Bibcode
Pravec, P.; Vokrouhlický, D.; Polishook, D.; Scheeres, D. J.; Harris, A. W.; Galád, A.; Vaduvescu, O.; Pozo, F.; Barr, A.; Longa, P.; Vachier, F.; Colas, F.; Pray, D. P.; Pollock, J.; Reichart, D.; Ivarsen, K.; Haislip, J.; Lacluyze, A.; Kušnirák, P.; Henych, T.; Marchis, F.; Macomber, B.; Jacobson, S. A.; Krugly, Yu. N.; Sergeev, A. V.; Leroy, A.
Referencia bibliográfica
Nature, Volume 466, Issue 7310, pp. 1085-1088 (2010).
Fecha de publicación:
8
2010
Revista
Número de citas
195
Número de citas referidas
182
Descripción
Pairs of asteroids sharing similar heliocentric orbits, but not bound
together, were found recently. Backward integrations of their orbits
indicated that they separated gently with low relative velocities, but
did not provide additional insight into their formation mechanism. A
previously hypothesized rotational fission process may explain their
formation-critical predictions are that the mass ratios are less than
about 0.2 and, as the mass ratio approaches this upper limit, the spin
period of the larger body becomes long. Here we report photometric
observations of a sample of asteroid pairs, revealing that the primaries
of pairs with mass ratios much less than 0.2 rotate rapidly, near their
critical fission frequency. As the mass ratio approaches 0.2, the
primary period grows long. This occurs as the total energy of the system
approaches zero, requiring the asteroid pair to extract an increasing
fraction of energy from the primary's spin in order to escape. We do not
find asteroid pairs with mass ratios larger than 0.2. Rotationally
fissioned systems beyond this limit have insufficient energy to disrupt.
We conclude that asteroid pairs are formed by the rotational fission of
a parent asteroid into a proto-binary system, which subsequently
disrupts under its own internal system dynamics soon after formation.
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