기관회원 [로그인]
소속기관에서 받은 아이디, 비밀번호를 입력해 주세요.
개인회원 [로그인]

비회원 구매시 입력하신 핸드폰번호를 입력해 주세요.
본인 인증 후 구매내역을 확인하실 수 있습니다.

회원가입
서지반출
황사 시 제주지역 에어로졸의 수농도 특성
[STEP1]서지반출 형식 선택
파일형식
@
서지도구
SNS
기타
[STEP2]서지반출 정보 선택
  • 제목
  • URL
돌아가기
확인
취소
  • 황사 시 제주지역 에어로졸의 수농도 특성
저자명
강창희,허철구,Kang. Chang-Hee,Hu. Chul-Goo
간행물명
Journal of environmental science international
권/호정보
2013년|22권 3호|pp.347-358 (12 pages)
발행정보
한국환경과학회
파일정보
정기간행물|
PDF텍스트
주제분야
기타
이 논문은 한국과학기술정보연구원과 논문 연계를 통해 무료로 제공되는 원문입니다.
서지반출

기타언어초록

The aerosol number concentration have measured with an aerodynamic particle sizer spectrometer(APS) at Gosan in Jeju Island, which is known as background area in Korea, from March 2010 to February 2011. The obtained results of asian dust events and non-asian dust period have been compared. The results show that the entire averaged aerosol number concentration from APS measurement during asian dust events and non-asian dust period are about 341 particles/$cm^3$ and 240 particles/$cm^3$, respectively. During asian dust events, the number concentration in small size ranges(${leq}0.4{mu}m$) are similar to non-asian dust period, however, those in large size ranges(${geq}0.7{mu}m$) are very higher than non-asian dust period. The contributions of the size resolved number concentration(23 channel in $0.25{sim}10.0{mu}m$) to total number concentration in that range are dramatically decreased with increased particle size. The contributions of smaller size ranges(${leq}0.4{mu}m$) during asian dust events are very low compared with non-asian dust period, on the other hand, those of larger size ranges(${geq}0.4{mu}m$) are higher than non-asian dust period. The number concentration in each size range are strongly correlated with the concentration in adjacent size range. And the total aerosol number concentration are depended on the number concentration in range of smaller than $0.58{mu}m$ during non-asian dust period and asian dust events. On the other hand, $PM_{10}$ mass concentration has mainly affected with the number concentration in range of smaller than $1.0{mu}m$ during non-asian dust period, however, during asian dust events, the mass concentration has mainly affected with the number concentration in range of $0.65{sim}3.0{mu}m$.