• Journal of Radiation Protection and Research
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• 제26권4호
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• pp.375-384
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• 2001

베타선 스펙트럼의 최대 에너지가 확실하게 구별되는 2개의 핵종만을 포함하는 혼합시료의 경우에는 최대 에너지가 다르다는 점을 이용하여 손쉽게 각 핵종의 방사능 값을 측정할 수 있다. 그러나 3개 이상의 베타 방출 핵종이 포함된 혼합물에 대해서는 각 핵종의 스펙트럼이 서로 겹치기 때문에 이러한 방법으로 구해진 방사능 값은 신뢰도가 떨어지게 된다. 따라서, 본 연구에서는 최소자승법을 이용하여 혼합물의 중첩된 베타선 스펙트럼을 각각 분리 정량분석 할 수 있는 방법을 제시하였다. 또한, 실제로 4개의 베타 방출 핵종($^3H,\;^{14}C,\;^{36}Cl\;^{90}Sr$)이 혼합된 시료를 조제하여 본 분석법을 검증한 결과 참고치(Reference value)와 분석치가 7% 이내에서 잘 일치함을 보였다.

• 생명과학회지
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• 제16권2호
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• pp.245-252
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• 2006

피부 트러블을 가진 남,여 40명의 피부에서 분리한 collagenase를 생산하는 균주를 분리, 동정한 결과 Staphylococcus aureus로 판명되었으며 이를 S. aureus JJ-11이라 명명하였다. S. aurells JJ-11 균주의 collagenase의 최적 생산 조건은 1.5%(w/v) gelatin, 1%(w/v) yeast extract, 0.4% (w/v) $K_2HPO_4$, 0.005%(w/v) $NiSO_4{\cdot}6H_2O$를 함유한 배지 (pH 7.0)에서 $37^{\circ}C$, 200 rpm으로 18시간 동안 배양하는 것이다. 분리 균주가 생산하는 collagenase를 정제하기 위해서 amberlite IRA-900과 sephacryl S-300 HR columns를 이용하였고, 6.66-folds로 정제되었다. S. allreus JJ-11 균주가 생산하는 collagenase를 정제한 결과 분자량은 약 62 kDa이었으며, pH 7.0과 $37^{\circ}C$에서 각각 최대의 활성을 가졌고, pH와 온도에 대한 안정성은 pH 4.0-8.0, $40^{\circ}C$까지 100%의 활성이 있었다. 금속이온에 대해서는 $Fe^{2+},\;Co^{2+},\;Ba^{2+}$ 존재 하에서는 5 mM 농도에서도 활성을 유지하였다. $Sr^{2+},\;Hg^{2+}$에서는 30% 이상이 저해를 받는 것으로 확인되었다. 또한 EDTA와 O-phenanthroline에 의해 65% 이상이 저해되는 일 반적인 collagenase의 특정인 metalloproteinase의 특정을 보였으며, 그리고, 여러 가지 기절에 대해 효소활성을 비교한 결과, insoluble collagen (type I)에 대해 효소 활성이 가장 높았다.

• 반도체디스플레이기술학회지
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• 제4권1호
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• pp.55-59
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• 2005

The ($Sr_{1-x}Ca_{x})Ti_{3}$(SCT) thin film are deposited on Pt-coated electrode (Pt/TiN/$SiO_{2}$/Si) using RF sputtering method. The maximum dielectric constant of SCT thin film is obtained by annealing at 600[$^{\circ}C$]. The temperature properties of the dielectric loss have a value within 0.02 in temperature lunges of -80 $\∼$ +90[$^{\circ}C$]). The capacitance characteristics had a stable value within ${\pm}4\%$. The drastic decrease of dielectric constant and increase of dielectric loss in SCT thin films is observed above 200[kHz).

• Bulletin of the Korean Chemical Society
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• 제18권9호
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• pp.976-981
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• 1997

The magnetic susceptibilities of molybdenum ions with 4d1 electronic configuration in the octahedral crystal field were calculated on the basis of ligand field theory. The experimental magnetic susceptibilities for molybdenum ions, which are stabilized at the octahedral site in the perovskite lattice of Ba2ScMoⅤO6 and Sr2YMoⅤO6, were compared with the theoretical ones. We have tried to fit their temperature dependence of magnetic susceptibility with ligand field parameters, spin-orbit coupling constant ζSO, and orbital reduction parameter κ according to intermediate field coupling and strong field theory. Strong field coupling theory could not explain experimental curves without unrealistically large axial ligand field, since it ignores the mixing up between different state via spin-orbit interaction and ligand field. On the other hand, the intermediate field coupling theory could successfully reproduce experimental data in octahedral and trigonal ligand field. The fitting result demonstrates not only the fact that spin-orbit interaction is primarily responsible for the variation of magnetic behavior but also the fact that effective orbital overlap, enhanced by cubic crystal structure, reduces significantly orbital angular momentum as indicated by κ parameter.

• 대한지하수환경학회지
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• 제6권4호
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• pp.171-179
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• 1999

충북 초청지역에서 산출되는 탄산수는 낮은 pH(5.0~5.8), 높은 이산화탄소분압(about 1 atm, Pc $o_2$) 및 높은 총용존이온함량(＜989 mg/L, TDS)을 보이며. 화학적으로 Ca-HC $O_3$ 유형을 갖는 특징을 보인다. 산소. 수소안정동위원소 및 삼중수소 결과에 따르면 초정탄산수는 천수기원이며. 지표수나 천층지하수와 상당히 혼합된 특성을 보여준다. 탄소동위원소결과($\delta$$^{13}$ $C_{{\Sigma}CO2}$)는 탄산수(-8.6~-5.3$ extperthousand$, $\delta$$^{13}$C)는 심부기원으로부터 유래된 특성을 보여주며. 화강암지역 일반지하수 (-14.4~-6.8$\textperthousand$. $\delta$$^{13}$C)는 탄산수의 영향을 받았으며. 변성퇴적암지역 일반지하수(-17.9~-15.2$\textperthousand$. $\delta$$^{13}$C)는 토양기원탄소와 방해석과의 반응에 의해 조절된 특성을 보여준다. 황동위원소특성($\delta$$^{34}$ $S_{SO4}$＝＋3.5~＋11.3$\textperthousand$)은 탄산수와 지표수와의 혼합과정을 뒷받침해준다. 스트론튬동위원소비($^{87}$ Sr/$^{86}$Sr)는 탄산수(0.7138~0.7156)는 천매암중의 방해석(0.7281~0.7346) 또는 부악광산의 방해석(0.7184)과의 반응과는 무관함을 보여준다. 또한 질소동위원소($\delta$$^{15}$ $N_{NO3}$)를 통하여 탄산수내 높은 함량의 질산염(최대 55.0 mg/L, N $O_3$) 기원으로서는 비료와 축산분뇨임을 확인할 수 있었으며. 질소순환과정에서 탈질산화작용이 수반되었을 가능성을 보여준다. 초정지역 탄산수에 대한 수리화학자료와 각종 동위원소자료를 근거로 초정지역 탄산수에 대한 가능한 직화학적 진화모델을 설정하였다. 탄산수는 심부기원의 $CO_2$의 공급으로 형성된 탄산수가 화강암과의 반응을 통해서 진화되었으며. 이러한 탄산수는 천부로 상승하는 과정에서 지표기원의 지하수와 상당히 혼합되어 형성되었음을 지시한다.시한다.

• Journal of Mechanical Science and Technology
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• 제18권1호
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• pp.74-81
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• 2004

The KSNP Steam Generators (Youngkwang Unit 3 and 4, Ulchin Unit 3 and 4) have a problem of U-tube fretting wear due to Flow Induced Vibration (FIV). In particular, the wear is localized and concentrated in a small area of upper part of U-bend in the Central Cavity region. The region has some conditions susceptible to the FIV, which are high flow velocity, high void fraction, and long unsupported span. Even though the FIV could be occurred by many mechanisms, the main mechanism would be fluid-elastic instability, or turbulent excitation. To remedy the problem, Eggcrate Flow Distribution Plate (EFDP) was installed in the Central Cavity region or Ulchin Unit 5 and 6 steam generators, so that it reduces the flow velocity in the region to a certain level. However, the cause of the FIV and the effectiveness of the EFDP was not thoroughly studied and checked. In this study, therefore the Stability Ratio (SR), which is the ratio of the actual velocity to the critical velocity, was compared between the value before the installation of EFDP and that after. Also the possibility of fluid-elastic instability of KSNP steam generator and the effectiveness of EFDP were checked based on the ATHOS3 code calculation and the Pettigrew's experimental results. The calculated results were plotted in a fluid-elastic instability criteria-diagram (Pettigrew, 1998, Fig. 9). The plotted result showed that KSNP steam generator with EFDP had the margin of Fluid-Elastic Instability by almost 25％.

• 한국정보디스플레이학회:학술대회논문집
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• 한국정보디스플레이학회 2006년도 6th International Meeting on Information Display
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• pp.1096-1099
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• 2006

$II-III_2-(S,Se)_4$ structured of phosphor have been used at various field because those have high luminescent efficiency and broad emission band. Among these phosphors, europium doped $BaGa_2S_4$ was prepared by solid-state method and we try to look into an application possibility due to an emissive property of UV region. Also, general sulfide phosphors were synthesized by using injurious $H_2S\;CS_2$ gas. However, this study prepared $BaGa_2S_4:Eu^{2+}$ phosphor is addition to excess sulfur under 5% $H_2/95%\;N_2$ reduction atmosphere. So, this process could large scale synthesis because of non-harmfulness and simple process. The photo-luminescence efficiency of the prepared $BaGa_2S_4:Eu^{2+}$ phosphor increased 20% than commercial $SrGa_2S_4:Eu^{2+}$ phosphor. The prepared $BaGa_2S_4:Eu^{2+}$ could apply to green phosphor for white LED of three wavelengths.

• 암석학회지
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• 제15권4호
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• pp.167-179
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• 2006

갈말-영북일대의 화강암류은 암상에 의하여 회색 각섬석흑운모화강암(JHBG), 흑운모화강암(JBG)과 홍색 각섬석흑운모화강암(CHBG)으로 분대될 수 있다. 전자는 북부에 소규모로 분포하는 중립질암으로서 미립질 스펜을 함유하며, JBG는 북부-동부일대에 주로 분포하는 담회색-회색의 중립질암이다. 주연구대상인 후자는 대부분 북부-남동부일대에 넓게 발달하는 중-조립질암으로 뚜렷한 홍색을 띠며, 국부적으로 미세 공동구조와 정동구조의 포켓상 페그마타이트질부가 발달된다. 광물연령(K-Ar 법)으로 미루어 JHBG와 JBG는 시기를 달리하는 쥬라기 대보조산운동기의, CHBG는 백악기 불국사변동기의 화성활동산물이다. 이는 야외산상 및 지질 선후관계 해석과도 잘 일치한다. CHBG는 석영, 사장석, 알칼리장석, 흑운모, 각섬석, 갈렴석, 인회석, 져어콘, 일부 방해석과 불투명광물 등으로 구성된다. 이 중에서 알칼리장석은 대부분 퍼다이트질 정장석이며, 드물게 수반되는 방해석은 미세공동의 이차적 충전광물로 보인다. 모우드 분석 및 QAP 삼각도에서 모두 화강암영역에 속하며, 대부분 섬장화강암과 몬조화강암의 경계부에 도시된다. 주원소 변화경향, A/CNK 몰비, $SiO_{2}$ 대 $K_{2}O$ 그리고 AMF 관계 등으로 미루어, 이 암은 단일한 화강암질 마그마에서 생성된 산성암, 고-칼륨의 캘크-알카린계열 그리고 과알루미나암질의 분화말기 산물이다. Ba 대 Sr 관계에서도 분화경향을 뚜렷이 이루며, CaO 대 Sr 그리고 $K_{2}O $ 대 Sr 관계로 미루어 Sr이 알칼리장석보다 사장석의 분별결정작용에 더 관여하였다. 희토류원소 표준화도에서 경희토류원소에서 중희토류원소로 갈수록 점진적으로 뚜렷이 결핍되는 양상을 이룬다. 그리고 Eu의 부 이상과 표준화값 등으로 미루어 사장석의 분별결정작용이 이 화강암 전체에 걸쳐 미약하게 일어난 것으로 보인다.

• 자원환경지질
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• 제15권3호
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• pp.123-154
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• 1982

Petrochemical, K-Ar dating, Sand Rb/Sr isotopes, metallogenic zoning, paleomagnetic and geotectonic studies of the Gyongsang basin were carried out to examine applicability of plate tectonics to the post-late Cretaceous igneous activity and metallogeny in the southeastern part of Korean Peninsula. The results obtained are as follows: 1. Bulgugsa granitic rocks range from granite to adamellite, whose Q-Ab-Or triangular diagram indicates that the depth and pressure at which the magma consolidated increase from coast to inland varying from 6 km, 0.5-3.3 kb in the coastal area to 17 km, 0.5-10 kb in the inland area. 2. The volcanic rocks in Gyongsang basin range from andesitic to basaltic rocks, and the basaltic rocks are generally tholeiitic in the coastal area and alkali basalt in the inland area. 3. The volcanic rocks of the area have the initial ratio of Sr^{87}/Sr^{86} varying from 0.706 to 0.707 which suggests a continental origin; the ratio of Rb/Sr changing from 0.079-0.157 in the coastal area to 0.021-0.034 in the inland area suggests that the volcanism is getting younger toward coastal side, which may indicate a retreat in stage of differentiation if they were derived from a same magma. The K_2O/SiO_2 (60%) increases from about 1.0 in the coastal area to about 3.0 in the inland area, which may suggest an increase indepth of the Benioff zone, if existed, toward inland side. 4. The K-Ar ages of volcanic rocks were measured to be 79.4 m.y. near Daegu, and 61.7 m.y. near Busan indicating a southeastward decrease in age. The ages of plutonic rocks also decrease toward the same direction with 73 m.y. near Daegu, and 58 m.y. near Busan, so that the volcanism predated the plutonism by 6 m.y. in the continental interior and 4 m.y. along the coast. Such igneous activities provide a positive evidence for an applicability of plate tectonics to this area. 5. Sulfur isotope analyses of sulfide minerals from 8 mines revealed that these deposits were genetically connected with the spacially associated ingeous rocks showing relatively narrow range of ${\delta}^{34}S$ values (-0.9‰ to +7.5‰ except for +13.3 from Mulgum Mine). A sequence of metallogenic zones from the coast to the inland is delineated to be in the order of Fe-Cu zone, Cu-Pb-Zn zone, and W-Mo zone. A few porphyry type copper deposits are found in the Fe-Cu zone. These two facts enable the sequence to be comparable with that of Andean type in South America. 6. The VGP's of Cretaceous and post Cretaceous rocks from Korea are located near the ones($71^{\circ}N$, $180^{\circ}E$ and $90^{\circ}N$, $110^{\circ}E$) obtained from continents of northern hemisphere. This suggests that the Korean peninsula has been stable tectonically since Cretaceous, belonging to the Eurasian continent. 7. Different polar wandering path between Korean peninsula and Japanese islands delineates that there has been some relative movement between them. 8. The variational feature of declination of NRM toward northwestern inland side from southeastern extremity of Korean peninsula suggests that the age of rocks becomes older toward inland side. 9. The geological structure(mainly faults) and trends of lineaments interpreted from the Landsat imagery reveal that NNE-, NWW- and NEE-trends are predominant in the decreasing order of intensity. 10. The NNE-trending structures were originated by tensional and/or compressional forces, the directions of which were parallel and perpendicular respectively to the subduction boundary of the Kula plate during about 90 m.y. B.P. The NWW-trending structures were originated as shear fractures by the same compressional forces. The NEE-trending structures are considered to be priginated as tension fractures parallel to the subduction boundary of the Kula plate during about 70 m.y. B.P. when Japanese islands had drifted toward southeast leaving the Sea of Japan behind. It was clearly demonstrated by many authors that the drifting of Japanese islands was accompanied with a rotational movement of a clock-wise direction, so that it is inferred that subduction boundary had changed from NNE- to NEE-direction. A number of facts and features mentioned above provide a suite of positive evidences enabling application of plate tectonics to the late Cretaceous-early Tertiary igneous activity and metallogeny in the area. Synthesizing these facts, an arc-trench system of continental margin-type is adopted by reconstructing paleogeographic models for the evolution of Korean peninsula and Japan islands. The models involve an extention mechanism behind the are(proto-Japan), by which proto-Japan as of northeastern continuation of Gyongsang zone has been drifted rotationally toward southeast. The zone of igneous activity has also been migrated from the inland in late-Cretaceous to the peninsula margin and southwestern Japan in Tertiary.

• JSTS:Journal of Semiconductor Technology and Science
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• 제1권1호
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• pp.1-14
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• 2001

Current status and prospects of FET-type FeRAMs (ferroelectric random access memories) are reviewed. First, it is described that the most important issue for realizing FET-type FeRAMs is to improve the data retention characteristics of ferroelectric-gate FETs. Then, necessary conditions to prolong the retention time are discussed from viewpoints of materials, device structure, and circuit configuration. Finally, recent experimental results related to the FET-type memories are introduced, which include optimization of a buffer layer that is inserted between the ferroelectric film and a Si substrate, development of a new ferroelectric film with a small remnant polarization value, proposal and fabrication of a 1T2C-type memory cell with good retention characteristics, and so on.