2022
DOI: 10.1061/(asce)em.1943-7889.0002153
|View full text |Cite
|
Sign up to set email alerts
|

A Perspective on Darcy’s Law across the Scales: From Physical Foundations to Particulate Mechanics

Abstract: This paper puts forward a perspective or opinion that we can demonstrate Darcy's law is valid at any scale where fluid can be modelled/analyzed as a continuum. Darcy's law describes the flow of a fluid through a porous medium by a linear relationship between the flow rate and the pore pressure gradient through the permeability tensor. We show that such a linear relationship can be established at any scale, so long as the permeability tensor is expressed as a function of adequate parameters that describe the po… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

0
3
0

Year Published

2023
2023
2024
2024

Publication Types

Select...
6

Relationship

0
6

Authors

Journals

citations
Cited by 6 publications
(3 citation statements)
references
References 77 publications
0
3
0
Order By: Relevance
“…According to Darcy's law [61], the head loss of the vertical infiltration flow is described using the filtration coefficient k f (i), which varies along y i in a stepwise manner, according to the layers:…”
Section: Hydrological Modelmentioning
confidence: 99%
“…According to Darcy's law [61], the head loss of the vertical infiltration flow is described using the filtration coefficient k f (i), which varies along y i in a stepwise manner, according to the layers:…”
Section: Hydrological Modelmentioning
confidence: 99%
“…Darcy's pioneering experiments on fluid flow through porous media laid the groundwork for comprehending fluid mechanics and hydrogeology [22]. Darcy's investigations unveiled a fundamental relationship linking flow velocity, head loss, and the length of the flow path [23]. The observed direct proportionality between flow velocity and head loss elucidates the energy loss sustained by the fluid as it traverses the porous medium.…”
Section: Introductionmentioning
confidence: 99%
“…where q is the the flux, k represents the absolute permeability of the porous domain, µ is the dynamic viscosity of the liquid, and dp/dx 1 denotes the pressure gradient. The above equation describes a linear relationship between the velocity field and the pressure gradient [10,11] and it is only valid for very low velocities or at low Reynolds numbers Re < 10. Nevertheless, in the case of relatively fast flow (Re > 10) or relatively high Knudsen numbers (Kn > 0.1) [12,13], Darcy's linear relation between the velocity and pressure drop is no longer valid; therefore, Equation ( 1) is not enough to describe this flow behavior, which is called non-Darcian flow, specifically in fractal objects, which present a nonlinear relationship between the flow velocity and hydraulic gradient (for a short review, see [14]).…”
Section: Introductionmentioning
confidence: 99%