Quantification of PM2.5 organic carbon sampling artifacts in US networks

被引:127
作者
Chow, J. C. [1 ,2 ]
Watson, J. G. [1 ,2 ]
Chen, L. -W. A. [1 ]
Rice, J. [3 ]
Frank, N. H. [3 ]
机构
[1] Univ Nevada, Desert Res Inst, Div Atmospher Sci, Reno, NV 89506 USA
[2] Chinese Acad Sci, Inst Earth Environm, Xian 710075, Peoples R China
[3] US EPA, Off Air Qual Planning & Stand, Res Triangle Pk, NC USA
关键词
POLYCYCLIC AROMATIC-HYDROCARBONS; SPECIATION TRENDS NETWORK; SOUTHEASTERN AEROSOL RESEARCH; TEFLON MEMBRANE FILTERS; PARTICULATE MATTER; UNITED-STATES; AIR-QUALITY; ELEMENTAL CARBON; COMPOUNDS SOCS; POLYCHLORINATED DIBENZODIOXINS;
D O I
10.5194/acp-10-5223-2010
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Field blanks (bQF) and backup filters (quartz-fiber behind quartz-fiber filter; QBQ) have been adopted by US long-term air quality monitoring networks to estimate QPM(2.5) organic carbon (OC) sampling artifacts. This study documents bQF and QBQ carbon levels for the: 1) Interagency Monitoring of Protected Visual Environments (IMPROVE); 2) Speciation Trends Network (STN; part of the Chemical Speciation Network [CSN]); and 3) Southeastern Aerosol Research and Characterization (SEARCH) networks and examines the similarities/differences associated with network-specific sampling protocols. A higher IMPROVE sample volume and smaller filter deposit area results in PM2.5 areal density (mu g/cm(2) on filter) 3-11 times those of STN/CSN and SEARCH samples for the same ambient PM2.5 concentrations, thus reducing the relative contribution of sampling artifacts from passive OC adsorption. A relatively short (1-15 min) passive exposure period of STN/CSN and SEARCH bQF OC (0.8-1 mu g/cm(2)) underestimates positive and negative OC artifacts resulting from passive adsorption or evaporation of semi-volatile organic compounds on quartz-fiber filters. This is supported by low STN/CSN and SEARCH bQF levels and lack of temporal or spatial variability among the sites within the networks. With a much longer period, similar to 7 days of ambient passive exposure, average IMPROVE bQF and QBQ OC are comparable (2.4 +/- 0.5 and 3.1 +/- 0.8 mu g/cm(2), respectively) and more than twice levels found in the STN/CSN and SEARCH networks. Sampling artifacts in STN/CSN were estimated from collocated IMPROVE samples based on linear regression. At six of the eight collocated sites in this study, STN/CSN bQFs underestimated OC artifacts by 11-34%. Using a preceding organic denuder in the SEARCH network minimized passive adsorption on QBQ, but OC on QBQ may not be attributed entirely to the negative sampling artifact (e. g., evaporated or volatilized OC from the front filter deposits after sample collection).
引用
收藏
页码:5223 / 5239
页数:17
相关论文
共 72 条
  • [1] [Anonymous], METHODS ASSESS CARBO
  • [2] [Anonymous], FED REG
  • [3] [Anonymous], T VISIBILITY FINE PA
  • [4] Effects of sampling artifacts and operating parameters on the performance of a semicontinuous particulate elemental carbon/organic carbon monitor
    Arhami, M
    Kuhn, T
    Fine, PM
    Delfino, RJ
    Sioutas, C
    [J]. ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2006, 40 (03) : 945 - 954
  • [5] ARP HPH, 2007, ATMOS ENVIRON
  • [6] ASHBAUGH LL, 2004, P REG GLOB PERSP HAZ
  • [7] PROBLEMS IN THE SAMPLING AND ANALYSIS OF CARBON PARTICULATE
    CADLE, SH
    GROBLICKI, PJ
    MULAWA, PA
    [J]. ATMOSPHERIC ENVIRONMENT, 1983, 17 (03) : 593 - 600
  • [8] Modeling reflectance and transmittance of quartz-fiber filter samples containing elemental carbon particles:: Implications for thermal/optical analysis
    Chen, LWA
    Chow, JC
    Watson, JG
    Moosmüller, H
    Arnott, WP
    [J]. JOURNAL OF AEROSOL SCIENCE, 2004, 35 (06) : 765 - 780
  • [9] Chow JC, 2001, AEROSOL SCI TECH, V34, P23, DOI 10.1080/027868201300081923
  • [10] THE DRI THERMAL OPTICAL REFLECTANCE CARBON ANALYSIS SYSTEM - DESCRIPTION, EVALUATION AND APPLICATIONS IN UNITED-STATES AIR-QUALITY STUDIES
    CHOW, JC
    WATSON, JG
    PRITCHETT, LC
    PIERSON, WR
    FRAZIER, CA
    PURCELL, RG
    [J]. ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1993, 27 (08): : 1185 - 1201