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Decomposition of HCN during Experimental Impacts in Dry and Wet Planetary Atmospheres

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61388955%3A_____%2F24%3A00586720" target="_blank" >RIV/61388955:_____/24:00586720 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11310/24:10484594

  • Result on the web

    <a href="https://pubs.acs.org/doi/10.1021/acsearthspacechem.4c00064" target="_blank" >https://pubs.acs.org/doi/10.1021/acsearthspacechem.4c00064</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1021/acsearthspacechem.4c00064" target="_blank" >10.1021/acsearthspacechem.4c00064</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Decomposition of HCN during Experimental Impacts in Dry and Wet Planetary Atmospheres

  • Original language description

    Hydrogen cyanide (HCN), a key molecule of significant importance in contemporary perspectives on prebiotic chemistry, originates in planetary atmospheres from various processes, such as photochemistry, thermochemistry, and impact chemistry, as well as from delivery by impacts. The resilience of HCN during periods of heavy bombardment, a phenomenon caused by an influx of material on unstable trajectories after accretion, remains relatively understudied. This study extensively investigates the stability of HCN under impact conditions simulated using a laboratory Nd:YAG laser in the ELISE experimental setup. High-resolution infrared spectroscopy was employed to monitor the gas phase composition during these simulations. Impact chemistry was simulated in bulk nitrogen atmospheres with varying mixing ratios of HCN and water vapor. The probed range of compositions spans from similar to 0 to 1.8% of HCN and 0 to 2.7% of H2O in a similar to 1 bar nitrogen atmosphere. The primary decomposition products of HCN are CO and CO2 in the presence of water and unidentified solid phase products in dry conditions. Our experiments revealed a range of initial HCN decomposition rates between 2.43 x 10(15) and 5.17 x 10(17) molec J(-1) of input energy depending on the initial composition. Notably, it is shown that the decomposition process induced by the laser spark simulating the impact plasma is nonlinear, with the duration of the irradiation markedly affecting the decomposition rate. These findings underscore the necessity for careful consideration and allowance for margins when applying these rates to chemical models of molecular synthesis and decomposition in planetary atmospheres.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10403 - Physical chemistry

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2024

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    ACS Earth and Space Chemistry

  • ISSN

    2472-3452

  • e-ISSN

    2472-3452

  • Volume of the periodical

    8

  • Issue of the periodical within the volume

    6

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    13

  • Pages from-to

    1246-1258

  • UT code for WoS article

    001231811600001

  • EID of the result in the Scopus database

    2-s2.0-85194234793