2019
DOI: 10.2136/vzj2019.10.0113
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Current Insights into Nonuniform Flow across Scales, Processes, and Applications

Abstract: Nonuniform flow has proven to be the rule rather than the exception in nearly all soils. Computational and technological advancements are promising for nonuniform flow. They allow improved visualization and characterization of structures across scales. We need to translate apparent complexity of geosystems into reproducible outcomes. Those outcomes must be of generalizable applicability in flow and transport research.

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Cited by 7 publications
(6 citation statements)
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“…Water recharge processes can be divided into slow uniform movements of water through smaller pores, and fast non-uniform water movement along larger and more active pathways referred to as preferential flow. 101 Preferential flow can contribute to the rapid transport of contaminants from the soil surface into receiving streams, bypassing the filtering capacity of the soil. 102 Developing appropriate approaches to study preferential water movement is a prerequisite to understanding groundwater recharge processes.…”
Section: Soil Water and Hydrologymentioning
confidence: 99%
“…Water recharge processes can be divided into slow uniform movements of water through smaller pores, and fast non-uniform water movement along larger and more active pathways referred to as preferential flow. 101 Preferential flow can contribute to the rapid transport of contaminants from the soil surface into receiving streams, bypassing the filtering capacity of the soil. 102 Developing appropriate approaches to study preferential water movement is a prerequisite to understanding groundwater recharge processes.…”
Section: Soil Water and Hydrologymentioning
confidence: 99%
“…The discussion has gradually moved from macropore flow to preferential flow that summarizes all the flows in unsaturated porous media not obeying the Richards equation [4]. Numerous reviews on macropore flows, preferential flows, non-equilibrium flows, and non-uniform flows in permeable media appear periodically, and only the latest are here referenced [5,27].…”
Section: Dual Porosity Approachesmentioning
confidence: 99%
“…Infiltration models typically include the assumptions that the sampled porous medium is rigid, homogeneous, isotropic, and has a uniform water content before the experiment (Angulo-Jaramillo et al, 2016). However, these conditions are more the exception than the rule, and for structured and other heterogeneous soils, water generally moves non-uniformly, leading to spatially irregular wetting of the soil profile (Abou Najm et al, 2019;Gerke, 2006). Different types of soil heterogeneity (e.g., water-repellent or sealed soils, multiporosity and multi-permeability systems, porous media possessing regions with distinct particle types or sizes) can induce non-uniform and preferential flow phenomena (e.g., Lassabatere et al, 2019).…”
Section: Introductionmentioning
confidence: 99%