• 한국임상수의학회지
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• 제20권1호
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• pp.142-144
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• 2003

A 3-year-old, 38 kg, male Golden Retriever dog was referred to Veterinary Teaching Hospital of Konkuk University because of chronic formation of crust on nasal bridge and planum nasale. Abnormalities of physical examination included hyperkeratosis on the footpad, symmetrical alopecia and erythma around olecranon, and crust on nasal bridge and planum nasale. Results of the hematological examination showed a mild leukopenia with neutropenia, monocytosis, and mild lymphocytosis. In addition, the result of serum chemistry and thyroid gland profile were normal. Results of fungal and bacterial culture was negative. Acanthocytes in cytological evaluation of nasal crust were observed in direct microscopic examination. Examination of skin biopsy exhibited vacuolation of basal cell layer, degeneration and necrosis of basal cell with defluxion, mild monocytes filtrations between epidermis and dermis, and mild acanthosis with hyperkeratinization. Based on results of examination described above, Discoid Lupus Erythematosus (DLE) was diagnosed.

• 자원환경지질
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• 제30권2호
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• pp.153-161
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• 1997

Diagrams of $^{87}Sr/^{86}Sr$ versus Ba/Nb and MgO/FeO are scattered, and $^{87}Sr/^{86}Sr$ variation with the increase of $SiO_2$ are scattered in Gwangju granitoid. Diagrams of $(^{87}Sr/^{86}Sr)$i versus $(^{143}Nd/^{144}Nd)$i and ${\varepsilon}Nd$ versus 1/Nd variation are also scattered in Gwangju granitoid. It shows that the source magma of Gwangju granitoid are derived from partial melting materials of heterogeneous upper crust. Very low ${\varepsilon}Nd$ values (-15.19~-19.49) and very high ${\varepsilon}Sr$ values (92.72~308.85) mean that the source magma of Gwangju granitoid is derived from sedimentary substance melting. According to $(^{87}Sr/^{86}Sr)$ 180Ma, and the plot of ${\varepsilon}Sr$ versus ${\varepsilon}Nd$, the Gwangju granitoid shows that the source magma is derived from upper crust materials. Nd model ages of Gwangju granitoid (1.82~2.42G.A.) are older than meta-sediments of Okcheon formation (1.15~1.60G.A.) and similar or close to Pre-Cambrian gneiss complex of Ryoungnam massif (2.17~2.47G.A.or 2.11~2.38G.A.).Therefore, the source magma of the Gwangju granitoid could be derived from the partial melting of Pre-Cambrian gneiss complex of Ryoungnam massif.

• 대한수의학회지
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• 제19권2호
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• pp.153-157
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• 1979

The authors encountered 78 cases of pig from two swine herds with severe dermatitis, which had been fed with commercial rations. Main clinical signs were hard crust formation or erythema and papules on the skin and retarted growth. The skin lesions were visible on the limb joints in all cases. In some cases, however, crusts occurred on the tail, perineum, hip, ear, back, or neck. In one case the entire body surface was covered with thick crust. No mites were detected on the microscopic examination of skin scrapings. Histological examination of biopsies skin specimens taken from the lesions revealed typical parakeratotic changes: the cornified layer of epidermis was irregularly inreased in thickness and contained numerous nuclei. The provision of dietary supplementation with zinc sulfate and soybean oil for 10 days showed marked curative effect.

• 한국결정성장학회지
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• 제19권6호
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• pp.298-304
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• 2009

고온 열수송시스템용 구조재료인 Inconel 617의 표면 처리에 따른 고온물성 개선에 대한 연구를 수행하였다. 표면처리 방법으로는 Inconel 617 기판 상에 급속가열(RTP) 및 수열처리를 통한 균질산화물 형성과 물리적 기상증착법(Arc discharge)법에 의한 TiAlN(두께 약 $2{\mu}m$ 박막 코팅을 적용하였다. 불균질 산화물($Cr_2O_3$) 형성 억제에 미치는 표면처리의 효과 및 표면 미세구조가 물성에 미치는 영향에 대해 알아보기 위해 표면처리된 Inconel 617 시편들을 $1000^{\circ}C$, 대기중에서 열처리 하였으며, 열처리된 시편들에 대해 고온 상형성 및 미세구조를 비교 분석하였다. RTP와 수열처리를 통한 표면산화물 형성보다는 TiAlN 박막 증착을 통한 보호피막의 형성이 Inconel 617 표면에서 생성되는 불균일 $Cr_2O_3$ 막의 성장을 효과적으로 억제할 수 있어서 더 균질한 미세구조와 가장 우수한 내마모 특성을 나타내었다.

• 자원환경지질
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• 제31권4호
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• pp.349-360
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• 1998

The alkali granite occurred as small stock and dyke is distributed in the Kyeomyeongsan Formation in the vicinity of the Chungju city. Geochemical characteristics in major and trace element of alkali granite in the Kyeomyeongsan Formation indicate that the alkali granites are peralkaline and have similar geochemical features to the A-type alkali granite. The rock enriched in HFSE such as Zr, Nb, Y, REE etc. According to the discrimination diagram the alkali granites mostly belong to the within-plate granite field, and to the $A_1$ group of A-type granite. This suggests that they might be emplaced in a extentional rift environment. The alkali granites are characterized by remarkably high total REE content, and enriched, relatively flat to somewhat HREE-depleted patterns with large negative Eu anomaly. The Sm-Nd age of the alkali granite is $338{\pm}30Ma$ with ${\varepsilon}_{Nd(t)}$ beings -7.3 to -8.5. On the basis of the geochemical studies the source magma was derived from a enriched mantle-like source and had a few or clearly interaction with sialic continental crust. In conclusion, the alkali granitic rock of the Kyeomyeongsan Formation might be formed from the high F peralkaline magma that was emplaced in continental rift environment, and generated at the early Carboniferous.

• 자원환경지질
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• 제34권1호
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• pp.147-156
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• 2001

티탄자철석(titanomagnetite)은 해양지각을 이루는 현무암에 존재하는 중요한 자성광물로서 일반적으로 저온산화에 의해 양이온이 결핍된(cation-deficient) 티탄맥히마이트(titanomaghemite)로 변한다. 실험실에서 철성분 제거방식(removal of iron mechanism)을 통해 자연에서 일어나는 티탄자철석의 수성 저온산화(low-temperature aqueous oxidation)를 재현하였으며, 산화정도에 따라 티탄맥히마이트의 자기적 특성이 민감하게 변화하는 것을 관찰하였다. 본 실험 결과 산화정도에 따라 티탄자철석의 큐리온도(Tc)는 166$^{\circ}C$에서 40$0^{\circ}C$로 증가하였고, 상온에서의 포화자화 강도(Ms)는 126.30 kA/m(25.26 emu/g)에서 16.55 kA/m(3.31 emu/g)로 감소하였으며, 항자기력(Hc)은 6.13 kA/m(77 Oe)에서 38.83 kA/m (488 Oe)로 잔류항자기력(Hcr)은 23.24 kA/m(292 Oe)에서 47.03 kA/m(591 Oe)로 증가함을 관찰하였다. 또한 대자율($\chi$)은 $2023{\times}10^{-6}SI$에서 $84{\times}10^{-6}SI$로 감소함을 나타내었다. 이와 같은 결과를 근거로 현재에서 30 Ma까지의 해양지각의 자화 강도의 변화는 티탄자철석의 저온산화에 의한 결과로 해석하였으며 30~120 Ma에 이르는 해양지각의 자화 강도의 변화는 해양지각에 포함된 티탄자철석의 산화와 산화에 순반되는 광물전에 의한 결과로 추정하였으며 보다 구체적인 원인은 해양지각에서 채취한 시료에 대한 체계적인 연구를 통해서 밝혀질 것으로 기대된다.

• 자원환경지질
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• 제46권5호
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• pp.455-468
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• 2013

몽골 중부 항가이 남서부 지역의 다신칠렌 Nb-Ta 및 산트 동 산출지에 대한 예비조사를 수행하였다. 조사 결과 다신칠렌 지역의 Nb-Ta은 조사 지역에 넓게 분포하는 거정질 화강암과 주로 사암으로 구성된 고생대 퇴적층을 관입하는 페그마타이트 내 백운모에서 산출되는 것으로 확인되었다. Nb, Ta의 품위는 높지 않으나 거정질 화강암 지대에서 Th 542 ppm, U 56.9 ppm으로 비교적 높은 값을 갖는 노두를 발견하였다. REE의 함량은 조사 지역의 평균 함량과 최대 함량이 각각 지각의 평균 함량의 약 세 배와 일곱 배로 분석되었다. 산트 지역의 동은 고생대 퇴적층 내 규암에서 말라카이트와 같은 동 산화물로 관찰되었다. 조사지역에서 약 200 km 떨어진 우기누르 철-망간 광화대와 같은 층에서 Mn의 값이 12.4에서 34.6 %로 품위가 비교적 좋게 나타나는 것으로 확인되었다. 또한 REE의 함량은 조사지역의 평균 함량과 최대 함량이 각각 지각의 평균 함량의 약 2.5 배와 일곱 배로 분석되었다. 조사 지역의 화학 분석 결과에 대해 다변량 통계분석(요인분석)을 수행한 결과 다신칠렌 지역의 Nb-Ta은 백운모와 높은 상관관계를 갖는 것으로 나타났고, 산트 지역의 동은 Mo, Sn, Bi와 높은 상관관계를 갖는 것으로 나타났다. 또한 요인분석 결과는 산트 지역의 철이 희토류 원소들과 함께 퇴적되었음을 지시한다.

• Nuclear Engineering and Technology
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• 제44권3호
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• pp.237-248
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• 2012

Corium behavior in the lower plenum of the reactor vessel during a severe accident is very important, as this affects a failure mechanism of the lower head vessel and a thermal load to the outer reactor vessel under the IVR-ERVC (In-Vessel corium Retention through External Reactor Vessel Cooling) condition. This paper discusses the state of the art and technical issues on corium behavior in the lower plenum, such as initial corium pool formation characteristics and its transient behavior, natural convection heat transfer in various geometries, natural convection heat transfer with a phase change of melting and solidification, and corium interaction with a lower head vessel including penetrations of the ICI (In-Core Instrumentation) nozzle are discussed. It is recommended that more detailed analysis and experiments are necessary to solve the uncertainties of corium behavior in the lower plenum of the reactor vessel.

• 자원환경지질
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• 제28권2호
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• pp.139-145
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• 1995

Tungsten skarn mineralization of the Sangdong mine is localized in the interbedded limestone layers of the Myobong Slate Formation and in the limestone of the Pungchon Limestone Formation of Cambrian age. Fluid inclusion, gas composition and Nd-Sr isotope for granites and skarns have been investigated. Gas compositions show $CO_2$ rich in the Sangdong granite and CH, rich in the Nonggeori and Eopyeong granites. The initial $^{87}Sr/^{86}Sr$ and $^{143}Nd/^{144}Nd$ ratios of the Sangdong granites have 0.714~0.716(${\varepsilon}_{Sr}$=138~162) and 0.51173~0.51178(${\varepsilon}_{Nd}$=-14.4~15.5), respectively. And their two stage model ages range from 1687 to 1764 Ma. The granite characterized by high strontium initial ratios and negative eNd value could have originated from the old continental crust source. Low homogenization temperature of the Sangdong granite having $203{\sim}296^{\circ}C$ with 1.9~9.2 NaCl equiv. wt% indicates the post-magmatic hydrothermal alteration temperature. Skarn ore fluid responsible for tungsten mineralization has been evolved from CH, rich fluid of early pyroxene garnet skarn to $CO_2$ rich later quartz-mica skarn.

• Nuclear Engineering and Technology
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• 제45권1호
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• pp.21-28
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• 2013

The flow and heat transfer characteristics of the ex-vessel core melt (corium) were investigated using a commercial CFD code along with the experimental data on the spreading of corium available in the literature (VULCANO VE-U7 test). In the numerical simulation of the unsteady two-phase flow, the volume-of-fluid model was applied for the spreading and interfacial surface formation of corium with the surrounding air. The effects of the key parameters were evaluated for the corium spreading, including the radiation, decay heat, temperature-dependent viscosity and initial temperature of corium. The results showed a reasonable trend of corium progression influenced by the changes in the radiation, decay heat, temperature-dependent viscosity and initial temperature of corium. The modeling of the viscosity appropriate for corium and the radiative heat transfer was critical, since the front progression and temperature profiles were strongly dependent on the models. Further development is required for the code to consider the formation of crust on the surfaces of corium and the interaction with the substrate.