2006
DOI: 10.1029/2005wr004511
|View full text |Cite
|
Sign up to set email alerts
|

Enhanced mixing and reaction through flow focusing in heterogeneous porous media

Abstract: [1] Transverse dispersion across adjacent streamlines can control the amount of mixing and reaction between one or more contaminants and a limiting substrate along the fringes of groundwater plumes. Streamlines in groundwater converge and diverge in heterogeneous porous media, depending on the permeability distribution. When flow is focused in a high-permeability zone, the distance required for a solute to cross a given number of streamlines decreases, and the time allowed for mixing and reaction is reduced. B… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

11
137
1

Year Published

2011
2011
2016
2016

Publication Types

Select...
10

Relationship

3
7

Authors

Journals

citations
Cited by 144 publications
(149 citation statements)
references
References 31 publications
11
137
1
Order By: Relevance
“…Dense flow lines enhance transverse dispersion (e.g. Werth et al, 2006;Cirpka et al, 2011 ), and the travel distance within the PFF also increases for these cases. Solutes that disperse to the left of the main plume trajectory have a shorter path to exit the PFF and thus, are transversely dispersed less than those that disperse to the right.…”
Section: Discussionmentioning
confidence: 96%
“…Dense flow lines enhance transverse dispersion (e.g. Werth et al, 2006;Cirpka et al, 2011 ), and the travel distance within the PFF also increases for these cases. Solutes that disperse to the left of the main plume trajectory have a shorter path to exit the PFF and thus, are transversely dispersed less than those that disperse to the right.…”
Section: Discussionmentioning
confidence: 96%
“…The fact that dissolution rates are several of orders of magnitude lower when measured in the field than the laboratory reflects a potential scale dependence of reaction kinetics [31]. A number of numerical studies (e.g., [32][33][34][35][36][37][38][39][40]) have also recognized the scaling effects of macroscopic transport and geochemical reaction properties by comparison of continuum and pore-scale models, and attributed such scale dependence to pore-scale heterogeneities. Specifically, Li et al [32] have developed a pore-scale network model to study the scale dependence of geochemical reaction kinetics controlling mineral dissolution and precipitation.…”
Section: Introductionmentioning
confidence: 97%
“…Meanwhile, several recent studies have used part of the data set for demonstration of geophysical forward (Kowalsky et al, 2001) or inverse modeling (Hu et al, 2009), for hydraulic or transport modeling (Maier et al, 2005;Maji et al, 2006;Werth et al, 2006), and for sedimentological analysis (Heinz et al, 2003). The developed dataset is provided as downloadable supplement and may be used in realistic 3D hydrogeological modeling studies.…”
Section: Introductionmentioning
confidence: 99%