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Magnetic characterisation of London's airborne nanoparticulate matter

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Magnetic characterisation of London's airborne nanoparticulate matter. / Muxworthy, A.R.; Lam, C.; Green, D. et al.
In: Atmospheric Environment, Vol. 287, 119292, 15.10.2022.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Muxworthy, AR, Lam, C, Green, D, Cowan, A, Maher, BA & Gonet, T 2022, 'Magnetic characterisation of London's airborne nanoparticulate matter', Atmospheric Environment, vol. 287, 119292. https://doi.org/10.1016/j.atmosenv.2022.119292

APA

Muxworthy, A. R., Lam, C., Green, D., Cowan, A., Maher, B. A., & Gonet, T. (2022). Magnetic characterisation of London's airborne nanoparticulate matter. Atmospheric Environment, 287, Article 119292. https://doi.org/10.1016/j.atmosenv.2022.119292

Vancouver

Muxworthy AR, Lam C, Green D, Cowan A, Maher BA, Gonet T. Magnetic characterisation of London's airborne nanoparticulate matter. Atmospheric Environment. 2022 Oct 15;287:119292. Epub 2022 Jul 19. doi: 10.1016/j.atmosenv.2022.119292

Author

Muxworthy, A.R. ; Lam, C. ; Green, D. et al. / Magnetic characterisation of London's airborne nanoparticulate matter. In: Atmospheric Environment. 2022 ; Vol. 287.

Bibtex

@article{db1781317b994d46b37ddfde2ebfb9dc,
title = "Magnetic characterisation of London's airborne nanoparticulate matter",
abstract = "Iron-bearing particulate matter produced by vehicle emissions is known to be toxic. To better quantify potential health risks, we have conducted the first magnetic study of a time-series of London's inhalable particulate matter (<10 μm, PM 10), captured by three monitoring stations in central London (Marylebone Road, Earl's Court Road and Oxford Street) through 2010 and 2012. We conducted room-temperature analysis on all the samples, and a limited number of samples were analysed at both high and low temperatures. The high-temperature measurements identified magnetite as the dominant magnetic phase. The low-temperature measurements revealed high numbers of nanoparticles, which, assuming magnetite, are in the grain-size range 1–4 nm. It is estimated that as much as ∼40% of the total magnetic signal at 10 K is from particles <4 nm, that are magnetically {\textquoteleft}invisible{\textquoteright} at room-temperature and are being routinely under-estimated in room temperature-based magnetic studies. From the low-temperature measurements, the total concentration of magnetite was estimated at ∼7.5%, significantly higher than previously reported. The room-temperature magnetic data were compared with other pollution data, e.g., NO X and PM 10, and meteorological data. Mass-dependent terms like the saturation magnetisation were found to display a strong correlation with NO X and PM 10, indicating a common source for these pollutants, i.e., vehicle emissions. Magnetic coercivity measurements, which are independent of abundance, and provide information on grain-size, were consistent across all three sampling localities, again suggesting a major dominant source. Relatively small variations in coercivity were correlated with meteorological events, e.g., temperature and precipitation, suggesting preferential removal of larger airborne grains, i.e., >50 nm. ",
author = "A.R. Muxworthy and C. Lam and D. Green and A. Cowan and B.A. Maher and T. Gonet",
year = "2022",
month = oct,
day = "15",
doi = "10.1016/j.atmosenv.2022.119292",
language = "English",
volume = "287",
journal = "Atmospheric Environment",
issn = "1352-2310",
publisher = "PERGAMON-ELSEVIER SCIENCE LTD",

}

RIS

TY - JOUR

T1 - Magnetic characterisation of London's airborne nanoparticulate matter

AU - Muxworthy, A.R.

AU - Lam, C.

AU - Green, D.

AU - Cowan, A.

AU - Maher, B.A.

AU - Gonet, T.

PY - 2022/10/15

Y1 - 2022/10/15

N2 - Iron-bearing particulate matter produced by vehicle emissions is known to be toxic. To better quantify potential health risks, we have conducted the first magnetic study of a time-series of London's inhalable particulate matter (<10 μm, PM 10), captured by three monitoring stations in central London (Marylebone Road, Earl's Court Road and Oxford Street) through 2010 and 2012. We conducted room-temperature analysis on all the samples, and a limited number of samples were analysed at both high and low temperatures. The high-temperature measurements identified magnetite as the dominant magnetic phase. The low-temperature measurements revealed high numbers of nanoparticles, which, assuming magnetite, are in the grain-size range 1–4 nm. It is estimated that as much as ∼40% of the total magnetic signal at 10 K is from particles <4 nm, that are magnetically ‘invisible’ at room-temperature and are being routinely under-estimated in room temperature-based magnetic studies. From the low-temperature measurements, the total concentration of magnetite was estimated at ∼7.5%, significantly higher than previously reported. The room-temperature magnetic data were compared with other pollution data, e.g., NO X and PM 10, and meteorological data. Mass-dependent terms like the saturation magnetisation were found to display a strong correlation with NO X and PM 10, indicating a common source for these pollutants, i.e., vehicle emissions. Magnetic coercivity measurements, which are independent of abundance, and provide information on grain-size, were consistent across all three sampling localities, again suggesting a major dominant source. Relatively small variations in coercivity were correlated with meteorological events, e.g., temperature and precipitation, suggesting preferential removal of larger airborne grains, i.e., >50 nm.

AB - Iron-bearing particulate matter produced by vehicle emissions is known to be toxic. To better quantify potential health risks, we have conducted the first magnetic study of a time-series of London's inhalable particulate matter (<10 μm, PM 10), captured by three monitoring stations in central London (Marylebone Road, Earl's Court Road and Oxford Street) through 2010 and 2012. We conducted room-temperature analysis on all the samples, and a limited number of samples were analysed at both high and low temperatures. The high-temperature measurements identified magnetite as the dominant magnetic phase. The low-temperature measurements revealed high numbers of nanoparticles, which, assuming magnetite, are in the grain-size range 1–4 nm. It is estimated that as much as ∼40% of the total magnetic signal at 10 K is from particles <4 nm, that are magnetically ‘invisible’ at room-temperature and are being routinely under-estimated in room temperature-based magnetic studies. From the low-temperature measurements, the total concentration of magnetite was estimated at ∼7.5%, significantly higher than previously reported. The room-temperature magnetic data were compared with other pollution data, e.g., NO X and PM 10, and meteorological data. Mass-dependent terms like the saturation magnetisation were found to display a strong correlation with NO X and PM 10, indicating a common source for these pollutants, i.e., vehicle emissions. Magnetic coercivity measurements, which are independent of abundance, and provide information on grain-size, were consistent across all three sampling localities, again suggesting a major dominant source. Relatively small variations in coercivity were correlated with meteorological events, e.g., temperature and precipitation, suggesting preferential removal of larger airborne grains, i.e., >50 nm.

U2 - 10.1016/j.atmosenv.2022.119292

DO - 10.1016/j.atmosenv.2022.119292

M3 - Journal article

VL - 287

JO - Atmospheric Environment

JF - Atmospheric Environment

SN - 1352-2310

M1 - 119292

ER -