Stresses around a circular opening in an elastoplastic porous medium subjected to repeated hydraulic loading

Abstract Stresses near a circular borehole under repeated interior loading are analyzed. In a porous material which is capable of plastic deformation, the stresses and strains adjacent to a borehole depend on the loading history. A solution for stresses and strains can only be determined once the stress paths and history to reach this condition are defined; therefore, to obtain meaningful solutions in poroplastic media, loading paths must be specified. In this paper, varying loadings inside a circular opening are imposed to simulate the non-monotonic pressure changes that arise during drilling and injection in a borehole. It is assumed that stresses under such loadings may be determined by considering the rocks as Mohr—Coulomb materials. A constitutive model is used that incorporates strain-weakening as a sudden strength loss after peak strength is reached, with perfect plastic behavior after weakening has occured. Plastic yielding related to different yielding modes, i.e. active (σr′ σgq′) stress states, is explored. Stages in the development of such stress states are analyzed, and the stress states in different zones under various circumstances are calculated separately and summed. The solutions presented can be used to understand stress development around boreholes, and can also be used to interpret hollow cylinder test results. They may be of use as parametric analysis tools to aid the drilling engineer analyze borehole stability, sand production and blow-out risks.

[1]  M. Dusseault,et al.  Borehole Yield and Hydraulic Fracture Initiation in Poorly Consolidated Rock Strata. Part II. Permeable Media. , 1991 .

[2]  Per Horsrud,et al.  Fracture initiation pressures in permeable poorly consolidated sands , 1982 .

[3]  J. C. Jaeger,et al.  Fundamentals of rock mechanics , 1969 .

[4]  T. Kennedy,et al.  Tunnel Closure for Nonlinear Mohr-Coulomb Functions , 1978 .

[5]  Emmanuel M Detournay,et al.  Elastoplastic model of a deep tunnel for a rock with variable dilatancy , 1986 .

[6]  M. Biot General Theory of Three‐Dimensional Consolidation , 1941 .

[7]  E. T. Brown,et al.  Ground Response Curves for Rock Tunnels , 1983 .

[8]  Elastic—plastic response of a circular hole to repeated loading , 1989 .

[9]  Emmanuel M Detournay,et al.  Poroelastic response of a borehole in a non-hydrostatic stress field , 1988 .

[10]  C. H. Yew,et al.  The determination of biot's parameters for sandstones , 1978 .

[11]  Herbert E. Lindberg,et al.  MODEL TESTS FOR PLASTIC RESPONSE OF LINED TUNNELS , 1978 .

[12]  M. Jefferies,et al.  DETERMINATION OF HORIZONTAL GEOSTATIC STRESS IN CLAY WITH SELF-BORED PRESSUREMETER: REPLY , 1988 .

[13]  Per Horsrud,et al.  Sand Stresses Around a Wellbore , 1982 .

[14]  Emmanuel M Detournay,et al.  Two-dimensional elastoplastic analysis of a long, cylindrical cavity under non-hydrostatic loading , 1987 .

[15]  C. Fairhurst,et al.  Influence of pore pressure on the deformation behaviour of saturated rocks : 4F, 27R. Proc. 3rd Congress ISRM, Denver, 1974, vol 2 part A, P538–644 , 1976 .

[16]  M. King Hubbert,et al.  Mechanics of Hydraulic Fracturing , 1972 .

[17]  P. Robertson,et al.  Interpretation of undrained self-boring pressuremeter test results incorporating unloading , 1992 .

[18]  Amos Nur,et al.  An exact effective stress law for elastic deformation of rock with fluids , 1971 .

[19]  Guy T. Houlsby,et al.  Analysis of the cone pressuremeter test in clay , 1988 .

[20]  A. L. Florence,et al.  Axisymmetric compression of a Mohr–Coulomb medium around a circular hole , 1978 .