A four cold-wire probe, which allows all three components of the temperature dissipation rate ɛ θ to be measured, is “calibrated” in decaying grid turbulence, where <ɛ θ >, the mean value of ɛ θ , can be determined accurately from the decay of the temperature variance <θ 2>. The probe yields values of the three components of <ɛ θ > which are in reasonable agreement with local isotropy, in the range x 1/M?50. The pdfs and spectra of the three temperature derivatives also satisfy local isotropy reasonably well.
Experiments in Fluids – Springer Journals
Published: Jan 1, 2000
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