Hostname: page-component-78c5997874-v9fdk Total loading time: 0 Render date: 2024-11-05T15:56:46.148Z Has data issue: false hasContentIssue false
  • English
  • Français

A Study of Coupled Thermomechanical, Thermohydrological and Hydromechanical Processes Associated with a Nuclear Waste Repository in a Fractured Rock Medium

Published online by Cambridge University Press:  21 February 2011

C. F. Tsang ,
J. Noorishad  and
J. S. Y. Wang
C. F. Tsang
Affiliation:
Earth Sciences Division, Lawrence Berkeley Laboratory, University of California, Berkeley, California 94720.
J. Noorishad
Affiliation:
Earth Sciences Division, Lawrence Berkeley Laboratory, University of California, Berkeley, California 94720.
J. S. Y. Wang
Affiliation:
Earth Sciences Division, Lawrence Berkeley Laboratory, University of California, Berkeley, California 94720.
Get access

Abstract

It has been recognized that coupled thermomechanical, thermohydrologic, and hydromechanical processes may play an important role in the behavior of the geologic formation around a nuclear waste repository. A numerical code, ROCMAS, was recently developed at Lawrence Berkeley Laboratory to calculate coupled heat transfer, fluid flow, and mechanical deformation in a fractured porous medium. Three scoping studies using this model are described in this paper, with the following preliminary conclusions. The thermomechanical simulations of a fractured rock mass show that the fractures can absorb the thermally induced rock deformations, thus possibly explaining the observed behavior of the granite rocks in the experiment at Stripa, Sweden. The variations in fracture aperture profiles in the hydromechanical simulations indicate that the rigid fracture assumptions used in most uncoupled studies may not be a good representation of fracture behavior. The thermohydromechanical model study reveals that perturbations induced by a heater may close a fracture near the heater borehole and stop the water inflow to the borehole.

Type
Research Article
Information
MRS Online Proceedings Library (OPL) , Volume 15: Symposium D – Scientific Basis for Nuclear Waste Management VI , 1982 , 515
Copyright
Copyright © Materials Research Society 1983

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

[1] Tsang, C. F., A review of state-of-the-art of thermomechanical-hydrochemical modeling of a hard rock repository, Workshop on Thermomechanical-Hydrochemical Modeling for a Hard Rock Waste Repository, Lawrence Berkeley Laboratory Report LBL-11204, July 1980.Google Scholar
[2] Noorishad, J., Ayatollahi, M. S., and Witherspoon, P. A., A finite-element method for coupled stress and fluid flow analysis of fractured rocks, International Journal of Rock Mechanics and Mining Sciences, 19, pp. 185–193 (1982).Google Scholar
[3] Witherspoon, P. A., Tsang, Y. W., Long, J. C. S., and Noorishad, J., New approaches to problems of fluid flow in fracture rock mass, 22nd U. S. Symposium on Rock Mechanics, pp. 1–20 (1981).Google Scholar
[4] Biot, M. A., General theory of three-dimensional consolidation, Journal of Applied Physics, 12, pp. 155–164 (1941).Google Scholar
[5] Witherspoon, P. A., Cook, N. G. W., and Gale, J. E., Geologic storage of radioactive waste: Field studies in Sweden. Science, 211, pp. 894–900 (1981).Google Scholar
[6] Noorishad, J., and Doe, T. W., Numerical simulation of fluid injection into deformable fractures, 23rd U. S. Symposium on Rock Mechanics, pp. 645–654 (1982).Google Scholar