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      Incorporating the Memory Effect of Turbulence Structures Into Suspended Sediment Transport Modeling

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      https://www.riss.kr/link?id=O112005749

      • 저자
      • 발행기관
      • 학술지명
      • 권호사항
      • 발행연도

        2021년

      • 작성언어

        -

      • Print ISSN

        0043-1397

      • Online ISSN

        1944-7973

      • 등재정보

        SCI;SCIE;SCOPUS

      • 자료형태

        학술저널

      • 수록면

        n/a-n/a   [※수록면이 p5 이하이면, Review, Columns, Editor's Note, Abstract 등일 경우가 있습니다.]

      • 소장기관
      • 구독기관
        • 전북대학교 중앙도서관  
        • 성균관대학교 중앙학술정보관  
        • 부산대학교 중앙도서관  
        • 전남대학교 중앙도서관  
        • 제주대학교 중앙도서관  
        • 중앙대학교 서울캠퍼스 중앙도서관  
        • 인천대학교 학산도서관  
        • 숙명여자대학교 중앙도서관  
        • 서강대학교 로욜라중앙도서관  
        • 계명대학교 동산도서관  
        • 충남대학교 중앙도서관  
        • 한양대학교 백남학술정보관  
        • 이화여자대학교 중앙도서관  
        • 고려대학교 도서관  
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      다국어 초록 (Multilingual Abstract)

      Modeling 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 corr...

      Modeling 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.



      The temporal scale of turbulence structures is mathematically represented by considering the memory effect in a random walk model

      The diffusive particle behavior has a transition from superdiffusion to normal diffusion with an increase in the observation time scale

      The effective diffusion coefficient of the proposed stochastic process on a long‐term time scale is formulated


      The temporal scale of turbulence structures is mathematically represented by considering the memory effect in a random walk model
      The diffusive particle behavior has a transition from superdiffusion to normal diffusion with an increase in the observation time scale
      The effective diffusion coefficient of the proposed stochastic process on a long‐term time scale is formulated

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