Summertime oxidative potential of atmospheric PM2.5 over New Delhi: effect of aerosol ageing

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dc.contributor.author Verma, P. K.
dc.contributor.author M., Devaprasad
dc.contributor.author Dave, J.
dc.contributor.author Meena, R.
dc.contributor.author Bhowmik, H.
dc.contributor.author Tripathi, S. N.
dc.contributor.author Rastogi, N.
dc.coverage.spatial United States of America
dc.date.accessioned 2024-02-28T10:27:37Z
dc.date.available 2024-02-28T10:27:37Z
dc.date.issued 2024-04
dc.identifier.citation Verma, P. K.; M., Devaprasad; Dave, J.; Meena, R.; Bhowmik, H.; Tripathi, S. N. and Rastogi, N., "Summertime oxidative potential of atmospheric PM2.5 over New Delhi: effect of aerosol ageing", Science of The Total Environment, DOI: 10.1016/j.scitotenv.2024.170984, vol. 920, Apr. 2024.
dc.identifier.issn 0048-9697
dc.identifier.issn 1879-1026
dc.identifier.uri https://doi.org/10.1016/j.scitotenv.2024.170984
dc.identifier.uri https://repository.iitgn.ac.in/handle/123456789/9811
dc.description.abstract Exposure to elevated particulate matter (PM) concentrations in ambient air has become a major health concern over urban areas worldwide. Reactive oxygen species (ROS) generation due to ambient PM (termed as their oxidative potential, OP) is shown to play a major role in PM-induced health effects. In the present study, the OP of the ambient PM2.5 samples, collected during summer 2019 from New Delhi, were measured using the dithiothreitol (DTT) assay. Average volume-normalized OP (OPV) was 2.9 ± 1.1 nmol DTT min−1 m−3, and mass-normalized OP (OPm) was 61 ± 29 pmol DTT min−1 μg−1. The regression statistics of OPv vs chemical species show the maximum slope of OPV with the elemental carbon (EC, r2 = 0.72) followed by water-soluble organic carbon (WSOC, r2 = 0.72), and organic carbon (OC, r2 = 0.64). A strong positive correlation between OPm and secondary inorganic aerosols (SIA, such as NH4+ and NO3− mass fractions) was also observed, indicating that the sources emitting NO2 and NH3, precursors of NO3− and NH4+, also emit DTT-active species. Interestingly, the slope value of OPv vs OC for aged aerosols (OM/OC > 1.7, f44 > 0.12 and f43 < 0.04) was 1.7 times higher than relatively fresh organic aerosols (OA, OM/OC < 1.7, f44 < 0.12, f43 > 0.04). An increase in OPv and OPoc with f44 indicates the formation of more DTT active species with the ageing of OA. A linear increase in OPoc with increasing Nitrogen/Carbon (N/C) ratio suggests that nitrogenous OA have higher OP.
dc.description.statementofresponsibility by P. K. Verma, Devaprasad M., J. Dave, R. Meena, H. Bhowmik, S. N. Tripathi and N. Rastogi
dc.format.extent vol. 920
dc.language.iso en_US
dc.publisher Elsevier
dc.title Summertime oxidative potential of atmospheric PM2.5 over New Delhi: effect of aerosol ageing
dc.type Article
dc.relation.journal Science of The Total Environment


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