Nitrated phenols in the atmosphere: a review

被引:350
作者
Harrison, MAJ
Barra, S
Borghesi, D
Vione, D
Arsene, C
Olariu, RL
机构
[1] Univ Edinburgh, Dept Chem, Edinburgh EH9 3JJ, Midlothian, Scotland
[2] Univ Turin, Dipartimento Chim Analit, I-10125 Turin, Italy
[3] Al I Cuza Univ Iasi, Fac Chem, Dept Analyt Chem, Iasi 700506, Romania
关键词
nitrophenols; nitroaromatic compounds; nitration; semivolatile organic compounds; phytotoxicity;
D O I
10.1016/j.atmosenv.2004.09.044
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This paper reviews the data concerning the atmospheric occurrence of nitrophenols, both in the gas and in the condensed phase (rainwater, cloud, fog and snow). Data obtained from field campaigns are reported, together with a description of the analytical techniques employed for the identification and quantification of nitrophenols. Analysis is usually performed using techniques such as High Performance Liquid Chromatography (HPLC) or Gas Chromatography-Mass Spectrometry (GC-MS), with the sampling method largely determined according to the matrix under investigation. The sources of atmospheric nitrophenols include direct emissions resulting from combustion processes, hydrolysis of pesticides (e.g. parathion) and the secondary formation of nitrophenols in the atmosphere. Atmospheric nitration of phenol can take place both in the gas and liquid phases, but the relative importance of these processes is still under discussion. The gas-phase nitration involves reaction between phenol and *OH+ *NO2 during the day or *NO3 + *NO2 during the night. Gas-phase nitration during the day yields only 2-nitrophenol (2-NP); while during the night it is thought that both 2-NP and 4-nitrophenol (4-NP) may be formed. Because of many gaps in the experimental evidence it is apparent that more research is required to indicate whether the 4-NP present in the environment can be accounted for by this nighttime process. Nitration in the condensed phase can be initiated by electrophilic nitration agents such as N2O5 and CINO2. Other liquid-phase processes can also take place, in the presence of *NO3, nitrate and nitrite, in the dark and under irradiation. Condensed-phase processes have been shown to yield 2-and 4-NP in similar amounts. It is also important to consider the atmospheric sinks of nitrophenols. The rate constant for the reaction between 2-NP and *OH in the gas phase is rather low (9.0 X 10(-13) cm(3) molecule(-1) s(-1)), while incomplete data are available for the reaction with *NO3. In addition, condensed-phase processes might also represent an important nitrophenol sink. Potential loss routes include the reaction with radicals such as *OH and *NO3 in aqueous solution as well as the nitration to form the dinitrophenols. (C) 2004 Elsevier Ltd. All rights reserved.
引用
收藏
页码:231 / 248
页数:18
相关论文
共 139 条
[1]   PHOTOCHEMISTRY AND ENVIRONMENT .14. PHOTOTRANSFORMATION OF NITROPHENOLS INDUCED BY EXCITATION OF NITRITE AND NITRATE IONS [J].
ALIF, A ;
BOULE, P .
JOURNAL OF PHOTOCHEMISTRY AND PHOTOBIOLOGY A-CHEMISTRY, 1991, 59 (03) :357-367
[2]   THE NITROUS ACID-CATALYZED NITRATION OF PHENOL [J].
ALOBAIDI, U ;
MOODIE, RB .
JOURNAL OF THE CHEMICAL SOCIETY-PERKIN TRANSACTIONS 2, 1985, (03) :467-472
[3]   Chemistry of fog waters in California's Central Valley: 1. In situ photoformation of hydroxyl radical and singlet molecular oxygen [J].
Anastasio, C ;
McGregor, KG .
ATMOSPHERIC ENVIRONMENT, 2001, 35 (06) :1079-1089
[4]   pH dependent photoformation of hydroxyl radical and absorbance of aqueous-phase N(III) (HNO2 and NO2-) [J].
Arakaki, T ;
Miyake, T ;
Hirakawa, T ;
Sakugawa, H .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1999, 33 (15) :2561-2565
[5]  
AREY J, 1998, PAHS RELATED COMPOUN, P347
[6]   Visible spectroscopy of aerosol particles collected on filters: iron-oxide minerals [J].
Arimoto, R ;
Balsam, W ;
Schloesslin, C .
ATMOSPHERIC ENVIRONMENT, 2002, 36 (01) :89-96
[7]   REACTIONS OF OH AND NO3 RADICALS WITH PHENOL, CRESOLS, AND 2-NITROPHENOL AT 296-K+-2-K [J].
ATKINSON, R ;
ASCHMANN, SM ;
AREY, J .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1992, 26 (07) :1397-1403
[8]   Atmospheric chemistry of VOCs and NOx [J].
Atkinson, R .
ATMOSPHERIC ENVIRONMENT, 2000, 34 (12-14) :2063-2101
[9]   Gas-phase degradation of organic compounds in the troposphere [J].
Atkinson, R .
PURE AND APPLIED CHEMISTRY, 1998, 70 (07) :1327-1334
[10]  
ATKINSON R, 1994, J PHYS CHEM REFENCE