Effective Diffusivity in Porous Media

on . Posted in Geotechnical Engineering

partially saturated soil 4Effective diffusivity in porous media, abbreviated as \( D_e \), is a measure of how quickly a substance can move or diffuse through a porous material, taking into account the complex structure and interconnectedness of the pores within that material.  It's an important concept in various fields, including chemical engineering, hydrogeology, and soil science, where the movement of fluids, gases, or solutes through porous media plays a crucial role. 

In a porous medium, such as soil, rock, or a packed bed of particles, there are multiple pathways and channels through which fluids or particles can move.  These pathways vary in size, shape, and connectivity, making it challenging to describe diffusion using a simple diffusion coefficient as you would in a homogeneous material. Instead, you need to consider the effective diffusivity.  The effective diffusivity is an apparent diffusion coefficient that represents the overall rate of diffusion in a porous medium.  It takes into account the tortuosity (the increased path length due to the convoluted pathways) and the obstruction (blockages or dead-end pores) within the porous structure.

Effective diffusivity is used in various applications, such as predicting the transport of contaminants in groundwater, designing catalytic reactors, understanding gas diffusion in soils, and optimizing the performance of materials in filtration systems.  Accurate determination of effective diffusivity is essential for modeling and engineering processes involving porous media to ensure that the movement of substances is properly understood and controlled.

 

Effective diffusivity in porous media formula

\( D_e =  D \; n \; \delta \;/\; \tau \)     (Effective Diffusivity in Porous Media)

\( D =   D_e \; \tau \;/\;  n \; \delta \)

\( n =   D_e \; \tau \;/\; D \; \delta \)

\( \delta =   D_e \; \tau \;/\; D \; n \)

\( \tau =  D \; n \; \delta \;/\; D_e \)

Symbol English Metric
\( D_e \) = effective diffusivity \(ft^2 \;/\; sec\) \(m^2 \;/\; s\)
\( D \) = diffusion coefficient in gas or liquid filling the pores \(ft^2 \;/\; sec\) \(m^2 \;/\; s\)
\( n \) = porosity available for transportation \(dimensionless\)
\( \delta \)  (Greek symbol delta) = constrictivity \(dimensionless\)
\( \tau \)  (Greek symbol tau) = tortuosity \(dimensionless\)

 

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Tags: Soil Diffusion