4.7 Article

Grain Size-Specific Engelund-Hansen Type Relation for Bed Material Load in Sand-Bed Rivers, With Application to the Mississippi River

期刊

WATER RESOURCES RESEARCH
卷 57, 期 2, 页码 -

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2020WR027517

关键词

bed material load; grain size‐ specific; grain sorting; Mississippi; River; morphodynamics; sand‐ bed river

资金

  1. National Key R&D Program of China [2017YFC0405305]
  2. National Natural Science Foundation of China [52009063, 52079095, 51525901]
  3. 111 Project [B18031]
  4. W. H. Johnson Professorship, University of Illinois Urbana-Champaign, USA

向作者/读者索取更多资源

Many sand-bed rivers worldwide are experiencing reductions in sediment load, leading to river delta drowning. This study proposes a grain size-specific relation to simulate river morphodynamic evolution, finding that sediment grain sorting accelerates bed surface armoring and reduces sediment load delivery to the delta. These results have practical implications for river delta restoration.
Many sand-bed rivers worldwide have been experiencing significant reductions in sediment load over the past several decades. This is one of the causes of river delta drowning worldwide. This problem, however, has not been studied in detail in the context of sediment grain sorting. Considering the good performance of the original Engelund-Hansen relation (OEH) for uniform sediment, and the fact that bulk grain size-specific relations for bed material load that allow for sorting are relatively rare in the case of sand-bed rivers, a grain size-specific Engelund-Hansen type relation (SEH) is proposed in this study based on data from a large flume. We embed both the OEH and the SEH in a one-dimensional river morphodynamic model to simulate the morphodynamic evolution of the middle Mississippi River in response to the upstream cutoff of sediment supply. Simulation results using a single characteristic grain size show that bed material load delivered to the delta reduces only gradually in response to the cutoff of sediment supply, in agreement with previous studies. However, implementing the full grain size distribution of sediment leads to a much faster reduction of bed material load delivered to the delta, because the bed surface coarsens in response to grain sorting. This armoring inhibits the bed degradation that would replenish sediment load along the channel. The bed material load of finer sediment declines more rapidly than that of coarser sediment. The results of this study have practical implications for river delta restoration.

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