Measurement of black carbon (BC) by an optical method and a thermal-optical method: Intercomparison for four sites

被引:89
作者
Ahmed, Tanveer [1 ]
Dutkiewicz, Vincent A. [1 ,2 ]
Shareef, Akhtar [2 ]
Tuncel, Gurdal [3 ]
Tuncel, Semra [3 ]
Husain, Liaquat [1 ,2 ]
机构
[1] SUNY Albany, Sch Publ Hlth, Dept Environm Hlth Sci, Albany, NY 12201 USA
[2] New York State Dept Hlth, Wadsworth Ctr, Albany, NY 12201 USA
[3] Middle E Tech Univ, TR-06531 Ankara, Turkey
基金
美国国家科学基金会;
关键词
Black carbon; Whatman; 41; Transmissometer; Light absorption; ATTENUATION CROSS-SECTION; LONG-TERM EXPOSURE; ELEMENTAL CARBON; AIR-POLLUTION; NEW-YORK; AEROSOL; MORTALITY; AMBIENT; MATTER; TRACER;
D O I
10.1016/j.atmosenv.2009.09.031
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Comparison of black carbon (BC) measurements obtained by two methods was performed for aerosols samples collected on Whatman 41 (W-41) filters, using an optical method (Magee Scientific Optical Transmissometer Model OT-21) and a thermal-optical method (Sunset Laboratory Thermal-optical analyzer). Samples were collected from four sites: Albany (a small urban site, NY), Antalya (coastal site, Turkey), Whiteface Mountain (remote site, NY) and Mayville (rural site, NY). At Albany, comparison between the two methods showed excellent agreement; a least-squares regression line yielded a slope of 1.02, and r(2) = 0.88. Similar comparisons at Antalya (slope of 1.02, r(2) = 0.5) and Whiteface Mountain (slope of 0.92 and r(2) = 0.58) also gave very good relationship. At Mayville, the relationship between the two methods yielded somewhat lower regression: a slope of 0.75, and r(2) = 0.44. The data from the four locations, when plotted together, yielded an excellent agreement: a slope of 0.91, and r(2) of 0.84. Based on our measurements, it appears that optical measurement using the OT-21 can be successfully applied to determination of BC in W-41 filters. However, because of the variability in the chemical composition of BC aerosol at different locations, it is suggested that the calibration of OT-21 when using W-41 filters should be performed with a statistically significant numbers of samples for specific sites. (C) 2009 Elsevier Ltd. All rights reserved.
引用
收藏
页码:6305 / 6311
页数:7
相关论文
共 36 条
[11]   THE RELATIONSHIP BETWEEN OPTICAL ATTENUATION AND BLACK CARBON CONCENTRATION FOR AMBIENT AND SOURCE PARTICLES [J].
GUNDEL, LA ;
DOD, RL ;
ROSEN, H ;
NOVAKOV, T .
SCIENCE OF THE TOTAL ENVIRONMENT, 1984, 36 (JUN) :197-202
[12]   A time-series analysis of acidic particulate matter and daily mortality and morbidity in the Buffalo, New York, region [J].
Gwynn, RC ;
Burnett, RT ;
Thurston, GD .
ENVIRONMENTAL HEALTH PERSPECTIVES, 2000, 108 (02) :125-133
[13]   THE AETHALOMETER - AN INSTRUMENT FOR THE REAL-TIME MEASUREMENT OF OPTICAL-ABSORPTION BY AEROSOL-PARTICLES [J].
HANSEN, ADA ;
ROSEN, H ;
NOVAKOV, T .
SCIENCE OF THE TOTAL ENVIRONMENT, 1984, 36 (JUN) :191-196
[14]   Long-term trends in atmospheric concentrations of sulfate, total sulfur, and trace elements in the northeastern United States [J].
Husain, L ;
Parekh, PP ;
Dutkiewicz, VA ;
Khan, AR ;
Yang, K ;
Swami, K .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2004, 109 (D18) :D183051-12
[15]   A LONG-TERM (1975-1988) STUDY OF ATMOSPHERIC SO4(2-) - REGIONAL CONTRIBUTIONS AND CONCENTRATION TRENDS [J].
HUSAIN, L ;
DUTKIEWICZ, VA .
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1990, 24 (05) :1175-1187
[16]   MN/V RATIO AS A TRACER OF AEROSOL SULFATE TRANSPORT [J].
HUSAIN, L ;
WEBBER, JS ;
CANELLI, E ;
DUTKIEWICZ, VA ;
HALSTEAD, JA .
ATMOSPHERIC ENVIRONMENT, 1984, 18 (06) :1059-1071
[17]   Trends in atmospheric elemental carbon concentrations from 1835 to 2005 [J].
Husain, Liaquat ;
Khan, A. J. ;
Ahmed, Tanveer ;
Swami, Kamal ;
Bari, A. ;
Webber, James S. ;
Li, Jianjun .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2008, 113 (D13)
[18]   Analysis of aerosol interactions with numerical techniques for solving coagulation, nucleation, condensation, dissolution, and reversible chemistry among multiple size distributions [J].
Jacobson, MZ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2002, 107 (D19) :AAC2-1
[19]   Strong radiative heating due to the mixing state of black carbon in atmospheric aerosols [J].
Jacobson, MZ .
NATURE, 2001, 409 (6821) :695-697
[20]   The comparison between thermal-optical transmittance elemental carbon and Aethalometer black carbon measured at multiple monitoring sites [J].
Jeong, CH ;
Hopke, PK ;
Kim, E ;
Lee, DW .
ATMOSPHERIC ENVIRONMENT, 2004, 38 (31) :5193-5204