The elements and richness of particle diffusion during sediment transport at small timescales

David Jon Furbish, Siobhan L. Fathel, Mark Schmeeckle, Douglas J. Jerolmack, Rina Schumer

Research output: Contribution to journalArticle

8 Citations (Scopus)

Abstract

The ideas of advection and diffusion of sediment particles are probabilistic constructs that emerge when the Master equation, a precise, probabilistic description of particle conservation, is approximated as a Fokker–Planck equation. The diffusive term approximates nonlocal transport. It ‘looks’ upstream and downstream for variations in particle activity and velocities, whose effects modify the advective term. High-resolution measurements of bedload particle motions indicate that the mean squared displacement of tracer particles, when treated as a virtual plume, primarily reflects a nonlinear increase in the variance in hop distances with increasing travel time, manifest as apparent anomalous diffusion. In contrast, an ensemble calculation of the mean squared displacement involving paired coordinate positions independent of starting time indicates a transition from correlated random walks to normal (Fickian) diffusion. This normal behavior also is reflected in the particle velocity autocorrelation function. Spatial variations in particle entrainment produce a flux from sites of high entrainment toward sites of low entrainment. In the case of rain splash transport, this leads to topographic roughening, where differential rain splash beneath the canopy of a desert shrub contributes to the growth of a soil mound beneath the shrub. With uniform entrainment, rain splash transport, often described as a diffusive process, actually represents an advective particle flux that is proportional to the land surface slope. Particle diffusion during both bedload and rain splash transport involves motions that mostly are patchy, intermittent and rarefied. The probabilistic framework of the Master equation reveals that continuous formulations of the flux and its divergence (the Exner equation) represent statistically expected behavior, analogous to Reynolds-averaged conditions. Key topics meriting clarification include the mechanical basis of particle diffusion, effects of rarefied conditions involving patchy, intermittent motions, and effects of rest times on diffusion of tracer particles and particle-borne substances.

Original languageEnglish (US)
Pages (from-to)214-237
Number of pages24
JournalEarth Surface Processes and Landforms
Volume42
Issue number1
DOIs
StatePublished - Jan 1 2017

Fingerprint

sediment transport
timescale
entrainment
bedload
desert
divergence
particle
shrub
tracer
conservation
travel
particle motion
autocorrelation
travel time
land surface
advection
time
spatial variation
plume
canopy

Keywords

  • Exner equation
  • master equation
  • particle diffusion
  • sediment transport

ASJC Scopus subject areas

  • Geography, Planning and Development
  • Earth-Surface Processes
  • Earth and Planetary Sciences (miscellaneous)

Cite this

The elements and richness of particle diffusion during sediment transport at small timescales. / Furbish, David Jon; Fathel, Siobhan L.; Schmeeckle, Mark; Jerolmack, Douglas J.; Schumer, Rina.

In: Earth Surface Processes and Landforms, Vol. 42, No. 1, 01.01.2017, p. 214-237.

Research output: Contribution to journalArticle

Furbish, David Jon ; Fathel, Siobhan L. ; Schmeeckle, Mark ; Jerolmack, Douglas J. ; Schumer, Rina. / The elements and richness of particle diffusion during sediment transport at small timescales. In: Earth Surface Processes and Landforms. 2017 ; Vol. 42, No. 1. pp. 214-237.
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