The transport of reactive solutes in the subsurface is influenced by a variety of physical and chemical processes. The processes are characteristically heterogeneous and often operate simultaneously at different temporal and spatial scales. In modeling reactive solute transport different models take different approaches, dependent on the scale of the system and the objective of the study. Two major approaches have been used to incorporate heterogeneous rate-limited mass transfer into mathematical models for solute transport. One focuses on processes operative at the microscopic scale and associated grain-scale heterogeneity, while the other stresses the macroscopic variability of the medium and the field-scale behavior of solute transport. ...
We characterize the role of preferential pathways in controlling the dynamics of bimolecular reactiv...
We characterize the role of preferential pathways in controlling the dynamics of bimolecular reactiv...
The fate of reactive solutes in groundwater is largely determined by mixing, since dilution and reac...
Physical and chemical heterogeneities have a large impact on reactive transport in porous media. Exa...
Physical and chemical heterogeneities have a large impact on reactive transport in porous media. Exa...
Physical and chemical heterogeneities have a large impact on reactive transport in porous media. Exa...
Physical and chemical heterogeneities have a large impact on reactive transport in porous media. Exa...
Understanding and predicting mass transfer coupled with solute transport in permeable media is centr...
Reactive Transport Models (RTMs) provide quantitative tools to analyze the interaction between trans...
The correct characterization of the effective reactive transport dynamics is an important issue for ...
We analyze the impact of physical and chemical heterogeneity on solute travel time to a pumping well...
We analyze the impact of physical and chemical heterogeneity on solute travel time to a pumping well...
We analyze the impact of physical and chemical heterogeneity on solute travel time to a pumping well...
<p>Transport and spreading behaviour of reactive solutes in heterogeneous porous formations is...
Transport and spreading behaviour of reactive solutes in heterogeneous porous formations is consider...
We characterize the role of preferential pathways in controlling the dynamics of bimolecular reactiv...
We characterize the role of preferential pathways in controlling the dynamics of bimolecular reactiv...
The fate of reactive solutes in groundwater is largely determined by mixing, since dilution and reac...
Physical and chemical heterogeneities have a large impact on reactive transport in porous media. Exa...
Physical and chemical heterogeneities have a large impact on reactive transport in porous media. Exa...
Physical and chemical heterogeneities have a large impact on reactive transport in porous media. Exa...
Physical and chemical heterogeneities have a large impact on reactive transport in porous media. Exa...
Understanding and predicting mass transfer coupled with solute transport in permeable media is centr...
Reactive Transport Models (RTMs) provide quantitative tools to analyze the interaction between trans...
The correct characterization of the effective reactive transport dynamics is an important issue for ...
We analyze the impact of physical and chemical heterogeneity on solute travel time to a pumping well...
We analyze the impact of physical and chemical heterogeneity on solute travel time to a pumping well...
We analyze the impact of physical and chemical heterogeneity on solute travel time to a pumping well...
<p>Transport and spreading behaviour of reactive solutes in heterogeneous porous formations is...
Transport and spreading behaviour of reactive solutes in heterogeneous porous formations is consider...
We characterize the role of preferential pathways in controlling the dynamics of bimolecular reactiv...
We characterize the role of preferential pathways in controlling the dynamics of bimolecular reactiv...
The fate of reactive solutes in groundwater is largely determined by mixing, since dilution and reac...