Abstract

Abstract. At stations on the Natsui River and the Same River in Fukushima Prefecture, Japan, effects of a heavy rain event on radiocesium export were studied after Typhoon Roke during 21–22 September 2011, six months after the Fukushima Dai-ichi Nuclear Power Plant accident. Radioactivity of 134Cs and 137Cs in river waters was 0.009–0.098 Bq L−1 in normal flow conditions during July–September 2011, but it increased to 0.85 Bq L−1 in high flow conditions because of heavy rains occurring with the typhoon. The particulate fractions of 134Cs and 137Cs were 21–56% of total radiocesium in the normal flow condition, but were close to 100% after the typhoon. These results indicate that the pulse input of radiocesium associated with suspended particles from land to coastal ocean occurred because of the heavy rain event. Export flux of 134Cs and 137Cs attributable to the heavy rain accounts for 30–50% of the annual radiocesium flux from inland to coastal ocean region in 2011. Results show that rain events are one factor contributing to the transport and dispersion of radiocesium in river watersheds and coastal marine environments.

Highlights

  • A nuclear accident at the Fukushima Dai-ichi Nuclear Power Plant (NPP) occurred after the 2011 Tohoku earthquake and tsunami

  • The radioactivity of 134Cs and 137Cs in the high flow condition after the typhoon was about one order higher than that in normal flow conditions, which indicates that high export of 134Cs and 137Cs occurred after the heavy rain event

  • During July–December, 2011, research was conducted for the Natsui River and the Same River, which run through a contaminated watershed in Fukushima Prefecture, to elucidate the transport of 134Cs and 137Cs from land to coastal ocean area after the Fukushima Dai-ichi NPP accident

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Summary

Introduction

A nuclear accident at the Fukushima Dai-ichi Nuclear Power Plant (NPP) occurred after the 2011 Tohoku earthquake and tsunami. About 15 PBq of both 134Cs and 137Cs was released from the NPP as a result of venting operations and hydrogen explosions (Japanese Government, 2011; Chino et al, 2011). Surface deposition of 134Cs and 137Cs shows considerable external radioactivity in a zone extending northwest from the NPP, about 20 km wide and 50–70 km long inside the 80 km zone of the NPP (MEXT, 2011; Yoshida and Takahashi, 2012). Moderate radioactivity (100–600 kBq m2) was detected in the Naka-dori region. A major part of radiocesium deposited on the ground surface is present at the surface to 5 cm depth (MEXT, 2012a; Koarashi et al, 2012). Chemical extraction of 134Cs and 137Cs from selected soil samples has revealed that both radionuclides in the soil are only slightly water-soluble

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