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Stress drop as a result of splitting, brittle and transitional faulting of rock samples in uniaxial and triaxial compression tests

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Języki publikacji
EN
Abstrakty
EN
Rock samples can behave brittle, transitional or ductile depending on test pressure, rate of loading and temperature. Axial stiffness and its changes, relative and absolute dilatancy, yield, and fracture thresholds, residual strength are strongly pressure dependent. In this paper the stress drop as an effect of rock sample strength loss due to failure was analyzed. Uniaxial and triaxial experiments on three types of rock were performed to investigate the stress drop phenomenon. The paper first introduces short background on rock behavior and parameters defining a failure process under uniaxial and triaxial loading conditions. Stress drop data collected with experiments are analyzed and its pressure dependence phenomenon is described. Two methods for evaluation of stress drop value are presented.
Wydawca
Rocznik
Strony
17--23
Opis fizyczny
Bibliogr. 19 poz., rys.
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autor
  • AGH University of Science and Technology, Department of Geomechanics, Civil Engineering and Geotechnics
Bibliografia
  • [1] BRACE W.F., BYERLEE J.D., Stick-slip as a mechanism for earthquakes, Science, 1966, 153, 990–992.
  • [2] BYERLEE J.D., Brittle-ductile transitions in rocks, J. Geophys. Res., 1968, 73, 4741–4750.
  • [3] BYERLEE J.D., Friction of rocks, Pure Appl. Geophys., 1978, 116, 615–626.
  • [4] BYERLEE J.D., BRACE W.F., Stick-slip stable sliding and earthquakes – effect of rock type, pressure, strain rate and stiffness, J. Geophys. Res., 1968, 73, 6031–6097.
  • [5] CIEŚLIK J., Results of triaxial compression tests on LGOM sandstone and dolomite in the context of the elastic-plastic constitutive model selection, Archives of Mining Sciences, 2007, 52 (3), 437–451.
  • [6] CIEŚLIK J., Scalar damage variable determined in the uniaxial and triaxial compression conditions of sandstone samples, Studia Geotechnica et Mechanica, 2013, 35 (1), 73–84.
  • [7] DIETERICH J.H., Time dependent friction in rock, J. Geophys. Res., 1972, 77, 3690–3697.
  • [8] DŁUGOSZ M., GUSTKIEWICZ J., WYSOCKI A., Apparatus for investigation of rocks in a triaxial state of stress. Part II, Archives of Mining Sciences, 1981, 26, 17–41.
  • [9] GUSTKIEWICZ J., Transition of the rocks from the brittle to ductile state. Strain at failure as a function of confining pressure, Acta Geophysica. Polonica, 1985, 33, 169–181.
  • [10] ISMAIL L.A.H., MURRELL S.A.F., The effect of confining pressure on stress-drop in compressive rock fracture, Technophysics, 1990, 175, 237–248.
  • [11] JAEGER J.C., COOK N.G.W., Fundamentals of Rock Mechanics, Chapman and Hall, London 1976.
  • [12] KWAŚNIEWSKI M., The effect of the state of stress, temperature and strain rate on the mechanical properties of rocks, Archives of Mining Sciences, 1986, 31, 384–414, (in Polish).
  • [13] KWAŚNIEWSKI M., Behavior of iso- and anisotropic rocks under triaxial compression conditions, Zeszyty Naukowe Politechniki Śląskiej, Górnictwo, nr 1510, (in Polish).
  • [14] LOCKNER D.A., Rock failure, [in:] AGU Handbook of Physical Constants, ed. Ahrens T.J., Am. Geophys. Union, Washington, D.C. 1995, 3–10, 127–147.
  • [15] MOGI K., Pressure dependence of rock strength and transition from brittle fracture to ductile flow, Bull. Erthquake Res. Inst., Tokyo Univ., 1966, 44, 215–232.
  • [16] MOGI K., Experimental Rock Mechanics, Taylor & Francis, Balkema, 2007.
  • [17] OROWAN E., Mechansm of seismic faulting, Geol. Soc. Am. Mem., 1960, 79, 323–345.
  • [18] PATERSON M.S., Experimental rock deformation – the brittle field, Springer-Verlag, Berlin, 1978.
  • [19] PATERSON M.S., WONG T.-F., Experimental rock deformation – the brittle field, second ed., Springer, 2005.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-6403708f-e85a-4cd8-bf4b-7b1138f7ad6c
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