The Relationship between Flux Coefficient and Entrainment Ratio in Density Currents
نویسندگان
چکیده
The authors explore the theoretical and empirical relationship between the nonlocal quantities of the entrainment ratio E, the appropriately depthand time-averaged flux coefficient G, and the bulk Froude number Fro in density currents. The main theoretical result is that E 5 0.125 G Fr 2 o(C 3 U /CL)/cosu, where u is the angle of the slope over which the density current flows, CL is the ratio the turbulent length scale to the depth of the density current, and CU is the ratio of the turbulent velocity scale to the mean velocity of the density current. In the case of high bulk Froude numbers G ; Fr 2 o and (CU /CL) 5 C ; 1, so E ; 0.1, consistent with observations of a constant entrainment ratio in unstratified jets and weakly stratified plumes. For bulk Froude numbers close to one, G is constant and has a value in the range of 0.1–0.3, which means that E ; Fro , again in agreement with observations and previous experiments. For bulk Froude numbers less than one, G decreases rapidly with bulk Froude number, explaining the sudden decrease in entrainment ratios that has been observed in all field and experimental observations.
منابع مشابه
Hydrodynamics Analysis of Density Currents
Density Current is formed when a fluid with heavier density than the surrounding fluid flows down an inclined bed. These types of flows are common in nature and can be produced by; salinity, temperature inhomogeneities, or suspended particles of silt and clay. Driven by the density difference between inflow and clear water in reservoirs, density current plunges clear water and moves towards a d...
متن کاملAn Analysis of changes in hydraulic parameters on water entrainment in converging channels
Building of Dam from thousands of years BC was known, and the humans with use of them alwaystry to preserve and utilize surface water resources, but sedimentation problem always is the mostimportant factor in shortening the useful life of dams , and a lot of reservoirs were filled by sedimentsdue to this process and therefore most of dams have been abandoned. One of the most importantphenomena ...
متن کاملEntraining gravity currents
Entrainment of ambient fluid into a gravity current, while often negligible in laboratory-scale flows, may become increasingly significant in large-scale natural flows. We present a theoretical study of the effect of this entrainment by augmenting a shallow water model for gravity currents under a deep ambient with a simple empirical model for entrainment, based on experimental measurements of ...
متن کاملتجزیه و تحلیل پروفیلهای سرعت در جریان غلیظ
In this paper, velocity profiles were analyzed under different conditions such as bed slope, discharge and concentration of density current, and water entrainment. Experiments were carried out in a tilting flume with the density currents being provided using salt and water solution. Results showed that the above mentioned factors have significant effects on the velocity profile characteristics....
متن کاملObservations of the volume flux of a seafloor hydrothermal plume using an acoustic imaging sonar
[2] We present a 26 day time series (October 2010) of physical properties (volume flux, flow velocity, expansion rate) of a vigorous deep-sea hydrothermal plume measured using our Cabled Observatory Vent Imaging Sonar (COVIS), which is connected to the Northeast Pacific Time Series Underwater Experiment Canada Cabled Observatory at the Main Endeavour Field on the Juan de Fuca Ridge. COVIS quant...
متن کامل