Your browser doesn't support javascript.
loading
Summertime oxidative potential of atmospheric PM2.5 over New Delhi: Effect of aerosol ageing.
Verma, P K; Devaprasad, M; Dave, J; Meena, R; Bhowmik, H; Tripathi, S N; Rastogi, N.
Afiliação
  • Verma PK; Geosciences Division, Physical Research Laboratory, Ahmedabad, Gujarat 380009, India. Electronic address: pkvrs.13@gmail.com.
  • Devaprasad M; Geosciences Division, Physical Research Laboratory, Ahmedabad, Gujarat 380009, India; Indian Institute of Technology, Gandhinagar, Gujarat 382355, India.
  • Dave J; Geosciences Division, Physical Research Laboratory, Ahmedabad, Gujarat 380009, India.
  • Meena R; Geosciences Division, Physical Research Laboratory, Ahmedabad, Gujarat 380009, India.
  • Bhowmik H; Department of Civil Engineering, Indian Institute of Technology, Kanpur, Uttar Pradesh 208016, India.
  • Tripathi SN; Department of Civil Engineering, Indian Institute of Technology, Kanpur, Uttar Pradesh 208016, India.
  • Rastogi N; Geosciences Division, Physical Research Laboratory, Ahmedabad, Gujarat 380009, India. Electronic address: nrastogi@prl.res.in.
Sci Total Environ ; 920: 170984, 2024 Apr 10.
Article em En | MEDLINE | ID: mdl-38365025
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.
Palavras-chave

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: Sci Total Environ Ano de publicação: 2024 Tipo de documento: Article

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: Sci Total Environ Ano de publicação: 2024 Tipo de documento: Article