Japan Geoscience Union Meeting 2015

Presentation information


Symbol A (Atmospheric and Hydrospheric Sciences) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS21] Atmospheric Chemistry

Thu. May 28, 2015 4:15 PM - 5:00 PM 201B (2F)

Convener:*Yousuke Sawa(Oceanography and Geochemistry Research Department, Meteorological Research Institute), Nobuyuki Takegawa(Graduate School of Science and Engineering, Tokyo Metropolitan University), Yugo Kanaya(Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology), Kenshi Takahashi(Research Institute for Sustainable Humanosphere, Kyoto University), Hiroshi Tanimoto(National Institute for Environmental Studies), Chair:Tomoki Nakayama(Solar-Terrestrial Environment Laboratory, Nagoya University)

4:15 PM - 4:30 PM

[AAS21-27] Speciation of sulfate in aerosols for the precise estimation of its global cooling effect

*Chihiro MIYAMOTO1, Yoshiaki YAMAKAWA1, Kohei SAKATA2, Aya MIYAHARA2, Hiroki SUGA2, Aya SAKAGUCHI3, Yasuo TAKEICHI4, Kanta ONO4, Yoshio TAKAHASHI1 (1.Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo, 2.Department of Earth and Planetary Systems Science, Graduate School of Science, Hiroshima University, 3.Faculty of Pure and Applied Science, University of Tsukuba, 4.Institute of Materials Structure Science, KEK)

Keywords:aerosol, speciation of sulfate, global cooling effect, X-ray absorption fine structure

Global cooling effect by aerosol is one of causes which influence earth’s climatic change (IPCC, 2013). In particular, sulfate aerosols are known to cool the earth indirectly by forming cloud condensation nuclei (CCN) because of their high hygroscopicity. However, the hygroscopicity can change depending on the sulfate species. For example, CaSO4●2H2O is sulfate having low hygroscopicity. Therefore, determination of sulfate species in aerosols is necessary to interpret the degree of cooling effect by sulfate aerosols in environment.
In this study, aerosol sampling was conducted in Higashi-Hiroshima (34.40 N, 123.71 E), Hiroshima, Japan. In addition, the samples were collected using two methods as to particle size. One method collected non-size-fractionated aerosols for about a year from September 2012 to September 2013. The other method collected size-fractionated aerosol in various periods such as winter when concentrations of anthropogenic aerosols were high (PA sample; collected from January 31 to February 1, 2013), spring (March 4 to 9, 2013), summer (July 22 to August 5, 2013), and fall (November 11 to 25, 2013). For these samples, major ion composition was measured by ion-chromatography, while chemical species of sulfur and calcium in the aerosol samples were determined by X-ray absorption fine structure (XAFS) spectroscopy. Furthermore, to unravel the function of CCN by sulfate aerosols in more detail, samples for single particle analysis were collected on May 31, 2014 during a dust event, which was analyzed individually using scanning transmission X-ray microscopy (STXM).
Atmospheric concentration of each major ion in the atmosphere had seasonal variation. Sulfate ion (SO42-) concentration was larger in PA, in which concentration of ammonium ion (NH4+) and nitrate ion (NO3-) were also larger than those in other seasons. Meanwhile, size distribution of aerosol is important to determine its origin, because it is widely recognized that aerosol larger than 1 μm diameter is of natural origin. On the other hand, particles finer than 1 μm is of anthropogenic origin. In general, concentrations of SO42- and NH4+ were larger in finer particles. Therefore, it is strongly suggested that the aerosol sample collected in this period was influenced by human activities. In spring, concentration of calcium ion (Ca2+) increased particularly in the coarse particles, which suggests that its origin was from natural source.
Subsequently, sulfate species in the aerosol samples was determined using XAFS, where it was found that concentration ratio of calcium sulfate (CaSO4●2H2O) which has low hygroscopicity to total concentration of SO42- in the aerosol sample ([CaSO4●2H2O]/[SO42-]t) was larger in spring than that in PA. The abundance of CaSO4●2H2O in atmosphere cannot be ignored because of its comparatively high [CaSO4●2H2O]/[SO42-]t ratio, especially in spring. It was also found that indirect cooling effect by sulfate will be small in spring due to the larger ratio of [CaSO4●2H2O]/[SO42-]t. To provide further details of the effect by CCN function, Ca species of single particle samples in the dust period was determined using STXM. It was shown that there was CaSO4●2H2O at the surface of the particle, which is the site of the chemical reactions with other species in aerosols. In addition, Ca(NO3)2●4H2O, which was minor Ca species in the bulk analysis, was also detected in the particles. Individual analysis of single particle is important to determine minor species in aerosol samples, which leads to better understanding of chemical processes in the atmosphere.
In conclusion, it was suggested that the degree of indirect cooling effects of sulfate aerosol can change seasonally because concentrations of low hygroscopicity sulfate species in the atmosphere are variable.