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Assessment of equivalent black carbon variations and its source apportionment over Varanasi, Indo-Gangetic Basin
被引:3
|作者:
Chauhan, Prashant Kumar
[1
]
Tiwari, Shani
[2
,3
]
Gupta, Dileep Kumar
[1
]
Kumar, Akhilesh
[4
]
Pratap, Vineet
[1
]
Singh, Abhay Kumar
[1
,5
,6
]
机构:
[1] Banaras Hindu Univ, Inst Sci, Dept Phys, Varanasi 221005, India
[2] CSIR Natl Inst Oceanog, Aerosol & Cloud Res Lab, Panaji 403004, Goa, India
[3] Acad Sci & Innovat Res AcSIR, Ghaziabad, India
[4] Kashi Naresh Govt Post Grad Coll Gyanpur, Bhadohi 221304, India
[5] Banaras Hindu Univ, DST Mahamana Ctr Excellence Climate Change Res, Varanasi, India
[6] Banaras Hindu Univ, Inst Sci, Dept Phys, Atmospher Res Lab, Varanasi 221005, Uttar Pradesh, India
关键词:
Black carbon (BC);
Biomass burning;
Fossil fuel;
Fire counts;
Indo-Gangetic Basin;
Long range transport;
BIOMASS BURNING AEROSOLS;
FOSSIL-FUEL CONTRIBUTION;
SEASONAL-VARIATIONS;
SOOT PARTICLES;
URBAN LOCATION;
HIGH-ALTITUDE;
SOUTH-ASIA;
DELHI;
PLAIN;
ABSORPTION;
D O I:
10.1016/j.apr.2024.102061
中图分类号:
X [环境科学、安全科学];
学科分类号:
08 ;
0830 ;
摘要:
In this study, the temporal variation of Equivalent Black Carbon (eBC) and its source apportionment is studied using a yearlong (Dec. 2020-Nov. 2021) multiwavelength Aethalometer (AE-33 model) measurements over Varanasi, located in the central Indo-Gangetic Basin (IGB). Results suggest that mean mass concentrations of eBC vary in the range between 0.46 +/- 0.13 to 11.22 +/- 5.09 mu g m(-3) with an annual mean value of similar to 3.57 +/- 2.39 mu g m(- 3) during the study period. A strong temporal variation in eBC and its components i.e., eBCff (eBC from fossil fuel), and eBCbb (eBC from biomass burning) are found which shows a large variation on different temporal scales with an average value during winter (6.21 +/- 3.56 mu g m(-3)), summer (5.09 +/- 3.61 mu g m(-3)), monsoon season (1.52 +/- 1.03 mu g m(-3)), and post-monsoon (3.75 +/- 2.68 mu g m(- 3)). The diurnal variation of eBC shows two different maxima between 07:00-08:00 a.m. and 08:00-10:00 p.m. An inverse relationship between eBC concentration and all meteorological parameters (temperature, wind speed, and boundary layer height) is found except relative humidity. The concentration of eBC increases with respect to RH (up to 70 %) suggesting hygroscopic growth while for higher RH (>70 %) value, eBC concentration decreases and indicates the possible wet scavenging processes in the atmosphere. Source apportionment of eBC using the "Aethalometer Model" reveals that eBCff is dominant over eBCbb in total eBC loading during the study period. Cluster analysis of HYSPLIT (Hybrid Single Particle Lagrangian Integrated Trajectory) model computed five days airmass back-trajectory suggests that airmass reached at Varanasi passes through a highly dense fire count region over the northwestern IGB and surrounding which could be the most responsible for the black carbon loading over the study region.
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页数:15
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