Multiphase flow and underpressured shale at the Bruce nuclear site, Ontario, Canada

Geological Society, London, Special Publications
By:  and 



Hydraulic testing has revealed dramatic underpressures in Paleozoic shales and carbonates at the Bruce nuclear site in Ontario. Although evidence from both laboratory and field studies suggests that a small amount of gas-phase methane could be present in the shale, previous studies examining causal linkages between the gas phase and the underpressure have been inconclusive. To better elucidate processes in such a system, we used a highly simplified 1D representation of the site to test, by using iTOUGH2-EOS7C, the effects of various factors on the evolution of gas-phase methane and pressures within the system. Heterogeneity was represented by three stratigraphic regions with slightly different capillary pressure characteristics and, in one case, three thin distinct zones with very different characteristics. Underpressure occurred only when gas pressures set as an initial condition required it, and even in this case it was geologically short-lived. We conclude that the presence of multiple fluid phases is unlikely to explain the underpressure at the site; we suggest that the influence of gas-phase methane on porewater flow is minimal. This is consistent with prior conceptualizations of the underpressured section as a thick aquiclude, in which solute transport occurs extremely slowly, bounded by aquifers of significantly higher permeability.

Publication type Article
Publication Subtype Journal Article
Title Multiphase flow and underpressured shale at the Bruce nuclear site, Ontario, Canada
Series title Geological Society, London, Special Publications
DOI 10.1144/SP482.5
Volume 482
Year Published 2018
Language English
Publisher Geological Society of London
Contributing office(s) National Research Program - Eastern Branch
Description 14 p.
First page 101
Last page 114
Country Canada
State Ontario
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