Distinction between Radiocesium (RCs)-bearing Microparticles and RCs-sorbing Minerals Derived from the Fukushima Nuclear Accident Using Acid Treatment
Author:
Affiliation:
1. Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-0033, Japan
2. Institute for Agro-Environmental Sciences, NARO, 3-1-3 Kannondai, Tsukuba, Ibaraki 305-0864, Japan
Publisher
The Chemical Society of Japan
Subject
General Chemistry
Link
http://www.journal.csj.jp/doi/pdf/10.1246/cl.200374
Reference18 articles.
1. Speciation of Radioactive Soil Particles in the Fukushima Contaminated Area by IP Autoradiography and Microanalyses
2. Cesium adsorption/desorption behavior of clay minerals considering actual contamination conditions in Fukushima
3. A review of Cs-bearing microparticles in the environment emitted by the Fukushima Dai-ichi Nuclear Power Plant accident
4. Emission of spherical cesium-bearing particles from an early stage of the Fukushima nuclear accident
5. Detection of Uranium and Chemical State Analysis of Individual Radioactive Microparticles Emitted from the Fukushima Nuclear Accident Using Multiple Synchrotron Radiation X-ray Analyses
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1. Dissolution behavior of radiocesium-bearing microparticles as a function of solution compositions;Scientific Reports;2023-03-15
2. Effect of radioactive cesium-rich microparticles on radioactive cesium concentration and distribution coefficient in rivers flowing through the watersheds with different contaminated condition in Fukushima;Journal of Environmental Management;2023-03
3. Structure, Composition, and Physicochemical Properties of Radiocesium-Bearing Microparticles Emitted by the Fukushima Daiichi Nuclear Power Plant Accident;Agricultural Implications of Fukushima Nuclear Accident (IV);2023
4. Contribution of Cesium-Bearing Microparticles to Cesium in Soil and River Water of the Takase River Watershed and Their Effect on the Distribution Coefficient;Agricultural Implications of Fukushima Nuclear Accident (IV);2023
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