Particle size dynamics in abrading pebble populations

<p>Abrasion of sedimentary particles in fluvial and eolian environments is widely associated with collisions encountered by the particle. Although the physics of abrasion is complex, purely geometric models recover the course of mass and shape evolution of individual particles in low- and midd...

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Main Authors: A. A. Sipos, G. Domokos, J. Török
Format: Article
Language:English
Published: Copernicus Publications 2021-03-01
Series:Earth Surface Dynamics
Online Access:https://esurf.copernicus.org/articles/9/235/2021/esurf-9-235-2021.pdf
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spelling doaj-d200925fd78e41b1b8256e212c369f752021-03-26T05:20:13ZengCopernicus PublicationsEarth Surface Dynamics2196-63112196-632X2021-03-01923525110.5194/esurf-9-235-2021Particle size dynamics in abrading pebble populationsA. A. Sipos0A. A. Sipos1G. Domokos2G. Domokos3J. Török4J. Török5MTA-BME Morphodynamics Research Group, Budapest University of Technology and Economics, Műegyetem rakpart 1–3, Budapest, HungaryDepartment of Mechanics, Materials and Structures, Budapest University of Technology and Economics, Műegyetem rakpart 1–3, Budapest, HungaryMTA-BME Morphodynamics Research Group, Budapest University of Technology and Economics, Műegyetem rakpart 1–3, Budapest, HungaryDepartment of Mechanics, Materials and Structures, Budapest University of Technology and Economics, Műegyetem rakpart 1–3, Budapest, HungaryMTA-BME Morphodynamics Research Group, Budapest University of Technology and Economics, Műegyetem rakpart 1–3, Budapest, HungaryDepartment of Theoretical Physics, Budapest University of Technology and Economics, Budafoki út 8, Budapest, Hungary<p>Abrasion of sedimentary particles in fluvial and eolian environments is widely associated with collisions encountered by the particle. Although the physics of abrasion is complex, purely geometric models recover the course of mass and shape evolution of individual particles in low- and middle-energy environments (in the absence of fragmentation) remarkably well. In this paper, we introduce the first model for the collision-driven collective mass evolution of sedimentary particles. The model utilizes results of the individual, geometric abrasion theory as a <i>collision kernel</i>; following techniques adopted in the statistical theory of coagulation and fragmentation, the corresponding Fokker–Planck equation is derived. Our model uncovers a startling fundamental feature of collective particle size dynamics: collisional abrasion may, depending on the energy level, either focus size distributions, thus enhancing the effects of size-selective transport, or it may act in the opposite direction by dispersing the distribution.</p>https://esurf.copernicus.org/articles/9/235/2021/esurf-9-235-2021.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. A. Sipos
A. A. Sipos
G. Domokos
G. Domokos
J. Török
J. Török
spellingShingle A. A. Sipos
A. A. Sipos
G. Domokos
G. Domokos
J. Török
J. Török
Particle size dynamics in abrading pebble populations
Earth Surface Dynamics
author_facet A. A. Sipos
A. A. Sipos
G. Domokos
G. Domokos
J. Török
J. Török
author_sort A. A. Sipos
title Particle size dynamics in abrading pebble populations
title_short Particle size dynamics in abrading pebble populations
title_full Particle size dynamics in abrading pebble populations
title_fullStr Particle size dynamics in abrading pebble populations
title_full_unstemmed Particle size dynamics in abrading pebble populations
title_sort particle size dynamics in abrading pebble populations
publisher Copernicus Publications
series Earth Surface Dynamics
issn 2196-6311
2196-632X
publishDate 2021-03-01
description <p>Abrasion of sedimentary particles in fluvial and eolian environments is widely associated with collisions encountered by the particle. Although the physics of abrasion is complex, purely geometric models recover the course of mass and shape evolution of individual particles in low- and middle-energy environments (in the absence of fragmentation) remarkably well. In this paper, we introduce the first model for the collision-driven collective mass evolution of sedimentary particles. The model utilizes results of the individual, geometric abrasion theory as a <i>collision kernel</i>; following techniques adopted in the statistical theory of coagulation and fragmentation, the corresponding Fokker–Planck equation is derived. Our model uncovers a startling fundamental feature of collective particle size dynamics: collisional abrasion may, depending on the energy level, either focus size distributions, thus enhancing the effects of size-selective transport, or it may act in the opposite direction by dispersing the distribution.</p>
url https://esurf.copernicus.org/articles/9/235/2021/esurf-9-235-2021.pdf
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