H<inf>3</inf>O<sup>+</sup>, NO<sup>+</sup> and O<inf>2</inf><sup>+</sup><sup>.</sup> reactions with saturated and unsaturated monoketones and diones, focus on hydration of product ions
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61388955%3A_____%2F19%3A00497665" target="_blank" >RIV/61388955:_____/19:00497665 - isvavai.cz</a>
Výsledek na webu
<a href="http://hdl.handle.net/11104/0290191" target="_blank" >http://hdl.handle.net/11104/0290191</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.ijms.2018.10.027" target="_blank" >10.1016/j.ijms.2018.10.027</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
H<inf>3</inf>O<sup>+</sup>, NO<sup>+</sup> and O<inf>2</inf><sup>+</sup><sup>.</sup> reactions with saturated and unsaturated monoketones and diones, focus on hydration of product ions
Popis výsledku v původním jazyce
A selected ion flow tube, SIFT, study has been carried out for the reactions of the SIFT-MS reagent ions H3O+, NO+ and O2+[rad] with 21 ketones, M, comprising 13 saturated monoketones of which 10 are linear and 3 are branched, 5 unsaturated monoketones and 3 diones. The collisional rate coefficients, kc, were calculated for the H3O+ reactions that all proceed via rapid proton transfer and the relative rate coefficients for the NO+ and O2+[rad] reactions were obtained experimentally. The product ion distributions for all 63 reactions were obtained at two sample gas absolute humidity (0.5% and 5.5%), the higher humidity intended to simulate that of exhaled breath. A major objective was to understand how the product ions of the reactions formed hydrates, which is important for accurate quantification of metabolites in humid air samples by SIFT-MS and by secondary electrospray ionisation, SESI. The MH+ product ions of the H3O+ reactions readily hydrate at the higher humidity, the monohydrate being dominant for both the saturated and unsaturated ketones, whereas the dihydrate was dominant for the dione reactions. In the NO+ reactions, formation of the NO+M adduct ions was dominant for the saturated and unsaturated ketones, but charge transfer producing the M+[rad] parent cation was very dominant in the dione reactions. The O2+[rad] reactions all proceeded via dissociative charge transfer producing the parent cation M+[rad] and closed shell and open shell cation fragments. Except for the dione parent cations, the M+[rad] ions hydrated, as did the open shell fragment ions of the O2+[rad] reactions, but the closed shell fragment ions did not hydrate.
Název v anglickém jazyce
H<inf>3</inf>O<sup>+</sup>, NO<sup>+</sup> and O<inf>2</inf><sup>+</sup><sup>.</sup> reactions with saturated and unsaturated monoketones and diones, focus on hydration of product ions
Popis výsledku anglicky
A selected ion flow tube, SIFT, study has been carried out for the reactions of the SIFT-MS reagent ions H3O+, NO+ and O2+[rad] with 21 ketones, M, comprising 13 saturated monoketones of which 10 are linear and 3 are branched, 5 unsaturated monoketones and 3 diones. The collisional rate coefficients, kc, were calculated for the H3O+ reactions that all proceed via rapid proton transfer and the relative rate coefficients for the NO+ and O2+[rad] reactions were obtained experimentally. The product ion distributions for all 63 reactions were obtained at two sample gas absolute humidity (0.5% and 5.5%), the higher humidity intended to simulate that of exhaled breath. A major objective was to understand how the product ions of the reactions formed hydrates, which is important for accurate quantification of metabolites in humid air samples by SIFT-MS and by secondary electrospray ionisation, SESI. The MH+ product ions of the H3O+ reactions readily hydrate at the higher humidity, the monohydrate being dominant for both the saturated and unsaturated ketones, whereas the dihydrate was dominant for the dione reactions. In the NO+ reactions, formation of the NO+M adduct ions was dominant for the saturated and unsaturated ketones, but charge transfer producing the M+[rad] parent cation was very dominant in the dione reactions. The O2+[rad] reactions all proceeded via dissociative charge transfer producing the parent cation M+[rad] and closed shell and open shell cation fragments. Except for the dione parent cations, the M+[rad] ions hydrated, as did the open shell fragment ions of the O2+[rad] reactions, but the closed shell fragment ions did not hydrate.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10403 - Physical chemistry
Návaznosti výsledku
Projekt
<a href="/cs/project/GA18-12902S" target="_blank" >GA18-12902S: Hmotnostní spektrometrie se sekundární elektrosprejovou ionizací (SESI-MS) pro kvantifikaci plynných analytů v ovzduší, prostoru nad vzorky a v dechu</a><br>
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2019
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
International Journal of Mass Spectrometry
ISSN
1387-3806
e-ISSN
—
Svazek periodika
435
Číslo periodika v rámci svazku
JAN 2019
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
8
Strana od-do
173-180
Kód UT WoS článku
000453773300023
EID výsledku v databázi Scopus
2-s2.0-85056246467