5040 Rabinowitz
5040 Rabinowitz, provisional designation, is a stony Phocaea asteroid from the inner regions of the asteroid belt, approximately 6 kilometers in diameter. It was discovered by Dutch–American astronomer Tom Gehrels at Palomar Observatory on 15 September 1972. Contrary to most of his discoveries, this asteroid is unrelated to the Palomar–Leiden survey and exclusively credited to Tom Gehrels.
Orbit and classification
The stony S-type asteroid is a member of the Phocaea family, a group of asteroids with similar orbital characteristics, named after its largest member, 25 Phocaea. It orbits the Sun in the inner main-belt at a distance of 1.9–3.0 AU once every 3 years and 9 months. Its orbit has an eccentricity of 0.23 and an inclination of 24° with respect to the ecliptic. A first precovery was taken at the discovering observatory in 1971, extending the body's observation arc by one year prior to its official discovery observation.Physical characteristics
Rotation period
In July 2013, a rotational lightcurve for this asteroid was obtained from photometric observations by Czech astronomer Petr Pravec at the Ondřejov Observatory. The well-defined lightcurve gave a rotation period of hours with a brightness variation of 0.33 in magnitude.During the same opposition opportunity, two more lightcurves – obtained by Robert Stephens at the Center for Solar System Studies and by Maurice Clark at the Preston Gott Observatory – gave a similar period of and hours, with an amplitude of 0.35 and 0.31 in magnitude, respectively.