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Nikora et al. 2002
Nikora, V., Habersack, H., Huber, T. and McEwan, I. (2002). On bed particle diffusion in gravel bed flows under weak bed load transport. Water Resources Research 38: doi: 10.1029/2001WR000513. issn: 0043-1397.

We introduce a new conceptual model for longitudinal and transverse diffusion of moving bed particles under weak bed load transport. For both rolling/sliding and saltating modes the model suggests that the particle motion is diffusive and comprises at least three ranges of temporal and spatial scales with different diffusion regimes: (1) the local range (ballistic diffusion), (2) the intermediate range (normal or anomalous diffusion), and (3) the global range (subdiffusion). The local range corresponds to ballistic particle trajectories between two successive collisions with the static bed particles. The intermediate range corresponds to particle trajectories between two successive periods of rest. These trajectories consist of many local trajectories and may include tens or hundreds of collisions with the bed. The global range of scales corresponds to particle trajectories consisting of many intermediate trajectories, just as intermediate trajectories consist of many local trajectories. Our data from the Balmoral Canal (the intermediate range) and Drake et al.'s <1988> data from the Duck Creek (the global range) provide strong support for this conceptual model and identify anomalous diffusion regimes for the intermediate range (superdiffusion) and the global range (subdiffusion).

BACKGROUND DATA FILES

Abstract

Keywords
Hydrology, Erosion and sedimentation, Hydrology, Geomorphology, Hydrology, Stochastic processes, Oceanography, Physical, Sediment transport
Journal
Water Resources Research
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Publisher
American Geophysical Union
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