Some considerations on heat transfer in
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M.H.I. Baird; W. McCrae; F. Rumford; C.G.M. Slesser
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Article
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1957
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Elsevier Science
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English
โ 347 KB
The sea-water samples used had a chlorinity of 16 and were obtained from the Firth of Clyde near the entrance to Loch Long. Their surface tension at IOWC was found to be 58.7 dyn/cm, as compared with 71.8 dyn/cm for a sample of freshwater. The freshwater used for comparison was Glasgow City water.