A11G-0151
Carbon and nitrogen isotopic composition of PM2.5 at a periurban Mt. Taehwa near Seoul and over the Yellow Sea

Monday, 14 December 2015
Poster Hall (Moscone South)
Saehee LIM1, Taekyu Joo1, Meehye Lee2, Claudia I Czimczik3, Sandra R Holden4, Gergana Mouteva4, Guaciara Santos4, Xiaomei Xu4, Saewung Kim4, Gangnam Cho5, Jungmin Park6, Beomcheol Shin7 and Sang-boom Ryoo8, (1)Korea University, Seoul, South Korea, (2)Korea Univ, Seoul, South Korea, (3)University of California Irvine, Earth System Science, Irvine, CA, United States, (4)University of California Irvine, Irvine, CA, United States, (5)3National institute of environmental research (NIER), Incheon, South Korea, (6)NIER National Institute of Environmental Research, Incheon, South Korea, (7)National Institute of Meteorological Research, Asian Dust Research Laboratory, Seoul, South Korea, (8)NIMR/KMA, Seoul, South Korea
Abstract:
Fine particular matter (PM2.5) is a major contributor to poor air quality in East Asia, with detrimental effects on air quality and climate. The elemental and isotopic composition of PM2.5 is powerful proxy for identifying emission sources, understanding atmospheric processing, and mitigating emissions of PM2.5. Here, we present a time-series of the elemental and isotopic composition of PM2.5 in East Asia, sampled at a periurban site (Mt. Taehwa, South Korea, August - October 2014) and over the Yellow Sea (onboard RV Gisang 1, November 2014). We measured the radiocarbon (14C) content of total carbon (TC) and elemental carbon (EC) with accelerator mass spectrometry and the carbon and nitrogen elemental and stable isotopic composition of bulk PM2.5 with isotope ratio mass spectrometry. At Mt. Taehwa, EC was depleted in 14C (fM-EC=0.224±0.071 (ave±SD, n=6)). The bulk PM2.5 was enriched in 14C above natural levels (fM-TC=1.19±0.47, n=9), with a δ13C of -25.6±0.5 (n=7), and a δ15N of 14.6±3.8 (n=4), and was strongly enriched in nitrogen (C:N=2.8±1.4, n=16). Over the Yellow Sea, bulk PM2.5 was depleted in 14C (fM-TC=0.57±0.07, n=5), with a δ13C of -24.2±0.8 (n=3), and a δ15N of 5.2±4.3 (n=3); EC was too small for 14C analysis.

 Our results confirm that periurban Mt. Taehwa site is exposed to combustion plumes of fossil fuels, especially from on-road sources. PM2.5 over the Yellow Sea turned out to be a mixture of fossil and biogenic emissions and experience more intense atmospheric processes. This isotope-based source apportionment of PM2.5 is a first step to characterize major sources of aerosols at Taehwa Research Forest, which was established to examine interactions of megacity and biogenic emissions and their impact on air quality.