Hostname: page-component-76fb5796d-skm99 Total loading time: 0 Render date: 2024-04-26T12:58:20.952Z Has data issue: false hasContentIssue false

4.9 On the Structure of Hyperbolic Interplanetary Dust Streams

Published online by Cambridge University Press:  12 April 2016

L. Kresák
Affiliation:
Astronomical Institute, Slovak Academy of Sciences, Bratislava, Czechoslovakia
E.M. Pittich
Affiliation:
Astronomical Institute, Slovak Academy of Sciences, Bratislava, Czechoslovakia

Extract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

The only type of concentration of cometary dust with a reasonable probability of being detected by deep-space probes, are the dust tails emanating from passing comets. Essentially all the dust released from long-period comets leaves the solar system on hyperbolic orbits, because the radiation pressure limit is high (corresponding to centimetre-sized grains emitted in the vicinity of the Earth’s orbit by comets of the Oort’s Cloud). For the short-period comets the dynamical conditions for retention of emitted particles within the solar system are much more favourable, but those which remain in circumsolar orbits tend to disperse rather rapidly (Kresák, 1976a).

Type
4 Meteors and their Relation to Interplanetary Dust
Copyright
Copyright © Springer-Verlag 1976

References

Ceplecha, Z. (1967). In: Meteor Orbits and Dust, Smithson. Contrib. Astrophys. 11 = NASA SP-135, p. 35.Google Scholar
Kresák, L. (1976a). This Volume.Google Scholar
Kresák, L. (1975b). Bull. Astron. Inst. Czech. 26, 92.Google Scholar
Kresáková, M. (1966). Contrib. Astron. Obs. Skalnaté Pleso 3, 75.Google Scholar
Poultney, S.K. (1972). Space Research 12, 403.Google Scholar
Poultney, S.K. (1974). Space Research 14, 707.Google Scholar
Verniani, P. (1973). J. Geophys. Res. 78, 8429.Google Scholar
Whipple, P.L. (1967). In: The Zodiacal Light and the Interplanetary Medium. MSA SP-150, p. 409.Google Scholar