Dynamic role of the liquid core of Mercury in its motion on Cassini's laws and in resonant librations

Physics

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Introduction New approaches to the study of Mercury dynamics and the construction of analytical theory of its resonant rotation are suggested. Within these approaches Mercury is considered as a system of two non-spherical interacting bodies: a core and a mantle. The mantle of Mercury is considered as non-spherical, rigid (or elastic) layer. Inner shell is a liquid core, which occupies a large ellipsoidal cavity of Mercury. This Mercury system moves in the gravitational field of the Sun in resonant traslatoryrotary regime 3n = 2Omega (n is the mean orbital motion and Omega is the rotational angular velocity). In considered model Mercury moves on elliptical precessing orbit with inclination to Laplace plane i = 7`0029 and with eccentricity e = 0.2056. The orbit plane precesses with respect to normal nL to Laplace plane with the small angular velocity n<0, executing the return (regressive) motion. We have n/n = -0.8294·10-6. For the study of Mercury rotation we have been used specially designed author's canonical equations of motion in Andoyer and Poincare variables.

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