flushing flows
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2022 ◽  
Author(s):  
Peter Talling ◽  
Megan Baker ◽  
Ed Pope ◽  
Ricardo Silva Jacinto ◽  
Maarten Heijnen ◽  
...  

Abstract Here we document for the first time how major rivers connect directly to the deep-sea, by analysing the longest runout sediment flows (of any type) yet measured in action. These seafloor turbidity currents originated from the Congo River-mouth, with one flow travelling >1,130 km whilst accelerating from 5.2 to 8.0 m/s. In one year, these turbidity currents eroded 1-2 km3 of sediment from just one submarine canyon, equivalent to 14-28% of the annual global-flux from rivers. It was known earthquakes trigger canyon-flushing flows. We show major river-floods also generate canyon-flushing flows, primed by rapid sediment-accumulation at the river-mouth, but triggered by spring tides weeks to months after the flood. This is also the first field-confirmation that turbidity currents which erode can self-accelerate, thereby travelling much further. These observations explain highly-efficient organic carbon transfer, and have important implications for hazards to seabed cables, or how terrestrial climate change impacts the deep-sea.


2021 ◽  
Vol 213 ◽  
pp. 103475
Author(s):  
Rémi Loire ◽  
Hervé Piégay ◽  
Jean-René Malavoi ◽  
G. Mathias Kondolf ◽  
Leah A. Bêche

2019 ◽  
Vol 80 (2) ◽  
pp. 290-299
Author(s):  
Haoming Yang ◽  
David Z. Zhu ◽  
Yiping Zhang ◽  
Yongchao Zhou

Abstract One of the most common strategies for sewer cleaning is to generate flushing flows using flushing gates to store water in the upstream sewer pipe. Therefore it is important to obtain the flow information on the flushing waves and their eroding effects. In this study, the flow characteristics of the flushing wave and the flushing effect were investigated by a transient flow calculation using a commercial computational fluid dynamics (CFD) code. The values of bottom shear stress were obtained and the effect of several factors are discussed. The water depth and the slope were related to the release rate of the storage volume, while the flushing volume determined the flushing distance at long sewer distances. The initial downstream water level was found to dramatically reduce the flushing effect. Equations based on the storage depth were developed to estimate the flushing effect, and suggestions for the installation and operation of flushing gates are provided.


Author(s):  
Dudley W. Reiser ◽  
Michael P. Ramey ◽  
Thomas A. Wesche
Keyword(s):  

2014 ◽  
Vol 14 (12) ◽  
pp. 2057-2069 ◽  
Author(s):  
Alvaro Tena ◽  
Damià Vericat ◽  
Ramon J. Batalla

2014 ◽  
Vol 518 ◽  
pp. 130-139 ◽  
Author(s):  
Carlos M. Gómez ◽  
C. Dionisio Pérez-Blanco ◽  
Ramon J. Batalla

2012 ◽  
Vol 39 ◽  
pp. 7-17 ◽  
Author(s):  
Ophelie Fovet ◽  
Xavier Litrico ◽  
Gilles Belaud

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