Spin-orbit evolution of Mercury revisited
arXiv:1307.0136 · doi:10.1016/j.icarus.2014.05.045
Abstract
While it is accepted that the eccentricity of Mercury (0.206) favours entrapment into the 3:2 spin-orbit resonance, open is the question how and when the capture took place. A recent work by Makarov (2012) has demonstrated that trapping into this resonance is certain if the eccentricity is larger than 0.2, provided that we use a realistic tidal model, the one which is based on the Darwin-Kaula expansion of the tidal torque. The physics-based tidal model changes dramatically the statistics of the possible final spin states. First, we discover that after only one encounter with the spin-orbit 3:2 resonance this resonance becomes the most probable end-state. Second, if a capture into this (or any other) resonance takes place, the capture becomes final, several crossings of the same state being forbidden by our model. Third, within our model the trapping of Mercury happens much faster than previously believed: for most histories, 10 - 20 Myr are sufficient. Fourth, even a weak laminar friction between the solid mantle and a molten core would most likely result in a capture in the 2:1 or even higher resonance. So the principal novelty of our paper is that the 3:2 end-state is more ancient than the same end-state obtained when the constant time lag model is employed. The swift capture justifies our treatment of Mercury as a homogeneous, unstratified body whose liquid core had not yet formed by the time of trapping. We also provide a critical analysis of the hypothesis by Wieczorek et al. (2012) that the early Mercury might had been retrograde, whereafter it synchronised its spin and then accelerated it to the 3:2 resonance. Accurate processing of the available data on cratering does not support that hypothesis, while the employment of a realistic rheology invalidates a key element of the hypothesis, an intermediate pseudosynchronous state needed to spin-up to the 3:2 resonance.
Extended version of the submitted paper, accepted for publication in Icarus
References in corpus (15)
- Tidal friction in close-in satellites and exoplanets. The Darwin theory re-visited
- Chaotic diffusion in the Solar System
- Tidal Friction and Tidal Lagging. Applicability Limitations of a Popular Formula for the Tidal Torque
- Spin-orbit evolution of Mercury revisited
- Dynamical evolution and spin-orbit resonances of potentially habitable exoplanets. The case of GJ 581d
- No pseudosynchronous rotation for terrestrial planets and moons
- Mercury's capture into the 3/2 spin-orbit resonance including the effect of core-mantle friction
- Photophoretic separation of metals and silicates: the formation of Mercury like planets and metal depletion in chondrites
- A simple model of the chaotic eccentricity of Mercury
- Constraining the primordial orbits of the Terrestrial Planets
- Tidal dissipation in a homogeneous spherical body. II. Three examples: Mercury, Io, and Kepler-10 b
- Bodily tides near the 1:1 spin-orbit resonance. Correction to Goldreich's dynamical model
- Impact cratering on Mercury: consequences for the spin evolution
- Long-term evolution of the spin of Mercury I. Effect of the obliquity and core-mantle friction
- The influence of orbital dynamics, shape and tides on the obliquity of Mercury
Cited by in corpus (42)
- Spin-orbit evolution of Mercury revisited
- Tidal Evolution of Asteroidal Binaries. Ruled by Viscosity. Ignorant of Rigidity
- Equilibrium rotation of semiliquid exoplanets and satellites
- Tidal dissipation in a homogeneous spherical body. II. Three examples: Mercury, Io, and Kepler-10 b
- Spin-orbital tidal dynamics and tidal heating in the TRAPPIST-1 multi-planet system
- Tidal insights into rocky and icy bodies: An introduction and overview
- Tidal synchronization of close-in satellites and exoplanets. II. Spin dynamics and extension to Mercury and exoplanets host stars
- Andrade rheology in time-domain. Application to Enceladus' dissipation of energy due to forced libration
- Solid tidal friction in multi-layer planets: Application to Earth, Venus, a Super Earth and the TRAPPIST-1 planets. Can a multi-layer planet be approximated as a homogeneous planet?
- Orbital relaxation and excitation of planets tidally interacting with white dwarfs
- Final spin states of eccentric ocean planets
- Numerical Simulation of Tidal Evolution of a Viscoelastic Body Modelled with a Mass-Spring Network
- Tidal Dissipation in Dual-Body, Highly Eccentric, and Non-synchronously Rotating Systems: Applications to Pluto-Charon and the Exoplanet TRAPPIST-1e
- Effects of Spin-Orbit Resonances and Tidal Heating on the Inner Edge of the Habitable Zone
- Spin-orbit coupling for close-in planets
- 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
- Tidal spin down rates of homogeneous triaxial viscoelastic bodies
- Is there a semi-molten layer at the base of the lunar mantle?
- Finding Mountains with Molehills: The Detectability of Exotopography
- Thermal and orbital evolution of low-mass exoplanets
- Tidal friction in satellites and planets. The new version of the creep tide theory
- Tilting Styx and Nix but not Uranus with a Spin-Precession-Mean-motion resonance
- Forced libration of tidally synchronized planets and moons
- A Gap in the Mass Distribution for Warm Neptune and Terrestrial Planets
- On the Secondary's Rotation in Synchronous Binary Asteroid
- Intermittent Signals and Planetary Days in SETI
- The high-order Euler method and the spin-orbit model A fast algorithm for solving differential equations with small, smooth nonlinearity
- Can tidal evolution lead to close-in planetary bodies around white dwarfs I: Orbital period distribution
- Periodic and quasi-periodic attractors for the spin-orbit evolution of Mercury with a realistic tidal torque
- Hamiltonian formulation of the spin-orbit model with time-varying non-conservative forces
- Rotation and figure evolution in the creep tide theory. A new approach and application to Mercury
- Can tidal evolution lead to close-in planetary bodies around white dwarfs II: volcanism and transits
- Effective resonant stability of Mercury
- Do Tides Destabilize Trojan Exoplanets?
- Initial conditions for tidal synchronisation of a planet by its moon
- A synchronous moon as a possible cause of Mars' initial triaxiality
- Tidal evolution of the Keplerian elements
- Chaos over Order: Mapping 3D Rotation of Triaxial Asteroids and Minor Planets
- Pseudo-synchronous solutions for dissipative non-autonomous systems
- Simulation of the spin evolution of some selected exoplanets and inferences on their climate
- The dynamical evolution of close-in binary systems formed by a super-Earth and its host star. Case of the Kepler-21 system