The logarithmic layer in a tidal channel

1997 ◽  
Vol 17 (14) ◽  
pp. 1785-1801 ◽  
Author(s):  
Rolf G. Lueck ◽  
Youyu Lu
2021 ◽  
Vol 916 ◽  
Author(s):  
Yongseok Kwon ◽  
Javier Jiménez
Keyword(s):  

Abstract


2018 ◽  
Vol 123 (6) ◽  
pp. 1386-1406 ◽  
Author(s):  
Christian Ferrarin ◽  
Fantina Madricardo ◽  
Federica Rizzetto ◽  
William Mc Kiver ◽  
Debora Bellafiore ◽  
...  
Keyword(s):  

2021 ◽  
Vol 118 (34) ◽  
pp. e2111144118 ◽  
Author(s):  
Kevin Patrick Griffin ◽  
Lin Fu ◽  
Parviz Moin

In this work, a transformation, which maps the mean velocity profiles of compressible wall-bounded turbulent flows to the incompressible law of the wall, is proposed. Unlike existing approaches, the proposed transformation successfully collapses, without specific tuning, numerical simulation data from fully developed channel and pipe flows, and boundary layers with or without heat transfer. In all these cases, the transformation is successful across the entire inner layer of the boundary layer (including the viscous sublayer, buffer layer, and logarithmic layer), recovers the asymptotically exact near-wall behavior in the viscous sublayer, and is consistent with the near balance of turbulence production and dissipation in the logarithmic region of the boundary layer. The performance of the transformation is verified for compressible wall-bounded flows with edge Mach numbers ranging from 0 to 15 and friction Reynolds numbers ranging from 200 to 2,000. Based on physical arguments, we show that such a general transformation exists for compressible wall-bounded turbulence regardless of the wall thermal condition.


PLoS ONE ◽  
2017 ◽  
Vol 12 (5) ◽  
pp. e0176405 ◽  
Author(s):  
Haley A. Viehman ◽  
Gayle Barbin Zydlewski

2012 ◽  
Vol 38 (2) ◽  
pp. 122-132 ◽  
Author(s):  
Wouter Vandenbruwaene ◽  
Tjeerd J. Bouma ◽  
Patrick Meire ◽  
Stijn Temmerman

2021 ◽  
Author(s):  
Daniel Collins ◽  
Howard Johnson

<p>The interaction of river and marine processes in the fluvial to marine transition zone (FMTZ) fundamentally impacts sedimentary dynamics and deposition. Heterolithics are important facies within ancient and modern FMTZs but the preserved signal of river flood, wave and tidal variations in heterolithics remains uncertain. This study integrates facies and ichnofacies characteristics of heterolithics in the Lambir Formation (Baram Delta Province, NW Borneo), with information of larger-scale stratigraphic architecture and modern analogue information, to interpret the preserved record of river flood deposits under the influence of tides and waves in an ancient FMTZ. Within the FMTZ of distributary channels, interpreted proximal–distal sedimentological and stratigraphic trends suggest: (1) a proximal fluvial-dominated, tide-influenced subzone; (2) a distal fluvial- to wave-dominated subzone; and (3) a conspicuously absent tide-dominated subzone. During coupled storm and river floods, fluvial processes dominated the FMTZ along major and minor distributary channels and channel mouths, causing significant overprinting of preceding interflood deposits and deposition of thicker, sandier event beds. Intervening interflood deposits are muddier, with increased bioturbation, and may variably preserve sedimentary indicators of tide and wave processes. Despite interpreted fluvial–tidal channel units and mangrove influence implying tidal processes, there is a paucity of unequivocal tidal indicators (e.g. cyclical heterolithic layering). This suggests that process preservation in the FMTZ preserved in the Lambir Formation primarily records episodic (flashy) river discharge, river flood and storm overprinting of tidal processes, and possible backwater dynamics. </p>


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