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Estimate of Particle Densities and Collision Danger for Spacecraft Moving Through the Asteroid Belt*

Published online by Cambridge University Press:  12 April 2016

Donald J. Kessler*
Affiliation:
NASA Manned Spacecraft Center

Extract

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The present lack of exact information about the distributions of asteroids and asteroidal meteoroids causes the largest uncertainty in the description of the interplanetary meteoroid environment between the orbits of Mars and Jupiter. Observed asteroids are inferred to have diameters from a few kilometers to a few hundred kilometers. The presence of these larger bodies suggests the presence of smaller, unobservable bodies. When asteroids collide, fragments are produced that eventually collide with other fragments. Because of this continuous collision process, much smaller asteroids most probably exist. Such asteroidal meteoroids, if present in sufficient number, could pose considerable danger to spacecraft.

Type
Part III-Possible Space Missions and Future Work
Copyright
Copyright © NASA 1971

Footnotes

*

The full text of this paper appears in NASA SP-8038, Oct. 1970.

References

Baldwin, Ralph B. 1964, Lunar Crater Counts. Astron. J. 69(5), 377392.Google Scholar
Brown, Harrison. 1960, The Density and Mass Distribution of Meteoritic Bodies in the Neighborhood of the Earth’s Orbit. J. Geophys. Res. 65(6), 16791683.Google Scholar
Dohnanyi, J.S. 1969, Collisional Model of Asteroids and Their Debris. J. Geophys. Res. 74(10), 25312554.Google Scholar
Hartmann, William K. 1965, Secular Changes in Meteoritic Flux Through the History of the Solar System. Icarus 4(2), 207213.Google Scholar
Hartmann, William K. 1968, Lunar Crater Counts-VI: The Young Craters Tycho, Aristarchus, and Copernicus. Communications of the Lunar and Planetary Lab., vol. 7, no. 119, pp. 145156. Univ. of Arizona Press. Tucson.Google Scholar
Hawkins, Gerald S. 1960, Asteroidal Fragments. Astron. J. 65(5), 318322.Google Scholar
Hawkins, G.S. 1964, Interplanetary Debris Near the Earth. Ann. Rev. Astron. Astrophys. 2, 149164.Google Scholar
Kessler, Donald J. 1968, Upper Limit on the Spatial Density of Asteroidal Debris. AIAA J. 6(12), 2450.Google Scholar
Kessler, D.J. 1969, Spatial Density of the Known Asteroids in the Ecliptic Plane. NASA TM X-58026.Google Scholar
Kuiper, G.P., Fujita, Y., Gehrels, T., Groeneveld, I., Kent, J., Van Biesbroeck, G., and Houten, C.J. van. 1958, Survey of Asteroids. Astrophys. J. Suppl. Ser. 32, vol. 3, pp. 289335.Google Scholar
Marcus, A.H. 1966, A Stochastic Model for the Formation and Survival of Lunar Craters. Icarus 5, 165200.Google Scholar
Marcus, A.H. 1968, Number Density of Martian Craters. Bellcomm Rept. TR-68-710-1.Google Scholar
NASA SP-8013. 1969, Meteoroid Environment Model-1969 (Near Earth to Lunar Surface).Google Scholar
NASA SP-8038. 1970, Meteoroid Environment Model-1970 (Interplanetary and Planetary).Google Scholar
Piotrowski, S. 1953, Collisions of Asteroids. Acta Astron. 5, (Oct.), 115138.Google Scholar
Wetherill, G.W. 1967, Collisions in the Asteroid Belt. J. Geophys. Res. 72(9), 24292444.CrossRefGoogle Scholar
Whipple, Fred L. 1967, On Maintaining the Meteoritic Complex. Smithson. Astrophys. Observ. Special Rept. 239. (Also available in NASA SP-150, 1967, pp. 409426.)Google Scholar