Abstract

This paper presents a linearised version of the Cam-Clay model fully integrated in the scope of the general theory of poroplasticity. The constitutive law which is developed in the scope of the effective plastic stress concept, only contains two plastic parameters (hardening modulus and slope of the critical state line). To be validated, the model is integrated over homogeneous stress paths (hydrostatic, drained triaxial and undrained triaxal) then compared with experimental data issued from conventional laboratory triaxial tests. In the second part, a simplified version of the model is applied to the wellbore boundary problem (vertical well) in an axisymmetric horizontal stress field and under undrained conditions. Given the linearity of the constitutive law and the a priori knowledge of the shape of the plastic region, the solution (stress, strain and pore pressure) is fully analytical. The solution shows that for an overconsolidated material (overconsolidation degree less than 2) the hoop stress is strongly relaxed in the plastic zone. The higher the compressibility of the saturating fluid, the larger the relaxation of the hoop stress. In terms of stability, the more compressible the fluid saturating the porous medium is, the more stable the well will be. Finally the larger the overconsolidation ratio is, the less stable the well will be.

Highlights

  • The propping of underground cavities is one of the most basic geotechnical problem in mining engineering and in civil engineering

  • In the case of an incompressible fluid, the undrained path corresponds to an isochore transformation: dε kk

  • The undrained path is plastic contractant for a normally consolidated material, elastic, contractant plastic in the case of an overconsolidated material

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Summary

INTRODUCTION

The propping of underground cavities is one of the most basic geotechnical problem in mining engineering (stability of underground galleries) and in civil engineering (tunnelling). From a general view point (Charlez, 1997), deep sedimentary rocks can be classified in damaging/brittle materials (cohesive sandstones and limestones) and poroplastic rocks (claystones, shales and loose sands). Due to their low shear strength, deep poroplastic materials are the most sensitive to stability problems (Veeken et al, 1989; Charlez and Heugas, 1991; Ewy, 1991; Zhou et al, 1996). More widely known under the name “Cam-Clay” it was developed in the mid 1960's by Burland and Roscoe (1968) It was initially written for normally consolidated clay materials from surface, the very realistic physics it integrates allows adapting it to deeper materials. We propose below a linearised version of the Cam-Clay which can be fully integrated in the case of the wellbore boundary problem

LINEARISATION OF THE CAM-CLAY MODEL
Main Hypothesis
Basic Equations
Strain Hardening Law
Integration on Homogeneous Stress Paths
M2 3
THE PLASTIC WELLBORE PROBLEM
Definition of the Problem
40 Rp σθθ 30 σρρ
Critical Instantaneous Pressure
Impact of the Consolidation Degree
CONCLUSION
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