2009
DOI: 10.1007/s10596-009-9140-3
|View full text |Cite
|
Sign up to set email alerts
|

Numerical modeling of coupled fluid flow and thermal and reactive biogeochemical transport in porous and fractured media

Abstract: Subsurface contamination problems of metals and radionuclides are ubiquitous. Metals and radionuclides may exist in the solute phase or may be bound to soil particles and interstitial portions of the geologic matrix. Accurate tools to reliably predict the migration and transformation of these metals and radionuclides in the subsurface environment enhance the ability of environmental scientists, engineers, and decision makers to analyze their impact and to evaluate the efficacy of alternative remediation techni… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
2
1

Citation Types

0
13
0

Year Published

2011
2011
2021
2021

Publication Types

Select...
4
2
1

Relationship

2
5

Authors

Journals

citations
Cited by 27 publications
(13 citation statements)
references
References 38 publications
0
13
0
Order By: Relevance
“…This effectively decouples the transport of components and kinetic variables from those for the rates of equilibrium reactions. As a result, it facilitates the iterative approach between a much-reduced number of partial differential equations of component and kinetic-variable transport and nonlinear algebraic equations that implicitly define the rates of equilibrium reactions [168,170,171]. In the geomechanics module, the media are treated as consisting of nonlinear viscous-elastic materials.…”
Section: Hydrogeochemmentioning
confidence: 99%
See 1 more Smart Citation
“…This effectively decouples the transport of components and kinetic variables from those for the rates of equilibrium reactions. As a result, it facilitates the iterative approach between a much-reduced number of partial differential equations of component and kinetic-variable transport and nonlinear algebraic equations that implicitly define the rates of equilibrium reactions [168,170,171]. In the geomechanics module, the media are treated as consisting of nonlinear viscous-elastic materials.…”
Section: Hydrogeochemmentioning
confidence: 99%
“…Starting with a reaction network of N reactions involving M species, each reaction can involve any number of species, one can write M species transport equations based on the principle of chemical kinetics [172]. Performing GaussJordan reduction of the reaction network [173][174][175], one obtains a system of M transport equations for M reaction extents, each of which is a linear combination of the M species concentrations [170,171]. A reaction extent is called a component when there is no reaction term appearing in its transport equation.…”
Section: Hydrogeochemmentioning
confidence: 99%
“…(17), depending on computation power and how dynamic the system is. Direct coupling with the reactive transport simulator HYDROGEOCHEM (66) was used in here. In this model, only the TEAP reaction of iron reduction was replaced with the in silico model of G. metallireducens.…”
Section: Methodsmentioning
confidence: 99%
“…The chemical system is a complex reaction network involving dissolution of the sorbing sites to form aqueous species, surface ionization of a solid and changes in sorption equilibria due to thermal transport (Example 16). In addition to the sample problems in the manuals, two recent review papers (Yeh et al 2009(Yeh et al , 2011 provide examples of applications of HYDROGEOCHEM to chemical scenarios relevant to the waste IPSC.…”
Section: Demonstrated Applicationsmentioning
confidence: 99%
“…Descriptions of such simulations are summarized in Yeh et al (2009Yeh et al ( , 2011 and described in more detail in Scheibe et al (2006) and Fang et al (2009).…”
Section: Demonstrated Applicationsmentioning
confidence: 99%