2D condensation model for the inner Solar Nebula: an enstatite-rich environment
arXiv:1601.01486 · doi:10.1093/mnras/stv3003
Abstract
Infrared observations provide the dust composition in the protoplanetary discs surface layers, but can not probe the dust chemistry in the midplane, where planet formation occurs. Meteorites show that dynamics was important in determining the dust distribution in the Solar Nebula and needs to be considered if we are to understand the global chemistry in discs. 1D radial condensation sequences can only simulate one disc layer at a time and cannot describe the global chemistry or the complexity of meteorites. To address these limitations, we compute for the first time the two dimensional distribution of condensates in the inner Solar Nebula using a thermodynamic equilibrium model, and derive timescales for vertical settling and radial migration of dust. We find two enstatite-rich zones within 1 AU from the young Sun: a band ~0.1 AU thick in the upper optically-thin layer of the disc interior to 0.8 AU, and in the optically-thick disc midplane out to ~0.4 AU. The two enstatite-rich zones support recent evidence that Mercury and enstatite chondrites shared a bulk material with similar composition. Our results are also consistent with infrared observation of protoplanetary disc which show emission of enstatite-rich dust in the inner surface of discs. The resulting chemistry and dynamics suggests that the formation of the bulk material of enstatite chondrites occurred in the inner surface layer of the disc, within 0.4~AU. We also propose a simple alternative scenario in which gas fractionation and vertical settling of the condensates lead to an enstatite-chondritic bulk material.
Astroph version. Accepted in MNRAS on 2015 December 23. Received 2015 December 16; in original form 2015 May 04
References in corpus (5)
- Coagulation, fragmentation and radial motion of solid particles in protoplanetary disks
- Gas- and dust evolution in protoplanetary disks
- SPH simulations of grain growth in protoplanetary disks
- Size-sorting dust grains in the surface layers of protoplanetary disks
- MBM 12: young protoplanetary discs at high galactic latitude
Cited by in corpus (14)
- Does a Differentiated, Carbonate-Rich, Rocky Object Pollute the White Dwarf SDSSJ104341.53+085558.2?
- The Elusive Origin of Mercury
- Formation of Comets
- On the impact origin of Phobos and Deimos III: resulting composition from different impactors
- Dust Condensation in Evolving Discs and the Composition of Planetary Building Blocks
- Dynamical avenues for Mercury's origin II: in-situ formation in the inner terrestrial disk
- The Exosphere as a Boundary: Origin and Evolution of Airless Bodies in the Inner Solar System and Beyond Including Planets with Silicate Atmospheres
- Explaining Mercury via a single giant impact is highly unlikely
- Maximum Temperatures in Evolving Protoplanetary Discs and Composition of Planetary Building Blocks
- Mid-infrared evidence for iron-rich dust in the multi-ringed inner disk of HD 144432
- Size and density sorting of dust grains in SPH simulations of protoplanetary disc II: Fragmentation
- Spatially resolving the chemical composition of the planet building blocks
- Stellar outbursts and chondrite composition
- Calorimetric Measurement of the Surface Energy of Enstatite, MgSiO