HOx and NOx production in oxidation flow reactors via photolysis of isopropyl nitrite, isopropyl nitrite-d7, and 1,3-propyl dinitrite at λ=254, 350, and 369 nm

被引:15
|
作者
Lambe, Andrew T. [1 ]
Krechmer, Jordan E. [1 ]
Peng, Zhe [2 ,3 ]
Casar, Jason R. [4 ]
Carrasquillo, Anthony J. [5 ]
Raff, Jonathan D. [6 ]
Jimenez, Jose L. [2 ,3 ]
Worsnop, Douglas R. [1 ,7 ]
机构
[1] Aerodyne Res Inc, Ctr Aerosol & Cloud Chem, Billerica, MA 01821 USA
[2] Univ Colorado, Dept Chem, Boulder, CO 80309 USA
[3] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[4] Harvey Mudd Coll, Dept Chem, Claremont, CA 91711 USA
[5] Williams Coll, Dept Chem, Williamstown, MA 01267 USA
[6] Indiana Univ, Sch Publ & Environm Affairs, Bloomington, IN USA
[7] Univ Helsinki, Dept Phys, Helsinki, Finland
基金
美国国家科学基金会;
关键词
SECONDARY ORGANIC AEROSOL; RADICAL-INITIATED REACTIONS; GAS-PHASE REACTIONS; RATE CONSTANTS; ATMOSPHERIC CHEMISTRY; PHOTOCHEMICAL DATA; QUANTUM YIELDS; RELATIVE RATE; OH RADICALS; PHOTOOXIDATION;
D O I
10.5194/amt-12-299-2019
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Oxidation flow reactors (OFRs) are an emerging technique for studying the formation and oxidative aging of organic aerosols and other applications. In these flow reactors, hydroxyl radicals (OH), hydroperoxyl radicals (HO2), and nitric oxide (NO) are typically produced in the following ways: photolysis of ozone (O-3) at), = 254 nm, photolysis of H2O at), = 185 nm, and via reactions of O(D-1) with H2O and nitrous oxide (N2O); O(D-1) is formed via photolysis of O-3 at = 254 nm and/or N2O at = 185 nm. Here, we adapt a complementary method that uses alkyl nitrite photolysis as a source of OH via its production of HO2 and NO followed by the reaction NO + HO2 -> NO2 + OH. We present experimental and model characterization of the OH exposure and NO, levels generated via photolysis of C3 alkyl nitrites (isopropyl nitrite, perdeuterated isopropyl nitrite, 1,3-propyl dinitrite) in the Potential Aerosol Mass (PAM) OFR as a function of photolysis wavelength (7, = 254 to 369 nm) and organic nitrite concentration (0.5 to 20 ppm). We also apply this technique in conjunction with chemical ionization mass spectrometer measurements of multifunctional oxidation products generated following the exposure of a-Pinene to HO, and NO, obtained using both isopropyl nitrite and O-3 + H2O + N2O as the radical precursors.
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页码:299 / 311
页数:13
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