Chemical Complementarity between the Gas Phase of the Interstellar Medium and the Rocky Material of Our Planetary System

Haiyang Wang, Charles Lineweaver

    Research output: Chapter in Book/Report/Conference proceedingConference contributionpeer-review

    Abstract

    We compare the elemental depletions in the gas phase of the interstellar medium (ISM) with the elemental depletions in the rocky material of our Solar System. Our analysis finds a high degree of chemical complementarity: elements depleted in the gas phase of the ISM are enriched in the rocky material of our Solar System, and vice versa. This chemical complementarity reveals the generic connections between interstellar dust and rocky planetary material. We use an inheritance model to explain the formation of primordial grains in the solar nebula. The primary dust grains inherited from the ISM, in combination with the secondary ones condensed from the solar nebula, constitute the primordial rocky material of our planetary system, from which terrestrial planets are formed through the effects of the progressive accretion and sublimation. The semi-major-axis-dependence of the chemical composition of rocky planetary material is also observed by comparing elemental depletions in the Earth, CI chondrites and other types of carbonaceous chondrites.
    Original languageEnglish
    Title of host publicationChemical Complementarity between the Gas Phase of the Interstellar Medium and the Rocky Material of Our Planetary System
    Place of PublicationCanberra
    PublisherNational Space Society of Australia Ltd
    Pages10pp
    EditionPeer Reviewed
    Publication statusPublished - 2015
    EventAustralian Space Research Conference ASRC 2015 - Canberra, Australia, Australia
    Duration: 1 Jan 2015 → …

    Conference

    ConferenceAustralian Space Research Conference ASRC 2015
    Country/TerritoryAustralia
    Period1/01/15 → …
    OtherSeptember 29- October 1 2015

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