The flow of heat through the floor of the Atlantic Ocean-Reference-Cited by-同舟云学术

The flow of heat through the floor of the Atlantic Ocean

Published:1954-03-18 Issue:1150 Volume:222 Page:408-429
ISSN:0080-4630
Container-title:Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences
language:en
Short-container-title:Proc. R. Soc. Lond. A

Author:

Abstract

The measurement of the temperature gradient and thermal conductivity in the sediments beneath the floor of the North Atlantic Ocean is described. Measurements were made at five stations. The mean heat flow and conductivity were found to be 0·98 × 10 -6 cal/cm 2 s and 25 × 10 -4 cal/cm °Cs. The heat flows at the individual stations range from 0·58 to 1·42 × 10 -6 cal/cm 2 s. The high heat flow is an unexpected result, and it is difficult to find a source for so much heat.

Publisher

The Royal Society

Subject

Pharmacology (medical)

Link

https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.1954.0085

Reference13 articles.

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4. Geol. Surv. no. 196-A 1-34. system ed. Kuiper G. P. 2 chap. 3. Chicago University Press.

5. Carslaw H. S. & Jaeger J. C. 1947 Conduction of heat in solids. Oxford: Clarendon Press.

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