Tidal Evolution of Close Binary Asteroid Systems
arXiv:1101.1500 · doi:10.1007/s10569-010-9308-0
Abstract
We provide a generalized discussion of tidal evolution to arbitrary order in the expansion of the gravitational potential between two spherical bodies of any mass ratio. To accurately reproduce the tidal evolution of a system at separations less than five times the radius of the larger primary component, the tidal potential due to the presence of a smaller secondary component is expanded in terms of Legendre polynomials to arbitrary order rather than truncated at leading order as is typically done in studies of well-separated system like the Earth and Moon. The equations of tidal evolution including tidal torques, the changes in spin rates of the components, and the change in semimajor axis (orbital separation) are then derived for binary asteroid systems with circular and equatorial mutual orbits. Accounting for higher-order terms in the tidal potential serves to speed up the tidal evolution of the system leading to underestimates in the time rates of change of the spin rates, semimajor axis, and mean motion in the mutual orbit if such corrections are ignored. Special attention is given to the effect of close orbits on the calculation of material properties of the components, in terms of the rigidity and tidal dissipation function, based on the tidal evolution of the system. It is found that accurate determinations of the physical parameters of the system, e.g., densities, sizes, and current separation, are typically more important than accounting for higher-order terms in the potential when calculating material properties. In the scope of the long-term tidal evolution of the semimajor axis and the component spin rates, correcting for close orbits is a small effect, but for an instantaneous rate of change in spin rate, semimajor axis, or mean motion, the close-orbit correction can be on the order of tens of percent.
40 pages, 2 tables, 8 figures
References in corpus (6)
- Tidal friction in close-in satellites and exoplanets. The Darwin theory re-visited
- Tidal Evolution of Rubble Piles
- Main Belt Binary Asteroidal Systems With Eccentric Mutual Orbits
- Main Belt Binary Asteroidal Systems With Circular Mutual Orbits
- Binary Asteroid Systems: Tidal End States and Estimates of Material Properties
- Angular Momemtum of Binary Asteroids: Implication for their possible origin
Cited by in corpus (17)
- Bodily tides near spin-orbit resonances
- Asteroid Systems: Binaries, Triples, and Pairs
- Complete Tidal Evolution of Pluto-Charon
- Tidal dissipation in a homogeneous spherical body. I. Methods
- Binary Asteroid Systems: Tidal End States and Estimates of Material Properties
- Tidal Evolution of Asteroidal Binaries. Ruled by Viscosity. Ignorant of Rigidity
- Tidal dissipation in a homogeneous spherical body. II. Three examples: Mercury, Io, and Kepler-10 b
- Tidal evolution of close-in exoplanets in co-orbital configurations
- Tidal decay and orbital circularization in close-in two-planet systems
- Energy Dissipation in Synchronous Binary Asteroids
- Dissipation in a tidally perturbed body librating in longitude
- Tides in a body librating about a spin-orbit resonance. Generalisation of the Darwin-Kaula theory
- Instability zones for satellites of asteroids. The example of the (87) Sylvia system
- Tidal evolution for any rheological model using a vectorial approach expressed in Hansen coefficients
- Tidal dissipation of binaries in asteroid pairs
- Rapid falling of an orbiting moon to its parent planet due to tidal-seismic resonance
- Tidal evolution of the Keplerian elements