Eng Geol 229:31–44
Li B, Liu R, Jiang Y (2016) Influences of hydraulic gradient, surface roughness, intersecting angle, and scale effect on nonlinear flow behavior at single fracture intersections. J Hydrol 538:440–453
Liu RC, Li B, Jiang YJ (2016) Critical hydraulic gradient for nonlinear flow through rock fracture networks: the roles of aperture, surface roughness, and number of interactions. Adv Water Resour 88:53–65
Liu R, Li B, Jiang Y, Yu L (2018) A numerical approach for assessing effects of shear on equivalent permeability and nonlinear flow characteristics of 2D fracture networks. Adv Water Resour 111:289–300
Marcoulaki EC, Venetsanos A, Papazoglou IA (2017) Quantitative safety analysis of cryogenic liquid releases in a deep underground large scale installation. Reliab Eng Syst Saf 162:51–63
Masri M, Sibai M, Shao JF, Mainguy M (2014) Experimental investigation of the effect of temperature on the mechanical behavior of Tournemire shale. Int J Rock Mech Min Sci 70(9):185–191
Nowamooz A, Radilla G, Fourar M (2009) Non-Darcian two-phase flow in a transparent replica of a rough-walled rock fracture. Water Resour Res 45(7):4542–4548
Olsson R, Barton N (2001) An improved model for hydromechanical coupling during shearing of rock joints. Int J Rock Mech Min Sci 38(3):317–329
Qian JZ, Chen Z, Zhan HB, Guan HC (2011) Experimental study of the effect of roughness and Reynolds number on fluid flow in rough-walled single fractures: a check of local cubic law. Hydrol Process 25(4):614–622
Quinn PM, Parker BL, Cherry JA (2011) Using constant head step tests to determine hydraulic apertures in fractured rock. J Contam Hydrol 126(1):85–99
Radilla G, Nowamooz A, Fourar M (2013) Modeling non-Darcian single- and two-phase flow in transparent replicas of rough-walled rock fractures. Transp Porous Media 98(2):401–426
Ranjith PG, Darlington W (2007) Nonlinear single-phase flow in real rock joints. Water Resour Res 43(9):146–156
Ranjith PG, Viete DR, Chen BJ, Perera MSA (2012) Transformation plasticity and the effect of temperature on the mechanical behaviour of Hawkesbury sandstone at atmospheric pressure. Eng Geol 151(151):120–127
Rong G, Yang J, Cheng L, Zhou C (2016) Laboratory investigation of nonlinear flow characteristics in rough fractures during shear process. J Hydrol 541:1385–1394
Salimzadeh S, Nick HM, Zimmerman RW (2018) Thermoporoelastic effects during heat extraction from low-permeability reservoirs. Energy 142:546–558
Schmittbuhl J, Steyer A, Jouniaux L, Toussaint R (2008) Fracture morphology and viscous transport. Int J Rock Mech Min Sci 45(3):422–430
Shafirovich E, Varma A (2009) Underground coal gasification: a brief review of current status. Ind Eng Chem Res 48(17):7865–7875
Sharifzadeh M, Mitani Y, Esaki T (2008) Rock joint surfaces measurement and analysis of aperture distribution under different normal and shear loading using GIS. Rock Mech Rock Eng 41(2):299–323
Skjetne E, Hansen A, Gudmundsson JS (2000) High-velocity flow in a rough fracture. J Fluid Mech 383(383):1–28
Su HJ, Jing HW, Yin Q, Yu L, Wang YC, Wu XJ (2017) Strength and deformation behaviors of veined marble specimens after vacuum heat treatment under conventional triaxial compression. Acta Mech Sin 33(5):886–898
Tian H, Ziegler M, Kempka T (2014) Physical and mechanical behavior of claystone exposed to temperatures up to 1000 °C. Int J Rock Mech Min Sci 70:144–153
Tiskatine R, Eddemani A, Gourdo L, Abnay B, Ihlal A, Aharoune A, Bouirden L (2016) Experimental evaluation of thermo-mechanical performances of candidate rocks for use in high temperature thermal storage. Appl Energy 171:243–255
Tse R, Cruden DM (1979) Estimating joint roughness coefficients. Int J Rock Mech Min Sci Geomech Abstr 16(5):303–307
Tzelepis V, Moutsopoulos KN, Papaspyros JNE, Tsihrintzis VA (2015) Experimental investigation of flow behavior in smooth and rough artificial fractures. J Hydrol 521(2):108–118
Ulusay R, Hudson JA (1978) Suggested methods for determining tensile strength of rock materials. Part 2: Suggested method for determining indirect tensile strength by the Brazil test. Int J Rock Mech Min Sci Geomech Abstr 15:99–103
Wang M, Chen YF, Ma GW, Zhou JQ, Zhou CB (2016) Influence of surface roughness on nonlinear flow behaviors in 3D self-affine rough fractures: lattice Boltzmann simulations. Adv Water Resour 96:373–388
Witherspoon PA, Wang JSY, Iwai K, Gale JE (1980) Validity of cubic law for fluid flow in a deformable rock fracture. Water Resour Res 16(6):1016–1024
Xia CC, Qian X, Lin P, Xiao WM, Gui Y (2016) Experimental investigation of nonlinear flow characteristics of real rock joints under different contact conditions. J Hydraul Eng. https://doi.org/10.1061/(ASCE)HY.1943-7900.0001238
Xie LZ, Gao C, Ren L, Li CB (2015) Numerical investigation of geometrical and hydraulic properties in a single rock fracture during shear displacement with the Navier–Stokes equations. Environ Earth Sci 73(11):7061–7074
Yasuhara H, Kinoshita N, Ohfuji H, Takahashi M, Ito K, Kishida K (2015) Long-term observation of permeability in sedimentary rocks under high-temperature and stress conditions and its interpretation mediated by microstructural investigations. Water Resour Res 51(7):5425–5449
Yin T, Li X, Cao W, Xia K (2015) Effects of thermal treatment on tensile strength of Laurentian granite using Brazilian test. Rock Mech Rock Eng 48(6):2213–2223
Yin Q, Jing HW, Zhu TT (2016) Mechanical behavior and failure analysis of granite specimens containing two orthogonal fissures under uniaxial compression. Arab J Geosci. https://doi.org/10.1007/s12517-015-2078-y
Yin Q, Ma GW, Jing HW, Su HJ, Liu RC (2017) Hydraulic properties of 3D rough-walled fractures during shearing: an experimental study. J Hydrol 555:169–184
Yin Q, Jing H, Liu R, Ma G, Yu L, Su H (2018) Experimental study on stress-dependent nonlinear flow behavior and normalized transmissivity of real rock fracture networks. Geofluids. https://doi.org/10.1155/2018/8217921
Zeng ZW, Grigg R (2006) A criterion for non-Darcy flow in porous media. Transp Porous Media 63(1):57–69
Zhang ZY, Nemcik J (2013) Fluid flow regimes and nonlinear flow characteristics in deformable rock fractures. J Hydrol 447(1):139–151
Zhang W, Sun Q, Hao S, Geng J, Lv C (2016) Experimental study on the variation of physical and mechanical properties of rock after high temperature treatment. Appl Therm Eng 98:1297–1304
Zhao Y, Feng Z, Zhao Y, Wan Z (2017) Experimental investigation on thermal cracking, permeability under HTHP and application for geothermal mining of HDR. Energy 132:305–314
Zharikov AV, Vitovtova VM, Shmonov VM, Grafchikov AA (2003) Permeability of the rocks from the Kola superdeep borehole at high temperature and pressure: implication to fluid dynamics in the continental crust. Tectonophysics 370(1):177–191
Zhou JQ, Hu SH, Fang S, Chen YF, Zhou CB (2015) Nonlinear flow behavior at low Reynolds numbers through rough-walled fractures subjected to normal compressive loading. Int J Rock Mech Min Sci 80:202–218
Zimmerman RW, Bodvarsson GS (1996) Hydraulic conductivity of rock fractures. Transp Porous Media 23(1):1–30
Zimmerman RW, Chen DW, Cook NGW (1992) The effect of contact area on the permeability of fractures. J Hydrol 139(1–4):79–96
Zimmerman RW, AL-Yaarubi A, Pain CC, Grattoni CA (2004) Non-linear regimes of fluid flow in rock fractures. Int J Rock Mech Min Sci 41(3):163–169
Zou L, Tarasov BG, Dyskin AV, Adhikary DP, Pasternak E, Xu W (2013) Physical modelling of stress-dependent permeability in fractured rocks. Rock Mech Rock Eng 46(1):67–81
Zuo JP, Wang JT, Sun YJ, Chen Y, Jiang GH, Li YH (2017) Effects of thermal treatment on fracture characteristics of granite from Beishan, a possible high-level radioactive waste disposal site in China. Eng Fract Mech 182:425–437
Acknowledgements
The financial supports from the National Natural Science Foundation of China, China (no. 51734009), the National Key Basic Research and Development Program of China, China (no. 2017YFC0603001), and Natural Science Foundation of Jiangsu Province, China (no. BK20180663) are gratefully acknowledged.
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Yin, Q., Liu, R., Jing, H. et al. Experimental Study of Nonlinear Flow Behaviors Through Fractured Rock Samples After High-Temperature Exposure. Rock Mech Rock Eng 52, 2963–2983 (2019). https://doi.org/10.1007/s00603-019-1741-0
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DOI: https://doi.org/10.1007/s00603-019-1741-0