Scaling study of diffusion in dynamic crowded spaces

Abstract We formulate a scaling theory for the long-time diffusive motion in a space occluded by a high density of moving obstacles in dimensions 1, 2 and 3. Our tracers diffuse anomalously over many decades in time, before reaching a diffusive steady state with an effective diffusion constant <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <mml:mrow> <mml:msub> <mml:mi>D</mml:mi> <mml:mrow> <mml:mi>eff</mml:mi> </mml:mrow> </mml:msub> </mml:mrow> </mml:math> , which depends on the obstacle diffusivity and density. The scaling of <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <mml:mrow> <mml:msub> <mml:mi>D</mml:mi> <mml:mrow> <mml:mi>eff</mml:mi> </mml:mrow> </mml:msub> </mml:mrow> </mml:math> , above and below a critical regime, is characterized by two independent critical parameters: the conductivity exponent µ , also found in models with frozen obstacles, and an exponent ψ , which quantifies the effect of obstacle diffusivity.

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Publication Details

Journal
Journal of Physics A Mathematical and Theoretical
Published
2024-10-08
DOI
https://doi.org/10.1088/1751-8121/ad8496
Citations
1
Primary Topic
Landslides and related hazards
Type
article
Field-Weighted Citation Impact
0.71

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article

Scaling study of diffusion in dynamic crowded spaces

Greg Huber, David Yllanes, Henry Bendekgey
1 citations
Journal of Physics A Mathematical and Theoretical
Landslides and related hazards
0.71
article

Scaling study of diffusion in dynamic crowded spaces

Greg Huber, David Yllanes, Henry Bendekgey
article en
1 citations

Abstract

Abstract We formulate a scaling theory for the long-time diffusive motion in a space occluded by a high density of moving obstacles in dimensions 1, 2 and 3. Our tracers diffuse anomalously over many decades in time, before reaching a diffusive steady state with an effective diffusion constant <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <mml:mrow> <mml:msub> <mml:mi>D</mml:mi> <mml:mrow> <mml:mi>eff</mml:mi> </mml:mrow> </mml:msub> </mml:mrow> </mml:math> , which depends on the obstacle diffusivity and density. The scaling of <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <mml:mrow> <mml:msub> <mml:mi>D</mml:mi> <mml:mrow> <mml:mi>eff</mml:mi> </mml:mrow> </mml:msub> </mml:mrow> </mml:math> , above and below a critical regime, is characterized by two independent critical parameters: the conductivity exponent µ , also found in models with frozen obstacles, and an exponent ψ , which quantifies the effect of obstacle diffusivity.

Journal of Physics A Mathematical and TheoreticalVol. 57(44)
University of California, Irvine (US), Universidad de Zaragoza (ES), Fundacion Agencia Aragonesa para la Investigacion y el Desarrollo (ES), Zaragoza Logistics Center (ES), Chan Zuckerberg Initiative (United States) (US), Irvine University (US), Instituto de Biocomputación y Física de Sistemas Complejos
Ministerio de Ciencia, Innovación y Universidades, Universidad de Zaragoza, European Regional Development Fund, Agencia Estatal de Investigación
Openalex Percentile: Top 21%
Landslides and related hazards
0.71
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Scaling study of diffusion in dynamic crowded spaces — Greg Huber, David Yllanes, et al. · Journal of Physics A Mathematical and Theoretical (2024) | TGRS Research Map | TGRS