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Nitrogen Oxide Production in Laser-Induced Breakdown Simulating Impacts on the Hadean Atmosphere

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    SYSNO ASEP0555463
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleNitrogen Oxide Production in Laser-Induced Breakdown Simulating Impacts on the Hadean Atmosphere
    Author(s) Heays, Alan (UFCH-W) ORCID, RID, SAI
    Kaiserová, Tereza (UFCH-W)
    Rimmer, P. B. (GB)
    Knížek, Antonín (UFCH-W) ORCID, RID, SAI
    Petera, Lukáš (UFCH-W) ORCID
    Civiš, Svatopluk (UFCH-W) RID, ORCID, SAI
    Juha, L. (CZ)
    Dudžák, R. (CZ)
    Krůs, M. (CZ)
    Scherf, M. (AT)
    Lammer, H. (AT)
    Pascal, R. (FR)
    Ferus, Martin (UFCH-W) ORCID, RID
    Article numbere2021JE006842
    Source TitleJournal of Geophysical Research: Planets. - : Wiley - ISSN 2169-9097
    Roč. 127, č. 3 (2022)
    Number of pages14 s.
    Languageeng - English
    CountryUS - United States
    Keywordsnitrogen oxide ; laser ; high-energy-density synthesis
    Subject RIVCF - Physical ; Theoretical Chemistry
    OECD categoryPhysical chemistry
    R&D ProjectsGA21-11366S GA ČR - Czech Science Foundation (CSF)
    EF16_019/0000778 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Method of publishingOpen access with time embargo (01.09.2022)
    Institutional supportUFCH-W - RVO:61388955
    UT WOS000781641100011
    EID SCOPUS85127288044
    DOI10.1029/2021JE006842
    AnnotationThe high-energy-density synthesis of NxOy species is simulated in gas mixtures representing an O2-free early-Earth atmosphere by terawatt-kilojoule-class laser-induced dielectric breakdown (LIDB). These experiments differ from previous LIDB experiments due to the 100 times greater energy delivered per pulse and sensitive analysis of products by high-resolution infrared spectroscopy. The measured yields of NO, N2O, and NO2 are 0.08–8 × 1015, 5 × 1012, and 0.03–7 × 1014 molec J −1. The high N2O yield is above the upper-limit constraint of previous tabletop LIDB experiments and the expected yield of a thermochemical freeze-out at any temperature between 2000 and 5000 K, while the NO and NO2 yields are in broad agreement with freeze-out models. Using a one dimensional chemical model of the Hadean atmosphere and a simple model of late bombardment, we compute the source flux of N2O assuming the same high production yield as measured experimentally and find the steady-state partial pressure of N2O is insufficient to warm the climate.
    WorkplaceJ. Heyrovsky Institute of Physical Chemistry
    ContactMichaela Knapová, michaela.knapova@jh-inst.cas.cz, Tel.: 266 053 196
    Year of Publishing2023
    Electronic addresshttp://hdl.handle.net/11104/0329977
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