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RAPID COMMUNICATION

Chemical states of fallout radioactive Cs in the soils deposited at Fukushima Daiichi Nuclear Power Plant accident

Fukushima NPP Accident Related

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Pages 473-478 | Received 10 Feb 2012, Accepted 07 Mar 2012, Published online: 24 Apr 2012

Figures & data

Figure 1. Percent fractions of radioactive Cs desorbed from the soils A, B, and C by 1 mole L−1 NH4Cl solution and 1 mole L−1 CH3COOH solution, and residual one.

Figure 1. Percent fractions of radioactive Cs desorbed from the soils A, B, and C by 1 mole L−1 NH4Cl solution and 1 mole L−1 CH3COOH solution, and residual one.

Figure 2. Percent fractions of radioactive Cs desorbed from the soils A, B, and C by 0.001 mole L−1 H2SO4 solution and 1 mole L−1 H2SO4 solution, and residual one. Arrows show fractions of Cs desorbed by 0.001 mole L−1 H2SO4 solution.

Figure 2. Percent fractions of radioactive Cs desorbed from the soils A, B, and C by 0.001 mole L−1 H2SO4 solution and 1 mole L−1 H2SO4 solution, and residual one. Arrows show fractions of Cs desorbed by 0.001 mole L−1 H2SO4 solution.

Figure 3. Percent fractions of the resided radioactive Cs in the elutriated fraction, the settled fraction less than 106 μm, the fraction between 106 μm and 300 μm, and the fraction larger than 300 μm of the soils A, B, and C after the treatment of 1 mole L−1 NH4Cl solution and 1 mole L−1 CH3COOH solution.

Figure 3. Percent fractions of the resided radioactive Cs in the elutriated fraction, the settled fraction less than 106 μm, the fraction between 106 μm and 300 μm, and the fraction larger than 300 μm of the soils A, B, and C after the treatment of 1 mole L−1 NH4Cl solution and 1 mole L−1 CH3COOH solution.

Figure 4. XRD patterns of the elutriated fraction (WE), the settled fraction less than 106 μm, the fraction between 106 μm and 300 μm, and the fraction larger than 300 μm of the soils A, B, and C after the treatment of 1 mole L−1 NH4Cl solution and 1 mole L−1 CH3COOH solution. Sm: smectite-like clay minerals, M: mica-like minerals, H: hornblende-like minerals, K: kaolinite-like minerals, Q: quartz, O: orthoclose, C: cristobalite, F: feldspar group, S: stishovite (SiO2), G: gibbsite-like minerals, SL: sodalite-like minerals, OL: olivine, SS: sorosilicate.

Figure 4. XRD patterns of the elutriated fraction (WE), the settled fraction less than 106 μm, the fraction between 106 μm and 300 μm, and the fraction larger than 300 μm of the soils A, B, and C after the treatment of 1 mole L−1 NH4Cl solution and 1 mole L−1 CH3COOH solution. Sm: smectite-like clay minerals, M: mica-like minerals, H: hornblende-like minerals, K: kaolinite-like minerals, Q: quartz, O: orthoclose, C: cristobalite, F: feldspar group, S: stishovite (SiO2), G: gibbsite-like minerals, SL: sodalite-like minerals, OL: olivine, SS: sorosilicate.

Table 1. The representative minerals and clay minerals in the fractions elutriated and sieved in the soils A, B, and C determined by XRD.

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