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Fine Particle (PM 2.5 ) Composition and Trace Gas Measurements in the Yangtze Delta Region In memoriam Dr. Glen Cass K. Baumann, M.H. Bergin, W.L. Chameides, F. Ift, C.S. Kiang, J.Z. Zhao School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta K.S. Shao, X.Y. Tang, M.L. Wang, L.M. Zeng Center for Environmental Sciences, Peking University, Beijing Locations, tools, and data quality Meteorological and trace gas characteristics at SheShan Spatial trends in PM 2.5 mass and composition Seasonal comparison based on ChangShu data
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2 Sampling Locations in the Yangtze Delta
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3 SheShan LinAn
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4 Continuous Trace Gas Measurements Yangtse network station set-up The inlet box, mounted on the roof of the SheShan observatory, allowed standard addition of NO, and NO 2 (via GPT) calibration gases. A single chemiluminescence detector was utilized, alternating between NO and NOy measure modes every 2 min with instrument zeroes overlapping every 15 min. The flow controller stream selector valve assembly was housed inside resulting in a sample residence time of ~7 s. The NOy converter is a 35 cm long, 0.48 cm ID MoO tube, temperature controlled at 330 ±2 oC. All air intake surfaces were Teflon coated and T-controlled at 40 oC. SheShan Nov-99 intensive NO/NOy
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5 Discrete PM fine Measurements via Particle Composition Monitor (PCM)
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6 PCM Data Quality Ca 2+ Na + K+K+ NH 4 + Cl - NO 3 - SO 4 2- AcetFormOxalOCEC DL (ug m -3 ) 0.030.500.160.070.490.430.130.560.420.000.910.51 Bias (%) 6056203015211753186341133 STD (%) 30392218111513413930725
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7 Trace Gas Data Quality NONO y O3O3 SO 2 DL (ppbv)0.0030.311 Precision (%)± 10± 15± 2± 5 Accuracy (%)± 10± 25± 2± 5 Note: values for NO/NO y are from GIT’s research grade analyzer, and uncertainty in NO y arises from MoO conversion efficiency determined for NO 2 Q(NO 2 ) = 67 ±14 %.
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8 Average PM 2.5 and PM 10 Concentrations for SheShan November 99 PM 2.5 (ug m -3 )PM 10 (ug m -3 )PM 2.5 /PM 10 Na + 0.31 ±0.120.89 ±0.430.41 ±0.21 K+K+ 2.19 ±1.41n/a Ca 2+ 0.43 ±0.251.25 ±0.760.32 ±0.08 NH 4 + 6.49 ±3.785.99 ±2.201.05 ±0.32 SO 4 2- 14.53 ±7.3415.82 ±8.060.93 ±0.12 NO 3 - 9.04 ±5.498.83 ±5.021.01 ±0.17 Cl - 3.03 ±1.293.55 ±1.250.88 ±0.25 Acetate2.33 ±2.384.40 ±4.600.66 ±0.35 Formate0.01 ±0.010.19 ±0.08n/a Oxalate0.29 ±0.110.30 ±0.131.04 ±0.31 ± 1-sigma Major ions represented mainly in fine fraction; bulk of sodium and calcium in coarse fraction
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9 SheShan November 99 Correlations with Wind, Wind Roses NO y indicative of influence from mobile sources, i.e. the Shanghai-Hangzhou Expressway to S and E, and metropolitan Shanghai to NE SO 2 points to possible point sources to W and NE
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10 SheShan November 99 Meteorological, Trace Gas, and [PM 2.5 ] Time Series
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11 SheShan PM 2.5 and Met. Data November 99 Change in synoptic conditions on 11/14 and 11/23 (cold fronts) accompanied by sharp drops in PM 2.5 and O 3, subsequent recovery High mass on 11/24 due to agricultural burning in close vicinity to the site
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12 Sampling Locations in the Yangtze Delta
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13 Regional Comparison of PM 2.5 Composition Lowest levels at LinAn background station, but temporal fluctuations similar to ChangShu Regional influence by cold front passages (11/14 and 11/23) noticeable at both sites Signatures of sporadic local influences on top of regional trend
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14 Average Mass Composition No significant regional differences in November 99, but noticeable seasonal differences at ChangShu
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15 Seasonal/Regional Averages Seasonal differences in K + due to post- harvest biomass burning activities in November ChangShu highest Na +, Cl -, suggesting maritime influence Aerosol slightly acidic regionally; but lower variability at LinAn
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16 Comparison with Seasonal/Regional Averages at U.S. Sites ATL: Atlanta, GA – urban HV: H’ville, TN – suburban DX: Dickson, TN - rural Significantly lower [PM 2.5 ] at U.S. sites, even during summer [O 3 ] comparable in fall, much higher in summer, esp. in urban Atlanta Slightly alkaline aerosol in fall and winter, as opposed to Yangtze sites, probably due to different emission patterns
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17 Summary NH 4 +, SO 4 2-, NO 3 -, and oxalate predominantly in fine mode (PM 2.5 ); alkaline, alkaline earth cations, Cl - and acetate represented indifferently between fine and coarse (PM 10 ) modes Despite low photochemical activity during November period, O 3 buildup along with PM 2.5 concentrations after frontal passage During this buildup period, close correlation of gas phase SO 2 and particle phase SO 4 2- observed Apparent influence from roadways and point sources at SheShan indicated by NO y and SO 2 Average PM 2.5 mass concentration levels highest at ChangShu, possibly due to close vicinity of traffic sources; lowest in LinAn (background site) No regional differences in fine particle composition, but noticeable seasonal differences, especially with respect to carbonaceous species and sulfate Seasonal differences most noticeable in K + indicating influence of post-harvest burning in November Significantly (~3x) lower PM 2.5 in SE-US with tendency to slightly alcalinic aerosol in fall and winter compared to slightly acidic conditions in the Yangtze Delta region
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18 Acknowledgements Prof. Du HuiFang, Fudan University, ShangHai, for invaluable help preparing and organizing the November intensive at SheShan Ms. Wu LiBo, Fudan University, ShangHai, for indispensable help and support at the SheShan site Prof. Ding Guoan, CAMS Beijing, for patient help clearing research equipment with Chinese customs The various local site operators at ChangShu, LinAn and SheShan for their diligence and willingness to help us out with anything, anytime!!
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19 SheShan November 99 Diurnal Trends Related to Air Mass Transport Symbol code: Size=WS / color=WD Winds driven by synoptic forces rather than convective (no diurnal trend) Strong winds carry background [O 3 ] ~30-40 ppbv NO peaks in morning and high levels carried into evening Weak photochemistry indicated by O 3 and NO/NO y
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20 PCM/Andersen Comparison SheShan 11/99 - Teflon
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21 PCM/Andersen Comparison SheShan 11/99 – Quartz
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