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주병규,김문수,김현구,김동수,김영록,정도환,양재하,박선화,김태승,Ju, Byoung Kyu,Kim, Moon Su,Kim, Hyun Koo,Kim, Dong Su,Kim, Young Rok,Jeong, Do Hwan,Yang, Jae Ha,Park, Sun Hwa,Kim, Tae Seung 한국지하수토양환경학회 2014 지하수토양환경 Vol.19 No.3
In order to study gross alpha analysis method using LSC, the efficiency tests with uranium standard materials were performed and then compared with the GPC method (US EPA 900.0 method) using 15 groundwater samples. For 15 groundwater samples, the average efficiencies of the GPC and LSC method were 7~11% and 90%, respectively. The average precisions of the GPC and LSC method were 16.16% and 6.00%, respectively. Also, The average standard deviations for 15 samples were 7.38 pCi/L and 2.95 pCi/L, respectively. The determination coefficient of the tested results by two methods was 0.9948. As a result, the LSC method tested in this study was applicable for the screening of the gross alpha and showed the advantages in the gross alpha measurement due to the simple measurement procedures.
국내 변성암 지역 음용지하수 중 자연방사성물질(<sup>238</sup>U, <sup>222</sup>Rn)의 환경 특성 연구
주병규,김문수,정도환,홍정기,김동수,노회정,윤정기,김태승,Ju, Byoung Kyu,Kim, Moon Su,Jeong, Do Hwan,Hong, Jung Ki,Kim, Dong Su,Noh, Hoe Jung,Yoon, Jeong Ki,Kim, Tae Seung 한국지하수토양환경학회 2013 지하수토양환경 Vol.18 No.3
This study has investigated naturally occurring radioactive materials (N.O.R.M; $^{238}U$, $^{222}Rn$) for 353 drinking groundwater wells in metamorphic rock areas in Korea. Uranium concentrations ranged from N.D (not detected) to 563.56 ${\mu}g/L$ (median value, 0.68 ${\mu}g/L$) and radon concentrations ranged from 108 to 11,612 pCi/L (median value, 1,400 pCi/L). Uranium and radon concentrations in the groundwater generally are similar to USA with similar geological setting. Uranium concentrations in 9 wells (2.6%) exceeded 30 ${\mu}g/L$, which is the maximum contaminant level (MCL) by the US environmental protection agency (EPA), radon concentrations in 46 wells (13%) exceeded 4,000 pCi/L, which is the Alternative MCL (AMCL) by the US.EPA. The log-log correlation coefficient between uranium and radon was 0.32. The correlation coefficient between uranium and pH was 0.12 and the correlation coefficient between radon and temperature was -0.01. The correlation coefficient between uranium and $HCO_3$ was 0.09 and the correlation coefficient between uranium and Ca was 0.11. The median value of uranium was high Chung-Buk (1.78 ${\mu}g/L$), Gyeong-Buk (1.37 ${\mu}g/L$), In-Cheon (1.06 ${\mu}g/L$) for each province. On the other hand, the median value of radon was high In-Cheon (2,962 pCi/L), Chung-Buk (2,339 pCi/L), Jeon-Buk (2,165 pCi/L) for each province. Jeon-Buk for log-log correlation coefficient is the highest (0.63) among provinces.
국내 화산암 지역 지하수 중 자연방사성 물질에 대한 환경 특성
정도환,김문수,주병규,홍정기,김동수,김현구,김혜진,박선화,한진석,김태승,Jeong, Do Hwan,Kim, Moon Su,Ju, Byoung Kyu,Hong, Jung Ki,Kim, Dong Su,Kim, Hyun Koo,Kim, Hye Jin,Park, Sun Hwa,Han, Jin Seok,Kim, Tae Seung 한국지하수토양환경학회 2013 지하수토양환경 Vol.18 No.1
We analyzed natural radionuclides in 80 wells in volcanic rock areas and investigated environmental characteristics. Uranium and radon concentrations ranged from ND to $9.70{\mu}g/L$ (median value: 0.21) ${\mu}g/L$, 38~29,222 pCi/L (median value: 579), respectively. In case of gross-${\alpha}$, 26 samples exceeded MDA (minimum detectable activity, < 0.9 pCi/L) value and the activity values ranged from 1.05 to 8.06 pCi/L. The radionuclides concentrations did not exceed USEPA MCL (maximum contaminant level) value of Uranium ($30{\mu}g/L$) and gross-${\alpha}$ (15 pCi/L). But Rn concentrations in 4 samples exceeded USEPA AMCL (Alternative maximum contaminant level, 4,000 pci/L) and one of them showed a significantly higher value (29,222 pCi/L) than the others. The levels of uranium concentrations in volcanic rock aquifer regions were detected in order of andesite, miscellaneous volcanic rocks, rhyolite, basalt aquifer regions. Radon, however, was detected in order of miscellaneous volcanic rocks, rhyolite, andesite, basalt aquifer regions. The correlation coefficient between uranium and radon was r = 0.45, but we found that correlations of radionuclides with in-situ data or major ions were weak or no significant. The correlation coefficient between the depth of wells and uranium concentrations was a slightly higher than that of depth of wells and radons. Radionuclide concentrations in volcanic rock aquifers showed lower levels than those of other rock aquifers such as granite, metamorphic rock aquifers, etc. This result may imply difference of host rock's bearing-radioactive-mineral contents among rock types of aquifers.
정도환,이영준,주병규,노회정,유순주,김문수,Jeong, Do-Hwan,Lee, Young-Joon,Ju, Byoung-Kyu,Noh, Hoe-Jung,Yu, Soon-Ju,Kim, Moon-Su 한국지하수토양환경학회 2011 지하수토양환경 Vol.16 No.5
Groundwaters were sampled from 730 wells being used for drinking purposes during 2007-2009. These samples were analysed using a gas-flow type GPC (Gas Proportional Counter) according to the USEPA method (900.0). We obtained a gross-alpha counting TDS (total dissolved solid) efficiency curve (Y = 0.0017X2 - 0.3122X + 19.165, X = TDS, Y = efficiency, $R^2$ = 0.9734) using natural uranium standard to get gross ${\alpha}$ value of the samples. The gross alpha values ranged from MDA (minimum detectable activity) to 14.88 pCi/L and 429 samples showed values higher than MDA (< 0.9 pCi/L). Correlations of the uranium values with the total alpha values and the gross-alpha values indicate that uranium values have high impacts on gross-alpha values. Groundwater samples of study areas were classified into four regions according to the rock types; plutonic (granite) rock region (427 areas), metamorphic rock region (181 aeras), sedimentary rock region (70 areas), volcanic rock region (52 areas). Groundwater of Cretaceous granite presented the highest gross-alpha value. Gross alpha in groundwaters showed no relationship with uranium in terms of the geological ages, rocks and minerals.
정도환,김문수,주병규,김태승,Jeong, Do-Hwan,Kim, Moon-Su,Ju, Byoung-Kyu,Kim, Tae-Seung 한국지하수토양환경학회 2011 지하수토양환경 Vol.16 No.6
In order to figure out the characteristics of radionuclides concentrations of nine provinces, we analyzed uranium and radon in 681 samples of groundwater. Most of uranium concentrations in each province were less than $10{\mu}g/L$, and Gyeongnam, Jeonnam, Jeju provinces did not have groundwaters exceeding the US EPA drinking water MCL ($30{\mu}g/L$) of uranium. The ratio of radon values exceeding US EPA drinking water AMCL (4,000 pCi/L) was 22.6% (154/681) and Gyeongnam and Jeju provinces had no groundwaters exceeding the AMCL (alternative maximum contaminant level). Uranium and radon concentrations in groundwaters of Gyeonggi, Chungbuk, Jeonbuk, Chungnam mainly composed of the Mesozoic granite and the Precambrian gneiss were relatively high, but the concentrations of Gyeongnam and Jeju widely comprised of the sedimentary rock and the volcanic rock were relatively low. A week correlation between uranium and radon values showed in Gangwon, Chungbuk, Gyeonggi provinces.
노회정,정도환,윤정기,김문수,주병규,전상호,김태승,Noh, Hoe-Jung,Jeong, Do-Hwan,Yoon, Jeong-Ki,Kim, Moon-Su,Ju, Byoung-Kyu,Jeon, Sang-Ho,Kim, Tae-Seung 한국지하수토양환경학회 2011 지하수토양환경 Vol.16 No.1
To investigate the natural reduction characteristics of radon with a short half-life (3.82 day) in drinking Qgroundwater, we analyzed the changes of radon concentrations of groundwater, waters in storage tanks, and tap waters from the small-scale groundwater-supply systems (N = 301) by LSC (Liquid Scintillation Counter). We also analyzed the concentrations of uranium (half-life 4.5 billion years) in the waters by ICP/MS to compare with natural reduction of radon concentration. The radon concentrations of 68 groundwater-supply systems occupying 22.6% of the total samples exceeded the US EPA's Alternative Maximum Contaminant Level (AMCL : 4,000 pCi/L), with the average radon concentration of 7,316 pCi/L (groundwaters), 3,833 pCi/L (tank waters) and 3,407 pCi/L (tap waters). Compared to the radon levels of pumped groundwaters, those of tank and tap waters naturally reduced significantly down to about 50%. Especially, in case of 29 groundwater-supply systems with the groundwater radon concentrations of 4,000~6,000 pCi/L, average radon concentrations of the tank and tap waters naturally decreased down to the AMCL. Therefore this study implies that radon concentrations of drinking groundwater can be effectively reduced by sufficient storage and residence in tanks.
지하수 중 라듐-226의 분석방법 및 환경 특성에 관한 예비 연구
정도환,김문수,노회정,윤윤열,김동수,이영준,주병규,홍정기,김태승,Jeong, Do-Hwan,Kim, Moon--Su,Noh, Hoe-Jung,Yoon, Yoon-Yeol,Kim, Dong-Soo,Lee, Young-Joon,Ju, Byoung-Kyu,Hong, Jung-Ki,Kim, Tae-Seung 한국지하수토양환경학회 2012 지하수토양환경 Vol.17 No.2
$^{226}Ra$ in groundwater could be analyzed by various methods. LSC (liquid scintillation counter) is used to measure its activity of Ba co-precipitates with Hisafe III scintillation cocktail solution. Counting efficiency was obtained using NIST $^{226}Ra$ standard solution in triplicate and calculated $^{226}Ra$ concentration using the efficiency values. $^{226}Ra$ values of 19 groundwaters having Gross-${\alpha}$ concentrations of more than 5 pCi/L ranged from ND (${\leq}$ 0.1 pCi/L) to 1.18 pCi/L. Geologic settings of the 19 areas are composed of granitic rocks of Pre-Cambrian and Jurassic and Cretaceous, gneiss (schist) of Pre-Cambrian, and volcanic rocks of Cretaceous. No relationship was shown among $^{226}Ra$ a concentrations and in-situ water quality data, and Gross-${\alpha}$, uranium, radon concentrations.
복운모화강암지역 지하수 중 자연방사성 물질의 경시적 붕괴특성 연구
김문수,김태승,김현구,김동수,정도환,주병규,홍정기,김혜진,박선화,정찬호,조병욱,한진석,Kim, Moon Su,Kim, Tae Seung,Kim, Hyun Koo,Kim, Dong Su,Jeong, Do Hwan,Ju, Byoung Kyu,Hong, Jung Ki,Kim, Hye Jin,Park, Sun Hwa,Jeong, Chan Ho,Cho, Byong 한국지하수토양환경학회 2013 지하수토양환경 Vol.18 No.4
To figure out the decay characteristics of naturally occurring radionuclides, eight sampled groundwaters from a monitoring borehole having high levels of uranium and radon concentrations in a two mica granitic area have analyzed by liquid scintillation counters (LSC) for over 1 year. In December 2011, three groundwater samples (DJ1, DJ2, DJ3) were obtained from each aquifer system located at -20 m, -40 m, -60 m of the monitoring borehole below the ground surface, respectively. Five samples (DJ4, DJ5, DJ6, DJ7, DJ8) were additionally gained from each aquifer positioned -20 m, -40 m, -60 m, -100 m, -105 m of the borehole in February 2012, respectively. Temporal variation characteristics of uranium and radon concentrations have showed over maximum 2.1 times and 1.4 times fluctuations of the values in the same sampling intervals over time, respectively. The intervals of -40 m and -105 m in the borehole have the highest values of uranium and radon concentrations, respectively. This may imply that the concentrations of naturally occurring radionuclides such as uranium and radon in groundwater have been changed over time and indicate that the qualities of groundwaters from the aquifers developed at each interval in the borehole are different each other. This discrepancy, moreover, could be caused by behaviour differences between uranium which is in ionic status having a half life of 4.6 billion years and is transported along with the flowing groundwater, and radon which is in gaseous status having a 3.82 day's half life in the aquifer systems. Physicochemical characteristics of groundwaters from the aquifer systems could be identified by the results of the on-situ measuring items such as pH and Eh, and the major ionic contents. The CPM values of eight groundwater samples analysed by LSC over one year have shown not to follow the theoretical decay curve of the radon. The CPM values of the samples have ranged from 2 to 7.5 after it had passed two months when the theoretical CPM values of the radon started zero since the initial analysis. Alpha and beta particle spectrums have shown the peaks of radium-226, however they have not revealed any peaks of radon and it's daughter products such as polonium-218 and 214, bismuth-214 for the late stage of the analysis. This implies that the groundwater from the borehole may contain radium-226 having a half life of 1,600 years which decays continuously.
지하수 중 <sup>222</sup>Rn 분석을 위한 정도관리
정도환,김문수,김현구,김혜진,박선화,한진석,주병규,전상호,김태승,Jeong, Do Hwan,Kim, Moon Su,Kim, Hyun Koo,Kim, Hye Jin,Park, Sun Hwa,Han, Jin Seok,Ju, Byoung Kyu,Jeon, Sang Ho,Kim, Tae Seung 한국분석과학회 2013 분석과학 Vol.26 No.1
짧은 반감기(3.82일)로 인하여 표준물질이 없어서 $^{226}Ra$ 표준선원을 이용하여 액체섬광계수기(Liquid Scintillation Counter)의 측정효율을 산정한 후 구하는 $^{222}Rn$ 농도 분석의 정도 관리를 위해서 blank(바탕)시료, 중복시료, 원수 채취전과 후의 시료 분석을 수행하였다. 현장 바탕시료는 0.44~6.28 pCi/L, 실험실 바탕시료는 1.66~4.95 pCi/L 값을 보였다. 둘 사이의 상관계수는 0.9691이였으며, 현장시료채취, 시료 이동, 시료 보관 상태에서 다른 오염원은 없었음을 확인하였다. 65개의 원시료와 중복시료의 상관계수는 0.9987을 보였다. 라돈은 불활성 기체이므로 시료를 채취할 때 손실에 의해 지하수 중 라돈 농도에 영향을 미칠 것으로 사료되어 증류수를 이용하여 현장 지하수 시료 채취 전과 후로 구분하여 비교분석하였으나 유의한 농도차이를 보이지 않았다. $^{222}Rn$ concentrations in the groundwater samples without standard material due to the short half-life (3.82 day) were measured through the establishment of the counting efficiency of LSC (Liquid Scintillation Counter) using a standard source of $^{226}Ra$. This study for Quality Assurance/Quality Control (QA/QC) of $^{222}Rn$ analysis was performed to analyze blank samples, duplicate samples, samples of groundwater sampling before and after. In-situ blank samples collected were in the range of 0.44~6.28 pCi/L and laboratory samples were in the range of 1.66~4.95 pCi/L. Their correlation coefficient was 0.9691 and the source contamination from sampling, migration and keeping of samples were not identified. The correlation coefficient between original and duplicate samples from 65 areas was 0.9987. Because radon is an inert gas, in case of groundwater sampling, it is considered to affect the radon concentration. We analyzed samples separately by groundwater sampling before and after using distilled water, but there is no significant difference for $^{222}Rn$ concentrations in distilled waters of two types.