Radiocesium distribution in soils of Tenerife Island (Canary Islands, Spain)

Author(s):  
María López Pérez ◽  
Pedro Ángel Salazar Carballo ◽  
María Candelaria Martín Luis ◽  
Francisco Javier Hernández ◽  
Esperanza Liger ◽  
...  

<p>Tenerife is the largest and most populated island of the Canary Islands; with a surface of 2,034 km<sup>2</sup> and 917,841 inhabitants (in January 2019), it hosts 43% of the total population of the archipelago.</p><p>Large amounts of <sup>137</sup>Cs, an artificial radionuclide with a half-life of 30.2 years, were released into the environment due to the nuclear weapon tests carried out from the 1950s to the 1970s and by nuclear power plant accidents, such as the Chernobyl in 1986. The most recent <sup>137</sup>Cs release into the environment was due to the Fukushima Daiichi Nuclear Power Plant accident, following the earthquake and tsunami of 11 March 2011. Radionuclides released by this accident were measured in air filters collected in the Canary Islands despite the tremendous distance to the source (López-Pérez et al., 2013).</p><p>In this work, we provide the concentrations of <sup>137</sup>Cs measured in 73 soil samples collected in 2013 in Tenerife. Besides, a second dataset of <sup>137</sup>Cs concentrations recorded in 103 soil samples collected in 1991 (22 years before) have been used to provide information on the spatial and temporal variability of this anthropogenic radionuclide at this site.</p><p>In both surveys, sampling sites were randomly selected on a predefined 3x3 km sampling grid covering the whole island and superficial samples were collected from uncultivated fields. Radiometric measurements were performed by gamma spectrometry with a coaxial-type germanium detector (Canberra Industries Inc., USA). The activity concentration of <sup>137</sup>Cs was directly measured by its gamma-ray photopeak at 661.65 KeV. The Minimum Detectable Activity was 0.08 Bq kg<sup>-1</sup>.</p><p><sup>137</sup>Cs activity concentrations in the 1991 survey ranged from 0.08 to 100.90 Bq kg<sup>-1</sup> and from 0.08 to 88.85 Bq kg<sup>-1</sup> in 2013. Comparing the results of both campaigns, <sup>137</sup>Cs activity concentrations were found to be rather similar, despite the 22 years gap between the measurements. We believe that, in addition to the <sup>137</sup>Cs atmospheric fallout, there is an additional contribution to the inventory of this radionuclide in the soils of this island produced by the deposition of <sup>137</sup>Cs-loaded dust particles frequently transported from the Sahara Desert as dust storms (Karlsson et al, 2008).</p><p>In terms of radiological risk, in some few locations, the contribution to the outdoor gamma absorbed dose from the <sup>137</sup>Cs activity concentrations present in the soils were as high as 50%. Therefore, it is important to identify the various sources of this radionuclide to the studied sites in order to enhance the understanding of the radiological hazard produced by this man-made radionuclide.</p><p><strong>References:</strong></p><p>Karlsson L, Hernandez F, Rodríguez S, López-Pérez M, Hernandez-Armas J, Alonso-Pérez S, Cuevas, E. (2008). Using <sup>137</sup>Cs and <sup>40</sup>K to identify natural Saharan dust contributions to PM10 concentrations and air quality impairment in the Canary Islands. Atmospheric Environment, 42: 7034-7042</p><p>López-Pérez M, Ramos-López R, Perestelo NR, Duarte-Rodriguez X, Bustos JJ, Alonso-Pérez S, E. Cuevas, J. Hernández-Armas. (2013). Arrival of radionuclides released by the Fukushima accident to Tenerife (Canary Islands). Journal of Environmental Radioactivity, 116: 180-186</p>

2015 ◽  
Vol 146 ◽  
pp. 125-133 ◽  
Author(s):  
Terumi Dohi ◽  
Yoshihito Ohmura ◽  
Hiroyuki Kashiwadani ◽  
Kenso Fujiwara ◽  
Yoshiaki Sakamoto ◽  
...  

2019 ◽  
Vol 20 (1) ◽  
pp. 392-403 ◽  
Author(s):  
Sharayu Kasar ◽  
Suchismita Mishra ◽  
Yasutaka Omori ◽  
Sarata Kumar Sahoo ◽  
Norbert Kavasi ◽  
...  

2020 ◽  
Author(s):  
Aurélie Diacre ◽  
Anne-Lare Faure ◽  
Agnès Moureau ◽  
Olivier Marie ◽  
Nina Griffiths ◽  
...  

<p>The Fukushima Dai-ichi Nuclear Power Plant (FDNPP) accident that occurred in March 2011 released significant quantities of radionuclides in the environment. So far, most of the research focused on radio-cesium and rarely on actinides. Until now, most of the studies on uranium and plutonium released by FDNPP were conducted on bulk environmental samples (soil, sediment, biota, etc.) and rarely on individual particles The investigation of individual particles allows working on the FDNPP signature alone compared to studies of bulk material which may also incorporate the signature of global fallout. Accordingly, the objective of the current research is to identify and characterize actinide-bearing particles in soil samples collected in the vicinity of FDNPP to get a better understanding of their formation mechanisms and of their fate in the environment. In order to identify and locate actinide-bearing particles in soil samples, we developed and implemented a method based on alpha-autoradiography (Jaegler et al., 2019), which allows identifying and locating specifically alpha-emitters, including plutonium isotopes 239Pu, 240Pu and 241Pu using a CR39 SSNTD device (Solid State Nuclear Tracks Detector).</p><p>Before alpha-autoradiography samples were dried, grinded with an agate mortar and sieved to several cutoffs: 1mm, 700µm, 400µm, 200µm, 100µm and 63µm. Cutoffs were chosen according to the sizes of actinide-bearing particles detected by Satou et al (2018). The absence of significant loss of uranium particles by the sieving process was demonstrated by the analysis of a test soil sample with a <sup>137</sup>Cs activity below 650 Bq/kg spiked with depleted uranium reference particles. After sieving, the test sample was deposited onto a carbon planchet for secondary ion mass spectrometry analysis in order to determine the particle recovery yield.</p><p>Then, the detection of actinide-bearing particles by means of alpha autoradiography was performed on various soil samples collected in the vicinity of FDNPP. Longer exposure times logically improve the detection efficiency of alpha-emitters-bearing particles. However, the exposure time should not exceed two months to limit the impact of emissions from naturally-occurring alpha-emitters.</p><p>We will present here the first results of detection of alpha-emitting particles in the analyzed soil samples.  Relative impacts of naturally-occurring alpha-emitters (<sup>234</sup>U/<sup>238</sup>U, <sup>235</sup>U, <sup>232</sup>Th and daughter nuclides) and of plutonium isotopes on alpha-radiography trace observation will be discussed.</p><p>The next steps of this study will be to develop and implement methods to sample and isolate alpha-emitting particles from the soil matrix and to characterize them in size, morphology, elemental and isotopic compositions. Full characterization of individual particles will be very helpful to determine their origin and to provide an understanding of their formation process and to determine their mobility and life-duration in the environment.</p><p>References:</p><ol><li>H. Jaegler, F. Pointurier, et al., 2019. Method for detecting and characterising actinide-bearing micro-particles in soils and sediment of the Fukushima Prefecture, Japan. Journal of Radioanalytical and Nuclear Chemistry, 321 (2019), 57–69. doi:10.1007/s10967-019-06575-w</li> <li>Y. Satou, K. Sueki,et al., 2018. Analysis of two forms of radioactive particles emitted during the early stages of the Fukushima Dai-ichi Nuclear Power Station accident. Geochemical Journal, 52 (2018), 1-7. doi:10.2343/geochemj.2.0514.</li> </ol>


Author(s):  
Toru Yamamoto

Based on radioactivity measurement of soil samples in the site of Fukushima Dai-Ichi Nuclear Power Station, radioactivity of Sr, Nb, Mo, Tc, Ru, Ag, Te, I, Cs, Ba, La, Pu, Am, and Cm isotopes were compiled as radioactivity ratios to 137Cs. By exponentially fitting or averaging, the radioactivity ratios at the core shutdown were estimated. They were divided by those of the fuel of the core at the shutdown to obtain a deposited radioactivity fractions of the nuclides as relative values to 137Cs, which also correspond to deposition fractions of the elements as relative values to Cs. They were estimated to be orders of 10−4 to 10−3 for Sr, 10−4 for Nb, 10−2 to 10−1 for Mo, 10−1 for Ag, 10−1 to 100 for Te, 100 for I, 10−3 for Ba, 10−6 to 10−5 for Pu, 10−6 to 10−5 for Am, and 10−6 for Cm. The observed radioactivity ratios to 137Cs were compared with those obtained by severe accident analysis to assess the validation of the analysis.


1994 ◽  
Vol 25 (5) ◽  
pp. 779-787 ◽  
Author(s):  
A.A. Ter-Saakov ◽  
M.V. Glebov ◽  
S.K. Gordeev ◽  
A.I. Ermakov ◽  
Yu.L. Luchkin ◽  
...  

Author(s):  
Donatas Butkus ◽  
Marina Konstantinova

Fern accumulates radionuclides in abundance, including 137Cs. Tranfer of 137Cs and 40K in plants which have different root systems (fern or grass), or have no roots at all (moss) was compared. Samplings were performed in regions contaminated with 137Cs after Chernobyl Nuclear Power Plant (ChNPP) accident in 1994 and 1997–2000. The male fern (Dryopteris filix‐mas) most prevailing in Lithuania was studied. Fern accumulates 137Cs more effectively than grass or moss. The average 137Cs activity concentration in fern is 180±60 Bq kg−1 and the transfer factor is 0,074 m2kg−1. The fern stipe accumulates 137Cs most of all (200±90 Bqkg‐1), the transfer factor is 0,087 m2 kg−1. Accumulation of 137Cs is influenced by the content of K in the soil. 137Cs and 40K activity concentrations in fern are higher than those in the soil what shows that fern accumulates 137Cs better than 40K. Fern can clean the soil because this plant accumulates radionuclides in its stipe rather than roots.


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