Abstract:Six years after the Fukushima Daiichi Nuclear Power Plant (FDNPP) accident, data for 236U and 236U/238U have remained limited to a few heavily contaminated samples. In the present study, activities of 236U, 239Pu, and 240Pu, along with other U isotopes in 46 soil samples both heavily and lightly contaminated by this accident were measured by inductively coupled plasma–mass spectrometry (ICP-MS) and triple-quadrupole ICP-MS. The 236U activities and 236U/238U atom ratios in these soil samples were in the range o… Show more
“…(0.103 ± 0.013) 21 as well as the 240 Pu/ 239 Pu atom ratio. As pointed out by previous studies 21,22 , these environmental samples were strongly influenced by global fallout, the value of which was 0.180 ± 0.007 for 240 Pu/ 239 Pu atom ratio 14–16 and 0.00194 ± 00014 for 241 Pu/ 239 Pu atom ratio 14 . The Pu contribution from the FDNPP accident can be estimated using the two end-member model 48 , and the extent of Pu contribution in soil samples was estimated as follows: 87% by Zheng et al .…”
Section: Discussionsupporting
confidence: 59%
“…21 and Yang et al . 22 were lower than that of DPs. The 241 Pu/ 239 Pu atom ratios in DPs agreed better with litters obtained by Zheng et al .…”
Section: Discussionmentioning
confidence: 61%
“…However, due to the relatively large error in the measured values, we cannot distinguish the source unit of the radioactive particles only from these atom ratios. The obtained 240 Pu/ 239 Pu and 241 Pu/ 239 Pu atom ratios in the radioactive particle were also compared with those of various environmental samples, such as soil 21,22 , litter 21,23 , black substance 23 , vegetation 24,25 , river water 26 , and air dust 27 , as shown in Figs 4 and 5. The 240 Pu/ 239 Pu atom ratio detected in environmental samples ranged from 0.14 to 0.381.…”
Section: Discussionmentioning
confidence: 99%
“…Thus, radioactive particle samples are completely free from the influence of the global fallout and the 240 Pu/ 239 Pu and 241 Pu/ 239 Pu atom ratio reflect the ratio in the core of the FDNPP directly. Therefore, both atom ratio of radioactive particles could provide us more accurate information on the ratio in the core of the FDNPP than other environmental samples and has great potential for source identification of the released radioactive particles in the environment, which should be further explored in a future study.…”
Radioactive particles were released into the environment during the Fukushima Dai-ichi Nuclear Power Plant (FDNPP) accident. Many studies have been conducted to elucidate the chemical composition of released radioactive particles in order to understand their formation process. However, whether radioactive particles contain nuclear fuel radionuclides remains to be investigated. Here, we report the first determination of Pu isotopes in radioactive particles. To determine the Pu isotopes (
239
Pu,
240
Pu and
241
Pu) in radioactive particles derived from the FDNPP accident which were free from the influence of global fallout, radiochemical analysis and inductively coupled plasma-mass spectrometry measurements were conducted. Radioactive particles derived from unit 1 and unit 2 or 3 were analyzed. For the radioactive particles derived from unit 1, activities of
239+240
Pu and
241
Pu were (1.70–7.06) × 10
−5
Bq and (4.10–8.10) × 10
−3
Bq, respectively and atom ratios of
240
Pu/
239
Pu and
241
Pu/
239
Pu were 0.330–0.415 and 0.162–0.178, respectively. These ratios were consistent with the simulation results from ORIGEN code and measurements from various environmental samples. In contrast, Pu was not detected in the radioactive particles derived from unit 2 or 3. The difference in Pu contents is clear evidence towards different formation processes of radioactive particles, and detailed formation processes can be investigated from Pu analysis.
“…(0.103 ± 0.013) 21 as well as the 240 Pu/ 239 Pu atom ratio. As pointed out by previous studies 21,22 , these environmental samples were strongly influenced by global fallout, the value of which was 0.180 ± 0.007 for 240 Pu/ 239 Pu atom ratio 14–16 and 0.00194 ± 00014 for 241 Pu/ 239 Pu atom ratio 14 . The Pu contribution from the FDNPP accident can be estimated using the two end-member model 48 , and the extent of Pu contribution in soil samples was estimated as follows: 87% by Zheng et al .…”
Section: Discussionsupporting
confidence: 59%
“…21 and Yang et al . 22 were lower than that of DPs. The 241 Pu/ 239 Pu atom ratios in DPs agreed better with litters obtained by Zheng et al .…”
Section: Discussionmentioning
confidence: 61%
“…However, due to the relatively large error in the measured values, we cannot distinguish the source unit of the radioactive particles only from these atom ratios. The obtained 240 Pu/ 239 Pu and 241 Pu/ 239 Pu atom ratios in the radioactive particle were also compared with those of various environmental samples, such as soil 21,22 , litter 21,23 , black substance 23 , vegetation 24,25 , river water 26 , and air dust 27 , as shown in Figs 4 and 5. The 240 Pu/ 239 Pu atom ratio detected in environmental samples ranged from 0.14 to 0.381.…”
Section: Discussionmentioning
confidence: 99%
“…Thus, radioactive particle samples are completely free from the influence of the global fallout and the 240 Pu/ 239 Pu and 241 Pu/ 239 Pu atom ratio reflect the ratio in the core of the FDNPP directly. Therefore, both atom ratio of radioactive particles could provide us more accurate information on the ratio in the core of the FDNPP than other environmental samples and has great potential for source identification of the released radioactive particles in the environment, which should be further explored in a future study.…”
Radioactive particles were released into the environment during the Fukushima Dai-ichi Nuclear Power Plant (FDNPP) accident. Many studies have been conducted to elucidate the chemical composition of released radioactive particles in order to understand their formation process. However, whether radioactive particles contain nuclear fuel radionuclides remains to be investigated. Here, we report the first determination of Pu isotopes in radioactive particles. To determine the Pu isotopes (
239
Pu,
240
Pu and
241
Pu) in radioactive particles derived from the FDNPP accident which were free from the influence of global fallout, radiochemical analysis and inductively coupled plasma-mass spectrometry measurements were conducted. Radioactive particles derived from unit 1 and unit 2 or 3 were analyzed. For the radioactive particles derived from unit 1, activities of
239+240
Pu and
241
Pu were (1.70–7.06) × 10
−5
Bq and (4.10–8.10) × 10
−3
Bq, respectively and atom ratios of
240
Pu/
239
Pu and
241
Pu/
239
Pu were 0.330–0.415 and 0.162–0.178, respectively. These ratios were consistent with the simulation results from ORIGEN code and measurements from various environmental samples. In contrast, Pu was not detected in the radioactive particles derived from unit 2 or 3. The difference in Pu contents is clear evidence towards different formation processes of radioactive particles, and detailed formation processes can be investigated from Pu analysis.
“…It is estimated that only a fraction (~0.002%) of Pu from the total reactor core inventory was introduced to the environment 3 . For the data available, only trace quantities of FDNPP-derived Pu have been measured in environmental materials and mixing of the FDNPP Pu with trace amounts of Pu derived from atmospheric nuclear weapons testing complicates interpretation of the observed isotopic signature 5 , 8 . Heterogeneity in both isotopic ratio and specific activity of Pu in the vicinity of FDNPP has raised questions about the source and composition of contamination 4 , 9 .…”
Plutonium and radiocaesium are hazardous contaminants released by the Fukushima Daiichi nuclear power plant (FDNPP) disaster and their distribution in the environment requires careful characterisation using isotopic information. Comprehensive spatial survey of 134Cs and 137Cs has been conducted on a regular basis since the accident, but the dataset for 135Cs/137Cs atom ratios and trace isotopic analysis of Pu remains limited because of analytical challenges. We have developed a combined chemical procedure to separate Pu and Cs for isotopic analysis of environmental samples from contaminated catchments. Ultra-trace analyses reveal a FDNPP Pu signature in environmental samples, some from further afield than previously reported. For two samples, we attribute the dominant source of Pu to Reactor Unit 3. We review the mechanisms responsible for an emergent spatial pattern in 134,135Cs/137Cs in areas northwest (high 134Cs/137Cs, low 135Cs/137Cs) and southwest (low 134Cs/137Cs, high 135Cs/137Cs) of FDNPP. Several samples exhibit consistent 134,135Cs/137Cs values that are significantly different from those deposited on plant specimens collected in previous works. A complex spatial pattern of Pu and Cs isotopic signature is apparent. To confidently attribute the sources of mixed fallout material, future studies must focus on analysis of individual FDNPP-derived particles.
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