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Three dimensional hydrodynamic modeling over bed forms in open channels

International Journal of Sediment Research 2010年第4期25卷 431-440页

作者： K.EL KHEIASHY J.MCCORQUODALE I.GEORGIOU E.MESELHE Kellogg Brown and Root Inc. (KBR) 4100 Clinton Drive 03-1130 Houston TX 77020 USA Civil and Environmental Engineering Department University of New Orleans New Orleans LA 70148 USA Earth and Environmental Sciences Department University of New Orleans New Orleans LA 70148 USA Civil Engineering Department University of Louisiana at Lafayette Lafayette LA 70504USA

Three dimensional numerical modeling ofidealized sand dunes was used to assess the capability of various modeling formulations to capture the flow structure and resistance introduced by bed forms which are similar to those in the Lower Mississippi River. The selected models were: ECOMSED (HydroQual), MIKE 3 [Danish Hydraulic Institute (DHI)] and H3D (Hayco). The study revealed that the hydrostatic versions of models did not capture the flow separation at the crest of the dunes; however, they did respond to the presence of bed forms and gave a total resistance similar to the nonhydrostatic models.

关键词： bed forms Alluvial rivers Three dimensional models Mississippi river

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A new mixing equation for bed material composition in bed form dominant conditions

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International Journal of Sediment Research 2022年第4期37卷 435-446页

作者： Baozhen Jia Deyu Zhong State Key Laboratory of Hydroscience and Engineering Tsinghua University Joint-Sponsored State Key Laboratory of Plateau Ecology and Agriculture Qinghai University

Vertical mixing beneath the bed surface and its effect on sediment composition has long been underestimated. This paper proposes a mixing equation to illustrate the temporal and spatial variations of bed material composition for bed form dominant rivers. A continuous mass conservation equation for elevation-specific nonuniform bed material composition is initially presented. A vertical mixing equation is finally derived as a diffusion-type partial differential equation with a source term characterized by a vertical diffusion coefficient and the geometric dimensions of bed forms. Coupled with boundary conditions, this equation is further developed in a vertical mixing model at the scale of bed forms, in which the variations of bed material composition are clearly illustrated. The equation accounts for vertical exchange fluxes driven by bed form migration and their effect on bed material composition, which helps elucidate the mixing mechanism. In application to riverbed degradation, the proposed equation is capable to describe armoring development in consideration of the interior mixing, which provides more satisfying predictions for bed surface materials. The new mixing equation helps gain insight into predicting the variations of bed material composition during morphological changes.

关键词： Mixing equation Active layer bed forms Grain size distribution

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Morphology and internal architecture of a banner bank off Chengshan Headland, Shandong Peninsula

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Acta Oceanologica Sinica 2009年第5期28卷 58-65页

作者： ZHOU Liangyong LIU Jia XUE Chunting KONG Xianghuai BAI Dapeng College of Marine Geo-science Ocean University of China Qingdao 266003 China The Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology Ministry of Land and Resources Qingdao 266071 China Qingdao Institute of Marine Geology Qingdao 266071 China

A banner bank off the north coast of the Chengshan Headland, Shandong Peninsula, has been described on the basis of echo sounder bathymetry, side-scan sonar and high-resolution seismic data sets. The bank is in NWW direction, approximately parallel to the coastline. The bank consists of sandy silt or clayed silt. Sand waves and megaripples are observed on the north side, which result from strong tidal currents around the headland and storm waves in winter. These bed forms indicate that the bank is influenced by the modern hydrodynamics. The bank is separated from the coast and Holocene subaqueous clinoform around the Shandong Peninsula in its east part. High-resolution seismic profiles reveal that the bank was formed during two periods： the earlier seismic unit Ua, and later seismic units Ub and Uc which overlays Ua with erosional surfaces on its south side and north side, respectively. As comparing with the clinoform, the bank has a different internal architecture. In the west of the bank, however, topography and surface sediment characteristics suggest that the bank links to the clinoform. The authors propose that seismic Ua is a residual part of early clinoform deposit. After the sediments in the north and south of Ua were eroded by strong currents, the Ub and Uc started to deposit probably by a complex hydrodynamic process. These results provide new insights into the evolution of the bank and its relation with the Holocene subqueous clinoform.

关键词： banner bank morphology internal architecture bed forms Holocene subqueous clinoform Huanghai Sea

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ON THE PREDICTION OF TRANSIENT bed LEVELS DUE TO AGGRADATION AND DEGRADATION INCLUDING ARMOURING

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International Journal of Sediment Research 1998年第1期 55-66+69-71页

作者： A.B.PALANIAPPAN 1,R.J.GARDE 2 and P.N.GODBOLE 3

ＯＮＴＨＥＰＲＥＤＩＣＴＩＯＮＯＦＴＲＡＮＳＩＥＮＴＢＥＤＬＥＶＥＬＳＤＵＥＴＯＡＧＧＲＡＤＡＴＩＯＮＡＮＤＤＥＧＲＡＤＡＴＩＯＮＩＮＣＬＵＤＩＮＧＡＲＭＯＵＲＩＮＧＡ．Ｂ．ＰＡＬＡＮＩＡＰＰＡＮ１，Ｒ．Ｊ．ＧＡＲＤ... 详细信息

ＯＮＴＨＥＰＲＥＤＩＣＴＩＯＮＯＦＴＲＡＮＳＩＥＮＴＢＥＤＬＥＶＥＬＳＤＵＥＴＯＡＧＧＲＡＤＡＴＩＯＮＡＮＤＤＥＧＲＡＤＡＴＩＯＮＩＮＣＬＵＤＩＮＧＡＲＭＯＵＲＩＮＧＡ．Ｂ．ＰＡＬＡＮＩＡＰＰＡＮ１，Ｒ．Ｊ．ＧＡＲＤＥ２ａｎｄＰ．Ｎ．ＧＯＤＢＯＬＥ３...

关键词： Aggradation Degradation Armouring Armour coat Mixing unit Mixing volume bed forms

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