Carbonaceous aerosols and pollutants over Delhi urban environment: Temporal evolution, source apportionment and radiative forcing

被引:151
作者
Bisht, D. S. [1 ]
Dumka, U. C. [2 ]
Kaskaoutis, D. G. [3 ]
Pipal, A. S. [4 ]
Srivastava, A. K. [1 ]
Soni, V. K. [5 ]
Attri, S. D. [5 ]
Sateesh, M. [5 ]
Tiwari, S. [1 ]
机构
[1] Indian Inst Trop Meteorol, New Delhi, India
[2] Aryabhatta Res Inst Observat Sci, Naini Tal, India
[3] Shiv Nadar Univ, Sch Nat Sci, Tehsil Dadri, India
[4] Savitribai Phule Pune Univ, Dept Chem, Pune, Maharashtra, India
[5] Indian Meteorol Dept, New Delhi, India
关键词
PM2.5; Carbonaceous aerosols; Inorganic ions; Agricultural burning; Radiative impact; Delhi; INDO-GANGETIC PLAIN; BIOMASS BURNING EMISSIONS; FINE PARTICULATE MATTER; SOLUBLE ORGANIC-CARBON; BLACK CARBON; OPTICAL-PROPERTIES; ELEMENTAL CARBON; CHEMICAL-COMPOSITION; MASS CONCENTRATIONS; TERPENE OZONOLYSIS;
D O I
10.1016/j.scitotenv.2015.03.083
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Particulate matter (PM2.5) samples were collected over Delhi, India during January to December 2012 and analysed for carbonaceous aerosols and inorganic ions (SO42 -and NO3-) in order to examine variations in atmospheric chemistry, combustion sources and influence of long-range transport. The PM2.5 samples are measured (offline) via medium volume air samplers and analysed gravimetrically for carbonaceous (organic carbon, OC; elemental carbon, EC) aerosols and inorganic ions (SO42 -and NO3-). Furthermore, continuous (online) measurements of PM2.5 (via Beta-attenuation analyser), black carbon (BC) mass concentration (via Magee scientific Aethalometer) and carbon monoxide (via CO-analyser) are carried out. PM2.5 (online) range from 18.2 to 500.6 mu gm(-3) (annual mean of 124.6 +/- 87.9 mu gm(-3)) exhibiting higher night-time (129.4 mu gm(-3)) than daytime (103.8 mu g m(-3)) concentrations. The online concentrations are 38% and 28% lower than the offline during night and day, respectively. In general, larger night-time concentrations are found for the BC, OC, NO3- and SO42-, which are seasonally dependent with larger differences during late post-monsoon and winter. The high correlation (R-2=0.74) between OC and EC along with the OC/EC of 7.09 (day time) and 4.55 (night-time), suggest significant influence of biomass-burning emissions (burning of wood and agricultural waste) as well as secondary organic aerosol formation during daytime. Concentrated weighted trajectory (CWT) analysis reveals that the potential sources for the carbonaceous aerosols and pollutants are local emissions within the urban environment and transported smoke from agricultural burning in northwest India during post-monsoon. BC radiative forcing estimates result in very high atmospheric heating rates (similar to 1.8-2.0 K day(-1)) due to agricultural burning effects during the 2012 post-monsoon season. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:431 / 445
页数:15
相关论文
共 121 条
[1]   Carbonaceous aerosols in a wood burning community in rural New Zealand [J].
Ancelet, Travis ;
Davy, Perry K. ;
Trompetter, William J. ;
Markwitz, Andreas ;
Weatherburn, David C. .
ATMOSPHERIC POLLUTION RESEARCH, 2013, 4 (03) :245-249
[2]   Black carbon or brown carbon?: The nature of light-absorbing carbonaceous aerosols [J].
Andreae, M. O. ;
Gelencser, A. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2006, 6 :3131-3148
[3]  
[Anonymous], 2020, Gothenburg Protocol to reduce transboundary air pollution, DOI DOI 10.5860/CHOICE.44-4512
[4]   Study of size and mass distribution of particulate matter due to crop residue burning with seasonal variation in rural area of Punjab, India [J].
Awasthi, Amit ;
Agarwal, Ravinder ;
Mittal, Susheel K. ;
Singh, Nirankar ;
Singh, Khem ;
Gupta, Prabhat K. .
JOURNAL OF ENVIRONMENTAL MONITORING, 2011, 13 (04) :1073-1081
[5]   Aerosol black carbon over a tropical coastal station in India [J].
Babu, SS ;
Moorthy, KK .
GEOPHYSICAL RESEARCH LETTERS, 2002, 29 (23) :13-1
[6]   Variations in CO, O3 and black carbon aerosol mass concentrations associated with planetary boundary layer (PBL) over tropical urban environment in India [J].
Badarinath, K. V. S. ;
Sharma, Anu Rani ;
Kharol, Shailesh Kumar ;
Prasad, V. Krishna .
JOURNAL OF ATMOSPHERIC CHEMISTRY, 2009, 62 (01) :73-86
[7]   Solar absorption by elemental and brown carbon determined from spectral observations [J].
Bahadur, Ranjit ;
Praveen, Puppala S. ;
Xu, Yangyang ;
Ramanathan, V. .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2012, 109 (43) :17366-17371
[8]   Comprehensive characterization of PM2.5 aerosols in Singapore -: art. no. 4523 [J].
Balasubramanian, R ;
Qian, WB ;
Decesari, S ;
Facchini, MC ;
Fuzzi, S .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D16)
[9]   Spatial distribution of aerosol black carbon over India during pre-monsoon season [J].
Beegum, S. Naseema ;
Moorthy, K. Krishna ;
Babu, S. Suresh ;
Satheesh, S. K. ;
Vinoj, V. ;
Badarinath, K. V. S. ;
Safai, P. D. ;
Devara, P. C. S. ;
Singh, Sacchidanand ;
Vinod ;
Durnka, U. C. ;
Pant, P. .
ATMOSPHERIC ENVIRONMENT, 2009, 43 (05) :1071-1078
[10]   Investigating the potential role of ammonia in ion chemistry of fine particulate matter formation for an urban environment [J].
Behera, Sailesh N. ;
Sharma, Mukesh .
SCIENCE OF THE TOTAL ENVIRONMENT, 2010, 408 (17) :3569-3575