• 제목/요약/키워드: Radon ($^{222}Rn$)

검색결과 68건 처리시간 0.026초

G광역시 N유치원의 라돈 농도 (Radon Concentration at N-Kindergarten in G-City)

  • 박윤;김원준
    • 한국방사선학회논문지
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    • 제9권6호
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    • pp.421-424
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    • 2015
  • 본 연구는 G광역시 N유치원을 대상으로 창문을 닫고 열은 상태에서 라돈 가스를 측정하였다. 측정 결과 라돈가스를 측정한 N유치원의 실내 평균 라돈농도는 창문을 닫았을 때 2.9pCi, 창문을 열었을 때 0.8pCi로 미국 일반인 공기 중 라돈가스 최대허용농도 기준치인 4pCi 이하의 값으로 나타났다. 이러한 결과는 N유치원에서 라돈 가스에 대한 피폭은 문제가 되지 않으나 라돈 가스가 폐에 축척이 되면 폐암과 같은 피해를 입을 수 있다. 따라서 방어적 측면에서 유치원 내의 창문을 자주 열어 환기를 하는 것이 매우 중요함을 알 수 있었다.

Analysis of radon depth profile in soil air after a rainfall by using diffusion model

  • Maeng, Seongjin;Han, Seung Yeon;Lee, Sang Hoon
    • Nuclear Engineering and Technology
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    • 제51권8호
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    • pp.2013-2017
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    • 2019
  • The radon concentrations in soil air were measured before and after a rainfall. 226Ra concentration, porosity, moisture content and temperature in soil were measured at Kyungpook National University in Daegu. As the results of measurement and analysis, the arithmetic mean of measured 222Rn concentration increased from 12100 ± 500 Bq/㎥ to 16200 ± 600 Bq/㎥ after the rainfall. And the measured 226Ra concentration was 61.4 ± 5.7 Bq/kg and the measured porosity was 0.5 in soil. The estimated values of 226Ra concentration and porosity using diffusion model of 222Rn in soil were 60.3 Bq/kg and 0.509, respectively. The estimated values were similar to the measured values. 222Rn concentration in soil increased with depth and moisture content. The estimations were obtained through fitting based on the diffusion model of 222Rn using the measurement values. The measured depth profiles of 222Rn were similar to the calculated depth profiles of 222Rn in soil. We hope that the results of this study will be useful for environmental radiation analysis.

코코넛 기반 활성탄 필터의 라돈 제거 효율 (Radon Removal Efficiency of Activated Carbon Filter from Coconut)

  • 안윤진;김기섭;김태환;김상록
    • 대한방사선기술학회지:방사선기술과학
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    • 제46권2호
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    • pp.141-149
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    • 2023
  • The Korea Institute of Radiological and Medical Sciences plans to produce 225Ac, a therapeutic radio-pharmaceutical for precision oncology, such as prostate cancer. Radon, a radioactive gas, is generated by radium, the target material for producing 225Ac. The radon concentration is expected to be about 2000 Bq·m-3. High-concentration radon-generating facilities must meet radioactive isotope emission standards by lowering the radon concentration. However, most existing studies concerning radon removal using activated carbon filters measured radon levels at concentrations lower than 1000 Bq·m-3. This study measured 222Rn removal of coconut-based activated carbon filter under a high radon concentration of about 2000 Bq·m-3. The 222Rn removal efficiency of activated carbon impregnated with triethylenediamine was also measured. As a result, the 222Rn removal amount of the activated carbon filter showed sufficient removal efficiency in a 222Rn concentration environment of about 2000 Bq·m-3. In addition, despite an expectation of low radon reduction efficiency of Triethylenediamine-impregnated activated carbon, it was difficult to confirm a significant difference in the results. Therefore, it is considered that activated carbon can be used as a radioisotope exhaust filter regardless of whether or not Triethylenediamine is impregnated. The results of this study are expected to be used as primary data when building an air purification system for radiation safety management in facilities with radon concentrations of about 2000 Bq·m-3.

The Correlation between Radon (Rn222) and Particulate Matters (PM10, PM2.5, PM1.0) in Subway Tunnel in Seoul.

  • Versoza, Michael;Park, Duckshin
    • 한국입자에어로졸학회지
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    • 제13권2호
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    • pp.87-95
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    • 2017
  • Radon ($Rn^{222}$) is a radioactive gas and is found at high concentrations underground. Investigations were done in many years specifically on public transportations such as in the subway stations, concourses and platforms for these are located underground areas. This study correlates the $Rn^{222}$ concentrations with the Particulate Matter (PM) concentration for the gas could be attached or trapped inside these particles. It was done on the opening subway tunnel of Miasageori Station going to Mia Station (Line 4) last August 2016. Based on the result, the $Rn^{222}$ were more influenced on the mass ratio (%) of PM present in the air instead of its mass concentration (${\mu}g/m^3$). As the $PM_{10}$ mass ratio increases ($42.32{\pm}1.03%$) during morning rush-hours, radon starts to increase up to $0.97{\pm}0.03pCi/L$. But during the afternoon $Rn^{222}$ concentrations decreased while the composition were stable at $22.96{\pm}3.0%$, $39.04{\pm}0.6%$ and $38.01{\pm}0.3%$ in $PM_1$, $PM_{2.5}$ and $PM_{10}$ respectively. It was then assumed that it could be the composition of the morning hours of the station were influencing the concentration of the radon.

기반암에 따른 토양가스 222Rn농도의 분포에 관한 기초연구 (A Preliminary Study on Soil-Gas 222Rn Concentrations Depending on Different Bedrock Geology)

  • 제현국;강치구;전효택
    • 자원환경지질
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    • 제31권5호
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    • pp.415-424
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    • 1998
  • In order to investigate soil-gas $^{222}Rn$ concentrations, Kwanak Campus (Seoul National University), Boeun (Choong-buk) and Gapyung (Kyonggi) areas were selected and classified depending on their base rock types. Radon risk indices of these study areas decrease in the order of Gapyung>Kwanak Campus>Boeun areas, and in the order of rock type as banded gneiss>granite gneiss>granite>black slate-shale>mica schist>shale-lirnestone>phyllite-schist. Radon emanating trends with water content and grain size of soils were assessed by modified Morse 3 min. method. Radon emanation increases with the increase of water content in soils which is lower than 6~16 wt.%, and decreases in the range of higher than 6-16 wt. %. It shows that Rn emanation increases with the decrease of soil grain size. Radioactivity analysis of radionuclides of 238U series in some soil samples shows that radioactive disequilibrium state between $^{226}Ra$ and $^{238}U$ exists owing to different geochemical behavior of each radionuclide, and, it is necessary to carry out radioactive isotope geochemical approach for soil-gas $^{222}Rn$ study.

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광주광역시 광산구 소재 신축 아파트 라돈가스 농도 계측 (Measurement of Rn-222 Gas Concentration of Newly Constructed Apartment House in Gwangju Gwangsan-Gu)

  • 장희준;이상복
    • 한국방사선학회논문지
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    • 제9권4호
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    • pp.257-261
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    • 2015
  • 라돈은 우라늄-238과 토륨-232가 방사성붕괴 과정을 거친 후 생성되며, 무색, 무취의 불활성 기체로서 지하 또는 밀폐된 공간에 축적된다. 우라늄-238과 토륨-232는 지각의 암석이나 토양 등에 포함 돼 있다. 건축자재는 암석이나 토양을 재료로하여 만들어 진다. 가스 형태의 라돈은 호흡기를 통해 폐로 유입되고 라돈의 딸핵종이 폐나 기관지에 침적 되어 폐암을 일으키는 원인이 된다. 본 연구는 광주광역시 광산구에 위치한 신축 아파트를 대상으로 창문을 닫고 열은 상태에서 라돈 측정기를 이용하여 측정하였다. 측정 결과로 보아 신축 아파트 실내 평균 라돈농도는 미국 일반인 공기 중 라돈가스 최대허용농도 기준치 4 pCi보다 이하의 값이 나타난다는 것을 볼 수 있다. 측정 결과로 볼 때 신축 아파트의 라돈농도로 인한 피폭은 크지 않을 것으로 예상한다. 그러나 라돈가스가 신체 내에 축적이 되면 폐와 같은 경우는 폐암과 같은 피폭에 의한 피해를 얻을 수 있으므로 방사선 방어적 측면에서 측정 결과와 같이 라돈 농도를 낮추기 위해 창문을 자주 열어 환기를 시켜 피폭을 줄이는 것이 필요하다고 생각 된다.

실내 라돈환경계의 선량감도분석에 의한 제어매개변수 모델링 (Modeling the Controllable Parameters of Radon Environment System with Dose Sensitivity Analysis)

  • 주운표;장시영;김건중
    • Journal of Radiation Protection and Research
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    • 제16권2호
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    • pp.41-54
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    • 1991
  • 라돈 및 붕괴생성물의 호흡에 의한 인체 피폭선량의 제어가능성을 찾기 위해 다음과 같은 과정을 거쳤다. 1) 라돈에 관련된 기존모델을 토양 기공모델, 실내붕괴 모델, 폐선량계산모델로 분류해석하고, 2) topology이론에 따라 물리유추개념으로써 회로망으로 전환하여, 라돈환경계통을 정식화, 검증계산을 거쳐, 3) 모의계산으로 선량감도를 분석하여 최적 매개변수의 범위를 모색하였다. 매개변수인 환기율, 침적율, 부착율가 제어범위내 변화될 때, 정식화된 111원 연립방정식의 해를 구하여 선량감도를 분석하였으며, 제어매개변수의 선량감도에 의한 효과를 3차원으로 도식화하였다. 본 연구 수행결과, 제어매개변수 변화에 따른 실내의 $^{222}Rn$ 및 Rn-D의 농도 변화과정은 새롭게 해석할 수 있는 벡터감도단층모형으로, 일부 제어매개변수의 조합변화에 따른 선량감도는 3차원 그래프모형으로 나타낼 수 있었다. 선량감도의 3차원 그래프에서는 실내환경의 대표적 매개변수 값 범위에서 변곡점이 나타났으며, 일반적으로 높은 환기조건$(>1h^{-1})$하에서는 공기정화에 의하여 선량이 전반적으로 증가되나, 불충분한 환기조건$(<0.5h^{-1})$하에서는 공기정화에 의하여, 선량이 40%정도로 감소되는 것으로 나타났다 (* 라돈 및 붕괴생성물은 이하 $^{222}Rn$ 및 Rn-D로 통일한다.)

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지하수의 라듐/라돈 동시측정을 위한 백그라운드 감마선 제어

  • 이길용;윤윤열;조수영;김용제
    • 한국지하수토양환경학회:학술대회논문집
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    • 한국지하수토양환경학회 2005년도 총회 및 춘계학술발표회
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    • pp.308-311
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    • 2005
  • [ $^{222}Rn\;and\;^{226}Ra$ ] in groundwater were determined simultaneously using a gamma-spectroscopy. A nitrogen flushing equipment has been used for elimination and stabilization of high and unstable background activity due to the radon and its progenies in counting shield and room. The aim of present work was to control the background activity for simultaneous measurement of radium$(^{226}Ra)$ and radon$(^{222}Rn)$ in groundwater using a gamma-spectrometry. Background activity was about 1.0dps and the standard deviation was about 50%, The background activity could be minimized using nitrogen flushing equipment in the range of 0.1 to 0.5 and the RSD was about 5% at the experimental condition. The detection limit of $^{222}Rn\;and\;^{226}Ra$ in groundwater was 0.5dps/L in the background control method. In most groundwater used in the work, radon activity was more than the detection limit. However, radium activity in some groundwater was less than the detection limit. If the low level radium in groundwater must be measured, preconcentration process such as concentration should be performed before measuring the groundwater.

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지하수와 지표수에서의 라돈 및 우라늄의 실태 조사 (The Study of Radon Activity and Uranium Concentration of Ground Water and Surface Water)

  • 오영미;이종복;신경진;김학철;이재희;황상철;정상기;이상태
    • 한국물환경학회지
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    • 제23권2호
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    • pp.201-205
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    • 2007
  • This paper reports the amount of $^{222}Rn$ and $^{238}U$ in 18 sites of ground water and 30 sites of surface water. The instrument used to count $^{222}Rn$ activity was the liquid scintillation counter (LSC) which could resolute ${\alpha}$ and ${\beta}$ radiations. And $^{238}U$ was analyzed by the inductively coupled plasma (ICP). Radon and Uranium were not detected in raw and treated water which were sampled in a water treatment plant. However, radon ($^{222}Rn$) was high concentration in ground water from Jeon-la, Gang-won. So was uranium ($^{238}U$) in case of ground water from Gang-won, Choong-chung. Radon ($^{222}Rn$) activities were detected less than 15 pCi/L at 5 sampling points, 15~300 pCi/L at 7 sampling points, 300~4000 pCi/L at 6 sampling points. However, Radon ($^{222}Rn$) activities of all ground water samples were less than 4,000 pCi/L, which was bellow American Alternative Maximum Contamination Level (AMCL). Uranium ($^{238}U$) concentrations were less than $0.1{\mu}g/L$ at 5 sampling points, from $0.1{\mu}g/L$ to $20{\mu}g/L$ at 13 sampling points. Uranium was not detected in about 30% of the whole samples, but the concentration ranged from relatively low to high concentrations depending on the sampling point. The minimum detectable activity (MDA) of radon was 15 pCi/L. and the detection limit of uranium was $0.1{\mu}g/L$.