Javascript is required
[1] Japan Meteorological Agency, https://www.jma.go.jp/jma/menu/menureport.html
[2] Otani, Shinji, et al., Dust storms from degraded drylands of Asia: dynamics and health impacts. Land, 6(4), p. 83, 2017.
[3] Shimizu, Atsushi, et al., Variations of Dust Extinction Coefficient Estimated by Lidar Observations over Japan, 2007–2016. SOLA, 13, pp. 205–208, 2017.
[4] Kanatani, Kumiko T., et al., Effect of desert dust exposure on allergic symptoms: a natural experiment in Japan. Annals of Allergy, Asthma & Immunology, 116(5), pp. 425–430, 2016.
[5] A, Wang, Qingyue, et al. Size-segregated Allergenic Particles Released from Airborne Cryptomeria japonica Pollen Grains during the Yellow Sand Events within the Pollen Scattering Seasons. Asian Journal of Atmospheric Environment (AJAE), 7(4), pp.191–198, 2013.
[6] Watanabe, Masanari, et al., Correlation between Asian dust storms and worsening asthma in Western Japan. Allergology International, 60(3), pp. 267–275, 2011.
[7] Dias, G.M., Differentiating natural and anthropogenic sources of metals to the environment. Human and Ecological Risk Assessment, 9(4), pp. 699–721, 2003.
[8] Tsai, Y.I., Characterization of Asian dust storm and non-Asian dust storm PM2.5 aerosol in southern Taiwan. Atmospheric Environment, 40(25), pp. 4734–4750, 2006.
[9] Saitama Prefecture air pollution continuous monitoring system, http://www.taiki-kansi.pref.saitama.lg.jp/
[10] Wang, qingyue & Weiqian, Wang, Survey of inorganic components in atmospheric particles of three urban areas caused by winter energy consumption in China and Japan. WIT Transactions on Ecology and the Environment, 217, pp. 469–479, 2018.
[11] Squizzato, S., et al., Factors determining the formation of secondary inorganic aerosol: a case study in the Po Valley (Italy). Atmospheric chemistry and physics, 13(4), pp. 1927–1939, 2013.
[12] Zhang, Yy., Chemical characteristics of PM2.5 during 2015 spring festival in Beijing, China. Aerosol and Air Quality Research , 17(5), pp. 1169–1180, 2017.
[13] Wang, Y., The variation of characteristics and formation mechanisms of aerosols in dust, haze, and clear days in Beijing. Atmospheric Environment, 40(34), pp. 6579–6591, 2006.
[14] Tan, J-H., Source of atmospheric heavy metals in winter in Foshan, China. Science of the Total Environment, 493, pp. 262–270, 2014.
[15] Bilos, C., Sources, distribution and variability of airborne trace metals in La Plata City area, Argentina. Environmental pollution, 111(1), p. 1, 2001.
[16] Arditsoglou, A., Levels of total suspended particulate matter and major trace elements in Kosovo: a source identification and apportionment study. Chemosphere, 59(5), pp. 669–678, 2005.
Search

Acadlore takes over the publication of IJEI from 2025 Vol. 8, No. 5. The preceding volumes were published under a CC BY 4.0 license by the previous owner, and displayed here as agreed between Acadlore and the previous owner. ✯ : This issue/volume is not published by Acadlore.

Open Access
Research article

Chemical Characteristics of Water-Soluble Ions and Metal Elements in Ambient Particles of Saitama, Japan During the Spring Asian Dust Event, 2017

Weiqian Wang,
Qingyue Wang
Graduate School of Science and Engineering, Saitama University, Japan
International Journal of Environmental Impacts
|
Volume 2, Issue 4, 2019
|
Pages 336-345
Received: N/A,
Revised: N/A,
Accepted: N/A,
Available online: N/A
View Full Article|Download PDF

Abstract:

Metropolitan Tokyo area in Japan suffered from a strong Asian dust event which was lasted for 3 days from May 6 to May 8 in 2017. Asian dust particles are usually originated from the deserts of Mongolia and Kazakhstan and could be absorbed air pollutants contained the metals, water-soluble and organic matters during transport process. In this research, two sampling sites called 10F (30m height above ground level) and roadside in Saitama were selected to collect five different size particles (PM1.1, PM1.1–2.0, PM2.0–3.3, PM3.3–7.0 and the coarse particles (>7.0 μm) of three different events: (1) before Asian dust event (B.A.), (2) during Asian dust event (D.A.) and (3) after Asian dust event (A.A.). Eight watersoluble ionic and 23 elemental species in D.A. event were higher than other periods. In D.A. event, the ionic contents in 10F were high to 10.3 μg/m3 and the elemental contents in roadside were 6.50 μg/m3 which were higher than those in roadside. Ionic contents were mainly distributed in PM1.1 with the high contents of secondary particles (NH4+, NO3 and SO42−). Ca2+, Cl and Na+ were more enriched in the coarse particles. Ion balance in D.A. event was more basic in 10F and more acidic in roadside. The higher ratios of NO3/SO42− in PM1.1 were also occurred in D.A. event. Total elements were high (6,050 ng/m3) in 10F with the several times increasing in PM3.3–7.0 and the coarse particles, and the great contribution form the crustal elements (Al, Fe, Na, Mg and K). Enrichment factors (EFs) of trace elements in PM1.1 indicating the anthropogenic sources might be the main sources of those ions. EFs in the coarse particles indicating high concentrations of crustal elements might be affected by the Asian dust event. The analysis of air masses backward trajectories showed that the deserts of Mongolia and Kazakhstan and the northern part of China were the important air pollutant origins in Asian dust events with long-distance transport.

Keywords: Asian dust, metal elements, Saitama, water-soluble inorganic ions

Data Availability

The data used to support the findings of this study are available from the corresponding author upon request.

Conflicts of Interest

The authors declare that they have no conflicts of interest.

References
[1] Japan Meteorological Agency, https://www.jma.go.jp/jma/menu/menureport.html
[2] Otani, Shinji, et al., Dust storms from degraded drylands of Asia: dynamics and health impacts. Land, 6(4), p. 83, 2017.
[3] Shimizu, Atsushi, et al., Variations of Dust Extinction Coefficient Estimated by Lidar Observations over Japan, 2007–2016. SOLA, 13, pp. 205–208, 2017.
[4] Kanatani, Kumiko T., et al., Effect of desert dust exposure on allergic symptoms: a natural experiment in Japan. Annals of Allergy, Asthma & Immunology, 116(5), pp. 425–430, 2016.
[5] A, Wang, Qingyue, et al. Size-segregated Allergenic Particles Released from Airborne Cryptomeria japonica Pollen Grains during the Yellow Sand Events within the Pollen Scattering Seasons. Asian Journal of Atmospheric Environment (AJAE), 7(4), pp.191–198, 2013.
[6] Watanabe, Masanari, et al., Correlation between Asian dust storms and worsening asthma in Western Japan. Allergology International, 60(3), pp. 267–275, 2011.
[7] Dias, G.M., Differentiating natural and anthropogenic sources of metals to the environment. Human and Ecological Risk Assessment, 9(4), pp. 699–721, 2003.
[8] Tsai, Y.I., Characterization of Asian dust storm and non-Asian dust storm PM2.5 aerosol in southern Taiwan. Atmospheric Environment, 40(25), pp. 4734–4750, 2006.
[9] Saitama Prefecture air pollution continuous monitoring system, http://www.taiki-kansi.pref.saitama.lg.jp/
[10] Wang, qingyue & Weiqian, Wang, Survey of inorganic components in atmospheric particles of three urban areas caused by winter energy consumption in China and Japan. WIT Transactions on Ecology and the Environment, 217, pp. 469–479, 2018.
[11] Squizzato, S., et al., Factors determining the formation of secondary inorganic aerosol: a case study in the Po Valley (Italy). Atmospheric chemistry and physics, 13(4), pp. 1927–1939, 2013.
[12] Zhang, Yy., Chemical characteristics of PM2.5 during 2015 spring festival in Beijing, China. Aerosol and Air Quality Research , 17(5), pp. 1169–1180, 2017.
[13] Wang, Y., The variation of characteristics and formation mechanisms of aerosols in dust, haze, and clear days in Beijing. Atmospheric Environment, 40(34), pp. 6579–6591, 2006.
[14] Tan, J-H., Source of atmospheric heavy metals in winter in Foshan, China. Science of the Total Environment, 493, pp. 262–270, 2014.
[15] Bilos, C., Sources, distribution and variability of airborne trace metals in La Plata City area, Argentina. Environmental pollution, 111(1), p. 1, 2001.
[16] Arditsoglou, A., Levels of total suspended particulate matter and major trace elements in Kosovo: a source identification and apportionment study. Chemosphere, 59(5), pp. 669–678, 2005.

Cite this:
APA Style
IEEE Style
BibTex Style
MLA Style
Chicago Style
GB-T-7714-2015
Wang, W. Q. & Wang, Q. Y. (2019). Chemical Characteristics of Water-Soluble Ions and Metal Elements in Ambient Particles of Saitama, Japan During the Spring Asian Dust Event, 2017. Int. J. Environ. Impacts., 2(4), 336-345. https://doi.org/10.2495/EI-V2-N4-336-345
W. Q. Wang and Q. Y. Wang, "Chemical Characteristics of Water-Soluble Ions and Metal Elements in Ambient Particles of Saitama, Japan During the Spring Asian Dust Event, 2017," Int. J. Environ. Impacts., vol. 2, no. 4, pp. 336-345, 2019. https://doi.org/10.2495/EI-V2-N4-336-345
@research-article{Wang2019ChemicalCO,
title={Chemical Characteristics of Water-Soluble Ions and Metal Elements in Ambient Particles of Saitama, Japan During the Spring Asian Dust Event, 2017},
author={Weiqian Wang and Qingyue Wang},
journal={International Journal of Environmental Impacts},
year={2019},
page={336-345},
doi={https://doi.org/10.2495/EI-V2-N4-336-345}
}
Weiqian Wang, et al. "Chemical Characteristics of Water-Soluble Ions and Metal Elements in Ambient Particles of Saitama, Japan During the Spring Asian Dust Event, 2017." International Journal of Environmental Impacts, v 2, pp 336-345. doi: https://doi.org/10.2495/EI-V2-N4-336-345
Weiqian Wang and Qingyue Wang. "Chemical Characteristics of Water-Soluble Ions and Metal Elements in Ambient Particles of Saitama, Japan During the Spring Asian Dust Event, 2017." International Journal of Environmental Impacts, 2, (2019): 336-345. doi: https://doi.org/10.2495/EI-V2-N4-336-345
WANG W Q, WANG Q Y. Chemical Characteristics of Water-Soluble Ions and Metal Elements in Ambient Particles of Saitama, Japan During the Spring Asian Dust Event, 2017[J]. International Journal of Environmental Impacts, 2019, 2(4): 336-345. https://doi.org/10.2495/EI-V2-N4-336-345