• Title/Summary/Keyword: 감마선분광분석기

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Assessment of Gamma-radiation dose Rate in the Ogcheon Lower Phyllite Area, Goesan County, Korea, Using Gamma-ray Spectrometry (감마선분광분석기를 이용한 괴산 옥천하부천매암대 일대의 감마선량 평가)

  • Yun, Uk;Cho, Byong-Wook
    • The Journal of Engineering Geology
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    • v.29 no.4
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    • pp.461-468
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    • 2019
  • Gamma-radiation dose rates were measured at 77 points around the Ogcheon lower phyllite zone (og2) in Goesan County, Korea, using gamma-ray spectrometry. Sample K contents were in the range 1.8-8.8% (average 4.6%), highest in Kgr. The eU contents were 0.2-217.9 ppm (average 16.7 ppm), highest in og2 (median 29.6 ppm). The eTh contents were 11.9-76.5 ppm (average 29.5 ppm) and the average eTh content of Kgr was 45.4 ppm, higher than those of Ogcheon meta-sedimentary rocks (og1, og2, and og3) (26.6-30.6 ppm). Except for some high-uranium sites in og2, 40K is the main radioactive material contributing to the gamma-radiation dose in the study area. Our results indicate that the outdoor effective dose rate of the area is 0.08-1.71 mSv y-1 (average 0.28 mSv y-1), with most areas apart from three points in og2 displaying dose rates <1 mSv y-1, which is the normal natural radiation background level.

Evaluation of 226Ra analysis methods using a gamma-ray spectrometer and a liquid scintillation counter (감마선분광분석기와 액체섬광계수기를 이용한 226Ra 분석법 비교 연구)

  • Ju, Byoung Kyu;Kim, Moon Su;Kim, Hyun Koo;Kim, Dong Su;Cho, Sung Jin;Yang, Jae Ha;Park, Sun Hwa;Kim, Hyoung Seop;Kwon, Oh Sang;Kim, Tae Seung
    • Analytical Science and Technology
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    • v.28 no.3
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    • pp.228-235
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    • 2015
  • The efficiency and applicability of the solid phase extraction disk method in a 226Ra analysis were examined by the gamma ray spectrometer (GRS) method using a Marinelli beaker and the liquid scintillation counter (LSC) method for groundwater. The recovered 226Ra, which was filtered by the solid phase extraction disk, was analyzed using gamma ray spectrometer The disks, which were pretreated for caulking the daughter nuclide, were sealed with polyethylene film. Distilled water was used for the blank value of the 226Ra activity. The recovery values of 214Bi and 214Pb in the solid phase extraction disk, which used 226Ra standard material, were 80% (295.21 Kev) and 104% (351.92 Kev), respectively, which were higher than 75% determined by the LSC. The injection of nitrogen gas into the measuring chamber reduced the interference values by about 10%. The detection limits of the 226Ra activity in a blank sample of 5 L were 0.17~0.40 pCi/L after 80,000 seconds of measuring time. The relationship of the 226Ra activity in the solid phase extraction disk method and in the LSC method in seven groundwater samples showed a correlation coefficient value 0.987, which implies the applicability of the solid phase extraction disk method. The results showed that 226Ra activity in groundwater using the solid phase extraction disk method has the following benefits: simple pretreatment, time saving, high recovery values, a low detection limit, and so on. Compared with the LSC method and the GRS method using the Marinelli beaker for the 226Ra analysis, the solid phase extraction disk method could be useful in groundwater samples with low levels of activities of radionuclides because the method is not restricted by the volume of the sample.

Evaluation of Terrestrial Gamma Radiation and Dose Rate of the Ogcheon Group Area (옥천층군 일대의 지표방사능과 감마선량 평가)

  • Yun, Uk;Cho, Byong-Wook
    • The Journal of Engineering Geology
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    • v.30 no.4
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    • pp.577-588
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    • 2020
  • We evaluated the distributions of primordial radionuclides and effective dose rate of the Ogcheon Group, which includes rocks with high uranium content. Terrestrial gamma radiation was measured at 421 points using a portable gamma ray spectrometer. Dividing the study area into five geological units (og1, og2, og3, og4, and igneous rocks) revealed no significant difference in the concentration of surface radioactivity among the types. The concentrations of 40K, eU, and eTh for all samples ranged from 0.7% to 10.3% (average 5.2%), 0.6 to 287.0 ppm (average 8.5 ppm), and 4.0 to 102.4 ppm (average 31.3 ppm), respectively. The absorbed dose rate in the study area (calculated from the activity concentrations of 40K, eU, and eTh) was in the range of 28.84 to 1,714.5 nGy/h (average 195.4 nGy/h). Among the five geological units, the lowest average was 166.3 nGy/h (for og1) and the highest average was 233.3 nGy/h (for og2; median 198.1 nGy/h). The outdoor effective dose rate for the area obtained from the absorbed dose rate was in the range of 0.04 to 2.10 mSv/y (average 0.24 mSv/y). Except for the four sites located in the uranium-bearing coal bed of og2, none of the studied sites exceeded 1 mSv/y.

The distribution of 137Cs activities in sediment samples of South-Han River basin (남한강수계 하천 퇴적물 시료 중 137Cs 분포)

  • Kim, Jiyu;Kang, Tae-Woo;Hong, Jung-Ki;An, Mijeong;Chang, Chaewon;Kim, Kyunghyun;Han, Young-Un;Kang, Taegu
    • Analytical Science and Technology
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    • v.29 no.6
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    • pp.293-299
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    • 2016
  • $^{137}Cs$ was investigated in river bottom sediments located in South-Han River basin and it was compared with international case studies to estimate the concentration level of $^{137}Cs$ in river sediment of Korea. The obtained values of $^{137}Cs$ which was analyzed by gamma-ray spectrometry were in the range of <$MDA{\sim}3.80{\pm}0.14Bq/kg{\cdot}dry$ and similar to the $^{137}Cs$ activities in soil of Korea. According to international case studies, $^{137}Cs$ activities were between 3.7 to $15,396Bq/kg{\cdot}dry$, when pollutants such as nuclear power plant accidents and radiation leaks were present near the rivers. The $^{137}Cs$ activities showed a variety of distribution depending on the country, when pollution occurs and survey time. Also, $^{137}Cs$ activities of river sediments without pollution sources were mostly less than $10Bq/kg{\cdot}dry$ in other countries. It was comparable with the obtained $^{137}Cs$ activities in this study. The obtained values provide useful information on the background concentration of $^{137}Cs$ in river sediment and will be able to use a basis for determining contamination of $^{137}Cs$ in the river.