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준실시간 연속관측을 통한 제주 고산 PM2.5 OC와 EC의 계절별 사례별 특성

Semi-continuous Measurements of PM2.5 OC and EC at Gosan: Seasonal Variations and Characteristics of High-concentration Episodes

  • 한지현 (고려대학교 지구환경과학과) ;
  • 방병조 (고려대학교 지구환경과학과) ;
  • 이미혜 (고려대학교 지구환경과학과) ;
  • 윤순창 (서울대학교 지구환경과학부) ;
  • 김상우 (서울대학교 지구환경과학부) ;
  • 장임석 (국립환경과학원 대기환경과) ;
  • 강경식 (제주대학교 해양과학부)
  • Han, Jihyun (Department of Earth and Environmental Sciences, Korea University) ;
  • Bahng, Byungjo (Department of Earth and Environmental Sciences, Korea University) ;
  • Lee, Meehye (Department of Earth and Environmental Sciences, Korea University) ;
  • Yoon, Soon-Chang (Department of Earth and Environmental Sciences, Seoul University) ;
  • Kim, Sang-Woo (Department of Earth and Environmental Sciences, Seoul University) ;
  • Chang, Limseok (National Institute of Environmental Research, Air Quality Research Division) ;
  • Kang, Kyeong-Sik (College of Ocean Science, Jeju National University)
  • 투고 : 2011.12.23
  • 심사 : 2013.05.14
  • 발행 : 2013.06.30

초록

At Gosan ABC superstation in Jeju Island, we measured organic carbon (OC) and elemental carbon (EC) in $PM_{2.5}$ from October 2009 to June 2010 using a Sunset Laboratory Model-4 Semi-Continuous OC/EC Field Analyzer. It employs TOT (Thermal-Optical-Transmittance) method with NIOSH 5040 protocol and enables to continuously monitor OC and EC concentrations with 1-hour time resolution. The mean values of OC and EC for the entire period of measurements were $2.1{\pm}1.4{\mu}g/m^3$ and $0.7{\pm}0.6{\mu}g/m^3$, respectively. The OC/EC ratio was 3 and EC accounted $25{\pm}2.1%$ of total carbon (TC, TC=OC+EC). Although OC and EC showed similar trend in seasonal variation, the ratio of OC to EC was the highest in early summer when temperature was the highest and the air was affected by biomass burning in the southern part of China. In winter, the high OC and EC concentrations were likely influenced by increased coal combustion from residential heating. The high OC and EC concentrations were observed during events such as haze, dust, and the combination of the two. During the haze events, OC and EC were enhanced with increase in $PM_{10}$, $PM_{2.5}$, $SO_2$, and $NO_2$ with broad maxima. When dust occurred, both OC and EC started decreasing after reaching their maxima a couple of hours before $PM_{10}$ maximum. The peak separation of carbonaceous species and aerosol masses with time was more noticeable when haze event was followed by dust plume. These results confirm that OC and EC are key components of haze occurring in the study region.

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