The Feeding Zones of Terrestrial Planets and Insights into Moon Formation
arXiv:1501.03816 · doi:10.1016/j.icarus.2015.01.013
Abstract
[Abridged] We present an extensive suite of terrestrial planet formation simulations that allows quantitative analysis of the stochastic late stages of planet formation. We quantify the feeding zone width, Delta a, as the mass-weighted standard deviation of the initial semi-major axes of the planetary embryos and planetesimals that make up the final planet. The size of a planet's feeding zone in our simulations does not correlate with its final mass or semi-major axis, suggesting there is no systematic trend between a planet's mass and its volatile inventory. Instead, we find that the feeding zone of any planet more massive than 0.1M_Earth is roughly proportional to the radial extent of the initial disk from which it formed: Delta a~0.25(a_max-a_min), where a_min and a_max are the inner and outer edge of the initial planetesimal disk. These wide stochastic feeding zones have significant consequences for the origin of the Moon, since the canonical scenario predicts the Moon should be primarily composed of material from Earth's last major impactor (Theia), yet its isotopic composition is indistinguishable from Earth. In particular, we find that the feeding zones of Theia analogs are significantly more stochastic than the planetary analogs. Depending on our assumed initial distribution of oxygen isotopes within the planetesimal disk, we find a ~5% or less probability that the Earth and Theia will form with an isotopic difference equal to or smaller than the Earth and Moon's. In fact we predict that every planetary mass body should be expected to have a unique isotopic signature. In addition, we find paucities of massive Theia analogs and high velocity moon-forming collisions, two recently proposed explanations for the Moon's isotopic composition. Our work suggests that there is still no scenario for the Moon's origin that explains its isotopic composition with a high probability event.
arXiv comment16 pages, 22 figures, accepted for publication in Icarus; fixed typos
References in corpus (21)
- A low mass for Mars from Jupiter's early gas-driven migration
- Making other Earths: Dynamical Simulations of Terrestrial Planet Formation and Water Delivery
- Building the Terrestrial Planets: Constrained Accretion in the Inner Solar System
- High-resolution simulations of the final assembly of Earth-like planets 1: terrestrial accretion and dynamics
- Equilibration in the Aftermath of the Lunar-Forming Giant Impact
- Formation of the Terrestrial Planets from a Narrow Annulus
- A huge reservoir of ionized gas around the Milky Way: Accounting for the Missing Mass?
- Interacting Supernovae and Supernova Impostors. SN 2009ip, is this the end?
- Highly Siderophile Elements in the Earth's Mantle as a Clock for the Moon-forming Impact
- A hit-and-run Giant Impact scenario
- Lunar and Terrestrial Planet Formation in the Grand Tack Scenario
- Indication of insensitivity of planetary weathering behavior and habitable zone to surface land fraction
- Terrestrial Planet Formation in Disks with Varying Surface Density Profiles
- The Moving Group Targets of the SEEDS High-Contrast Imaging Survey of Exoplanets and Disks: Results and Observations from the First Three Years
- A Compound model for the origin of Earth's water
- Terrestrial Planet Formation in a protoplanetary disk with a local mass depletion: A successful scenario for the formation of Mars
- Water Cycling Between Ocean and Mantle: Super-Earths Need Not be Waterworlds
- Formation and accretion history of terrestrial planets from runaway growth through to late time: implications for orbital eccentricity
- The Effect of Planets Beyond the Ice Line on the Accretion of Volatiles by Habitable-Zone Rocky Planets
- Interaction Between The Broad-lined Type Ic Supernova 2012ap and Carriers of Diffuse Interstellar Bands
- Dynamical Evolution of the Earth-Moon Progenitors - Whence Theia?
Cited by in corpus (54)
- Oxygen isotopic evidence for vigorous mixing during the Moon-forming Giant Impact
- The Nitrogen Budget of Earth
- Melting and Mixing States of the Earth's Mantle after the Moon-Forming Impact
- Mars' Growth Stunted by an Early Giant Planet Instability
- Multiple Impact Origin for the Moon
- Characterizing Exoplanet Habitability
- Origin of Earth's water: sources and constraints
- The Elemental Abundances (with Uncertainties) of the Most Earth-like Planet
- Solar System Formation in the Context of Extra-Solar Planets
- The early instability scenario: terrestrial planet formation during the giant planet instability, and the effect of collisional fragmentation
- Reconciling Magma-Ocean Crystallization Models with the present-day Structure of the Earth's mantle
- On the Origin of Earth's Moon
- Enhanced constraints on the interior composition and structure of terrestrial exoplanets
- Stochastic accretion of the Earth
- The Lunar Gravitational-wave Antenna: Mission Studies and Science Case
- Growing Mars fast: High-resolution GPU simulations of embryo formation
- Enhanced mixing in giant impact simulations with a new Lagrangian method
- Constraints on the pre-impact orbits of Solar System giant impactors
- Numerous chondritic impactors and oxidized magma ocean set Earth's volatile depletion
- Dynamical Constraints on Mercury's Collisional Origin
- The terrestrial planet formation paradox inferred from high-resolution N-body simulations
- Terrestrial planet formation from a ring
- Formation of Terrestrial Planets in Disks with Different Surface Density Profiles
- Formation of Terrestrial Planets
- The composition of Solar system asteroids and Earth/Mars moons, and the Earth-Moon composition similarity
- Collision Chains among the Terrestrial Planets. III. Formation of the Moon
- Origin and dynamical evolution of the asteroid belt
- The role of multiple giant impacts in the formation of the Earth-Moon system
- The early instability scenario: Mars' mass explained by Jupiter's orbit
- The curious case of Mars formation
- Dynamical avenues for Mercury's origin II: in-situ formation in the inner terrestrial disk
- Isotopically distinct terrestrial planets via local accretion
- A race against the clock: Constraining the timing of cometary bombardment relative to Earth's growth
- Magneto-rotational instability in the protolunar disk
- Explaining Mercury via a single giant impact is highly unlikely
- Can a jumping-Jupiter trigger the Moon's formation impact?
- Comparisons of the core and mantle compositions of earth analogs from different terrestrial planet formation scenarios
- Rethinking the role of the giant planet instability in terrestrial planet formation models
- Mercury's formation within the Early Instability Scenario
- Brief Follow-up on Recent Studies of Theia's Accretion
- Mars' formation can constrain the primordial orbits of the gas giants
- Moonfalls: Collisions between the Earth and its past moons
- How the presence of a giant planet affects the outcome of terrestrial planet formation simulations
- Accretion regions of meteorite parent bodies inferred from a two-endmember isotopic mixing model
- Formation of embryos of the Earth and the Moon from the common rarefied condensation and their subsequent growth
- Extreme close encounters between proto-Mercury and proto-Venus in terrestrial planet formation
- Prevalance of Chaos in Planetary Systems Formed Through Embryo Accretion
- A Systematic Survey of Moon-Forming Giant Impacts. II. Rotating bodies
- Terrestrial planet formation during giant planet formation and giant planet migration I: The first 5 million years
- Planet formation: key mechanisms and global models
- Evidence of a primordial isotopic gradient in the inner region of the solar protoplanetary disc
- Spatial distribution of isotopes and compositional mixing in the inner protoplanetary disk
- Formation of terrestrial planets in eccentric and inclined giant planet systems
- The Dynamical Viability of an Extended Jupiter Ring System