• Nuclear Engineering and Technology
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• 제55권11호
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• pp.3935-3939
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• 2023

The paper presents the results of a study of radioactive noble gases and from decay products in the atmosphere of the reactor hall of the research nuclear reactor IVV-2M. The distribution of short-lived ⁸⁸Rb and ¹³⁸Cs activity by sizes of aerosol particles was measured in the range of 0.5-1000 nm. It is shown that radioactive aerosols are characterized by three main modes with AMTD 2-3 nm, 7-15 nm and 400 nm. About 70% of aerosol activity is due to ⁸⁸Rb. The equilibrium factor between ⁸⁸Kr and ⁸⁸Rb is 0.2 ± 0.1. The total concentration of aerosols particles was measured using an aerosol diffusion spectrometer. The value of unattached fraction of radioactive aerosols in the atmosphere of reactor hall IVV2M was f = 0.15-0.25 at the average total aerosol particles concentration from 20,000 cm³ to 53,000 cm³.

• 자원리싸이클링
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• 제9권6호
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• pp.31-35
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• 2000

Mn-Zn ferrite 폐기물을 시멘트와 혼합한 복합전파흡수체를 제작하여 재료정수 및 반사감쇠량을 조사하였다. 지지재로 사용한 시멘트는 실리콘 고무의 재료정수와 비교하여 높은 복소유전율($\varepsilon$=$_{r}$': 7.6, $\varepsilon_{r}$ ": 0.6)을 나타내었고, Mn-Zn ferrite 폐기물과 시멘트의 혼합무게비(F/C)가 증가함에 따라 복소유전율은 감소하였고, 복소투자율은 증가하였다. 최대반사감쇠량을 나타내는 주파수는 F/C가 1에서 3으로 증가함에 따라 2.7 GHz에서1.3 GHz로 감소하였고, 정합두께는 8.7 mm에서 12.7 mm로 증가하는 경향이 나타났다. 모든 시편에서 최대반사감쇠량은 -40 dB 이상으로 Mn-Zn ferrite 폐기물을 전파흡수체로 활용이 가능하다.

• 한국전기전자재료학회논문지
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• 제14권3호
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• pp.197-201
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• 2001

The microwave dielectric properties of (1-x)Ba(Mg$_{1}$3/Ta$_{2}$3/)O$_3$-xBa(Co$_{1}$3/Nb$_{2}$3)O$_3$(x=0.25~0.5) ceramics depending on the Ba(Co$_{1}$3/Nb$_{2}$3/)O$_3$[BCN] contents and the possibility of application as a microwave dielectric resonator were investigated. The specimens were prepared by he conventional mixed oxide method using there sintering temperature of 1575$^{\circ}C$. It was found that Ba(Mg$_{1}$3/Ta$_{2}$3/)O$_3$[BMT] and BCN formed a solid solution with complex perovskite structure. As the mole fraction of BCN increased, dielectric constant increased while temperature coefficient of resonant frequency decreased. The highest value of quality factor, Qxf$_{0}$=138,205GHz, obtained in the sample of 0.9BMT-0.1BCN ceramics. In the range of x$\geq$0.4, the dielectric constant was about 30. The 0.55BMT-0.45BCN ceramics showed excellent microwave dielectric properties with $\varepsilon$$_{r}$=30.84, Qxf$_{0}$=75,325GHz and $\tau$$_{f}$=2.9015ppm/$^{\circ}C$.EX>.EX>.

• 한국지구과학회지
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• 제28권6호
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• pp.720-732
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• 2007

수도권과 경상 분지 동부일대의 98 개 지진자료에 확장 Coda 규격화법을 적용하여 $Q_P^{-1}$과 $Q_S^{-1}$을 구하였다. 중심 주파수 1.5 Hz에서 24 Hz로 증가할수록 수도권 일대의 $Q_P^{-1}$은 $(4.0{\pm}9.2){\times}10^{-3}$에서 $(4.1{\pm}4.2){\times}10^{-4}$로 $Q_S^{-1}$은 $(5.5{\pm}5.6){\times}10^{-3}$에서 $(3.4{\pm}1.3){\times}10^{-4}$로 감소한다. 경상분지 동부일대의 $Q_P^{-1}$은 $(5.4{\pm}8.8){\times}10^{-3}$에서 $(3.7{\pm}3.4){\times}10^{-4}$로 $Q_S^{-1}$은 $(5.7{\pm}4.2){\times}10^{-3}$에서 $(3.5{\pm}1.6){\times}10^{-4}$로 감소한다. 수도권 일대의 결과를 주파수의 지수형태로 나타내면 $Q_P^{-1}$와 $Q_S^{-1}$는 $0.005f^{-0.89}$ 와 $0.004f^{-0.88}$이며, 경상분지 동부 일대에서는 $0.007f^{-1.02}$와 $0.006f^{-0.99}$로 각각 나타낼 수 있다. 이는 $Q_S^{-1}$는 두 지역이 거의 유사하나 $Q_P^{-1}$값이 경상 분지 동부 일대가 수도권 일대에 비해 상대적으로 약간 높음을 알 수 있다. 이는 아마도 경상분지 동부 지역의 지각이 지진학적으로 불균질성이 다소 더 크다고 추정된다. 그러나, 세 계의 여러 다른 지역의 값과 비교해 보면 수도권 일대와 경상 분지 동부 일대 지각은 모두 순상지의 범주에 해당하는 값을 나타낸다.

• 한국농공학회지
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• 제19권1호
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• pp.4296-4311
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• 1977

This study was conducted to derive an Instantaneous Unit Hydrograph for the accurate and reliable unitgraph which can be used to the estimation and control of flood for the development of agricultural water resources and rational design of hydraulic structures. Eight small watersheds were selected as studying basins from Han, Geum, Nakdong, Yeongsan and Inchon River systems which may be considered as a main river systems in Korea. The area of small watersheds are within the range of 85 to 470$\textrm{km}^2$. It is to derive an accurate Instantaneous Unit Hydrograph under the condition of having a short duration of heavy rain and uniform rainfall intensity with the basic and reliable data of rainfall records, pluviographs, records of river stages and of the main river systems mentioned above. Investigation was carried out for the relations between measurable unitgraph and watershed characteristics such as watershed area, A, river length L, and centroid distance of the watershed area, Lca. Especially, this study laid emphasis on the derivation and application of Instantaneous Unit Hydrograph (IUH) by applying Nash's conceptual model and by using an electronic computer. I U H by Nash's conceptual model and I U H by flood routing which can be applied to the ungaged small watersheds were derived and compared with each other to the observed unitgraph. 1 U H for each small watersheds can be solved by using an electronic computer. The results summarized for these studies are as follows; 1. Distribution of uniform rainfall intensity appears in the analysis for the temporal rainfall pattern of selected heavy rainfall event. 2. Mean value of recession constants, Kl, is 0.931 in all watersheds observed. 3. Time to peak discharge, Tp, occurs at the position of 0.02 Tb, base length of hlrdrograph with an indication of lower value than that in larger watersheds. 4. Peak discharge, Qp, in relation to the watershed area, A, and effective rainfall, R, is found to be {{{{ { Q}_{ p} = { 0.895} over { { A}^{0.145 } } }}}} AR having high significance of correlation coefficient, 0.927, between peak discharge, Qp, and effective rainfall, R. Design chart for the peak discharge (refer to Fig. 15) with watershed area and effective rainfall was established by the author. 5. The mean slopes of main streams within the range of 1.46 meters per kilometer to 13.6 meter per kilometer. These indicate higher slopes in the small watersheds than those in larger watersheds. Lengths of main streams are within the range of 9.4 kilometer to 41.75 kilometer, which can be regarded as a short distance. It is remarkable thing that the time of flood concentration was more rapid in the small watersheds than that in the other larger watersheds. 6. Length of main stream, L, in relation to the watershed area, A, is found to be L=2.044A0.48 having a high significance of correlation coefficient, 0.968. 7. Watershed lag, Lg, in hrs in relation to the watershed area, A, and length of main stream, L, was derived as Lg=3.228 A0.904 L-1.293 with a high significance. On the other hand, It was found that watershed lag, Lg, could also be expressed as {{{{Lg=0.247 { ( { LLca} over { SQRT { S} } )}^{ 0.604} }}}} in connection with the product of main stream length and the centroid length of the basin of the watershed area, LLca which could be expressed as a measure of the shape and the size of the watershed with the slopes except watershed area, A. But the latter showed a lower correlation than that of the former in the significance test. Therefore, it can be concluded that watershed lag, Lg, is more closely related with the such watersheds characteristics as watershed area and length of main stream in the small watersheds. Empirical formula for the peak discharge per unit area, qp, ㎥/sec/$\textrm{km}^2$, was derived as qp=10-0.389-0.0424Lg with a high significance, r=0.91. This indicates that the peak discharge per unit area of the unitgraph is in inverse proportion to the watershed lag time. 8. The base length of the unitgraph, Tb, in connection with the watershed lag, Lg, was extra.essed as {{{{ { T}_{ b} =1.14+0.564( { Lg} over {24 } )}}}} which has defined with a high significance. 9. For the derivation of IUH by applying linear conceptual model, the storage constant, K, with the length of main stream, L, and slopes, S, was adopted as {{{{K=0.1197( {L } over { SQRT {S } } )}}}} with a highly significant correlation coefficient, 0.90. Gamma function argument, N, derived with such watershed characteristics as watershed area, A, river length, L, centroid distance of the basin of the watershed area, Lca, and slopes, S, was found to be N=49.2 A1.481L-2.202 Lca-1.297 S-0.112 with a high significance having the F value, 4.83, through analysis of variance. 10. According to the linear conceptual model, Formular established in relation to the time distribution, Peak discharge and time to peak discharge for instantaneous Unit Hydrograph when unit effective rainfall of unitgraph and dimension of watershed area are applied as 10mm, and $\textrm{km}^2$ respectively are as follows; Time distribution of IUH {{{{u(0, t)= { 2.78A} over {K GAMMA (N) } { e}^{-t/k } { (t.K)}^{N-1 } }}}} (㎥/sec) Peak discharge of IUH {{{{ {u(0, t) }_{max } = { 2.78A} over {K GAMMA (N) } { e}^{-(N-1) } { (N-1)}^{N-1 } }}}} (㎥/sec) Time to peak discharge of IUH tp=(N-1)K (hrs) 11. Through mathematical analysis in the recession curve of Hydrograph, It was confirmed that empirical formula of Gamma function argument, N, had connection with recession constant, Kl, peak discharge, QP, and time to peak discharge, tp, as {{{{{ K'} over { { t}_{ p} } = { 1} over {N-1 } - { ln { t} over { { t}_{p } } } over {ln { Q} over { { Q}_{p } } } }}}} where {{{{K'= { 1} over { { lnK}_{1 } } }}}} 12. Linking the two, empirical formulars for storage constant, K, and Gamma function argument, N, into closer relations with each other, derivation of unit hydrograph for the ungaged small watersheds can be established by having formulars for the time distribution and peak discharge of IUH as follows. Time distribution of IUH u(0, t)=23.2 A L-1S1/2 F(N, K, t) (㎥/sec) where {{{{F(N, K, t)= { { e}^{-t/k } { (t/K)}^{N-1 } } over { GAMMA (N) } }}}} Peak discharge of IUH) u(0, t)max=23.2 A L-1S1/2 F(N) (㎥/sec) where {{{{F(N)= { { e}^{-(N-1) } { (N-1)}^{N-1 } } over { GAMMA (N) } }}}} 13. The base length of the Time-Area Diagram for the IUH was given by {{{{C=0.778 { ( { LLca} over { SQRT { S} } )}^{0.423 } }}}} with correlation coefficient, 0.85, which has an indication of the relations to the length of main stream, L, centroid distance of the basin of the watershed area, Lca, and slopes, S. 14. Relative errors in the peak discharge of the IUH by using linear conceptual model and IUH by routing showed to be 2.5 and 16.9 percent respectively to the peak of observed unitgraph. Therefore, it confirmed that the accuracy of IUH using linear conceptual model was approaching more closely to the observed unitgraph than that of the flood routing in the small watersheds.

• 멤브레인
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• 제17권2호
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• pp.99-111
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• 2007

먹는 물 내에 존재하는 발암원인으로 의심되는 유기화학물질을 재래식 정수처리방법으로 제거한다는 것은 불가능하다. 이들을 AOP산화 & M/F membrane 혼성공정법을 이용하여 목적하는 처리수로 처리하고자 지하수를 반응조에 유효용량으로 유입하고 유기화학물질을 인위적으로 투입 혼합하여 충분히 희석시키고 이것을 효율적으로 처리하기 위해 최적운전조건을 도출하였다. 유기 화학물질 중 VOCs는 페놀과 톨루엔을 그리고 농약은 파라치온, 다이아지논과 카바닐을 대상으로 조사하였다. 실험은 각각 분류별 단일용액과 혼합용액으로 수행하였으며, 실험결과 충분한 분해 및 제거를 위한 운전조건은 $H_2O_2$는 150 mL로 정량 주입하고, pH는 $5.5{\sim}6.0$, 온도는 $12{\sim}16^{\circ}C$로 일정하게 유지하고, 용존오존량은 5.0 mg/L이상, 반응시간은 $30{\sim}40$분이 최적 조건이었으며 그리고 같은 반응기 내 분리막의 사용은 $0.45{\mu}m$ 공경크기의 M/F membrane을 이용하여 대량의 음용수를 얻기 위한 결정이었다.

• Korean Journal of Radiology
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• 제22권3호
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• pp.425-434
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• 2021

Objective: To investigate the potential value of ¹⁸F-fluorodeoxyglucose (FDG) PET/CT in predicting the survival of patients with primary tracheal malignant tumors. Materials and Methods: An analysis of FDG PET/CT findings in 37 primary tracheal malignant tumor patients with a median follow-up period of 43.2 months (range, 10.8-143.2 months) was performed. Cox proportional hazards regression analyses were used to assess the associations between quantitative ¹⁸F-FDG PET/CT parameters, other clinic-pathological factors, and overall survival (OS). A risk prognosis model was established according to the independent prognostic factors identified on multivariate analysis. A survival curve determined by the Kaplan-Meier method was used to assess whether the prognosis prediction model could effectively stratify patients with different risks factors. Results: The median survival time of the 37 patients with tracheal tumors was 38.0 months, with a 95% confidence interval of 10.8 to 65.2 months. The 3-year, 5-year and 10-year survival rate were 54.1%, 43.2%, and 16.2%, respectively. The metabolic tumor volume (MTV), total lesion glycolysis (TLG), maximum standardized uptake value, age, pathological type, extension categories, and lymph node stage were included in multivariate analyses. Multivariate analysis showed MTV (p = 0.011), TLG (p = 0.020), pathological type (p = 0.037), and extension categories (p = 0.038) were independent prognostic factors for OS. Additionally, assessment of the survival curve using the Kaplan-Meier method showed that our prognosis prediction model can effectively stratify patients with different risks factors (p < 0.001). Conclusion: This study shows that ¹⁸F-FDG PET/CT can predict the survival of patients with primary tracheal malignant tumors. Patients with an MTV > 5.19, a TLG > 16.94 on PET/CT scans, squamous cell carcinoma, and non-E1 were more likely to have a reduced OS.

• 한국축산시설환경학회지
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• 제8권3호
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• pp.135-144
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• 2002

본 연구는 농촌지역에 많이 보급되어 있는 50 마력급 트랙터의 견인 및 주행성능을 우리나라의 주요 수도 포장을 대상으로 컴퓨터 모의 시험을 통해 예측하여 최근 이용이 증대되고 있는 액상가축분뇨 살포기의 적정용량을 구하기 위해 수행되었다. 모의 시험은 액상가축분뇨 살포기의 용량에 영향을 미치는 토양인자와 차량인자를 포함하는 수학적 모델을 이용하였다. 토양 물리적 특성은 우리나라 수도재배의 대표적인 지역중의 일부라고 볼 수 있는 이리, 남양간척지, 아산만지역, 평택, 밀양, 상주, 김해, 김포, 안동, 강화 지역에서 3곳의 서로 다른 면 단위 지역을 선택하여 측정하였다. 결과를 요약하면 다음과 같다. 1. 28개 조사지역의 토성은 미사질양토(SiL) 지역이 19곳으로 제일 많았으며 미사질식양토(SiCL), 사질양토(SL), 양토(L)가 한두 곳으로 조사지역의 대부분 토양은 양토 계통이었다. 이들 지역에서 경운정지 시기의 토양수분 함량은 주로 30~40%의 범위이었으며, 드물게 20% 범위의 지역과 50%가 넘는 지역이 한두 곳 있었다. 겉보기밀도는 대부분 1,500~l,700 kg/㎥의 범위이었다. 원추지수는 1부터 18kg/$\textrm{cm}^2$ 이상까지 넓은 범위에 걸쳐 나타났으며, l0cm와 15cm 사이에서 원추지수가 급격히 증가하여 이 깊이에서 경반이 존재한다는 것을 알 수 있었다. 2. 논토양의 토양물리성을 고려한 액상가축분뇨 살포기의 용량은 슬립에 따라 차이는 있으나, 아주 연약한 지역을 제외하고는 대부분의 지역에서 3,000kg$_{f}$ 이상이었으며, 대부분 4,000~6,000kg$_{f}$ 의 범위에 있었다. 그러나 안동 일부지역과 남양만 지역과 같이 아주 연약한 지역에서는 액상가축분뇨 살포기의 용량이 1,000kg$_{f}$ 전후이거나 음의 값을 갖는 경우도 있어 이 지역에서의 액상가축분뇨 살포기의 용량은 다른 지역에 비해 적게 설계하거나 액상가축분뇨 살포기의 사용에 문제가 있을 수 있다고 판단된다.본 연구는 농촌지역에 많이 보급되어 있는 50 마력급 트랙터의 견인 및 주행성능을 우리나라의 주요 수도 포장을 대상으로 컴퓨터 모의 시험을 통해 예측하여 최근 이용이 증대되고 있는 액상가축분뇨 살포기의 적정용량을 구하기 위해 수행되었다. 모의 시험은 액상가축분뇨 살포기의 용량에 영향을 미치는 토양인자와 차량인자를 포함하는 수학적 모델을 이용하였다. 토양 물리적 특성은 우리나라 수도재배의 대표적인 지역중의 일부라고 볼 수 있는 이리, 남양간척지, 아산만지역, 평택, 밀양, 상주, 김해, 김포, 안동, 강화 지역에서 3곳의 서로 다른 면 단위 지역을 선택하여 측정하였다. 결과를 요약하면 다음과 같다. 1. 28개 조사지역의 토성은 미사질양토(SiL) 지역이 19곳으로 제일 많았으며 미사질식양토(SiCL), 사질양토(SL), 양토(L)가 한두 곳으로 조사지역의 대부분 토양은 양토 계통이었다. 이들 지역에서 경운정지 시기의 토양수분 함량은 주로 30~40%의 범위이었으며, 드물게 20% 범위의 지역과 50%가 넘는 지역이 한두 곳 있었다. 겉보기밀도는 대부분 1,500~l,700 kg/$m^3$의 범위이었다. 원추지수는 1부터 18kg/$cm^2$ 이상까지 넓은 범위에 걸쳐 나타났으며, l0cm와 15cm 사이에서 원추지수가 급격히 증가하여 이 깊이에서 경반이 존재한다는 것을 알 수 있었다. 2. 논토양의 토양물리성을 고려한 액상가축분뇨 살포기의 용량은 슬립에 따라 차이는 있으나, 아주 연약한 지역을 제외하고는 대부분의 지역에서 3,000$kg_f$ 이상이었으며, 대부분 4,000~6,000$kg_f$의 범위에 있었다. 그러나 안동 일부지역과 남양만 지역과 같이 아주 연약한 지역에서는 액상가축분뇨 살포기의 용량이 1,000$kg_f$ 전후이거나 음의 값을 갖는 경우도 있어 이 지역에서의 액상가축분뇨 살포기의 용량은 다른 지역에 비해 적게 설계하거나 액상가축분뇨 살포기의 사용에 문제가 있을 수 있다고 판단된다.

• Asian-Australasian Journal of Animal Sciences
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• 제29권3호
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• pp.327-332
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• 2016

The genetic relationships between different populations and breeds of exotic dairy goats in Thailand were studied using 12 microsatellite markers. Blood samples were obtained from 211 goats from Department of Livestock Development breeding and research farms: 29 Anglonubian (AN), 21 Alpine (AP), 23 Jamunapari (JAM), 50 Saanen (SN), and 88 Toggenburg (TG). Five of the 12 microsatellite markers were found to be polymorphic. A mean of 7.40 alleles per locus was found, with a range from 5 (SPS115 and ETH225) to 11 (TGLA122). We found 24, 27, 19, 32, and 24 alleles in the AN, AP, JAM, SN, and TG breeds, respectively; 37 alleles were present in all breeds. The mean number of alleles in each population ranged from 3.2 (ETH225 locus) to 7.6 (TGLA122 locus). Genetic variability within the breeds was moderate as evidenced by the mean expected heterozygosity of 0.539. The average observed heterozygosity across the 5 markers in all breeds was 0.529 with the maximum observed at the BM1818 locus (0.772) and the minimum at the ETH225 locus (0.248). The observed and expected heterozygosity for all breeds for the 5 microsatellite markers ranged from 0.419 to 0.772 and 0.227 to 0.792, respectively. On the basis of their means, the TGLA122 and BM1818 loci were the most suitable markers for distinguishing genetic diversity among the goats. The estimated average $F_{is}$ value for the breeds ranged from -0.044 (ETH225) to 0.180 (SPS115), while the estimated average $F_{st}$ value ranged from 0.021 (SPS115) to 0.104 (ETH10). These results indicated that TGLA122 and BM1818 markers are suitable to be used for aiding conservation and breeding improvement strategies of dairy.

• Food Science and Biotechnology
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• 제18권5호
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• pp.1193-1198
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• 2009

Ethylacetate and butanol fractions of leaf extracts (OLE) showed the higher contents of total phenolic compounds than hexane and water fractions. Oleuropein contents were $4.21{\pm}0.57,\;3.92{\pm}0.43,\;0.32{\pm}0.03,\;5.76{\pm}0.32$, and $32.47{\pm}0.25mg$/100g for ethanol extract, and hexane, chloroform, ethyl acetate, and butanol fraction, respectively. Treatment of ultraviolet-B (UVB) irradiated cells with 3 OLEs prepared by using ethylacetate and butanol at concentrations 0.001, 0.005, and 0.01% respectively showed significant recovery of cell viabilities. Treatment of dexametason 1 mM reduced tumor necrotic factor (TNF)-${\alpha}$ secretion by about 40%. UVB irradiated immortalized human keratinocytes (HaCaT) cells were treated with 3 different OLEs at the same concentrations. Ethylacetate fraction showed the strongest inhibition activity with respect of reduction of the elevated (TNF)-${\alpha}$. Cytotoxicity of OLEs on the B16-F1 cells was evaluated through thiazolyl blue tetrazolium bromide (MTT) assay. Ethylacetate fraction has no cytotoxicity in the range of 0.005-0.01%. A slight cytotoxicity was observed at the concentration of 0.1% butanol fraction of OLE that caused 10% decrease in cell viability.