Tsai C.WSHIH-HSUN HUANGHung S.Y.WAN-SHAN TSAI2022-03-222022-03-22202100431397https://www.scopus.com/inward/record.uri?eid=2-s2.0-85103236953&doi=10.1029%2f2020WR028475&partnerID=40&md5=8bcb65c17a0b6b822f5733678f3df97fhttps://scholars.lib.ntu.edu.tw/handle/123456789/597984Modeling of the random movement of fine sediment particles in open-channel turbulent flow is mostly built upon the memoryless Brownian motion process. Such a process describes the chaotic behavior of small particles without considering temporal correlations in terms of the particle moving velocity and direction (i.e., memory). However, when particles are transported in time-persistent turbulent flow, the movements of the suspended particles may exhibit persistency that depends on the various temporal durations of turbulent flow structures—such persistence results in direction and magnitude variations in the velocity of the fine moving particles. The diffusion property of the particles may then deviate from normal diffusion. The conventional memoryless random walk models may not provide a comprehensive description of the particle diffusion process for the duration of turbulence structures when the particles are subject to memory effects. In this study, a novel random walk model is proposed to present the temporal correlation of the suspended sediment particle velocity caused by turbulence structures in open channel flow. The probabilistic properties of the proposed model are discussed. In particular, enhanced physical insights are obtained regarding the particle diffusion behavior in turbulent flows. Numerical simulations are conducted to demonstrate that, similar to the conventional memoryless random walk models, the proposed model shows normal diffusion for long-term observations, despite its local superdiffusion behavior. The effective diffusion coefficient of the proposed stochastic process on a long-term time scale is formulated. ? 2021. American Geophysical Union. All Rights Reserved.anomalous diffusionnon-Markovian processrandom-walk based modelstochastic sediment transportsuspended sediment transport modeltemporal correlationBrownian movementDiffusion in solidsOpen channel flowSediment transportStochastic systemsSuspended sedimentsTurbulenceTurbulent flowVelocity controlBrownian motion processEffective diffusion coefficientsLong term observationsParticle diffusion processProbabilistic propertiesRandom walk modelingTemporal correlationsTurbulence structuresElementary particle sourcesBrownian motionmodelingopen channel flowpersistencesediment transportstochasticitysuspended sedimentturbulenceturbulent flowjournal article10.1029/2020WR0284752-s2.0-85103236953