On turbulent entrainment and dissipation in dilute polymer solutions

被引:18
|
作者
Liberzon, A. [1 ]
Holzner, M. [2 ]
Luethi, B. [2 ]
Guala, M. [3 ]
Kinzelbach, W. [2 ]
机构
[1] Tel Aviv Univ, Fac Engn, Sch Mech Engn, IL-69978 Tel Aviv, Israel
[2] ETH, Inst Environm Engn, CH-8093 Zurich, Switzerland
[3] CALTECH, Grad Aeronaut Labs, Pasadena, CA 91125 USA
关键词
flow visualisation; fluid oscillations; polymer solutions; stratified flow; turbulence; GRID-GENERATED TURBULENCE; ISOTROPIC TURBULENCE; ADDITIVES; REDUCTION; INTERFACE; WATER;
D O I
10.1063/1.3097006
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
We present a comparative experimental study of a turbulent flow developing in clear water and dilute polymer solutions (25 and 50 wppm polyethylene oxide). The flow is forced by a planar grid that oscillates vertically with stroke S and frequency f in a square container of initially still fluid. Two-component velocity fields are measured in a vertical plane passing through the center of the tank by using time resolved particle image velocimetry. After the forcing is initiated, a turbulent layer develops that is separated from the initially irrotational fluid by a sharp interface, the so-called turbulent/nonturbulent interface (TNTI). The turbulent region grows in time through entrainment of surrounding fluid until the fluid in the whole container is in turbulent motion. From the comparison of the experiments in clear water and polymer solutions we conclude: (i) Polymer additives modify the large scale shape of the TNTI. (ii) Both, in water and in the polymer solution the mean depth of the turbulent layer, H(t), follows the theoretical prediction for Newtonian fluids H(t)proportional to Kt, where K proportional to S(2)f is the "grid action." (iii) We find a larger grid action for dilute polymer solutions than for water. As a consequence, the turbulent kinetic energy of the flow increases and the rate of energy input becomes higher. (iv) The entrainment rate beta=v(e)/v(rms) (where v(e)=dH/dt is the interface propagation velocity and v(rms) is the root mean square of the vertical velocity) is lower for polymers (beta(p)approximate to 0.7) than for water (beta(w)approximate to 0.8). The measured values for beta are in good agreement with similarity arguments, from which we estimate that in our experiment about 28% of the input energy is dissipated by polymers.
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页数:6
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