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Comparative heat and gas exchange measurements in the Heidelberg Aeolotron, a large annular wind-wave tank

机译:海德堡Aeolotron(大型环形风箱)中的热和气体交换比较测量

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A comparative study of simultaneous heat and gas exchange measurements wasperformed in the large annular Heidelberg Air–Sea Interaction Facility, theAeolotron, under homogeneous water surface conditions. The use of two gastracers, N2O and C2HF5, resulted not only in gas transfervelocities, but also in the measurement of the Schmidt number exponent nwith a precision of ±0.025. The original controlled flux, or activethermographic, technique proposed by J?hne et al. (1989) was applied byheating a large patch at the water surface to measure heat transfervelocities. Heating a large patch, the active thermography technique islaterally homogeneous, and problems of lateral transport effects are avoided.Using the measured Schmidt number exponents, the ratio of the scaled heattransfer velocities to the measured gas transfer velocities is 1.046 ±0.040, a good agreement within the limits of experimental uncertainties.This indicates the possibility to scale heat transfer velocities measured byactive thermography to gas transfer velocities, provided that the Schmidt numberexponent is known and that the heated patch is large enough to reach thethermal equilibrium.
机译:在均匀的水面条件下,在大型环形海德堡空海相互作用设施theAeolotron中进行了同时进行热和气体交换测量的比较研究。 N 2 O和C 2 HF 5 这两种气体示踪剂的使用不仅导致气体传输速度,而且还导致了气体的测量。施密特数指数n的精度为±0.025。 J?hne等人提出的原始控制通量或主动热成像技术。 (1989)通过加热水表面的大块来测量传热速度。加热大的补丁,主动热成像技术在横向上是同质的,并且避免了横向传输效应的问题。使用测得的施密特数指数,缩放后的传热速度与测得的气体传递速度之比为1.046±0.040,在这表明有可能将主动热成像法测得的传热速度定标为气体传热速度,前提是已知Schmidt数指数并且加热的块足够大以达到热平衡。

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