Micro-PIXE analysis of the distribution of cesium in clay particles for environmental remediation of Fukushima

Author:

Ishii K.1,Itoh S.2,Sata D.2,Matsuyama S.2,Terakawa A.2,Kim S.2,Arai H.1,Osada N.1,Satoh T.3,Koka M.3,Kitamua A.3,Kamiya T.3

Affiliation:

1. Research Center for Remediation Engineering of Environments Contaminated with Radioisotopes, Graduate School of Engineering, Tohoku University, 6-6-01-2 Aramaki Aza-Aoba, Aoba-ku, Sendai 980-8579, Japan

2. Department of Quantum Science and Energy Engineering, Tohoku University, 6-6-01-2 Aramaki Aza-Aoba, Aoba-ku, Sendai 980-8579, Japan

3. Takasaki Advanced Radiation Research Institute, Japan Atomic Energy Agency, Watanuki-machi 1233, Takasaki 370-1292, Japan

Abstract

The Fukushima Daiichi nuclear power plant accident caused radioactive pollution by 131I, 134Cs and 137Cs. The surface of the ground was contaminated at a volume of 3 × 107 m3. The government has mandated that the top 5 cm of the contaminated soil be removed and stored, in this way, it is desirable to reduce its volume. Soil samples were collected from a mountain, a rice field and a vegetable field in northern Japan, and the silt was extracted from the muddy water by washing the soil. Next, the silt was sprayed with a solution of cesium carbonate (Cs2CO3). We determined the amounts of Al, Si, K and Cs in the silt particles using micro-particle-induced X-ray emission (micro-PIXE) analysis. The silt particles from a vegetable field, a rice field and a mountain were mainly formed from smectite or vermiculite, which absorbs Cs atoms. The measurements at multiple detection angles confirmed that Cs atoms were uniformly absorbed within silt particles less than [Formula: see text] in diameter. This resulted that the radioactive Cs atoms were adsorbed in silt particles within [Formula: see text] of the surface.

Publisher

World Scientific Pub Co Pte Lt

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