2005
DOI: 10.1016/j.advwatres.2005.01.003
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Advantages of using adaptive remeshing and parallel processing for modelling biodegradation in groundwater

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Cited by 12 publications
(7 citation statements)
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“…1 and 2), inclusion of aqueous speciation and mineral solubility equilibria (Table S2 in the Supporting Information), and parameter values in specific rate equations (Table S3). The same data set (), used to test the previous model ( , ), was used for calibration of the current model. Key changes to the previous model included increased model complexity in terms of (1) conceptualization and mathematical representation of the physical heterogeneity of the permeability field, (2) full 2-D simulation of reactive transport, also including microbial acclimatization in simple form, (3) inclusion of fermentation processes with subsequent respiration of H 2 (aq) as TEAPs, and (4) inclusion of Fe 2+ and Mn 2+ adsorption as surface complexation reactions, instead of considering the mineral phases FeCO 3 (s) and MnCO 3 (s).…”
Section: Modeling Methodsmentioning
confidence: 99%
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“…1 and 2), inclusion of aqueous speciation and mineral solubility equilibria (Table S2 in the Supporting Information), and parameter values in specific rate equations (Table S3). The same data set (), used to test the previous model ( , ), was used for calibration of the current model. Key changes to the previous model included increased model complexity in terms of (1) conceptualization and mathematical representation of the physical heterogeneity of the permeability field, (2) full 2-D simulation of reactive transport, also including microbial acclimatization in simple form, (3) inclusion of fermentation processes with subsequent respiration of H 2 (aq) as TEAPs, and (4) inclusion of Fe 2+ and Mn 2+ adsorption as surface complexation reactions, instead of considering the mineral phases FeCO 3 (s) and MnCO 3 (s).…”
Section: Modeling Methodsmentioning
confidence: 99%
“…1 and 2), inclusion of aqueous speciation and mineral solubility equilibria (Table S2 in the Supporting Information), and parameter values in specific rate equations (Table S3). The same data set (17), used to test the previous model (8,22), was used for calibration of the current model. Key changes to the previous model included increased model complexity in terms of (1) 16) point out that limited computational capacity still may render proper numerical simulation of natural attenuation within plumes impossible for codes based on conventional methods.…”
Section: Modeling Methodsmentioning
confidence: 99%
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“…Their results were similar to those from a sophisticated and fully coupled multi-phase, multi-constituent numerical simulator. Watson et al (2005) reported using unstructured grids to simulate fieldscale reactive biogeochemistry including Monod kinetics, NAPL dissolution, mineral precipitation/dissolution, and ion exchange. They used parallel processing and locally adaptive remeshing depending on the relatively reactive zones around the fringes and less reactive zones in the core to reduce the runtime.…”
Section: Introductionmentioning
confidence: 99%
“…Parallel computation provides an alternative that may facilitate the simulation of fine grids at large scales. Although parallel computation strategies have been used in ground water modeling and ground water remediation optimization (e.g., Ashby et al 1999;Garrett et al 1999;Payne et al 2003;Sinha and Minsker 2007;Wai and Lu, 2000;Watson et al 2005), parallel computational environments have not been applied directly to solve flow and transport problems in large fine-grid domains. The recent development of the multiple-grid method provides an efficient platform for extending existing parallel computation strategies to simulation domains that require fine discretization throughout the domain.…”
Section: Introductionmentioning
confidence: 99%