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Modelling anomalous diffusion in semi-infinite disordered systems and porous media
by
Berkowitz, Brian
, Metzler, Ralf
, Rajyaguru, Ashish
in
anomalous diffusion
/ Bias
/ Boundary conditions
/ breakthrough curves
/ constant boundary concentration
/ Diffusion
/ Experiments
/ Particle tracking
/ Physics
/ Porous materials
/ Porous media
/ Random variables
/ Random walk
/ Semiconductors
/ System effectiveness
/ Tracer particles
2022
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Modelling anomalous diffusion in semi-infinite disordered systems and porous media
by
Berkowitz, Brian
, Metzler, Ralf
, Rajyaguru, Ashish
in
anomalous diffusion
/ Bias
/ Boundary conditions
/ breakthrough curves
/ constant boundary concentration
/ Diffusion
/ Experiments
/ Particle tracking
/ Physics
/ Porous materials
/ Porous media
/ Random variables
/ Random walk
/ Semiconductors
/ System effectiveness
/ Tracer particles
2022
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Do you wish to request the book?
Modelling anomalous diffusion in semi-infinite disordered systems and porous media
by
Berkowitz, Brian
, Metzler, Ralf
, Rajyaguru, Ashish
in
anomalous diffusion
/ Bias
/ Boundary conditions
/ breakthrough curves
/ constant boundary concentration
/ Diffusion
/ Experiments
/ Particle tracking
/ Physics
/ Porous materials
/ Porous media
/ Random variables
/ Random walk
/ Semiconductors
/ System effectiveness
/ Tracer particles
2022
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Modelling anomalous diffusion in semi-infinite disordered systems and porous media
Journal Article
Modelling anomalous diffusion in semi-infinite disordered systems and porous media
2022
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Overview
For an effectively one-dimensional, semi-infinite disordered system connected to a reservoir of tracer particles kept at constant concentration, we provide the dynamics of the concentration profile. Technically, we start with the Montroll–Weiss equation of a continuous time random walk with a scale-free waiting time density. From this we pass to a formulation in terms of the fractional diffusion equation for the concentration profile C ( x , t ) in a semi-infinite space for the boundary condition C ( 0 , t ) = C 0 , using a subordination approach. From this we deduce the tracer flux and the so-called breakthrough curve (BTC) at a given distance from the tracer source. In particular, BTCs are routinely measured in geophysical contexts but are also of interest in single-particle tracking experiments. For the ‘residual’ BTCs, given by 1 − P ( x , t ) , we demonstrate a long-time power-law behaviour that can be compared conveniently to experimental measurements. For completeness we also derive expressions for the moments in this constant-concentration boundary condition.
Publisher
IOP Publishing
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