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• W2138017391 abstract "In situ measurements of PM (PM2.5 and PM10) particles were carried out using a medium volume air sampler (offline) and particle number concentrations of PM were measured by a Grimm aerosol spectrophotometer (online) during the study period of 2010–2011. The morphology and elemental composition analyses of PM were performed by Scanning Electron Microscopy (SEM) and Energy Dispersive Spectrometry (EDS), respectively. The average mass concentrations of PM2.5 and PM10 were 97.2 and 242.6 µg/m 3 at roadside (RD) and 121.2 and 230.5 µg/m 3 at a semirural (SR) site, respectively. These concentrations were substantially higher than the NAAQS, WHO and USEPA standards. The highest mass and number concentrations of PM2.5 and PM10 were observed during winter, followed by those during the post-monsoon period and summer, with the lowest in the monsoon period. SEM and EDS analysis of PM indicated the presence of soot, mineral, tarballs, fly ash, aluminosilicates/silica, fluorine, carbon rich, and Cl-Na rich particles. Of these particles, soot, tarballs, and F-C rich particles dominate in PM2.5, whereas mineral, aluminosilicates, and Cl-Na rich particles dominate in PM10. The morphology and elemental composition of the particles varied over the seasons due to atmospheric processing. The highest carbon concentration (56%) was observed in PM2.5 during summer at the RD, while in the monsoon, postmonsoon period and winter the carbon concentration was ~9% lower at the RD as compared to the SR. However, the concentration of carbon in PM10 was ~38% higher at the RD as compared to SR during both summer and winter. Air mass backward trajectory cluster analysis was performed, and the results indicate that the aerosol loadings over Agra are mainly transported from the Middle East and Arabian Sea during the summer and monsoon period, while during the pre-monsoon period and winter the aerosol loadings came from the northern region, and were due to the burning of biomass and coal, as well as other local activities." @default.
• W2138017391 created "2016-06-24" @default.
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• W2138017391 date "2014-01-01" @default.
• W2138017391 modified "2023-10-03" @default.
• W2138017391 title "Study of Surface Morphology, Elemental Composition and Origin of Atmospheric Aerosols (PM2.5 and PM10) over Agra, India" @default.
• W2138017391 cites W1560749659 @default.
• W2138017391 cites W1965515554 @default.
• W2138017391 cites W1966854849 @default.
• W2138017391 cites W1977019592 @default.
• W2138017391 cites W1977279835 @default.
• W2138017391 cites W1981191512 @default.
• W2138017391 cites W1981220449 @default.
• W2138017391 cites W1982691078 @default.
• W2138017391 cites W1984394892 @default.
• W2138017391 cites W1988469779 @default.
• W2138017391 cites W1989767807 @default.
• W2138017391 cites W1994898280 @default.
• W2138017391 cites W1996032974 @default.
• W2138017391 cites W1996488940 @default.
• W2138017391 cites W1997175293 @default.
• W2138017391 cites W2001382889 @default.
• W2138017391 cites W2003949149 @default.
• W2138017391 cites W2005527134 @default.
• W2138017391 cites W2005963568 @default.
• W2138017391 cites W2006331303 @default.
• W2138017391 cites W2007441004 @default.
• W2138017391 cites W2009013300 @default.
• W2138017391 cites W2010022429 @default.
• W2138017391 cites W2014047982 @default.
• W2138017391 cites W2018409134 @default.
• W2138017391 cites W2019386450 @default.
• W2138017391 cites W2022405142 @default.
• W2138017391 cites W2029454907 @default.
• W2138017391 cites W2031888471 @default.
• W2138017391 cites W2041538630 @default.
• W2138017391 cites W2045313951 @default.
• W2138017391 cites W2045650795 @default.
• W2138017391 cites W2049024244 @default.
• W2138017391 cites W2050439389 @default.
• W2138017391 cites W2058311077 @default.
• W2138017391 cites W2060943905 @default.
• W2138017391 cites W2062801727 @default.
• W2138017391 cites W2065829262 @default.
• W2138017391 cites W2066684918 @default.
• W2138017391 cites W2075489374 @default.
• W2138017391 cites W2077663322 @default.
• W2138017391 cites W2081431827 @default.
• W2138017391 cites W2084075863 @default.
• W2138017391 cites W2085130189 @default.
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• W2138017391 doi "https://doi.org/10.4209/aaqr.2014.01.0017" @default.
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