Document Type : Original Research Paper

Authors

State Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xu Zhou 221116, Jiangsu

Abstract

Mudstone is a common rock in underground engineering, and mudstone with fractures, have the certain self-closing capability. In this paper, we employed experiments and numerical analyses to investigate the mechanism of such a characteristic, and also examined the permeability pattern of mudstone overburdens. The experiments were performed with the MTS815.02 testing system, involving material properties under different water contents and their crack-closing behaviors. The principal task of numerical analysis is to determine the permeability of fractured mudstone layers, working with the COMSOL platform. The experimental results show that the Young’s Modulus of water-saturated mudstone is just 2.2% of that of natural mudstone, and the saturated also exhibit a remarkably obvious creep behavior. As the surrounding pressures increase, the permeability coefficient of fractured mudstone decrease exponentially, even dropping by two orders of magnitude corresponding to over 2.0MPa pressures. Based on these experiment outcomes, we can easily infer that rapid or complete fracture-closing is the main reason of permeability drop, and furthermore, both softening and creep are the major factors of self-closure of mudstone fractures, and especially, the softening behavior plays an absolutely fundamental role. The numerical analyses show that either a higher in-situ stress or lower fracture density can obviously become one of the advantageous conditions for fractured mudstone layers to restore towards impermeability. These results are also verified by the engineering observation in Yili No. 4 mine of China. There obviously existed the recovery of water-blocking capacity of overlying strata after a period of time. We hereby recommend this investigation as refences for underground mining or engineering construction involving mudstone.

Keywords

Main Subjects

[1]. Davy, C. A., Skoczylas, F., Barnichon, J. D., & Lebon, P. (2007). Permeability of macro-cracked argillite under confinement: Gas and water testing. Physics and Chemistry of the Earth, Parts A/B/C, 32(8–14), 667–680.
[2]. Van Marcke, P., & Bastiaens, W. (2010). Excavation induced fractures in a plastic clay formation: Observations at the Hades URF. Journal of Structural Geology, 32(11), 1677–1684.
[3]. Qin, H., Tang, H., Yin, X., Cheng, X., & Li, J. (2024). Study on water–rock interaction failure mechanism and constitutive model of mudstone damaged by pre-peak disturbance. Theoretical and Applied Fracture Mechanics, 133, 104539.
[4]. Pan, D., Liu, C., Liang, D., Zhou, J., & Zhang, L. (2024). Study on time-dependent injectability evaluation of mudstone considering the self-healing effect. Open Geosciences, 16, 16–27.
[5]. Zhang, D., Fan, G., Ma, L., & Wang, X. (2011). Aquifer protection during longwall mining of shallow coal seams: A case study in the Shendong coalfield of China. International Journal of Coal Geology, 86(2), 190–196.
[6]. Li, X., Li, X., Wang, Y., Peng, W., Fan, X., Cao, Z., & Liu, R. (2023). The seepage evolution mechanism of variable mass of broken rock in karst collapse column under the influence of mining stress. Geofluids, 1–10.
[7]. Zhang, C. (2011). Experimental evidence for self-sealing of fractures in claystone. Physics and Chemistry of the Earth, Parts A/B/C, 36(17–18), 1972–1980.
[8]. Abdollahipour, A., Marji, M. F., Bafghi, A. Y., & Gholamnejad, J. (2016). Numerical investigation of effect of crack geometrical parameters on hydraulic fracturing process of hydrocarbon reservoirs. Journal of Mining and Environment, 7(2), 205–214.
[9]. Abdollahipour, A., Marji, M. F., Bafghi, A. Y., & Gholamnejad, J. (2016). A complete formulation of an indirect boundary element method for poroelastic rocks. Computers and Geotechnics, 74, 15–25.
[10]. Ma, T., Rutqvist, J., Oldenburg, C. M., & Liu, W. (2017). Coupled thermal–hydrological–mechanical modeling of CO2-enhanced coalbed methane recovery. International Journal of Coal Geology, 179, 81–91.
[11]. Baghbanan, A., & Jing, L. (2008). Stress effects on permeability in a fractured rock mass with correlated fracture length and aperture. International Journal of Rock Mechanics and Mining Sciences, 45(8), 1320–1334.
[12]. Bastiaens, W., Bernier, F., & Li, X. L. (2007). Selfrac: Experiments and conclusions on fracturing, self-healing and self-sealing processes in clays. Physics and Chemistry of the Earth, Parts A/B/C, 32(8–14), 600–615.
[13]. Wang, L. L., Bornert, M., Héripré, E., Chanchole, S., Pouya, A., & Halphen, B. (2015). The mechanisms of deformation and damage of mudstones: A micro-scale study combining ESEM and DIC. Rock Mechanics and Rock Engineering, 48(5), 1913–1926.
[14]. Nahazanan, H., Clarke, S., Asadi, A., Md. Yusoff, Z., & Kim Huat, B. (2013). Effect of inundation on shear strength characteristics of mudstone backfill. Engineering Geology, 158, 48–56.
[15]. Fukuda, D., Maruyama, M., Nara, Y., Hayashi, D., Ogawa, H., & Kaneko, K. (2014). Observation of fracture sealing in high-strength and ultra-low-permeability concrete by micro-focus X-ray CT and SEM/EDX. International Journal of Fracture, 188(2), 159–171.
[16]. Cao, P., Karpyn, Z. T., & Li, L. (2015). Self-healing of cement fractures under dynamic flow of CO2-rich brine. Water Resources Research, 51(6), 4684–4701.
[17]. Polak, A., Elsworth, D., Yasuhara, H., Grader, A. S., & Halleck, P. M. (2003). Permeability reduction of a natural fracture under net dissolution by hydrothermal fluids. Geophysical Research Letters, 30(20).
[18]. Hearn, N., & Morley, C. T. (1997). Self-sealing property of concrete—Experimental evidence. Materials & Structures, 30(7), 404–411.
[19]. Brunet, J. L., Li, L., Karpyn, Z. T., & Huerta, N. J. (2016). Fracture opening or self-sealing: Critical residence time as a unifying parameter for cement–CO2–brine interactions. International Journal of Greenhouse Gas Control, 47, 25–37.
[20]. Hou, Z. (2003). Mechanical and hydraulic behavior of rock salt in the excavation disturbed zone around underground facilities. International Journal of Rock Mechanics and Mining Sciences, 40(5), 725–738.
[21]. Zhong, Y., Kuru, E., Zhang, H., Kuang, J., & She, J. (2019). Effect of fracturing fluid/shale rock interaction on the rock physical and mechanical properties, the proppant embedment depth and the fracture conductivity. Rock Mechanics and Rock Engineering, 52(4), 1011–1022.
[22]. Vahab, M., & Khalili, N. (2018). X-FEM modeling of multizone hydraulic fracturing treatments within saturated porous media. Rock Mechanics and Rock Engineering, 51(10), 3219–3239.
[23]. Malama, B., & Kulatilake, P. H. S. W. (2003). Models for normal fracture deformation under compressive loading. International Journal of Rock Mechanics and Mining Sciences, 40(6), 893–901.
[24]. Misra, A., & Marangos, O. (2011). Rock-joint micromechanics: Relationship of roughness to closure and wave propagation. International Journal of Geomechanics, 11(6), 431–439.
[25]. Hopkins, D. L. (2000). The implications of joint deformation in analyzing the properties and behavior of fractured rock masses, underground excavations, and faults. International Journal of Rock Mechanics and Mining Sciences, 37(1), 175–202.
[26]. Sevostianov, I., & Kachanov, M. (2008). Normal and tangential compliances of interface of rough surfaces with contacts of elliptic shape. International Journal of Solids and Structures, 45(9), 2723–2736.
[27]. Marache, A., Riss, J., & Gentier, S. (2008). Experimental and modelled mechanical behaviour of a rock fracture under normal stress. Rock Mechanics and Rock Engineering, 41(6), 869–892.
[28]. Matsuki, K., Wang, E. Q., Sakaguchi, K., & Okumura, K. (2001). Time-dependent closure of a fracture with rough surfaces under constant normal stress. International Journal of Rock Mechanics and Mining Sciences, 38(5), 607–619.
[29]. Rutqvist, J., Wu, Y. S., Tsang, C. F., & Bodvarsson, G. (2002). A modeling approach for analysis of coupled multiphase fluid flow, heat transfer, and deformation in fractured porous rock. International Journal of Rock Mechanics and Mining Sciences, 39(4), 429–442.
[30]. Daley, T. M., Schoenberg, M. A., Rutqvist, J., & Nihei, K. T. (2006). Fractured reservoirs: An analysis of coupled elastodynamic and permeability changes from pore-pressure variation. Geophysics, 71(5), 33–41.