2012
DOI: 10.1007/s12665-012-1674-3
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Estimating effective rates of convective mixing from commercial-scale injection

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Cited by 23 publications
(19 citation statements)
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“…[], who showed that at the Sleipner site geochemical changes to reservoir parameers such as porosity and permeability are unimportant. Mykkeltvedt and Nordbotten [] and Cavanagh [] simulated dissolution of CO 2 into the brine, with the former using an enhanced vertical equilibrium model that includes capillary trapping and dissolution [see Gasda et al ., ] and the latter using a standard simulator. Both show significant dissolution rates, with Mykkeltvedt and Nordbotten [] showing that the theoretical effective convective mixing rates are consistent with the gravity measurements by Alnes et al .…”
Section: Practical Models and Their Applicationsmentioning
confidence: 99%
See 1 more Smart Citation
“…[], who showed that at the Sleipner site geochemical changes to reservoir parameers such as porosity and permeability are unimportant. Mykkeltvedt and Nordbotten [] and Cavanagh [] simulated dissolution of CO 2 into the brine, with the former using an enhanced vertical equilibrium model that includes capillary trapping and dissolution [see Gasda et al ., ] and the latter using a standard simulator. Both show significant dissolution rates, with Mykkeltvedt and Nordbotten [] showing that the theoretical effective convective mixing rates are consistent with the gravity measurements by Alnes et al .…”
Section: Practical Models and Their Applicationsmentioning
confidence: 99%
“…Mykkeltvedt and Nordbotten [] and Cavanagh [] simulated dissolution of CO 2 into the brine, with the former using an enhanced vertical equilibrium model that includes capillary trapping and dissolution [see Gasda et al ., ] and the latter using a standard simulator. Both show significant dissolution rates, with Mykkeltvedt and Nordbotten [] showing that the theoretical effective convective mixing rates are consistent with the gravity measurements by Alnes et al . [] which indicate an upscaled dissolution rate of up to 1.8% per year, while Cavanagh [] simulated around 10% dissolved mass after 12 years of injection.…”
Section: Practical Models and Their Applicationsmentioning
confidence: 99%
“…Early studies focused on VE models with a sharpinterface assumption [24][25][26], and models that only account for the basic effects of buoyant migration were successfully used to simulate long-term migration in the Utsira [27] and Johansen [28] aquifers. Later, the class of VE models has been extended to incorporate most of the flow effects that are pertinent to large-scale migration, including compressibility [29], convective dissolution [30,31], capillary fringe [32], small-scale caprock topography variations [33][34][35], various hysteretic effects [36][37][38], multiple geological layers [39,40], and heat transfer [41]. In particular, several studies show that vertical equilibrium simulations compare well with 3D simulators on case studies of the Johansen aquifer [42] and the 9 th layer of the Sleipner injection [27,43].…”
Section: Introductionmentioning
confidence: 99%
“…Similarly, it is essential that efforts continue to incorporate fundamental insights into field-scale modelling (e.g. Mykkeltvedt & Nordbotten 2012), and to benchmark models such as Hewitt et al's against field observations. Nevertheless, the encouraging agreement between detailed numerical simulations and the box-model predictions illustrates the ability of physically informed asymptotic descriptions to capture the behaviour of such complex flows.…”
Section: Futurementioning
confidence: 99%