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• W2953753822 abstract "The coupling of sediment transport with the flow that drives it allows rivers to shape their own bed. Cross-stream fluxes of sediment play a crucial, yet poorly understood, role in this process. Here, we track particles in a laboratory flume to relate their statistical behavior to the self-organization of the granular bed they make up. As they travel downstream, the transported grains wander randomly across the bed's surface, thus inducing cross-stream diffusion. The balance of diffusion and gravity results in a peculiar Boltzmann distribution, in which the bed's roughness plays the role of thermal fluctuations, while its surface forms the potential well that confines the sediment flux." @default.
• W2953753822 created "2019-07-12" @default.
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• W2953753822 date "2019-07-01" @default.
• W2953753822 modified "2023-10-18" @default.
• W2953753822 title "Boltzmann Distribution of Sediment Transport" @default.
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• W2953753822 doi "https://doi.org/10.1103/physrevlett.123.014501" @default.
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