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Diurnal and seasonal cycles of ozone precursors observed from continuous measurement at urban site in Taiwan Kuang-Ling Yang, Chien-Chung Ting, Jia-Lin.

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Presentation on theme: "Diurnal and seasonal cycles of ozone precursors observed from continuous measurement at urban site in Taiwan Kuang-Ling Yang, Chien-Chung Ting, Jia-Lin."— Presentation transcript:

1 Diurnal and seasonal cycles of ozone precursors observed from continuous measurement at urban site in Taiwan Kuang-Ling Yang, Chien-Chung Ting, Jia-Lin wang, Oliver W. Wingenter, Chang-Chuan Chan

2 VOCs measurement http://www.showmecleanair.com/images/ozone_chart.jpg 2

3 Monitoring site description Fig. (a) Satellite mapping of Taiwan. Fig. (b) The enlarged area in (a) shows the deployment of the three stations in central Taiwan.

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5 Instrumental condition Auto-GC system in monitoring station (Perkin-Elmer, USA) A cryogen-free sorbent trap (Peltier cooling device, -30)with dual columns and dual FIDs was configured to cope with wide volatility range of components. Excess water vapor is removed by Nafion dryer. Denas’ switch Columns : DB-1 (60m x 0.25mm x 1μm) C 6 -C 12 PLOT (30m x 0.25mm x 8 μm) C 2 -C 5

6 Dual-trap dual-column GC system

7 Aspect on data quality control 56 target compounds with absolute concentration range 20 to 40 ppb C prepared by gravimetric method (Spctra gases). The hourly measurement within a day comprised 23 ambient sample injections plus one standard gas injection.

8 Emission source LPG leakage Gasoline evaporation Biogenic emission Vehicular exhaust Ethane, propane benzenebenzene Isoprene

9 Results and discussion

10 Fig. (a) benzene in February; (b)m, p-xylene in February

11 Fig. (a) Propane in February; (b)ethane in February

12 Fig. (a) Isoprene in February; (b)Isoprene in August

13 Diurnal and seasonal

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18 Conclusion For species such as ethane and propane with relatively constant source characteristics, the change in mixing height is the dominant factor modulating abundance to reveal characteristic diurnal patterns. Chemical removal is only important from the seasonal point of view, which together with temperature inversion caused the observed seasonal variations


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