Abstract
This work is devoted to characterization of the deformation and strength properties of cataclastic sandstones. Before conducting mechanical tests, the physical properties were first examined. These sandstones are characterized by a loose damaged microstructure and poorly cemented contacts. Then, a series of mechanical tests including hydrostatic, uniaxial, and triaxial compression tests were performed to study the mechanical strength and deformation of the sandstones. The results obtained show nonlinear stress–strain responses. The initial microcracks are closed at hydrostatic stress of 2.6 MPa, and the uniaxial compressive strength is about 0.98 MPa. Under triaxial compression, there is a clear transition from volumetric compressibility to dilatancy and a strong dependency on confining pressure. Based on the experimental evidence, an elastoplastic model is proposed using a linear yield function and a nonassociated plastic potential. There is good agreement between numerical results and experimental data.
Similar content being viewed by others
References
Andreev GE (1995) Brittle failure of rock materials: test results and constitutive models. Balkema, Rotterdam
Bourgeois F, Shao JF, Ozanam O (2002) An elastoplastic model for unsaturated rocks and concrete. Mech Res Commun 29:383–390
Budiansky B, O’Connell RJ (1976) Elastic moduli of a cracked solid. Int J Solids Struct 12:81–97
Burgi C (1999) Cataclastic fault rocks in underground excavations: a geological characterisation. Dissertation, EPF-Lausanne, Lausanne
Burgi C, Parriaux A, Franciosi G, Rey J-Ph (1999) Cataclastic rocks in underground structures-terminology and impact on the feasibility of projects (initial results). Eng Geol 51:225–235
Chen H, Hu ZY (2003) Some factors affecting the uniaxial strength of weak sandstones. Bull Eng Geol Env 62:323–332
Chen X, Liao ZH, Peng X (2012) Deformability characteristics of jointed rock masses under uniaxial compression. Int J Min Sci Technol 22:213–221
Cristescu ND (1994) A procedure to determine non-associated constitutive equations for geomaterials. Int J Plast 10:103–132
Dahou A, Shao JF, Bederiat M (1995) Experimental and numerical investigations on transient creep of porous chalk. Mech Mater 21:147–158
De Gennaro V, Delage P, Priol G, Collin F, Cui YJ (2004) On the collapse behavior of oil reservoir chalk. Géotechnique 54:415–420
Elodie S, Christopher AJW (2010) Evolution of cataclastic faulting in high-porosity sandstone, Bassin du Sud-Est, Provence, France. J Struct Geol 32(11):1590–1608
Fischer GJ, Paterson MS (1989) Dilatancy during rock deformation at high temperatures and pressures. J Geophys Res 78:607–617
Gudmundsson A, Simmenes TH, Belinda L, Sonja LP (2010) Effects of internal structure and local stresses on fracture propagation, deflection, and arrest in fault zones. J Struct Geol 32:1643–1655
Habimana J, Labiouseb V, Descoeudres F (2002) Geomechanical characterisation of cataclastic rocks: experience from the Cleuson-Dixence project. Int J Rock Mech Min Sci 39:677–693
Haimson B (2006) True triaxial stresses and the brittle fracture of rock. Rock Damage Fluid Transp Part I 163:1101–1130
Homand S, Shao JF (2000) Mechanical behavior of a porous chalk and water/chalk interaction. Part I: experimental study. Oil Gas Sci Technol 55:591–598
Hudson JA, Harrison JP (1997) Engineering rock mechanics: an introduction to the principles. Elsevier, Oxford, pp 106–111
Li DY, Wong LNY, Liu G, Zhang XP (2012) Influence of water content and anisotropy on the strength and deformability of low porosity meta-sedimentary rocks under triaxial compression. Eng Geol 126:46–66
Lori AK, James KR (2012) Cataclastic production of volcanic ash at Mount Saint Helens. Phys Chem Earth Parts A/B/C 45:40–49
Lu YF, Tian B, Huang WJ, Shao JF (2005) Laboratory study of sandstone with large porosity. J Hust (Urban Science Edition) 22:56–58
Meerea PA, Mulchrone KF (2003) The effect of sample size on geological strain estimation from passively deformed clastic sedimentary rocks. J Struct Geol 25:1587–1595
Mogi K (2007) Experimental rock mechanics. Taylor & Francis, London
Renner J, Rummel F (1996) The effect of experimental and micro-structural parameters on the transition from brittle failure to cataclastic flow of carbonate rocks. Tectonophysics 258:151–169
Shao JF, Zhu QZ, Su K (2003) Modeling of creep in rock materials in terms of material degradation. Comput Geotech 30:549–555
Wang HL, Xu WY, Shao JF (2013) Experimental researches on hydro-mechanical properties of altered rock under confining pressures. Rock Mech Rock Eng. doi:10.1007/s00603-013-0439-y
Xie SY, Shao JF (2006) Elastoplastic deformation of a porous rock and water interaction. Int J Plast 22:2195–2225
Yang SQ, Jiang YZ, Xu WY, Chen XQ (2008) Experimental investigation on strength and failure behavior of pre-cracked marble under conventional triaxial compression. Int J Solids Struct 45:4796–4819
Zhang Y, Xu WY, Gu JJ, Wang W (2013) Triaxial creep tests of weak sandstone from the deflection zone of high dam foundation. J Central South Univ Technol 20:2528–2536
Acknowledgments
Financial support from the Natural Science Foundation of China under grant no. 11172090, the state 973 project under grant no. 2011CB013504, and the Fundamental Research Funds for the Central Universities under grant no. 13CX02095A is gratefully acknowledged.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Zhang, Y., Shao, J.F., Xu, W.Y. et al. Experimental and Numerical Investigations on Strength and Deformation Behavior of Cataclastic Sandstone. Rock Mech Rock Eng 48, 1083–1096 (2015). https://doi.org/10.1007/s00603-014-0623-8
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00603-014-0623-8