z-logo
open-access-imgOpen Access
Atmospheric Chemistry of 2-Amino-2-methyl-1-propanol: A Theoretical and Experimental Study of the OH-Initiated Degradation under Simulated Atmospheric Conditions
Author(s) -
Wen Siang Tan,
Liang Zhu,
Tomáš Mikoviny,
Claus J. Nielsen,
Yizhen Tang,
Armin Wisthaler,
Philipp Eichler,
Markus Müller,
Barbara D’Anna,
Naomi J. Farren,
Jacqueline F. Hamilton,
Jan B. C. Pettersson,
Mattias Hallquist,
Simen Antonsen,
Yngve Stenstrøm
Publication year - 2021
Publication title -
the journal of physical chemistry a
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.756
H-Index - 235
eISSN - 1520-5215
pISSN - 1089-5639
DOI - 10.1021/acs.jpca.1c04898
Subject(s) - chemistry , hydrogen atom abstraction , radical , atmospheric chemistry , photodissociation , reaction mechanism , quantum chemistry , molecule , kinetic isotope effect , hydroxyl radical , mass spectrometry , formaldehyde , photochemistry , computational chemistry , deuterium , organic chemistry , ozone , catalysis , physics , quantum mechanics , chromatography
The OH-initiated degradation of 2-amino-2-methyl-1-propanol [CH 3 C(NH 2 )(CH 3 )CH 2 OH, AMP] was investigated in a large atmospheric simulation chamber, employing time-resolved online high-resolution proton-transfer reaction-time-of-flight mass spectrometry (PTR-ToF-MS) and chemical analysis of aerosol online PTR-ToF-MS (CHARON-PTR-ToF-MS) instrumentation, and by theoretical calculations based on M06-2X/aug-cc-pVTZ quantum chemistry results and master equation modeling of the pivotal reaction steps. The quantum chemistry calculations reproduce the experimental rate coefficient of the AMP + OH reaction, aligning k ( T ) = 5.2 × 10 -12 × exp (505/ T ) cm 3 molecule -1 s -1 to the experimental value k exp,300K = 2.8 × 10 -11 cm 3 molecule -1 s -1 . The theoretical calculations predict that the AMP + OH reaction proceeds via hydrogen abstraction from the -CH 3 groups (5-10%), -CH 2 - group, (>70%) and -NH 2 group (5-20%), whereas hydrogen abstraction from the -OH group can be disregarded under atmospheric conditions. A detailed mechanism for atmospheric AMP degradation was obtained as part of the theoretical study. The photo-oxidation experiments show 2-amino-2-methylpropanal [CH 3 C(NH 2 )(CH 3 )CHO] as the major gas-phase product and propan-2-imine [(CH 3 ) 2 C═NH], 2-iminopropanol [(CH 3 )(CH 2 OH)C═NH], acetamide [CH 3 C(O)NH 2 ], formaldehyde (CH 2 O), and nitramine 2-methyl-2-(nitroamino)-1-propanol [AMPNO 2 , CH 3 C(CH 3 )(NHNO 2 )CH 2 OH] as minor primary products; there is no experimental evidence of nitrosamine formation. The branching in the initial H abstraction by OH radicals was derived in analyses of the temporal gas-phase product profiles to be B CH 3 / B CH 2 / B NH 2 = 6:70:24. Secondary photo-oxidation products and products resulting from particle and surface processing of the primary gas-phase products were also observed and quantified. All the photo-oxidation experiments were accompanied by extensive particle formation that was initiated by the reaction of AMP with nitric acid and that mainly consisted of this salt. Minor amounts of the gas-phase photo-oxidation products, including AMPNO 2 , were detected in the particles by CHARON-PTR-ToF-MS and GC×GC-NCD. Volatility measurements of laboratory-generated AMP nitrate nanoparticles gave Δ vap H = 80 ± 16 kJ mol -1 and an estimated vapor pressure of (1.3 ± 0.3) × 10 -5 Pa at 298 K. The atmospheric chemistry of AMP is evaluated and a validated chemistry model for implementation in dispersion models is presented.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom