2021
DOI: 10.1016/j.ijrmms.2020.104558
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The large-scale in situ PRACLAY heater test: First observations on the in situ thermo-hydro-mechanical behaviour of Boom Clay

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Cited by 15 publications
(4 citation statements)
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“…[Fig. 1] For deep geological disposal, performance assessment of the host formation focused on isolating the HLW from the biosphere requires that in-situ experiments are complemented by numerical simulations to allow predictions of THM behaviour for extended periods of time (Armand et al, 2017;Chen et al, 2011aChen et al, , 2021De-Bruyn and Labat, 2002;Dizier et al, 2021;François et al, 2009;Selvadurai and Nguyen, 1997), or to allow investigating the effect of host rock degradation due to excavation (Nguyen et al, 2009;Pan et al, 2009;Perras and Diederichs, 2016;Rutqvist et al, 2009a). Mathematical models for such coupled geomechanical systems are often characterized by high dimensionality in which the associated computational cost becomes critical when dealing with inverse problems.…”
Section: Fundingmentioning
confidence: 99%
“…[Fig. 1] For deep geological disposal, performance assessment of the host formation focused on isolating the HLW from the biosphere requires that in-situ experiments are complemented by numerical simulations to allow predictions of THM behaviour for extended periods of time (Armand et al, 2017;Chen et al, 2011aChen et al, , 2021De-Bruyn and Labat, 2002;Dizier et al, 2021;François et al, 2009;Selvadurai and Nguyen, 1997), or to allow investigating the effect of host rock degradation due to excavation (Nguyen et al, 2009;Pan et al, 2009;Perras and Diederichs, 2016;Rutqvist et al, 2009a). Mathematical models for such coupled geomechanical systems are often characterized by high dimensionality in which the associated computational cost becomes critical when dealing with inverse problems.…”
Section: Fundingmentioning
confidence: 99%
“…The above behaviour may potentially alter the permeability of host rock as a result. To investigate the thermal effects on the THM behaviour of the host rock, some underground research laboratories (URL) have been already developing large scale in-situ heating tests, for instance in the HADES URF in Belgium (CER-BERUS, ATLAS and PRACLAY tests) (De Bruyn and Labat, 2002;Dizier et al, 2021), in the Mont Terri URL in Switzerland (HE-D test) (Jobmann and Polster, 2007;Garitte et al, 2017), and in the Meuse/Haute-Marne URL in France (TED, EPT, ALC1604, ALC1605 and CRQ tests) (Conil et al, 2020;Seyedi et al, 2021;Bumbieler et al, 2021;Armand et al, 2017;Narkuniene et al, 2022).…”
Section: Introductionmentioning
confidence: 99%
“…The strategy proposed here takes advantage of the typical scenario for coupled THM problems in geomechanics, where the occurrence of plasticity is restricted to specific regions of small size with respect to the model size [51][52][53]. We divide the full domain into two sub-domains: an elastic region governed by linear THM equations and a region in which we may assume that the (evolving) plastic zone remains restricted spatially throughout the simulation, and which is governed by the nonlinear elasto-plastic constitutive law.…”
mentioning
confidence: 99%