The exceptional sediment load of fine-grained dispersal systems: Example of the Yellow River, China
dc.citation.articleNumber | e1603114 | en_US |
dc.citation.issueNumber | 5 | en_US |
dc.citation.journalTitle | Science Advances | en_US |
dc.citation.volumeNumber | 3 | en_US |
dc.contributor.author | Ma, Hongbo | en_US |
dc.contributor.author | Nittrouer, Jeffrey A. | en_US |
dc.contributor.author | Naito, Kensuke | en_US |
dc.contributor.author | Fu, Xudong | en_US |
dc.contributor.author | Zhang, Yuanfeng | en_US |
dc.contributor.author | Moodie, Andrew J. | en_US |
dc.contributor.author | Wang, Yuanjian | en_US |
dc.contributor.author | Wu, Baosheng | en_US |
dc.contributor.author | Parker, Gary | en_US |
dc.date.accessioned | 2017-07-14T15:23:43Z | en_US |
dc.date.available | 2017-07-14T15:23:43Z | en_US |
dc.date.issued | 2017 | en_US |
dc.description.abstract | Sedimentary dispersal systems with fine-grained beds are common, yet the physics of sediment movement within them remains poorly constrained. We analyze sediment transport data for the best-documented, fine-grained river worldwide, the Huanghe (Yellow River) of China, where sediment flux is underpredicted by an order of magnitude according to well-accepted sediment transport relations. Our theoretical framework, bolstered by field observations, demonstrates that the Huanghe tends toward upper-stage plane bed, yielding minimal form drag, thus markedly enhancing sediment transport efficiency. We present a sediment transport formulation applicable to all river systems with silt to coarse-sand beds. This formulation demonstrates a remarkably sensitive dependence on grain size within a certain narrow range and therefore has special relevance to silt-sand fluvial systems, particularly those affected by dams. | en_US |
dc.identifier.citation | Ma, Hongbo, Nittrouer, Jeffrey A., Naito, Kensuke, et al.. "The exceptional sediment load of fine-grained dispersal systems: Example of the Yellow River, China." <i>Science Advances,</i> 3, no. 5 (2017) AAAS: https://doi.org/10.1126/sciadv.1603114. | en_US |
dc.identifier.digital | e1603114.full | en_US |
dc.identifier.doi | https://doi.org/10.1126/sciadv.1603114 | en_US |
dc.identifier.uri | https://hdl.handle.net/1911/95195 | en_US |
dc.language.iso | eng | en_US |
dc.publisher | AAAS | en_US |
dc.rights | Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC). | en_US |
dc.rights.uri | https://creativecommons.org/licenses/by-nc/4.0/ | en_US |
dc.subject.keyword | sediment transport | en_US |
dc.subject.keyword | Fine-grained | en_US |
dc.subject.keyword | Bed form | en_US |
dc.subject.keyword | Upper-regime plane bed | en_US |
dc.subject.keyword | Phase transition | en_US |
dc.subject.keyword | Equilibrium transport | en_US |
dc.subject.keyword | Yellow River | en_US |
dc.subject.keyword | Large aspect ratio dunes | en_US |
dc.title | The exceptional sediment load of fine-grained dispersal systems: Example of the Yellow River, China | en_US |
dc.type | Journal article | en_US |
dc.type.dcmi | Text | en_US |
dc.type.publication | publisher version | en_US |
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