Characterization of the Sunset Semi-Continuous Carbon Aerosol Analyzer

被引:110
作者
Bauer, Jace J. [2 ]
Yu, Xiao-Ying [1 ]
Cary, Robert [3 ]
Laulainen, Nels [1 ]
Berkowitz, Carl [1 ]
机构
[1] Pacific NW Natl Lab, Div Atmospher Sci & Global Change, Richland, WA 99352 USA
[2] Purdue Univ, Dept Earth & Atmospher Sci, W Lafayette, IN 47907 USA
[3] Sunset Lab Inc, Tigard, OR USA
关键词
THERMAL-OPTICAL METHOD; ELEMENTAL CARBON; ORGANIC-CARBON; REGRESSION; PARTICLES; ARTIFACTS;
D O I
10.3155/1047-3289.59.7.826
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The field-deployable Sunset Semi-Continuous Organic Carbon/Elemental Carbon (Sunset OCEC) aerosol analyzer utilizes the modified National Institute for Occupational Safety and Health thermal-optical method to determine total carbon (TC), organic carbon (OC),. and elemental carbon (EC) at near real-time. Two sets of OC and EC are available: thermal OC and EC, and optical OC and EC. The former is obtained by the thermal-optical approach, and the latter is obtained by directly determining EC optically and deriving optical OC from TC. However, the performance of the Sunset OCEC is not yet fully characterized. Two collocated Sunset OCEC analyzers, Unit A and Unit B, were used to determine the pooled relative standard deviation (RSD) and limit of detection (LOD) between September 18 and November 6, 2007 in Richland, WA. The LOD of Unit A was approximately 0.2 mu gC/m(3) (0.1 mu gC/cm(2)) for TC, optical OC, and thermal OC, and 0.01 mu gC/m(3) (0.01 mu gC/cm(2)) for optical EC. Similarly, Unit B had an LOD of approximately 0.3 mu gC/m(3) (0.2 mu gC/cm(2)) for TC, optical OC, and thermal OC, and 0.02 mu gC/m(3) (0.01 mu gC/cm(2)) for optical EC. The LOD for thermal EC is estimated to be 0.2 [mu gC/m(3) (0.1 mu gC/cm(2)) for both units. The pooled RSDs were 4.9% for TC (carbon mass loadings 0.6-6.0 mu gC/cm(2)), 5.6% for optical OC (carbon mass loadings 0.6-5.4 mu gC/cm(2)), 5.3% for thermal OC (carbon mass loadings 0.6-5.3 mu gC/cm(2)), and 9.6% for optical EC (carbon mass loadings 0-1.4 mu gC/cm(2)), which indicates good precision between the instruments. The RSD for thermal EC is higher at 24.3% (carbon mass loadings 0-1.2 mu gC/cm(2)). Low EC mass loadings in Richland contributed to the poor RSD of EC. The authors found that excessive noise from the non-dispersive infrared (NDIR) laser in the Sunset OCEC analyzer could result in a worsened determination of OC and EC. It is recommended. that a "quieter" NDIR laser and detector be used in the Sunset OCEC analyzer to improve quantification. Future work should re-evaluate the precision of the EC parameters in an environment favorable for EC collection. Investigation among quantification differences using various thermal-optical protocols to determine OC and EC is also in need.
引用
收藏
页码:826 / 833
页数:8
相关论文
共 19 条
[1]  
[Anonymous], 2007, CLIMATE CHANGE 2007
[2]   Effects of sampling artifacts and operating parameters on the performance of a semicontinuous particulate elemental carbon/organic carbon monitor [J].
Arhami, M ;
Kuhn, T ;
Fine, PM ;
Delfino, RJ ;
Sioutas, C .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2006, 40 (03) :945-954
[3]  
Armitage P., 2002, STAT METHODS MED RES
[4]   Validation of a semi-continuous instrument for elemental carbon and organic carbon using a thermal-optical method [J].
Bae, MS ;
Schauer, JJ ;
DeMinter, JT ;
Turner, JR ;
Smith, D ;
Cary, RA .
ATMOSPHERIC ENVIRONMENT, 2004, 38 (18) :2885-2893
[5]   Light absorption by carbonaceous particles: An investigative review [J].
Bond, TC ;
Bergstrom, RW .
AEROSOL SCIENCE AND TECHNOLOGY, 2006, 40 (01) :27-67
[6]  
CARY RA, 2004, SEMICONTINUOUS OCEC
[7]  
Chow JC, 2001, AEROSOL SCI TECH, V34, P23, DOI 10.1080/027868201300081923
[8]   Comparison of PM2.5 carbon measurement methods in Hong Kong, China [J].
Chow, JC ;
Watson, JG ;
Louie, PKK ;
Chen, LWA ;
Sin, D .
ENVIRONMENTAL POLLUTION, 2005, 137 (02) :334-344
[9]  
CORNBLEET PJ, 1979, CLIN CHEM, V25, P432
[10]   Measurements of organic and elemental carbon in Asian outflow during ACE-Asia from the NSF/NCAR C-130 [J].
Huebert, B ;
Bertram, T ;
Kline, J ;
Howell, S ;
Eatough, D ;
Blomquist, B .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2004, 109 (D19) :D19S111-16