T. Yasutaka, Y. Kanai, M. Kurihara, T. Kobayashi, A. Kondoh, T. Takahashi, Y. Kuroda
Radioprotection 55(3) 215-224 2020年7月 査読有り
This paper describes the involvement of the residents of the Yamakiya district of the Kawamata town, a former evacuation area after the accident of Fukushima Daiichi Nuclear Power Plant (FDNPP), in the on-going research activities of the authors on the behaviour of radioactive caesium in the environment. By relying on dialogue, measuring radiation, and other collaborative practices, this involvement enabled a series of actions to be taken to resolve the challenges related to the recovery after the lifting of the evacuation order that were appreciated by the residents. The paper also discusses the effects of the interactive program led by the Yamakiya School organized by the authors in cooperation with the residents including among others lectures, voluntary works and radiological surveys on local issues. Based on the above, the authors make recommendations on the desirable form of relationship between residents and experts after an event of large-scale environmental pollution including radiological contamination. Through these activities the authors have also gradually changed their research approach.
X. Wang, N. Matsuoka, H. Tani, R. Kimura, T. Kobayashi, Y. Guirui, H. He, S. Matsumura
Proceedings, 32nd International Symposium on Remote Sensing of Environment: Sustainable Development Through Global Earth Observations 2007年12月1日
The area that was studies and analyzed is in Yulin Prefecture, Shanxi Province of China, located in the transitional morphology from the Maowusu Sandland to the Ocher Plateau. It is half the size of the Maowusu Sandland: 570,000 ha. This study uses Landsat data and climate data to analyze how the land cover has changed as a result of human reforestation on the land that had recently turned to desert. A significant decrease of desert land area occurred in the Yulin region between 2000 and 2005. During the 19 years between 1986 and 2005, approximately 24% of the desert land (about 5000 km2) became grassland, concomitant with the rise of NDVI. These changes were caused not by the influences of precipitation and temperature, but by artificial greening. However, the decreased size of the lakes was attributed to both climate change and human activity.