Hostname: page-component-cb9f654ff-5jtmz Total loading time: 0 Render date: 2025-08-29T11:58:54.708Z Has data issue: false hasContentIssue false

Gas Migration in MX80 Buffer Bentonite

Published online by Cambridge University Press:  03 September 2012

S. T. Horseman
Affiliation:
Fluid Processes Group, British Geological Survey, Nottingham, NG12 5GG, UK
J. F. Harrington
Affiliation:
Fluid Processes Group, British Geological Survey, Nottingham, NG12 5GG, UK
P. Sellin
Affiliation:
Svensk Kärbränslehantering AB (SKB), PO Box 5864, S102 48 Stockholm, Sweden.
Get access

Abstract

Controlled flow-rate gas injection experiments have been performed onpre-compacted samples of KBS-3 specification M×801 bufferbentonite using helium as a safe replacement for hydrogen. By simultaneouslyapplying a confining pressure and backpressure, specimens wereisotropically-consolidated and fully water-saturated under pre-determinedeffective stress conditions, before injecting gas using a syringe pump.Ingoing and outgoing gas fluxes were monitored. All tests exhibited aconspicuous threshold pressure for breakthrough, somewhat larger than thesum of the swelling pressure and the backpressure. All tests showed apost-peak negative transient leading to steady-state gas flow. Using astepped history of flow rate, the flow law was shown to be nonlinear. Withthe injection pump stationary (i.e. zero applied flow rate), gas pressuredeclined with time to a finite value. When gas flow was reestablished, thethreshold value for gas breakthrough was found to be significantly lowerthan in virgin clay. There is strong evidence to suggest that the capillarypressure for the penetration of interparticle pore space of buffer bentoniteis of such a magnitude that normal two-phase flow is impossible. Gas entryand breakthrough is therefore accompanied by the development of microcrackswhich propagate through the clay from gas source to sink. The experimentssuggest that these pathways open under high gas pressure conditions andpartially close if gas pressure falls, providing a possible explanation ofthe nonlinearity of the flow law.

Information

Type
Research Article
Copyright
Copyright © Materials Research Society 1997

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.)

Article purchase

Temporarily unavailable

References

REFERENCES

Horseman, S., Higgo, J., Alexander, J. and Harrington, J.. Water, gas and solute movement in argillaceous media. Prepared by BGS for NEA SEDE Working Group on Measurement and Physical Understanding of Groundwater Flow Through Argillaceous Media. Rept. No. CC-96/1, OECD Nuclear Energy Agency, Paris, 1996, 290 pp, 26 figs.Google Scholar
Sen, M., Horseman, S. and Harrington, J.. Further studies on the movement of gas and water in an overconsolidatedclay. EU MEGAS Project Phase 2. Fluid Processes Group, British Geological Survey, Technical Rept. No. WE/96/8, 1996.Google Scholar