Summary
IT WAS OBSERVED THAT THE NATURAL CONVECTION OCCURRED WHICH PROMOTED THE THERMAL HOMOGENIZING EFFECT IN THE POROUS LAYER, AND CONSEQUENTLY THE STEADY STATE WAS OBTAINED IN A SHORTER TIME BY THE CONTRIBUTION OF NATURAL CONVECTION. IT WAS POSSIBLE TO CONTROL THE TIME TAKEN TO REACH A STEADY STATE AND THE AMOUNT OF HEAT STORED IN THE POROUS LAYER.
Details
- Original title: AN EXPERIMENTAL STUDY OF TRANSIENT HEAT TRANSFER CHARACTERISTICS IN A POROUS LAYER ENCLOSED BETWEEN TWO OPPOSING VERTICAL SURFACES WITH DIFFERENT TEMPERATURES.
- Record ID : 1982-1861
- Languages: English
- Source: International Journal of Heat and Mass Transfer - vol. 24 - n. 11
- Publication date: 1981/11
Links
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Indexing
- Themes: Mass transfer
- Keywords: Free convection; Measurement; Heat transfer; Transient state; Porous medium
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- Date : 1990
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