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Some Remarks on the Liberation of Gases from Cometary Nuclei

Published online by Cambridge University Press:  14 August 2015

B. Yu. Levin*
Affiliation:
O. Schmidt Institute of Physics of the Earth, Moscow, U.S.S.R.

Abstract

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According to modern data water ice is the main constituent of cometary nuclei. The rate of its evaporation determines the rate of liberation of other constituents, including those that determine the photometric properties of comets. The estimates of the total mass loss per perihelion passage seem to give values about one order of magnitude smaller than those necessary to explain the nongravitational forces as due to the reactive force of material leaving the nuclei. Thus the conventional explanation of the nongravitational forces deserves further study from the point of view of the physical theory of comets.

Type
Part IV/Physical Processes in Comets
Copyright
Copyright © Reidel 1972 

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