Intercomparison of OH and OH reactivity measurements in a high isoprene and low NO environment during the Southern Oxidant and Aerosol Study (SOAS)

被引:23
作者
Sanchez, Dianne [1 ]
Jeong, Daun [1 ]
Seco, Roger [1 ]
Wrangham, Ian [1 ]
Park, Jeong-Hoo [2 ,4 ]
Brune, William H. [3 ,4 ]
Koss, Abigail [4 ]
Gilman, Jessica
de Gouw, Joost
Misztal, Pawel [5 ]
Goldstein, Allen [5 ]
Baumann, Karsten [6 ]
Wennberg, Paul O. [7 ,8 ]
Keutsch, Frank N. [9 ,10 ]
Guenther, Alex [1 ]
Kim, Saewung [1 ]
机构
[1] Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA USA
[2] Natl Inst Environm Res, Incheon, South Korea
[3] Penn State Univ, Dept Meteorol & Atmospher Sci, University Pk, PA 16802 USA
[4] NOAA, Div Chem Sci, Earth Syst Res Lab, Boulder, CO USA
[5] Univ Calif Berkeley, Dept Environm Sci Policy & Management, Berkeley, CA 94720 USA
[6] Univ N Carolina, Gillings Sch Global Publ Hlth, Chapel Hill, NC USA
[7] CALTECH, Div Engn & Appl Sci, Pasadena, CA 91125 USA
[8] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
[9] Harvard Univ, Paulson Sch Engn & Appl Sci, Cambridge, MA 02138 USA
[10] Harvard Univ, Dept Chem & Chem Biol, Cambridge, MA 02138 USA
基金
美国国家科学基金会;
关键词
Hydroxyl radical; OH reactivity; Intercomparison; Isoprene; SOAS; LASER-INDUCED FLUORESCENCE; ATMOSPHERIC OXIDATION; SULFURIC-ACID; TROPOSPHERIC CHEMISTRY; RADICAL CHEMISTRY; MASS-SPECTROMETRY; PEROXY-RADICALS; BOREAL FOREST; HYDROXYL; HOX;
D O I
10.1016/j.atmosenv.2017.10.056
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We intercompare OH and OH reactivity datasets from two different techniques, chemical ionization mass spectrometry (CIMS) and laser-induced fluorescence (LIF) in a high isoprene and low NO environment in a southeastern US forest during the Southern Oxidant and Aerosol Study (SOAS). An LIF instrument measured OH and OH reactivity at the top of a tower, a CIMS instrument measured OH at the top of the tower, and a CIMS based comparative reactivity method (CRM-CIMS) instrument deployed at the base of the tower measured OH reactivity. Averaged diel variations of OH and OH reactivity from these datasets agree within analytical uncertainty and correlations of LIF versus CIMS for OH and OH reactivity have slopes of 0.65 and 0.97, respectively. However, there are systematic differences between the measurement datasets. The CRM-CIMS measurements of OH reactivity were 16% lower than those by the LIF technique in the late afternoon. We speculate that it is caused by losses in the sampling line down to the CRM-CIMS instrument. On the other hand, we could not come up with a reasonable explanation for the difference in the LIF and CIMS OH datasets for early morning and late afternoon when OH is below 1 x 10(6) molecules cm(-3). Nonetheless, results of this inter comparison exercise strengthen previous publications from the field site on OH concentrations and atmospheric reactivity.
引用
收藏
页码:227 / 236
页数:10
相关论文
共 72 条
[1]   FORMATION OF OH RADICALS IN THE GAS-PHASE REACTIONS OF O3 WITH A SERIES OF TERPENES [J].
ATKINSON, R ;
ASCHMANN, SM ;
AREY, J ;
SHOREES, B .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D5) :6065-6073
[2]   Particle partitioning potential of organic compounds is highest in the Eastern US and driven by anthropogenic water [J].
Carlton, A. G. ;
Turpin, B. J. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2013, 13 (20) :10203-10214
[3]   OZONE PRECURSOR RELATIONSHIPS IN THE AMBIENT ATMOSPHERE [J].
CHAMEIDES, WL ;
FEHSENFELD, F ;
RODGERS, MO ;
CARDELINO, C ;
MARTINEZ, J ;
PARRISH, D ;
LONNEMAN, W ;
LAWSON, DR ;
RASMUSSEN, RA ;
ZIMMERMAN, P ;
GREENBERG, J ;
MIDDLETON, P ;
WANG, T .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D5) :6037-6055
[4]   Peroxy radical isomerization in the oxidation of isoprene [J].
Crounse, John D. ;
Paulot, Fabien ;
Kjaergaard, Henrik G. ;
Wennberg, Paul O. .
PHYSICAL CHEMISTRY CHEMICAL PHYSICS, 2011, 13 (30) :13607-13613
[5]   THE CHANGING PHOTOCHEMISTRY OF THE TROPOSPHERE [J].
CRUTZEN, PJ ;
ZIMMERMANN, PH .
TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 1991, 43 (04) :136-151
[7]   REACTIVITY SCALE FOR ATMOSPHERIC HYDROCARBONS BASED ON REACTION WITH HYDROXYL RADICAL [J].
DARNALL, KR ;
LLOYD, AC ;
WINER, AM ;
PITTS, JN .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1976, 10 (07) :692-696
[8]   Missing OH reactivity in a forest: Evidence for unknown reactive biogenic VOCs [J].
Di Carlo, P ;
Brune, WH ;
Martinez, M ;
Harder, H ;
Lesher, R ;
Ren, XR ;
Thornberry, T ;
Carroll, MA ;
Young, V ;
Shepson, PB ;
Riemer, D ;
Apel, E ;
Campbell, C .
SCIENCE, 2004, 304 (5671) :722-725
[9]   First direct measurements of formaldehyde flux via eddy covariance: implications for missing in-canopy formaldehyde sources [J].
DiGangi, J. P. ;
Boyle, E. S. ;
Karl, T. ;
Harley, P. ;
Turnipseed, A. ;
Kim, S. ;
Cantrell, C. ;
Maudlin, R. L., III ;
Zheng, W. ;
Flocke, F. ;
Hall, S. R. ;
Ullmann, K. ;
Nakashima, Y. ;
Paul, J. B. ;
Wolfe, G. M. ;
Desai, A. R. ;
Kajii, Y. ;
Guenther, A. ;
Keutsch, F. N. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2011, 11 (20) :10565-10578
[10]   Direct observation of OH production from the ozonolysis of olefins [J].
Donahue, NM ;
Kroll, JH ;
Anderson, JG ;
Demerjian, KL .
GEOPHYSICAL RESEARCH LETTERS, 1998, 25 (01) :59-62