TY - JOUR
T1 - Measurement of number and mass size distributions of light-absorbing iron oxide aerosols in liquid water with a modified single-particle soot photometer
AU - Mori, Tatsuhiro
AU - Kondo, Yutaka
AU - Goto-Azuma, Kumiko
AU - Moteki, Nobuhiro
AU - Yoshida, Atsushi
AU - Fukuda, Kaori
AU - Ogawa-Tsukagawa, Yoshimi
AU - Ohata, Sho
AU - Koike, Makoto
N1 - Funding Information:
This work was supported by the Japanese Ministry of Education, Culture, Sports, Science and Technology (MEXT); Japan Society for the Promotion of Science KAKENHI Grants (JP1604452, JP18H04140, JP19H05699, JP19K20441, JP20H04980, JP20H00638, and JP22H01294); the GRENE Arctic Climate Change Research Project; the Arctic Challenge for Sustainability (ArCS) project (JPMXD1300000000); the Arctic Challenge for Sustainability II (ArCS II) project (JPMXD1420318865); and the Environment Research and Technology Development Funds (JPMEERF20172003 and JPMEERF20202003) of the Environmental Restoration and Conservation Agency of Japan. EGRIP is supported by funding agencies and institutions in Denmark (A. P. Møller Foundation, UCPH), the United States (US NSF, Office of Polar Programs), Germany (AWI), Japan (NIPR and ArCS), Norway (BFS), Switzerland (SNF), France (IPEV, IGE), and China (CAS). The authors thank J. Matsushita, T. Aoki, F. Nakazawa, W. Shigeyama of the National Institute of Polar Research; A. Sato, formerly of the Snow and Ice Research Center; A. Tsushima of Chiba University; S. Omiya of the Civil Engineering Research Institute for Cold Region; S. Matoba, A. Sugimoto, and S. Takano of Hokkaido University; M. Schneebeli and K. Steffen of the WSL Institute for Snow and Avalanche Research; and the staff of the Norwegian Polar Institute for collecting the precipitation samples at Ny-Ålesund and melted snow (i.e., surface, subsurface, snowpack, and pit) samples from Alaska, Finland, North Siberia, Ny-Ålesund, and Greenland. The pit samples were collected under The East Greenland Ice-Core Project (EGRIP) directed and organized by the Center of Ice and Climate at the Niels Bohr Institute and US NSF, Office of Polar Programs. We also thank K. Adachi of Meteorological Research Institute for useful comments on FeOx on dust particles.
Publisher Copyright:
© 2022 The Author(s). Published with license by Taylor & Francis Group, LLC.
PY - 2022
Y1 - 2022
N2 - Here, we used a modified single-particle soot photometer (SP2) coupled with a concentric pneumatic nebulizer to measure the size-resolved number and mass concentrations of light-absorbing iron oxide aerosols (FeOx) in liquid water (C NFeOx and C MFeOx, respectively). The SP2 could selectively detect individual FeOx particles in mixed wüstite–fullerene soot laboratory samples and melted Arctic snow samples. The nebulizer efficiency for FeOx particles was about 50% within the 70–650 nm diameter range, as derived from the ratio of the volume of ammonium sulfate before and after extraction by the nebulizer and the size-resolved transmission efficiency in the nebulizer–SP2 sampling line. Uncertainty from the boundary lines empirically drawn to discriminate the scatterplots of FeOx and black carbon in the mixed wüstite–fullerene soot suspensions and snow samples was approximately 3.0% and 10%, respectively. Overall uncertainty in total C NFeOx and C MFeOx (220–1400 nm) was approximately 19% and 18%, respectively. After storage at 4 °C for 16 months, the FeOx particle size distributions in melted Arctic snow had remained stable, and C NFeOx and C MFeOx had changed by less than 19% and 1.0%, on average, respectively. Most of the FeOx on dust particles measured by this system was estimated to be in the diameter range smaller than 1000 nm, considering the nebulizer efficiency for dust particles. The high accuracy of the C NFeOx and C MFeOx measurements will help to improve our quantitative understanding of the wet deposition of FeOx and provide more accurate estimates of the effects of FeOx on snow surface albedo.
AB - Here, we used a modified single-particle soot photometer (SP2) coupled with a concentric pneumatic nebulizer to measure the size-resolved number and mass concentrations of light-absorbing iron oxide aerosols (FeOx) in liquid water (C NFeOx and C MFeOx, respectively). The SP2 could selectively detect individual FeOx particles in mixed wüstite–fullerene soot laboratory samples and melted Arctic snow samples. The nebulizer efficiency for FeOx particles was about 50% within the 70–650 nm diameter range, as derived from the ratio of the volume of ammonium sulfate before and after extraction by the nebulizer and the size-resolved transmission efficiency in the nebulizer–SP2 sampling line. Uncertainty from the boundary lines empirically drawn to discriminate the scatterplots of FeOx and black carbon in the mixed wüstite–fullerene soot suspensions and snow samples was approximately 3.0% and 10%, respectively. Overall uncertainty in total C NFeOx and C MFeOx (220–1400 nm) was approximately 19% and 18%, respectively. After storage at 4 °C for 16 months, the FeOx particle size distributions in melted Arctic snow had remained stable, and C NFeOx and C MFeOx had changed by less than 19% and 1.0%, on average, respectively. Most of the FeOx on dust particles measured by this system was estimated to be in the diameter range smaller than 1000 nm, considering the nebulizer efficiency for dust particles. The high accuracy of the C NFeOx and C MFeOx measurements will help to improve our quantitative understanding of the wet deposition of FeOx and provide more accurate estimates of the effects of FeOx on snow surface albedo.
KW - Hans Moosmüller
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U2 - 10.1080/02786826.2022.2144113
DO - 10.1080/02786826.2022.2144113
M3 - Article
AN - SCOPUS:85142870069
SN - 0278-6826
VL - 57
SP - 35
EP - 49
JO - Aerosol Science and Technology
JF - Aerosol Science and Technology
IS - 1
ER -