Broad Energy HPGe Gamma Spectrometry for Dose Rate Estimation for Trapped Charge Dating

2010 ◽  
Vol 1 (2) ◽  
pp. 98-108 ◽  
Author(s):  
Jeong Hee Han
2021 ◽  
Author(s):  
Susanna Salminen-Paatero ◽  
Paul Dutheil ◽  
Timo Sundström ◽  
Ilia Rodushkin ◽  
Jussi Paatero

<p>Lichen and moss samples were collected from Russian Arctic areas (Kola Peninsula, Franz Josef Land and few other locations) in the 1990s. In 2020, <sup>137</sup>Cs was determined by HPGe gamma spectrometry from these samples after which isotopes of Pu and U were radiochemically separated from the samples. Mass ratios <sup>240</sup>Pu/<sup>239</sup>Pu and <sup>235</sup>U/<sup>238</sup>U were determined by ICP-MS for utilizing the characteristic isotopic fingerprints of different nuclear events. The aim of the work was to survey radioactive contamination sources in terrestrial environment in Russian Arctic regions, which have not yet been completely explored in respect to anthropogenic isotopes and their origin in the environment.</p>


2015 ◽  
Vol 143 ◽  
pp. 123-134 ◽  
Author(s):  
Shoichi Fuma ◽  
Sadao Ihara ◽  
Isao Kawaguchi ◽  
Takahiro Ishikawa ◽  
Yoshito Watanabe ◽  
...  
Keyword(s):  

Author(s):  
Tai Soo Chong ◽  
Hiroyuki Ohta ◽  
Yoshiyuki Nakashima ◽  
Takao Iida ◽  
Kengo Ieda ◽  
...  

Nukleonika ◽  
2016 ◽  
Vol 61 (3) ◽  
pp. 379-384 ◽  
Author(s):  
Jácint Jónás ◽  
Zoltán Sas ◽  
Janja Vaupotic ◽  
Erika Kocsis ◽  
János Somlai ◽  
...  

Abstract The health risk from thoron (Rn-220) is usually ignored owing to its short half-life (55.6 s), but the generated thoron decay products can cause a significant dose contribution. In this study, altogether 51 Slovenian soil samples were investigated using an accumulation chamber technique to obtain information about thoron exhalation features. The obtained (massic) thoron exhalation results varied between 6.9 and 149 mBq·kg−1·s−1 (average: 55.2 mBq·kg−1·s−1). The Th-232 content was determined using HPGe gamma spectrometry. The Th-232 activity concentration ranged between 9.3 and 161.7 Bq·kg−1 (average: 64.6 Bq·kg−1). The thoron emanation features were also calculated from the obtained results (2.9 to 21.2% with an average of 8.6%). The thoron exhalation and emanation properties were compared with the radon exhalation and emanation features determined in a previous study. It was found that there was no correlation between the radon and thoron emanation features, according to the obtained data. This can be explained by the different Ra-224 and Ra-226 distributions in the soil grains. As a result, the thoron emanation factor cannot be predicted from radon emanation and vice versa.


2019 ◽  
Vol 322 (2) ◽  
pp. 961-967 ◽  
Author(s):  
Mai Thanh Man ◽  
Vu Ngoc Ba ◽  
Dang Thi Thao My ◽  
Dang Nguyen Phuong ◽  
Truong Thi Hong Loan ◽  
...  

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