Laboratory measurements of trace gas emissions from biomass burning of fuel types from the southeastern and southwestern United States

被引:201
作者
Burling, I. R. [1 ]
Yokelson, R. J. [1 ]
Griffith, D. W. T. [2 ]
Johnson, T. J. [3 ]
Veres, P. [4 ,5 ]
Roberts, J. M. [5 ]
Warneke, C. [5 ,6 ]
Urbanski, S. P. [7 ]
Reardon, J. [7 ]
Weise, D. R. [8 ]
Hao, W. M. [7 ]
de Gouw, J. [5 ,6 ]
机构
[1] Univ Montana, Dept Chem, Missoula, MT 59812 USA
[2] Univ Wollongong, Dept Chem, Wollongong, NSW 2522, Australia
[3] Pacific NW Natl Lab, Richland, WA 99354 USA
[4] Univ Colorado, Dept Chem & Biochem, Boulder, CO 80309 USA
[5] Natl Ocean & Atmospher Adm, Earth Syst Res Lab, Div Chem Sci, Boulder, CO 80305 USA
[6] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[7] US Forest Serv, USDA, Rocky Mt Res Stn, Fire Sci Lab, Missoula, MT 59808 USA
[8] US Forest Serv, USDA, Pacific SW Res Stn, Forest Fire Lab, Riverside, CA USA
基金
美国国家科学基金会;
关键词
TRANSFORM INFRARED-SPECTROSCOPY; NITROUS-ACID HONO; ENGLAND AIR-QUALITY; NI-PT-CIMS; FIRE EMISSIONS; SAVANNA FIRES; HETEROGENEOUS CONVERSION; SOUTHERN-CALIFORNIA; TROPICAL FOREST; AFRICAN;
D O I
10.5194/acp-10-11115-2010
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Vegetation commonly managed by prescribed burning was collected from five southeastern and southwestern US military bases and burned under controlled conditions at the US Forest Service Fire Sciences Laboratory in Missoula, Montana. The smoke emissions were measured with a large suite of state-of-the-art instrumentation including an open-path Fourier transform infrared (OP-FTIR) spectrometer for measurement of gas-phase species. The OP-FTIR detected and quantified 19 gas-phase species in these fires: CO2, CO, CH4, C2H2, C2H4, C3H6, HCHO, HCOOH, CH3OH, CH3COOH, furan, H2O, NO, NO2, HONO, NH3, HCN, HCl, and SO2. Emission factors for these species are presented for each vegetation type burned. Gas-phase nitrous acid (HONO), an important OH precursor, was detected in the smoke from all fires. The HONO emission factors ranged from 0.15 to 0.60 g kg(-1) and were higher for the southeastern fuels. The fire-integrated molar emission ratios of HONO (relative to NOx) ranged from approximately 0.03 to 0.20, with higher values also observed for the southeastern fuels. The majority of non-methane organic compound (NMOC) emissions detected by OP-FTIR were oxygenated volatile organic compounds (OVOCs) with the total identified OVOC emissions constituting 61 +/- 12% of the total measured NMOC on a molar basis. These OVOC may undergo photolysis or further oxidation contributing to ozone formation. Elevated amounts of gas-phase HCl and SO2 were also detected during flaming combustion, with the amounts varying greatly depending on location and vegetation type. The fuels with the highest HCl emission factors were all located in the coastal regions, although HCl was also observed from fuels farther inland. Emission factors for HCl were generally higher for the southwestern fuels, particularly those found in the chaparral biome in the coastal regions of California.
引用
收藏
页码:11115 / 11130
页数:16
相关论文
共 66 条
[1]   Emission of trace gases and aerosols from biomass burning [J].
Andreae, MO ;
Merlet, P .
GLOBAL BIOGEOCHEMICAL CYCLES, 2001, 15 (04) :955-966
[2]  
[Anonymous], 1989, TECHNICAL PUBLICATIO
[3]  
Biswell H., 1999, PRESCRIBED BURNING C
[4]  
Bröske R, 2003, ATMOS CHEM PHYS, V3, P469
[5]   Review of the governing equations, computational algorithms, and other components of the models-3 Community Multiscale Air Quality (CMAQ) modeling system [J].
Byun, Daewon ;
Schere, Kenneth L. .
APPLIED MECHANICS REVIEWS, 2006, 59 (1-6) :51-77
[6]   Comprehensive laboratory measurements of biomass-burning emissions: 2. First intercomparison of open-path FTIR, PTR-MS, and GC- MS/FID/ECD [J].
Christian, TJ ;
Kleiss, B ;
Yokelson, RJ ;
Holzinger, R ;
Crutzen, PJ ;
Hao, WM ;
Shirai, T ;
Blake, DR .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2004, 109 (D2)
[7]   Comprehensive laboratory measurements of biomass-burning emissions: 1. Emissions from Indonesian, African, and other fuels [J].
Christian, TJ ;
Kleiss, B ;
Yokelson, RJ ;
Holzinger, R ;
Crutzen, PJ ;
Hao, WM ;
Saharjo, BH ;
Ward, DE .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D23)
[8]   Biomass burning and urban air pollution over the Central Mexican Plateau [J].
Crounse, J. D. ;
DeCarlo, P. F. ;
Blake, D. R. ;
Emmons, L. K. ;
Campos, T. L. ;
Apel, E. C. ;
Clarke, A. D. ;
Weinheimer, A. J. ;
McCabe, D. C. ;
Yokelson, R. J. ;
Jimenez, J. L. ;
Wennberg, P. O. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2009, 9 (14) :4929-4944
[9]   BIOMASS BURNING IN THE TROPICS - IMPACT ON ATMOSPHERIC CHEMISTRY AND BIOGEOCHEMICAL CYCLES [J].
CRUTZEN, PJ ;
ANDREAE, MO .
SCIENCE, 1990, 250 (4988) :1669-1678
[10]   Emission sources and ocean uptake of acetonitrile (CH3CN) in the atmosphere -: art. no. 4329 [J].
de Gouw, JA ;
Warneke, C ;
Parrish, DD ;
Holloway, JS ;
Trainer, M ;
Fehsenfeld, FC .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D11)