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Nitrogen Oxide Production in Laser-Induced Breakdown Simulating Impacts on the Hadean Atmosphere
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SYSNO ASEP 0555463 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Nitrogen 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, RIDArticle number e2021JE006842 Source Title Journal of Geophysical Research: Planets. - : Wiley - ISSN 2169-9097
Roč. 127, č. 3 (2022)Number of pages 14 s. Language eng - English Country US - United States Keywords nitrogen oxide ; laser ; high-energy-density synthesis Subject RIV CF - Physical ; Theoretical Chemistry OECD category Physical chemistry R&D Projects GA21-11366S GA ČR - Czech Science Foundation (CSF) EF16_019/0000778 GA MŠMT - Ministry of Education, Youth and Sports (MEYS) Method of publishing Open access with time embargo (01.09.2022) Institutional support UFCH-W - RVO:61388955 UT WOS 000781641100011 EID SCOPUS 85127288044 DOI 10.1029/2021JE006842 Annotation The 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.
Workplace J. Heyrovsky Institute of Physical Chemistry Contact Michaela Knapová, michaela.knapova@jh-inst.cas.cz, Tel.: 266 053 196 Year of Publishing 2023 Electronic address http://hdl.handle.net/11104/0329977
Number of the records: 1