Journals / Atmospheric Pollution Research / 2018 / Cilt: 9 - Sayı: 5

Investigation of fungal spore characteristics in PM2.5 through organic tracers in Shanghai, China

Pages
894–900
DOI
—
🏛️Bibliographic metadata and full text access for this article are provided via DergiPark.
DergiPark Record ↗
✨

AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

The analysis results showed that the average concentration of airborne mannitol and arabitol were 5.79 and 3.86 ng m−3 , respectively.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:In order to investigate the fungal spore tracers in fine particles (PM2.5), including mannitol and arabitol at an urban site in a Chinese megacity, PM2.5 samples were collected in Shanghai from May 22 to June 19, 2015.
📊
Key Findings & Data:The analysis results showed that the average concentration of airborne mannitol and arabitol were 5.79 and 3.86 ng m−3 , respectively.
💡
Conclusion & Impact:The number concentration of fungal spores was 10513.16 spores m−3 , while fungal spores contributed about 1.91% for organic carbon OC using conversion factors.
🔬Design:Research Article
📍Scope:2015 · 2.5 samples
⚙️Variables:Domain Parameters

Özet

In order to investigate the fungal spore tracers in fine particles (PM2.5), including mannitol and arabitol at an urban site in a Chinese megacity, PM2.5 samples were collected in Shanghai from May 22 to June 19, 2015. The analysis results showed that the average concentration of airborne mannitol and arabitol were 5.79 and 3.86 ng m−3 , respectively. Mannitol and arabitol exhibited obvious positive correlations at ambient temperature, resulting from improving fungal spores formation rate and emission strength along with higher temperature. The concentrations of fungal spore tracers with Relative humidity-RH 70%–85% were higher than that RH > 85% and RH < 70%, which reflected that fungal spores released would be restrained under higher humidity. The concentrations between arabitol and mannitol showed negative correlation with wind speed, probably due to the dilution effect of wind. Three ions components (sulfate, nitrate and ammonium) exhibited poor correlations with fungal spore tracer. Based on the results, mannitol had a similar formation pathway with arabitol, resulting in strong correlation between them during our campaign. The number concentration of fungal spores was 10513.16 spores m−3 , while fungal spores contributed about 1.91% for organic carbon OC using conversion factors.

🔖

Cite This Article

ZHU, W., CHENG, Z., LUO, L., LOU, S., MA, Y., YAN, N. (2018). Investigation of fungal spore characteristics in PM2.5 through organic tracers in Shanghai, China. Atmospheric Pollution Research, Cilt: 9 - Sayı: 5, 894–900. https://ajindex.com/articles/204373

📄 Full Text PDF Viewer

📄

PDF görüntüleyici hazırlanıyor...

References (11)

  1. Bauer, H., Claeys, M., Vermeylen, R., Schueller, E., Weinke, G., Berger, A., Puxbaum, H., 2008a. Arabitol and mannitol as tracers for the quantification of airborne fungal spores. Atmos. Environ. 42, 588–593.
  2. Bauer, H., Kasper-Giebl, A., Löflund, M., Giebl, H., Hitzenberger, R., Zibuschka, F., Puxbaum, H., 2002a. The contribution of bacteria and fungal spores to the organic carbon content of cloud water, precipitation and aerosols. Atmos. Res. 64, 109–119.
  3. Bauer, H., Kasper-Giebl, A., Zibuschka, F., Hitzenberger, R., Kraus, G.F., Puxbaum, H., 2002b. Determination of the carbon content of airborne fungal spores. Anal. Chem. 74, 91–95.
  4. Bauer, H., Schueller, E., Weinke, G., Berger, A., Hitzenberger, R., Marr, I.L., Puxbaum, H., 2008b. Significant contributions of fungal spores to the organic carbon and to the aerosol mass balance of the urban atmospheric aerosol. Atmos. Environ. 42, 5542–5549.
  5. Buiarelli, F., Canepari, S., Filippo, P.D., Perrino, C., Pomata, D., Riccardi, C., Speziale, R., 2013. Extraction and analysis of fungal spore biomarkers in atmospheric bioaerosol by HPLC–MS–MS and GC–MS. Talanta 105, 142–151.
  6. Burshtein, N., Langyona, N., Rudich, Y., 2011. Ergosterol, arabitol and mannitol as tracers for biogenic aerosols in the eastern Mediterranean. Atmos. Chem. Phys. 11, 829–839.
  7. Carlile, M.J., Watkinson, S.C., Gooday, G.W., 2001. Genetic Variation and Evolution in the Fungi, second ed. Academic Press, London, pp. 245–295.
  8. Cheng, J.Y.W., Chan, C.K., Lee, C.T., Lau, A.P.S., 2009. Carbon content of common airborne fungal species and fungal contribution to aerosol organic carbon in a subtropical city. Atmos. Environ. 43, 2781–2787.
  9. Christner, B.C., Morris, C.E., Foreman, C.M., Cai, R., Sands, D.C., 2008. Ubiquity of biological ice nucleators in snowfall. Science 319 1214-1214.
  10. Chysirichote, T., Reiji, T., Asami, K., Ohtaguchi, K., 2014. Quantification of the glucosamine content in the filamentous fungus Monascus ruber cultured on solid surfaces. J. Basic Microbiol. 54, 350–357.
  11. Claeys, M., Kourtchev, I., Pashynska, V., Vas, G., Vermeylen, R., Wang, W., Cafmeyer, J., Chi, X., Artaxo, P., Andreae, M.O., 2010. Polar organic marker compounds in atmospheric aerosols during the LBA-SMOCC 2002 biomass burning experiment in Rondônia, Brazil: sources and source processes, time series, diel variations and size distributions. Atmos. Chem. Phys. 10, 9319–9331. Després, V.R., Huffman, J.A., Burrows, S.M., Hoose, C., Safatov, A.S., Buryak, G., Fröhlich-Nowoisky, J.,