Japan Geoscience Union Meeting 2018

Presentation information

[EE] Evening Poster

A (Atmospheric and Hydrospheric Sciences) » A-HW Hydrology & Water Environment

[A-HW20] Materials transport and nutrient cycles in watersheds; Human and climate impacts

Mon. May 21, 2018 5:15 PM - 6:30 PM Poster Hall (International Exhibition Hall7, Makuhari Messe)

convener:Mitsuyo Saito(Graduate School of Environmental and Life Science, Okayama University), Shin-ichi Onodera(Graduate School of Integrated and Arts Sciences, Hiroshima University), Takahiro Hosono(熊本大学大学院先導機構, 共同), Adina Paytan(University of California Santa Cruz)

[AHW20-P06] A comparison of initial deposition and current inventory of radiocesium in forest ecosystems surrounding Tokyo metropolitan area

*Yuko Itoh1, Masahiro Kobayashi1, Akihiro Imaya2, Shigeto Ikeda1 (1.Forestry and Forest Products Research Institute, Japan, 2.Japan International Research Center for Agricultural Sciences)

The Fukushima Daiichi Nuclear Power Plant (FD1NPP) accident in March 2011 resulted in the release of enormous amounts of radionuclides into the atmosphere. Those radionuclides were deposited over a large forested area in the Tohoku and Kanto districts. Using preserved rainfall monitoring samples that we had collected prior to the accident, we identified the initial radiocesium influx to the forested area in the Kanto region. The results show that the initial radiocesium deposition by bulk precipitation was not related to the distance from the FD1NPP. Atmospheric radiocesium inputs to forest sites were strongly influenced by interception and temporal retention by the forest canopy. We collected litter-layer and forest surface soil (0–20 cm depth) samples at the same forest sites in 2011, 2014, and 2016 after the accident. We then investigated the radiocesium inventory of forest floor and soil. Within five years, most of the radiocesium that had reached the forest floor had migrated into the surface soil. At all sites, we found the amount of radiocesium on the forest floor and surface soil layer in 2016 to be greater than the initial radiocesium influx by bulk precipitation. This suggests that the atmospheric radiocesium inputs to the forest sites were affected by dry depositions as well as rainfall and snowfall.