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How is the orbital period of a test particle modified by the Dvali–Gabadadze–Porrati gravity?

Lorenzo Iorio JCAP01(2006)008   doi: 10.1088/1475-7516/2006/01/008  Help

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Lorenzo Iorio
Viale Unità di Italia 68, 70125, Bari, Italy
E-mail: lorenzo.iorio@libero.it

Abstract. In addition to the pericentre ω, the mean anomaly \mathcal {M} and, thus, the mean longitude λ, also the orbital period Pb and the mean motion n of a test particle, are modified by the Dvali–Gabadadze–Porrati gravity. While the correction to Pb depends on the mass of the central body and on the geometrical features of the orbital motion around it, the correction to n is independent of them, up to terms of second order in the eccentricity e. The latter amounts to about 2 × 10−3 arcsec per century. The present-day accuracy in determining the mean motions of the inner planets of the solar system from radar ranging and differential very long baseline interferometry (ΔVLBI) is 10−2–5 × 10−3 arcsec per century, but it should be improved in the near future when the data from the spacecraft to Mercury and Venus will be available.

Key words: extra dimensions; gravity

Received 11 October 2005, accepted for publication 19 December 2005
Published 10 January 2006

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