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| Home > Publications database > Experimental budgets of OH, HO<sub>2</sub> and RO<sub>2</sub> radicals and implications for ozone formation in the Pearl River Delta in China 2014 > print |
| Home > Publications database > Experimental budgets of OH, HO<sub>2</sub> and RO<sub>2</sub> radicals and implications for ozone formation in the Pearl River Delta in China 2014 > print |
| 001 | 857600 | ||
| 005 | 20240712101036.0 | ||
| 024 | 7 | _ | |a 10.5194/acp-2018-801 |2 doi |
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| 037 | _ | _ | |a FZJ-2018-06585 |
| 082 | _ | _ | |a 550 |
| 100 | 1 | _ | |a Tan, Zhaofeng |0 P:(DE-Juel1)173726 |b 0 |e Corresponding author |
| 245 | _ | _ | |a Experimental budgets of OH, HO2 and RO2 radicals and implications for ozone formation in the Pearl River Delta in China 2014 |
| 260 | _ | _ | |a Katlenburg-Lindau |c 2018 |b EGU |
| 336 | 7 | _ | |a article |2 DRIVER |
| 336 | 7 | _ | |a Output Types/Journal article |2 DataCite |
| 336 | 7 | _ | |a Journal Article |b journal |m journal |0 PUB:(DE-HGF)16 |s 1562057403_18409 |2 PUB:(DE-HGF) |
| 336 | 7 | _ | |a ARTICLE |2 BibTeX |
| 336 | 7 | _ | |a JOURNAL_ARTICLE |2 ORCID |
| 336 | 7 | _ | |a Journal Article |0 0 |2 EndNote |
| 520 | _ | _ | |a Hydroxyl (OH) and peroxy radicals (HO2, RO2) were measured in the Pearl River Delta which is one of the most polluted areas in China, in autumn 2014. The radical observations were complemented by measurements of OH reactivity (inverse OH lifetime) and a comprehensive set of trace gases including CO, NOx and VOCs. OH reactivity was in the range between 15s−1 and 80s−1, of which about 50% was unexplained by the measured OH reactants. In the three weeks of the campaign, maximum median radical concentrations were 4.5×106cm−3 for OH at noon, and 3×108cm−3 and 2.0×108cm−3 for HO2 and RO2, respectively, in the early afternoon. The completeness of the daytime radical measurements made it possible to carry out experimental budget analyses for all radicals (OH, HO2, and RO2) and their sum (ROx). The maximum loss rates for OH, HO2, and RO2 reached values between 10ppbv/h and 15ppbv/h during daytime. The largest fraction of this can be attributed to radical interconveresio reactions while the real loss rate of ROx remained below 3ppbv/h. Within experimental uncertainties, the destruction rates of HO2 and the sum of OH, HO2, and RO2 are balanced by their respective production rates. In case of RO2, the budget can only be closed when the missing OH reactivity is attributed to unmeasured VOCs. Thus, the existence of unmeasured VOCs is directly confirmed by RO2 measurements. Although the closure of the RO2 budget is greatly improved by the additional unmeasured VOCs, a significant imbalance in the afternoon remains indicating a missing RO2 sink. In case of OH, the destruction in the morning is compensated by the quantified OH sources from photolysis (HONO, O3), ozonolysis of alkenes and OH recycling (HO2+NO). In the afternoon, however, the OH budget indicates a missing OH source of (4–6)ppbv/h. The diurnal variation of the missing OH source shows a similar pattern as that of the missing RO2 sink so that both largely compensate each other in the ROx budget. These observations suggest the existence of a chemical mechanism that converts RO2 to OH without the involvement of NO. The photochemical net ozone production rate calculated from the reaction of HO2 and RO2 with NO yields a daily integrated amount of 102ppbv ozone with daily integrated ROx primary sources being 22ppbv in this campaign. This value can be attributed to the oxidation of measured (18%) and unmeasured (60%) hydrocarbons, formaldehyde (14%) and CO (8%). An even larger integrated net ozone production of 140ppbv would be calculated from the oxidation rate of VOCs with OH, if HO2 and all RO2 radicals would react with NO. However, the unknown RO2 loss (evident in the RO2 budget) causes 30% less ozone production than would be expected from the VOC oxidation rate. |
| 536 | _ | _ | |a 243 - Tropospheric trace substances and their transformation processes (POF3-243) |0 G:(DE-HGF)POF3-243 |c POF3-243 |f POF III |x 0 |
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| 700 | 1 | _ | |a Lu, Keding |0 0000-0001-9425-9520 |b 1 |
| 700 | 1 | _ | |a Hofzumahaus, Andreas |0 P:(DE-Juel1)16326 |b 2 |
| 700 | 1 | _ | |a Fuchs, Hendrik |0 P:(DE-Juel1)7363 |b 3 |
| 700 | 1 | _ | |a Bohn, Birger |0 P:(DE-Juel1)2693 |b 4 |
| 700 | 1 | _ | |a Holland, Frank |0 P:(DE-Juel1)16342 |b 5 |
| 700 | 1 | _ | |a Liu, Yuhan |0 P:(DE-HGF)0 |b 6 |
| 700 | 1 | _ | |a Rohrer, Franz |0 P:(DE-Juel1)16347 |b 7 |
| 700 | 1 | _ | |a Shao, Min |0 P:(DE-HGF)0 |b 8 |
| 700 | 1 | _ | |a Sun, Kang |0 P:(DE-HGF)0 |b 9 |
| 700 | 1 | _ | |a Wu, Yusheng |0 0000-0001-7548-8272 |b 10 |
| 700 | 1 | _ | |a Zeng, Limin |0 P:(DE-HGF)0 |b 11 |
| 700 | 1 | _ | |a Zhang, Yinsong |0 P:(DE-Juel1)157908 |b 12 |
| 700 | 1 | _ | |a Zou, Qi |0 0000-0002-1218-9221 |b 13 |
| 700 | 1 | _ | |a Kiendler-Scharr, Astrid |0 P:(DE-Juel1)4528 |b 14 |
| 700 | 1 | _ | |a Wahner, Andreas |0 P:(DE-Juel1)16324 |b 15 |
| 700 | 1 | _ | |a Zhang, Yuanhang |0 P:(DE-HGF)0 |b 16 |e Corresponding author |
| 773 | _ | _ | |a 10.5194/acp-2018-801 |g p. 1 - 28 |0 PERI:(DE-600)2069857-4 |p 1 - 28 |t Atmospheric chemistry and physics / Discussions Discussions [...] |v acp-2018-801 |y 2018 |x 1680-7375 |
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