Spontaneous oxygen isotope exchange between carbon dioxide andnnatural clays: Refined rate constants referenced to TiO2 (anatase/rutile)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61388955%3A_____%2F17%3A00466724" target="_blank" >RIV/61388955:_____/17:00466724 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.clay.2016.11.031" target="_blank" >http://dx.doi.org/10.1016/j.clay.2016.11.031</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.clay.2016.11.031" target="_blank" >10.1016/j.clay.2016.11.031</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Spontaneous oxygen isotope exchange between carbon dioxide andnnatural clays: Refined rate constants referenced to TiO2 (anatase/rutile)

Popis výsledku v původním jazyce

In a series of our previously published papers, we reported a broad range of experiments and theoretical studies devoted to the interaction of carbon dioxide with the anatase titania surface. In the current study, we demonstrate oxygen mobility between gaseous carbon dioxide and solid natural clay minerals. This surprising feature implies that such behaviour is typical not only for titania but also for oxides with different chemical composition and structure. The oxygen mobility was demonstrated by the interaction of isotopically labelled carbon dioxide – C18O2 – with the mineral surfaces. In most cases, we observed rapid oxygen exchange between the gas and the mineral. It was therefore discovered that carbon dioxide is more active than was previously thought because it exchanges its oxygen atoms with inorganic surfaces. Moreover, this feature seems to be very significant in natural clays of various compositions. This finding points not only towards high activity of CO2 but also towards high surface reactivity of clays, which are quite common surface minerals on Earth and other planets.

Název v anglickém jazyce

Spontaneous oxygen isotope exchange between carbon dioxide andnnatural clays: Refined rate constants referenced to TiO2 (anatase/rutile)

Popis výsledku anglicky

In a series of our previously published papers, we reported a broad range of experiments and theoretical studies devoted to the interaction of carbon dioxide with the anatase titania surface. In the current study, we demonstrate oxygen mobility between gaseous carbon dioxide and solid natural clay minerals. This surprising feature implies that such behaviour is typical not only for titania but also for oxides with different chemical composition and structure. The oxygen mobility was demonstrated by the interaction of isotopically labelled carbon dioxide – C18O2 – with the mineral surfaces. In most cases, we observed rapid oxygen exchange between the gas and the mineral. It was therefore discovered that carbon dioxide is more active than was previously thought because it exchanges its oxygen atoms with inorganic surfaces. Moreover, this feature seems to be very significant in natural clays of various compositions. This finding points not only towards high activity of CO2 but also towards high surface reactivity of clays, which are quite common surface minerals on Earth and other planets.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10403 - Physical chemistry

Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2017

Kód důvěrnosti údajů

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

Název periodika

Applied Clay Science

ISSN

0169-1317

e-ISSN

—

Svazek periodika

137

Číslo periodika v rámci svazku

MAR 2017

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

5

Strana od-do

6-10

Kód UT WoS článku

000393002300002

EID výsledku v databázi Scopus

2-s2.0-85002976451