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Structural properties of mobile armors formed at different flow strengths in gravel-bed rivers

机译：砾石河道中不同水流强度形成的活动装甲的结构特性

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©2016. The Authors.udThis is an open access article under theudterms of the Creative CommonsudAttribution License, which permits use,uddistribution and reproduction in anyudmedium, provided the original work isudproperly cited.

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Powell D. Mark; Ockelford Annie; Rice Stephen P.; Hillier John K.; Nguyen Thao; Reid Ian; Tate Nicholas J.; Ackerley David;
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年度 2016
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1. Structural properties of mobile armors formed at different flow strengths in gravel-bed rivers [J] . Powell D. Mark, Ockelford Annie, Rice Stephen P., Journal of geophysical research. Earth Surface: JGR . 2016,第8期

机译：砾石河道中不同水流强度形成的活动装甲的结构特性
2. Relation between flow, surface-layer armoring and sediment transport in gravel-bed rivers [J] . Pitlick J, Mueller ER, Segura C, Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group . 2008,第8期

机译：砾石河床流量，表层装甲与输沙量的关系
3. Floodplain inundation response to climate, valley form, and flow regulation on a gravel-bed river in a Mediterranean-climate region [J] . Cienciala P., Pasternack G. B. Geomorphology . 2017,第APRa1期

机译：地中海气候地区洪水泛滥对气候，山谷形态和砾石河道流量调节的响应
4. Shallow gravel-bed river flows: The behaviour of the free surface and the flow information contained within [C] . A. Nichols, K.V. Horoshenkov, S.J. Tait Conference on Fluvial Hydraulics . 2014

机译：浅砾石河河流流动：自由表面的行为和包含在内的流量信息
5. The Effect of Cool Deformation on the Microstructural Evolution and Flow Strength of Microalloyed Steels [D] . Mousavi Anijdan, Seyyed Hashem 2011

机译：冷变形对微合金钢组织演变和流动强度的影响
6. Gravel-bed river floodplains are the ecological nexus of glaciated mountain landscapes [O] . F. Richard Hauer, Harvey Locke, Victoria J. Dreitz, 2016

机译：砾石床河漫滩是冰川山脉景观的生态联系
7. Structural properties of mobile armors formed at different flow strengths in gravel-bed rivers [O] . Powell Mark, Ockelford Anne, Rice S.P., 2016

机译：砾石河道中不同水流强度形成的活动装甲的结构特性

Structural properties of mobile armors formed at different flow strengths in gravel-bed rivers

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