Aromatic hydrocarbons at urban, sub-urban, rural (8°52′N; 67°19′W) and remote sites in Venezuela

被引:22
作者
Holzinger, R
Kleiss, B
Donoso, L
Sanhueza, E
机构
[1] Max Planck Inst Chem, D-55020 Mainz, Germany
[2] Inst Venezolano Invest Cient, Atmospher Chem Lab, Caracas 1020A, Venezuela
基金
奥地利科学基金会;
关键词
toluene; benzene; proton transfer reaction mass spectrometry; traffic emissions; biomass burning; HO radical;
D O I
10.1016/S1352-2310(01)00286-2
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Using the novel on-line proton transfer reaction mass spectrometry (PTR-MS) technique, atmospheric concentrations of benzene, toluene, xylenes, and Cg-benzenes were measured in Caracas (urban), Altos de Pipe (suburban), Calabozo, (rural) and Parupa (remote), during various campaigns in 1999 and 2000. Average daytime mixing ratios measured in Caracas are 1.1, 3.2, 3.7, and 2.7 nmol/mol for benzene, toluene, xylenes, and Cg-benzenes. At the sub-urban site, located only few km from Caracas, relatively low levels (similar to 20% of the levels measured in Caracas) of these aromatic hydrocarbons were observed. At the rural site during the dry season, higher concentrations of benzene (0.15 nmol/mol) were recorded, whereas those of toluene (0.08 nmol/mol) were lower during that time. The aromatic hydrocarbon ratios in the wet season (benzene: 0.08 nmol/mol; toluene: 0.09 nmol/mol) are consistent with an aged urban plume, whereas biomass burning emissions dominate during the dry season. From rural and urban [benzene]/[toluene] ratios a mean HO concentration of 2.6 x 10(6) molecules/cm(3) was estimated during the wet season. This value must be considered an overestimate because it does not account for background concentrations which are likely for benzene and toluene. At the remote "La Gran Sabana" region (Parupa) very low mixing ratios (0.031 and 0.015 nmol/mol for benzene and toluene) are showing the pristine region to be unaffected by local sources. From the [benzene]/[toluene] ratio we deduced, that "urban" air arriving from the coastline (350 km) is likely mixed with air containing some background of benzene and toluene. Urban emissions (automobiles) should be the major source of aromatic compounds, however, during the dry season biomass burning seems to make an important contribution. (C) 2001 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:4917 / 4927
页数:11
相关论文
共 30 条
[1]   Atmospheric chemistry of VOCs and NOx [J].
Atkinson, R .
ATMOSPHERIC ENVIRONMENT, 2000, 34 (12-14) :2063-2101
[2]   GAS-PHASE TROPOSPHERIC CHEMISTRY OF ORGANIC-COMPOUNDS - A REVIEW [J].
ATKINSON, R .
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1990, 24 (01) :1-41
[3]   SPECIATED HYDROCARBON EMISSIONS FROM VEHICLES OPERATED OVER THE NORMAL SPEED RANGE ON THE ROAD [J].
BAILEY, JC ;
SCHMIDL, B ;
WILLIAMS, ML .
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1990, 24 (01) :43-52
[4]   SEASONAL-VARIATION OF ATMOSPHERIC NONMETHANE HYDROCARBONS ON THE WESTERN COAST OF BRITTANY, FRANCE [J].
BOUDRIES, H ;
TOUPANCE, G ;
DUTOT, AL .
ATMOSPHERIC ENVIRONMENT, 1994, 28 (06) :1095-1112
[5]  
CRUTZEN PJ, 1996, ANGEWANDATE CHEM INT, V35, P1756
[6]   NONMETHANE HYDROCARBONS IN REMOTE TROPICAL, CONTINENTAL, AND MARINE ATMOSPHERES [J].
GREENBERG, JP ;
ZIMMERMAN, PR .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1984, 89 (ND3) :4767-4778
[7]   HYDROCARBONS AND CARBON-MONOXIDE IN AFRICAN SAVANNAH AIR [J].
GREENBERG, JP ;
ZIMMERMAN, PR ;
CHATFIELD, RB .
GEOPHYSICAL RESEARCH LETTERS, 1985, 12 (03) :113-116
[8]   Characterization of non-methane hydrocarbons in the rural southeast United States [J].
Hagerman, LM ;
Aneja, VP ;
Lonneman, WA .
ATMOSPHERIC ENVIRONMENT, 1997, 31 (23) :4017-4038
[9]   PROTON-TRANSFER REACTION MASS-SPECTROMETRY - ONLINE TRACE GAS-ANALYSIS AT THE PPB LEVEL [J].
HANSEL, A ;
JORDAN, A ;
HOLZINGER, R ;
PRAZELLER, P ;
VOGEL, W ;
LINDINGER, W .
INTERNATIONAL JOURNAL OF MASS SPECTROMETRY, 1995, 149 :609-619
[10]   Toluene emissions from plants [J].
Heiden, AC ;
Kobel, K ;
Komenda, M ;
Koppmann, R ;
Shao, M ;
Wildt, J .
GEOPHYSICAL RESEARCH LETTERS, 1999, 26 (09) :1283-1286