Japan Geoscience Union Meeting 2015

Presentation information


Symbol M (Multidisciplinary and Interdisciplinary) » M-TT Technology & Techniques

[M-TT44] Frontiers in Geochemistry: Prospect for geochemistry in 30 years

Tue. May 26, 2015 3:15 PM - 4:00 PM 102B (1F)

Convener:*Takafumi Hirata(Graduate School of Science, Kyoto University), Yoshio Takahashi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Urumu Tsunogai(Graduate School of Environmental Studies, Nagoya University), Hajime Obata(Marine inorganic chemistry division, Atmosphere and Ocean Research Institute, University of Tokyo), Shogo Tachibana(Department of Natural History Scieces, Hokkaido University), Katsuhiko Suzuki(Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology), Gen Shimoda(Geological Survey of Japan, AIST), Hiroyuki Kagi(Geochemical Laboratory, Graduate School of Science, University of Tokyo), Yusuke Yokoyama(Atmosphere and Ocean Research Institute, University of Tokyo), Tetsuya Yokoyama(Department of Earth and Planetary Sciences, Graduate School of Science and Engineering, Tokyo Institute of Technology), Chair:Takafumi Hirata(Graduate School of Science, Kyoto University), Yoshio Takahashi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo)

3:15 PM - 3:30 PM

[MTT44-01] Detection of low isotopic ratio of iron in anthropogenic aerosols and evaluation of its contribution to the ocean

*Minako KURISU1, Tsuyoshi IIZUKA1, Aya MIYAHARA2, Yoshiaki YAMAKAWA1, Chihiro MIYAMOTO1, Kohei SAKATA2, Aya SAKAGUCHI3, Yoshio TAKAHASHI1 (1.Graduate School of Science, The University of Tokyo, 2.Graduate School of Science, Hiroshima University, 3.Faculty of Pure and Applied Sciences, University of Tsukuba)

Keywords:iron isotopic composition, aerosol, anthropogenic iron

Productivity of phytoplankton affects global carbon cycle, and may also affect the climate. Iron (Fe) is an essential element for phytoplankton, but its solubility is low and much of it is removed as Fe (III) hydroxide. Therefore, it has been reported that phytoplankton growth in the High Nutrient-Low Chlorophyll (HNLC) regions is limited by Fe concentration (Martin and Fitzwater, 1988). Aerosols are important sources of Fe species to the surface seawater. They are classified into anthropogenic and natural ones. Particle sizes of anthropogenic aerosols are generally smaller than those of natural ones because of their different formation processes (Whitby, 1977). Previous studies have shown that high soluble Fe species were included in anthropogenic aerosols (e.g., Takahashi et al., 2013). In terms of Fe isotope composition, Mead et al. (2013) compared Fe isotopic compositions between course aerosols (›2.5 μm) and fine ones (‹2.5 μm) and suggested that the Fe isotopic composition of finer aerosols (anthropogenic source; δ56Fe = -0.10‰) is lighter than that of coarse aerosols (natural source; δ56Fe = 0.08‰). However, it is possible that the separation of the aerosols at the particle size of 2.5 μm cannot fully separate the two sources. The purpose of this study, therefore, was to detect anthropogenic aerosols and measure their Fe iron isotopic compositions. Size-fractioned aerosol samples were collected at Higashi-Hiroshima City using a cascade impactor (particle sizes: ›10.2 μm, 4.2 〜 10.2 μm, 2.1 〜 4.2 μm, 1.3 〜 2.1 μm, 0.69 〜 1.3 μm, 0.39 〜 0.69 μm, ‹0.39 μm), which could specify the isotopic compositions of anthropogenic Fe. Iron isotopic compositions of bulk aerosols and soluble aerosols for simulated rain water were measured using multi-collector inductivity-coupled plasma mass spectrometry (MC-ICP-MS; Neptune Plus, Thermo Scientific). The chemical species were also identified by employing Fe K-edge X-ray absorption fine structure (XAFS) spectroscopy and their solubility for seawater was evaluated by leaching experiments. As a result, Fe isotopic compositions (δ56Fe) of larger particles were around +0.25‰, whereas smaller particles showed lower isotopic composition (-0.5 〜 -2‰). In addition, smaller particles of soluble component for simulated rain water showed much lower δ56Fe values (δ56 = -3.9‰) than bulk particles, suggesting that anthropogenic Fe has much lower isotopic compositions. The value was the lowest among other environmental samples reported so far. This means that the large isotopic fractionation of anthropogenic aerosols occurs when Fe species evaporate. δ56Fe value of the remaining materials after the water-extraction experiment was calculated using the values of bulk Fe and soluble Fe, and it was revealed to be similar to that of earth's crust (+0.25‰). This means that the anthropogenic Fe in aerosol is completely soluble and has very low δ56Fe. It has been suggested that Fe in aerosol contributed significantly to the supply of Fe in surface seawater. When considering Fe isotopic budget for surface seawater using the value measured in this study as a δ56Fe of anthropogenic aerosol (-3.9‰), it is suggested that aerosols is main source of Fe dissolved in the surface seawater.