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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 30, issue 1
Ann. Geophys., 30, 49–56, 2012
https://doi.org/10.5194/angeo-30-49-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ann. Geophys., 30, 49–56, 2012
https://doi.org/10.5194/angeo-30-49-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Regular paper 05 Jan 2012

Regular paper | 05 Jan 2012

Settlement process of radioactive dust to the ground inferred from the atmospheric electric field measurement

M. Yamauchi1, M. Takeda2, M. Makino3, T. Owada4, and I. Miyagi3 M. Yamauchi et al.
  • 1Swedish Institute of Space Physics, Box 812, 98128 Kiruna, Sweden
  • 2Data Analysis Center for Geomagnetism and Space Magnetism, Faculty of Science, Kyoto University, Japan
  • 3National Institute of Advanced Industrial Science and Technology, Tsukuba, Japan
  • 4Kakioka Magnetic Observatory, Japan Meteorological Agency, Ishioka, Japan

Abstract. Radioactive materials from the accident at Fukushima Dai-ichi nuclear power plant (FNPP) in March 2011 spread over a large area, increasing the atmospheric electric conductivity by their ionizing effect, and reducing the vertical (downward) component of the DC electric field near the ground, or potential gradient (PG). PG data at Kakioka, 150 km away from the FNPP, showed independent changes compared to the radiation dose rate, and a comparison of these data revealed the local dynamics of the radioactive dust.

(1) The initial drop of the PG to almost zero during 14–15 March is most likely due to radioactive dust suspended in the air near the ground during cloudy weather. (2) An episode of PG increase to more than 50 V m−1 on 16 March is most likely due to the re-suspension of the radioactive dust from the surface and subsequent removal from Kakioka by the strong wind from the non-contaminated area. (3) Low but finite values of the PG during 16–20 March most likely reflect a reduced amount of radioactive material near the ground after the above wind transported away the majority of the suspended radioactive dust. (4) Very low values of the PG after substantial rain on 20–22 March most likely reflect settlement of the radioactive material by rain-induced fallout. (5) Temporal recovery of daily variations from the end of March to the middle of April with low nighttime fair-weather baseline PG most likely reflects re-suspension of the radioactive dust into the air from the ground and trees, and subsequent transport to the other region or fallout to the ground until late April. (6) Weakening of the daily variation and gradual recovery of the nighttime fair-weather baseline after mid-April suggests a complete settlement of the radioactive material to the ground with partial migration to the subsurface.

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