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Permeability
Permeability-Best-Of.mp3
Permeability-Best-Of.mp4
Permeability.mp3
Permeability.mp4
Permeability-Animation-1.mp4
Permeability-Animation-2.mp4
Permeability-Best-Of.mp4
[Intro]
Porosity
(Versus permeability)
Fluid reality
[Verse 1]
Fluid dynamic
(Nature’s music)
The ebb and flow
(Oh, you know, you know)
[Bridge]
What’s our ability
Porosity
(Versus permeability)
[Chorus]
Fluid reality
(Pressure gradient)
Physical geometry
(Capacity to transmit)
[Verse 2]
Is man at our prime
(Of anthropic crime)
It’s an empirical law
(After all….)
[Bridge]
What’s our ability
Porosity
(Versus permeability)
[Chorus]
Fluid reality
(Pressure gradient)
Physical geometry
(Capacity to transmit)
[Bridge]
What’s our ability
Porosity
(Versus permeability)
[Outro]
Fluid reality
(Pressure gradient)
Physical geometry
(Capacity to transmit)
Can the knowledge flow
(Can the knowledge go)
… flow and go to know
(Seriously…)
What’s our permeability?
ABOUT THE SCIENCE
Porosity vs. Permeability: These two terms are related but distinct.
* Porosity is the amount of empty space available.
* Permeability is a measure of how easily fluids can flow through those spaces (e.g., clay can be highly porous, but its tiny, disconnected pores give it very low permeability, trapping water).
The physics of permeability center on fluid dynamics and the physical geometry of the material’s pore spaces. It is an intrinsic property that describes a porous material’s capacity to transmit a fluid under the influence of a pressure gradient. The fundamental governing principle for fluid flow through porous media at low velocities is Darcy’s Law.
Darcy’s Law: The Core Physics Henry Darcy, a French engineer, formulated an empirical law in 1856 which established the relationship between flow rate and pressure drop through a sand filter. Darcy’s Law states that the volumetric flow rate (Q) is proportional to the pressure difference (Delta P) and the cross-sectional area (A), and inversely proportional to the fluid’s dynamic viscosity (mu) and the length of the flow path (L).
From the album “Porous“
View all episodes
By Permeability-Best-Of.mp3
Permeability-Best-Of.mp4
Permeability.mp3
Permeability.mp4
Permeability-Animation-1.mp4
Permeability-Animation-2.mp4
Permeability-Best-Of.mp4
[Intro]
Porosity
(Versus permeability)
Fluid reality
[Verse 1]
Fluid dynamic
(Nature’s music)
The ebb and flow
(Oh, you know, you know)
[Bridge]
What’s our ability
Porosity
(Versus permeability)
[Chorus]
Fluid reality
(Pressure gradient)
Physical geometry
(Capacity to transmit)
[Verse 2]
Is man at our prime
(Of anthropic crime)
It’s an empirical law
(After all….)
[Bridge]
What’s our ability
Porosity
(Versus permeability)
[Chorus]
Fluid reality
(Pressure gradient)
Physical geometry
(Capacity to transmit)
[Bridge]
What’s our ability
Porosity
(Versus permeability)
[Outro]
Fluid reality
(Pressure gradient)
Physical geometry
(Capacity to transmit)
Can the knowledge flow
(Can the knowledge go)
… flow and go to know
(Seriously…)
What’s our permeability?
ABOUT THE SCIENCE
Porosity vs. Permeability: These two terms are related but distinct.
* Porosity is the amount of empty space available.
* Permeability is a measure of how easily fluids can flow through those spaces (e.g., clay can be highly porous, but its tiny, disconnected pores give it very low permeability, trapping water).
The physics of permeability center on fluid dynamics and the physical geometry of the material’s pore spaces. It is an intrinsic property that describes a porous material’s capacity to transmit a fluid under the influence of a pressure gradient. The fundamental governing principle for fluid flow through porous media at low velocities is Darcy’s Law.
Darcy’s Law: The Core Physics Henry Darcy, a French engineer, formulated an empirical law in 1856 which established the relationship between flow rate and pressure drop through a sand filter. Darcy’s Law states that the volumetric flow rate (Q) is proportional to the pressure difference (Delta P) and the cross-sectional area (A), and inversely proportional to the fluid’s dynamic viscosity (mu) and the length of the flow path (L).
From the album “Porous“