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Local heat transfer from a hot plate to a water jet
Authors:H?Robidou  Email author" target="_blank">H?AuracherEmail author  P?Gardin  M?Lebouché  L?Bogdani?
Institution:1.Berlin, Germany;2.Maizieres-les-Metz Cedex, France;3.Vandoeuvre Cedex, France;4.TU Berlin, Institut für Energietechnik, Sekr. KT1, Marchstra?e 18, D-10587 Berlin, Germany
Abstract:Jet impingement boiling is very efficient in cooling of hot surfaces as a part of the impinging liquid evaporates. Because of its importance to many cooling procedures, investigations on basic mechanisms of jet impingement boiling heat transfer are needed. Until now, most of the experimental studies, carried out under steady-state conditions, used a heat flux controlled system and were limited by the critical heat flux (CHF). The present study focuses on steady-state experiments along the entire boiling curve for hot plate temperatures of up to 700°C. A test section has been built up simulating a hot plate. It is divided into 8 independently heated modules of 10 mm length to enable local heat transfer measurements. By means of temperature controlled systems for each module local steady-state experiments in the whole range between single phase heat transfer and film boiling are possible. By solving the two dimensional inverse heat conduction problem, the local heat flux and the corresponding wall temperature on the surface of each module can be computed. The measurements show important differences between boiling curves measured at the stagnation line and those obtained in the parallel flow region. At the stagnation line, the transition boiling regime is characterised by very high heat fluxes, extended to large wall superheats. Inversely, boiling curves in the parallel flow region are very near to classical ones obtained for forced convection boiling. The analysis of temperature fluctuations measured at a depth of 0.8 mm from the boiling surface enables some conclusions on the boiling mechanism in the different boiling regimes.
Keywords:Jet impingement boiling  Boiling curves  Local measurements  High temperatures  Temperature fluctuations
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