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Acidic Hydrogen Enhanced Photocatalytic Reduction of CO2 on Planetary Surfaces

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    SYSNO ASEP0536891
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleAcidic Hydrogen Enhanced Photocatalytic Reduction of CO2 on Planetary Surfaces
    Author(s) Knížek, Antonín (UFCH-W) ORCID, RID, SAI
    Kubelík, Petr (UFCH-W) RID, ORCID
    Bouša, Milan (UFCH-W) RID, ORCID
    Ferus, Martin (UFCH-W) ORCID, RID
    Civiš, Svatopluk (UFCH-W) RID, ORCID, SAI
    Source TitleACS Earth and Space Chemistry. - : American Chemical Society - ISSN 2472-3452
    Roč. 4, č. 7 (2020), s. 1001-1009
    Number of pages9 s.
    Languageeng - English
    CountryUS - United States
    Keywordsdiffuse-reflectance measurements ; oxygen-isotope exchange ; carbon-dioxide ; band-gap ; tio2 ; methane ; mechanisms ; conversion ; complexes ; photocatalytic reduction of CO2 ; IR spectroscopy ; photocatalysis ; natural minerals ; reflectance ; band gap ; rate constant ; acidic conditions
    Subject RIVCF - Physical ; Theoretical Chemistry
    OECD categoryPhysical chemistry
    R&D ProjectsGA19-03314S GA ČR - Czech Science Foundation (CSF)
    EF16_019/0000778 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Method of publishingLimited access
    Institutional supportUFCH-W - RVO:61388955
    UT WOS000551545600006
    EID SCOPUS85088695421
    DOI10.1021/acsearthspacechem.0c00039
    AnnotationThe photocatalytic reduction of CO2 to CH4 is a chemical process that to some extent occurs on the surface of rocky planets. The effect of an acidic proton on the rate of the photocatalytic reduction of CO2 on mineral surfaces was explored through the addition of HCl to our reaction system. HCl serves a dual role: it is a Hdonor (reactant) and creates a band gap in the case of siderite and kaolinite (modifies the chemical environment of the reaction). Of the tested minerals, Al2O3, ilmenite (FeTiO3), and one sample of soil containing fossilized remains of diatoms from the Soos Nature Reserve (Czech Republic) have shown significant activity in the methanogenesis process. Kaolinite, natural rutile, MgO, basalt, acidic and ferrous synthetic clays, the Nakhla meteorite, and two diatomaceous earth samples from the Soos Nature Reserve showed weak photocatalytic properties, the reaction was slower than that on, e.g., Al2O3. The newly recognized photocatalytic activity of some of these natural minerals and the effect of the acidic proton should be included in the atmospheric models of both our planet and exoplanets alike, as it may play a role in the estimation of methane production from CO2 in the presence of minerals on the planetary surface upon UV radiation.
    WorkplaceJ. Heyrovsky Institute of Physical Chemistry
    ContactMichaela Knapová, michaela.knapova@jh-inst.cas.cz, Tel.: 266 053 196
    Year of Publishing2021
    Electronic addresshttp://hdl.handle.net/11104/0314646
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