Unraveling the impact of sediment size distribution on flow-sediment hysteresis in estuarine environments: insights from size-resolved sediment transport modeling
Flow-sediment hysteresis, a nonlinear time-lagged relationship between sediment transport and hydrodynamic conditions, is particularly important yet difficult to simulate in tidal estuarine environments. This study introduces a size-resolved sediment transport model to simulate flow-sediment hystere...
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| Published in | Environmental Research Communications Vol. 7; no. 6; pp. 61011 - 61026 |
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| Format | Journal Article |
| Language | English |
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01.06.2025
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| Abstract | Flow-sediment hysteresis, a nonlinear time-lagged relationship between sediment transport and hydrodynamic conditions, is particularly important yet difficult to simulate in tidal estuarine environments. This study introduces a size-resolved sediment transport model to simulate flow-sediment hysteresis, with an application in the Hudson River estuary. By incorporating variations in sediment size distribution induced by flocculation, the model allows for a more accurate simulation of flow-sediment hysteresis compared to traditional size-fixed models, achieving accuracy improvements of 4.89% ∼ 12.19% during tidal cycles. Moreover, budget analyses and correlation matrix analyses are conducted. The results indicate that the dynamics of small and large flocs influence hysteresis differentially: flocculation processes dominate the behavior of small flocs, while settling and vertical diffusion processes primarily affect large flocs. These insights offer a deeper understanding of sediment transport in tidal estuaries, providing a robust framework for enhanced predictive modeling which can be adapted to other estuarine environments. |
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| AbstractList | Flow-sediment hysteresis, a nonlinear time-lagged relationship between sediment transport and hydrodynamic conditions, is particularly important yet difficult to simulate in tidal estuarine environments. This study introduces a size-resolved sediment transport model to simulate flow-sediment hysteresis, with an application in the Hudson River estuary. By incorporating variations in sediment size distribution induced by flocculation, the model allows for a more accurate simulation of flow-sediment hysteresis compared to traditional size-fixed models, achieving accuracy improvements of 4.89% ∼ 12.19% during tidal cycles. Moreover, budget analyses and correlation matrix analyses are conducted. The results indicate that the dynamics of small and large flocs influence hysteresis differentially: flocculation processes dominate the behavior of small flocs, while settling and vertical diffusion processes primarily affect large flocs. These insights offer a deeper understanding of sediment transport in tidal estuaries, providing a robust framework for enhanced predictive modeling which can be adapted to other estuarine environments. Flow-sediment hysteresis, a nonlinear time-lagged relationship between sediment transport and hydrodynamic conditions, is particularly important yet difficult to simulate in tidal estuarine environments. This study introduces a size-resolved sediment transport model to simulate flow-sediment hysteresis, with an application in the Hudson River estuary. By incorporating variations in sediment size distribution induced by flocculation, the model allows for a more accurate simulation of flow-sediment hysteresis compared to traditional size-fixed models, achieving accuracy improvements of 4.89% ∼ 12.19% during tidal cycles. Moreover, budget analyses and correlation matrix analyses are conducted. The results indicate that the dynamics of small and large flocs influence hysteresis differentially: flocculation processes dominate the behavior of small flocs, while settling and vertical diffusion processes primarily affect large flocs. These insights offer a deeper understanding of sediment transport in tidal estuaries, providing a robust framework for enhanced predictive modeling which can be adapted to other estuarine environments. |
| Author | Xu, Fanghua Zhang, Xueyang Fang, Zheng |
| Author_xml | – sequence: 1 givenname: Zheng orcidid: 0000-0002-9782-6890 surname: Fang fullname: Fang, Zheng organization: University of Exeter Department of Mathematics and Statistics, College of Engineering, Mathematics and Physical Sciences, Devon EX4 4QE, United Kingdom – sequence: 2 givenname: Fanghua orcidid: 0000-0003-4057-8387 surname: Xu fullname: Xu, Fanghua organization: Tsinghua University Department of Earth System Science, Ministry of Education Key Laboratory for Earth System Modeling, Institute for Global Change Studies, Beijing 100084, People’s Republic of China – sequence: 3 givenname: Xueyang orcidid: 0000-0002-7389-5728 surname: Zhang fullname: Zhang, Xueyang organization: University of Reading Department of Meteorology, School of Mathematical, Physical and Computational Sciences, Berkshire RG6 6ET, United Kingdom |
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| Snippet | Flow-sediment hysteresis, a nonlinear time-lagged relationship between sediment transport and hydrodynamic conditions, is particularly important yet difficult... |
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| SubjectTerms | Correlation analysis Estuaries estuarine environment Estuarine environments Flocculation flow-sediment hysteresis Hysteresis numerical simulation Prediction models Sediment transport Size distribution size-resolved sediment transport model Tidal cycles Tides |
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| Title | Unraveling the impact of sediment size distribution on flow-sediment hysteresis in estuarine environments: insights from size-resolved sediment transport modeling |
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