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Ambient pressure CO2 hydrogenation over a cobalt/manganese-oxide nanostructured interface: A combined in situ and ex situ study

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A90116%2F20%3A10513089" target="_blank" >RIV/00216208:90116/20:10513089 - isvavai.cz</a>

  • Result on the web

    <a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=OzWQbWqdLj" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=OzWQbWqdLj</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.jcat.2020.03.028" target="_blank" >10.1016/j.jcat.2020.03.028</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Ambient pressure CO2 hydrogenation over a cobalt/manganese-oxide nanostructured interface: A combined in situ and ex situ study

  • Original language description

    We report on a cobalt/manganese-oxide interface catalyst with outstanding activity and selectivity towards methane even at high temperatures and ambient pressure in CO2 hydrogenation. The catalyst was formed from a MnCo2O4-based spinel structure during the oxidative-reductive pretreatment process just before the catalytic tests. Several Mn-, Fe- and Ni-containing cobaltite spinel and reverse spinel structures were tested to find the best overall performer. The reusable MnCo2O4-based structure featured a CO2 consumption rate of similar to 8500 nmol*g(-1)*s(-1). Even though methane is not the thermodynamically favoured product, it was produced with similar to 80% and similar to 50% selectivity at ambient pressure at 673 K and 823 K, respectively. This unexpected finding is linked to the presence of a unique nanostructured Co/Mn(II)O catalyst with a surface composition of Mn3.3Co2.0O4.7 formed after the pretreatment activation step. Over this phase, the reduction of CO2 progresses through bridge bonded formate located at the Co/Mn2+ interface and this is mostly responsible for high temperature methane formation. This hypothesis is proven here by the reported combination of ex-situ XRD, TPR, HRTEM-ED, HAADF-EDX and in-situ NAP-XPS and DRIFTS techniques. (C) 2020 The Authors. Published by Elsevier Inc.

  • 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

    10305 - Fluids and plasma physics (including surface physics)

Result continuities

  • Project

  • Continuities

Others

  • Publication year

    2020

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Journal of Catalysis

  • ISSN

    0021-9517

  • e-ISSN

    1090-2694

  • Volume of the periodical

    386

  • Issue of the periodical within the volume

    Jun

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    11

  • Pages from-to

    70-80

  • UT code for WoS article

    000533629300008

  • EID of the result in the Scopus database

    2-s2.0-85083682788