Dynamics of Fluids in Porous Media¶
Bear, J. (1972). Dynamics of Fluids in Porous Media. Elsevier.
Cited by¶
2 citations across 2 artifacts.
Each citation links to the sentence it supports in the citing article.
Primes¶
- Permeability
- Darcy's law states the flux arithmetic exactly: volumetric flow \(Q = \frac{k A}{\mu} \cdot \frac{\Delta P}{L}\), where \(k\) is the permeability (the can, a property of the pore geometry alone), \(\Delta P/L\) is the gradient (the want), and \(\mu\) is the fluid viscosity (the cost, the resistance term).
This sourceCanonical text deriving Darcy flow Q = (kA/μ)(ΔP/L) and the role of connected porosity in permeability.
- Darcy's law states the flux arithmetic exactly: volumetric flow \(Q = \frac{k A}{\mu} \cdot \frac{\Delta P}{L}\), where \(k\) is the permeability (the can, a property of the pore geometry alone), \(\Delta P/L\) is the gradient (the want), and \(\mu\) is the fluid viscosity (the cost, the resistance term).
- Porosity
- Earth sciences and hydrology — aquifer storage and groundwater flow, petroleum reservoir capacity, soil water retention, karst formation; porosity sets storage while permeability (connectivity) sets transmissibility, the operative pair.
This sourceFoundational text distinguishing porosity (storage) from permeability (transmissibility) in porous-media flow.
- Earth sciences and hydrology — aquifer storage and groundwater flow, petroleum reservoir capacity, soil water retention, karst formation; porosity sets storage while permeability (connectivity) sets transmissibility, the operative pair.
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