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Boiling Heat Transfer from a Dike

P. Cheng, A.K. Verma

Conference
Stanford Geothermal Workshop
Year
1980
Session
Modeling
Language
English

Full text

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Abstract

It is known that hot dike complexes are one type of heat sources in a volcanic geothermal reservoir. To extract energy from a geothermal reservoir, it is important to know the cooling rate of the intrusives by groundwater. With a maximum temperature of 1,200?C, the intrusives are most likely to be cooled by film boiling during the initial sages and by single-phase convection during the later stages when its temperature becomes lower that the saturated temperature corresponding to the pressure. At the Second Workshop on Geothermal Reservoir Engineering, Cheng [l] has reported that the cooling rate of a dike by free convection of single-phase groundwater can be computed according to...

Copyright 1980, Stanford Geothermal Program. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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