Reflection on Jarvis (2007), “Review of non‐equilibrium water flow and solute transport in soil macropores: Principles, controlling factors and consequences for water quality”. European Journal of Soil Science, 58, 523–546

Jarvis, Nicholas

doi:10.1111/ejss.12914

European J Soil Science

2020

DOI: 10.1111/ejss.12914

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Reflection on Jarvis (2007), “Review of non‐equilibrium water flow and solute transport in soil macropores: Principles, controlling factors and consequences for water quality”. European Journal of Soil Science, 58, 523–546

Nicholas Jarvis

Abstract: How to cite this article: Jarvis N. Reflection on Jarvis (2007), "Review of non-equilibrium water flow and solute transport in soil macropores: Principles, controlling factors and consequences for water quality".

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Soil pores in preferential flow terminology and permeability equations

Manns,

Jiang,

Parkin

2024

Vadose Zone Journal

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Linkages between the micro‐scale of soil water and landscape scale of hydrological data could be improved with the analysis of soil factors in preferential flow rates. This rearrangement of the terminology on soil pore size from published literature focused on the relationship between aggregate and pore size. In the range of pore size relevant to water flow (>0.005 mm), a 2:1 ratio of aggregate to pore diameter approximated the mean of proposed pore size categories. Major functional change points in soil pore size were identified where water becomes mobile in soil (0.005 mm), where preferential flow among aggregate surfaces begins (0.3 mm), and where water flows without soil interaction (bypass flow ∼1.0 mm). A number of published equations supported the application of soil pore size in permeability estimation for modeling hydraulic conductivity. Common understanding of soil pore terminology would support water flow estimation from soil to landscape scales.

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Soil pores in preferential flow terminology and permeability equations

Manns,

Jiang,

Parkin

2024

Vadose Zone Journal

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Solute Transport with Non-Equilibrium Adsorption In A Non-Homogeneous Porous Medium

Mustafokulov

Dzhiyanov

et al. 2022

Wseas Transactions on Fluid Mechanics

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In this paper, a solute transport problem with non-equilibrium adsorption in a non-homogeneous porous medium consisting of two zones, one with high permeability (mobile zone) and another one with low permeability (immobile liquid zone) are considered. In the mobile zone, there are two zones in both of which adsorption of solute with reversible kinetics occurs. The results of this approach are compared with known, traditional approaches. It is shown that this method of modeling the process gives a satisfactory result. By appropriate selection of the parameters of the source term, one can obtain results close to those of the well-known bicontinuum approach.

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Reflection on Jarvis (2007), “Review of non‐equilibrium water flow and solute transport in soil macropores: Principles, controlling factors and consequences for water quality”. European Journal of Soil Science, 58, 523–546

Abstract: How to cite this article: Jarvis N. Reflection on Jarvis (2007), "Review of non-equilibrium water flow and solute transport in soil macropores: Principles, controlling factors and consequences for water quality".

Cited by 2 publications

References 55 publications

Soil pores in preferential flow terminology and permeability equations

Soil pores in preferential flow terminology and permeability equations

Solute Transport with Non-Equilibrium Adsorption In A Non-Homogeneous Porous Medium

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