• 신재생에너지
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• 제5권3호
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• pp.26-31
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• 2009

Using MBE growth method, GaAs/AlGaAs solar cell structure was grown. Deposited electrodes are Au/Ni/Ge for n-type and Au/Pt/Ti for p-type electrodes were deposited by E-beam evaporator. Indoor light concentrators were devised and fabricated in order to concentrate artificial solar rays. Also mirror and prism and Fresnel lens concentration system with solar simulator were devised and fabricated. Results of solar cell characteristics were measured with shutting system which can control the amount of light. Maximum power density was 2.13 W/$cm^2$ and maximum concentration was 124 sun, when mirror with Fresnel lens was used at $7854\;mm^2$ of shutter hole.

• Journal of the Korean Wood Science and Technology
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• 제46권5호
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• pp.449-470
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• 2018

본 총설에서는 외부에 사용되는 목재를 풍화인자로부터 보호하기 위해 실행되고 있는 최근의 연구동향에 대해 조사 분석하였다. 주요 기상열화 인자로부터 목재의 표면 보호를 위한 연구 동향에 대하여 조사한 결과 다음과 같은 결론을 얻었다. 목재보존제로 사용된 크롬, 구리 등의 무기화합물이 목재를 기상열화로부터 보호할 수 있는 것으로 보고되었다. 또한 ACQ처리 목재의 표면에 wax나 oil같은 소수성물질과 UV 흡수제, HALS(Hindered Amine Light Stabilizers) 등을 방부목재 표면에 precoating하면 기상열화 저항성을 강화할 수 있다고 보고되었다. 또한 방부목재 표면에 불투명 도막형성의 페인트/스테인 및 반투명스테인등이 기상열화방지에 대한 시너지 효과가 높힐수 있다는 보고들이 다수 있었다. 또한 방부목재의 표면보호를 위한 재도장 처리의 필요성이 시사되었다. 투명성의 도막에 UV방지를 위한 첨가물로서 미세입자의 ZnO 또는 $TiO_2$, Co, Cr, Fe, Mn, Ni과 Ti 등의 금속이온, Tris-resorcinol triazine derivatives, triazine 및 Benzotriazole과 같은 UV흡수제 등이 소개되었다. Methylation, acetylation 또는 alkylation 등과 같이 화학적으로 개질된 경우에는 이로 인한 중량증가가 높은 경우 기상열화 방지효과가 상승된다는 연구들이 소개되었다, 열처리목재의 기상열화 저항성에 대해서는 여러 가지 상반되는 연구보고 들이 있었고, UV저항성을 지닌 도장의 필요성이 강조된 보고가 있어 보다 심도 있는 연구의 필요성이 시사되었다.

• 대한치과교정학회지
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• 제43권4호
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• pp.201-206
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• 2013

This article describes the orthodontic treatment of a 25-year-old Korean female patient with anterior crowding, including palatally displaced lateral incisors. Her facial profile was satisfactory, but 3.5 mm of maxillary anterior crowding was observed. To correct this crowding, we decided to minimize the use of the conventional fixed orthodontic appliances and employed a less bulky and more aesthetic appliance for applying light continuous force. We determined the final positions of the maxillary teeth via a working model for diagnostic set up and achieved space gaining and alignment with simple Ni-Ti spring and stainless steel round tubes. Tooth alignment was achieved efficiently and aesthetically without the conventional brackets.

• Restorative Dentistry and Endodontics
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• 제36권3호
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• pp.231-237
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• 2011

연구목적: 본 연구에서는 micro CT를 사용하여 SS K-file, Profile, LightSpeed로 #25부터 #40 크기까지 근관을 형성할 때 근단부 근관 형태의 연속되는 변화를 평가하였다. 연구 재료 및 방법: 30개 하악 대구치의 근심 근관을 ProFile, LightSpeed와 SS K-file로 #25번에서 #40번까지 순차적으로 근관 형성하였고, 매 단계 확대 후 micro CT를 시행하였다. 치근단 1, 2, 3, 5 mm 에서 근관 중심 변위와 삭제되지 않은 단면의 비율을 측정하여 'repeated nested design' 분석방법과 Mann-Whitney test로 유의 수준 p = 0.05에서 검정하였다. 결과: SS K-file군에서 #30 이상 근관 형성 후 유의할 만한 근관 중심 변위가 증가하였고, 근관 형성 과정 어느 단계에서도 삭제되지 않은 면적의 비율이 유의성 있게 감소되지 않았다. ProFile군에서는 치근단 1, 2 mm에서 #40 file로 근관 형성 후 근관 중심 변위가 크게 증가하였고, 치근단 1 mm에서 #35 크기로 근관 형성한 후에 삭제되지 않은 면적의 비율이 유의성 있게 감소하였다. LightSpeed군에서는 급격한 근관 중심 변위를 관찰할 수 없었고, 근관 중심 변위가 ProFile군보다 적게 관찰되었다. 결론: SS K-file, Profile, LightSpeed에서 형성되는 근관의 변이 정도는 근단부 근관 형성 크기에 따라 다르게 나타났다.

• 자원환경지질
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• 제56권6호
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• pp.745-764
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• 2023

In the Republic of Congo, Banded iron formations (BIFs) occur in two areas: the Chaillu Massif and the Ivindo Basement Complex, which are segments of the Archean Congo craton outcropping in the northwestern and southwestern parts of the country. They show interesting potential with significant mineral resources reaching 2 Bt and grades up to 60% Fe. BIFs consist mostly of oxide-rich facies (hematite/magnetite), but carbonate-rich facies are also highlighted. They are found across the country within the similar geological sequences composed of amphibolites, gneisses and greenschists. The Post-Archean Australian Shale (PAAS)-normalized patterns of BIFs show enrichment in elements such as SiO₂, Fe₂O₃, CaO, P₂O₅, Cr, Cu, Zn, Nb, Hf, U and depletion in TiO₂, Al₂O₃, MgO, Na₂O, K₂O, Sc, Th, Ba, Zr, Rb, Ni, V. REE diagrams show slight light REEs (rare earth elements; LREEs) compared to heavy REEs (HREEs), and positive La and Eu anomalies. The lithological associations, as well as the very high (Eu/Eu^*)_SN ratios> 1.8 shown by the BIFs, suggest that they are related to Algoma-type BIFs. The positive correlations between Zr and TiO₂, Al₂O₃, Hf suggest that the contamination comes mainly from felsic rocks, while the absence of correlations between MgO and Cr, Ni argues for negligeable contributions from mafic sources. Pr/Pr^* vs. Ce/Ce^* diagram indicates that the Congolese BIFs were formed in basins with redox heterogeneity, which varies from suboxic to anoxic and from oxic to anoxic conditions. They were formed through hydrothermal vents in the seawater, with relatively low proportions of detrital inputs derived from igneous sources through continental weathering. Some Congolese BIFs show high contents in Cr, Ni and Cu, which suggest that iron (Fe) and silicon (Si) have been leached through hydrothermal processes associated with submarine volcanism. We discussed their tectonic setting and depositional environment and proposed that they were deposited in extensional back-arc basins, which also recorded hydrothermal vent fluids.

• 한국진공학회:학술대회논문집
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• 한국진공학회 2011년도 제40회 동계학술대회 초록집
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• pp.148-148
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• 2011

일반적으로 LED 제작에 사용되는 c-plane GaN는 c축 방향으로 발생하는 분극의 영향을 받게 된다. 분극은 LED내 양자우물의 밴드를 기울게 하여 그 결과 전자와 홀의 재결합 확률을 감소시켜 낮은 내부양자효율을 가지게 된다. 이러한 문제를 해결하기 위한 여러 가지 방법들이 제시되었는데 그 중에서도 특히 a-plane 혹은 m-plane면과 같은 무분극 면을 사용하는 GaN LED가 주목받고 있다. 그 이유는 무분극 면은 분극이 발생하는 c축과 수직이기 때문에 분극의 영향을 받지 않아 높은 내부 양자효율을 가질수 있다. 본 연구에서는 MOCVD 장비를 사용하여 2인치 r-plane 사파이어 기판위에 3um두께의 a-plane GaN을 성장하였다. 그위에 2um정도로 Si을 도핑하여 n-type GaN 형성한후 단일 양자우물, 그리고 Mg을 도핑하여 p-type GaN을 성장하였다. 장파장대역의 a-plane LED의 특성을 알아보기 위해서 양자우물 형성시 In의 조성비를 높였다. 일반적인 포토리소그래피 공정과 Dry etching 공정을 사용하여 메사구조를 형성하였으며 Ti/Al/Pt/Au와 Ni/Au를 각각 n-type과 p-type의 전극 물질로 사용하였다. 제작된 LED의 특성을 파악하기 위해서 인가전류를 0부터 100mA까지 출력 스펙트럼을 측정하였으며 orange대역의 파장을 갖는 LED를 얻었다. 인가전류별 Peak 파장의 변화와 반측폭의 변화를 파악하여 장파장 대역의 a-plane LED의 특성을 확인하였다.

• Journal of Ceramic Processing Research
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• 제13권spc1호
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• pp.128-131
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• 2012

The selective area growth light emitting diode on GaN substrate was grown using mixed-source HVPE method with multi-sliding boat system. The GaN substrate was grown using mixed-source HVPE system. Te-doped AlGaN/AlGaN/Mg-doped AlGaN/Mg-doped GaN multi-layers were grown on the GaN substrate. The appearance of epi-layers and the thickness of the DH was evaluated by SEM measurement. The DH metallization was performed by e-beam evaporator. n-type metal and p-type metal were evaporated Ti/Al and Ni/Au, respectively. At the I-V measurement, the turn-on voltage is 3 V and the differential resistance is 13 Ω. It was found that the SAG-LED grown on GaN substrate using mixed-source HVPE method with multi-sliding boat system could be applied for developing high quality LEDs.

• 한국분말야금학회:학술대회논문집
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• 한국분말야금학회 2002년도 제3회 최신 분말제품 응용기술 Workshop
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• pp.25-37
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• 2002

The most important industrial application of gamma radiation in characterizing green compacts is the determination of the density. Examples are given where this method is applied in manufacturing technical components in powder metallurgy. The requirements imposed by modern quality management systems and operation by the workforce in industrial production are described. The accuracy of measurement achieved with this method is demonstrated and a comparison is given with other test methods to measure the density. The advantages and limitations of gamma ray densitometry are outlined. The gamma ray densitometer measures the attenuation of gamma radiation penetrating the test parts (Fig. 1). As the capability of compacts to absorb this type of radiation depends on their density, the attenuation of gamma radiation can serve as a measure of the density. The volume of the part being tested is defined by the size of the aperture screeniing out the radiation. It is a channel with the cross section of the aperture whose length is the height of the test part. The intensity of the radiation identified by the detector is the quantity used to determine the material density. Gamma ray densitometry can equally be performed on green compacts as well as on sintered components. Neither special preparation of test parts nor skilled personnel is required to perform the measurement; neither liquids nor other harmful substances are involved. When parts are exhibiting local density variations, which is normally the case in powder compaction, sectional densities can be determined in different parts of the sample without cutting it into pieces. The test is non-destructive, i.e. the parts can still be used after the measurement and do not have to be scrapped. The measurement is controlled by a special PC based software. All results are available for further processing by in-house quality documentation and supervision of measurements. Tool setting for multi-level components can be much improved by using this test method. When a densitometer is installed on the press shop floor, it can be operated by the tool setter himself. Then he can return to the press and immediately implement the corrections. Transfer of sample parts to the lab for density testing can be eliminated and results for the correction of tool settings are more readily available. This helps to reduce the time required for tool setting and clearly improves the productivity of powder presses. The range of materials where this method can be successfully applied covers almost the entire periodic system of the elements. It reaches from the light elements such as graphite via light metals (AI, Mg, Li, Ti) and their alloys, ceramics ($AI_20_3$, SiC, Si_3N_4, $Zr0_2$, ...), magnetic materials (hard and soft ferrites, AlNiCo, Nd-Fe-B, ...), metals including iron and alloy steels, Cu, Ni and Co based alloys to refractory and heavy metals (W, Mo, ...) as well as hardmetals. The gamma radiation required for the measurement is generated by radioactive sources which are produced by nuclear technology. These nuclear materials are safely encapsulated in stainless steel capsules so that no radioactive material can escape from the protective shielding container. The gamma ray densitometer is subject to the strict regulations for the use of radioactive materials. The radiation shield is so effective that there is no elevation of the natural radiation level outside the instrument. Personal dosimetry by the operating personnel is not required. Even in case of malfunction, loss of power and incorrect operation, the escape of gamma radiation from the instrument is positively prevented.

• Current Research on Agriculture and Life Sciences
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• 제30권2호
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• pp.76-81
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• 2012

본 연구에서는 검정팥 종피에 함유된 천연색소에 대한 연구의 일환으로, 천연염료로서의 적용을 위해 염색조건 즉 염색온도, 염색시간, 염색 pH, 욕비에 따른 K/S 값을 측정하여 적정 염색조건을 설정하고, 여러 매염제를 적용하여 색상변화에 미치는 영향 및 견뢰도를 측정하여 다음과 같은 결과를 얻었다. 1. pH에 따른 염색성에서는 견직물의 경우 pH 4에서 가장 염착량이 많았고, 면직물의 경우에는 주어진 범위 내에서 는 pH가 높을수록 염착량이 많았다. 2. 염색온도와 시간에 따른 염색성은, 견직물의 경우, 염색온도 $40^{\circ}C$와 $60^{\circ}C$에서는 전반적으로 염착량이 낮고 시간에 따른 염착량의 차이도 크지 않았으나 염색온도 $80^{\circ}C$에서는 시간이 경과할수록 K/S 값이 크게 나타났다. 면직물의 경우도 견직물과 비슷한 결과로 온도가 높아질수록 염색시간이 경과될수록 K/S 값이 크게 나타났다. 3. 견직물에 대한 매염제 종류별 표면색의 변화에서는 Fe 매염포만 YR${\rightarrow}$Y 로 변화되었을 뿐 다른 매염제에서는 매염후에도 색상 변화는 크지 않았다. Sn 매염과 Ti 매염포는 무 매염포 보다 $L^*$값이 상승하였으나 나머지 매염제는 $L^*$값이 크게 감소되었다. 면직물에 대한 표면색의 변화는 견직물에서와 같은 경향으로 나타났으며, $L^*$값에 있어서는 견직물과 다르게 Ni 매염포만 무매염포보다 $L^*$ 값이 크게 나타났다. 4. 매염처리 전 견직물의 일광 견뢰도는 무매염이 4~6등급, Al 처리포는 4~5등급, Cu와 Sn은 3~4등급으로 나타났고 Fe는 2~3등급으로 가장 낮게 나타났으며, 세탁견뢰도에서는 무매염 2등급, 매염제 처리포는 전부 2내지 3등급으로 나타났다. 무매염 면직물의 일광견뢰도는 1~2등급, Fe 매염은 2~3등급, Cu 2등급 Al과 Sn은 1~2등급으로 매염처리에 의해 전혀 개선되지 않았으며, 세탁견뢰도의 경우 Cu매염이 4등급으로 양호하게 나타났으며 무매염, Al, Sn과 Fe는 3등급으로 나타났다.

• 자원환경지질
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• 제20권2호
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• pp.85-95
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• 1987

The host rocks of titaniferous magnetite deposits in Gonamsan are alkaline gabbros, which are typical of undersaturated alkaline rocks in terms of the lack of normative quartz. According to field occurrences and petrographic features, these alkaline gabbros are divided into 3 rock types: coarse-grained and pegmatitic rock, medium-grained rock with equigranular texture, and layered cumulate rock. All these rocks mainly contain clinopyroxene(salite), plagioclase(An 43-66), pargasite, and ilmenite. The accessory minerals are apatite, sphene, quartz, and sometimes titaniferous magnetite. Pargasite, sphene, and quartz are considered to be secondary minerals formed by the reaction among clinopyroxene, plagioclase and Fe-Ti oxide at deuteric stage. Fe-Ti oxides generally occur as ilmenite in the alkaline rocks, and titaniferous magnetite in the ore deposits. Layered cumulate rocks are characterized by a recurrence of discontinuous thin mesolayer of clinopyroxene-pargasite within leucolayer mainly composed of plagioclase. Clinopyroxene is cumulus mineral whereas plagioclase, ilmenite and apatite occur as intercumulus minerals. According to the variation diagrams of oxide and trace element contents against the differentiation index, incompatible elements, such as Na, Ba and Sr, show positive correlations whereas compatible elements, such as Mg and Cr, show negative correlations. However some compatible elements, such as Co, Ni and V show irregular variations, reflecting relative cumulate status of cumulus and intercumulus minerals. On the de la Roche multicationic diagram, these alkaline gabbros are distributed along the differentiation curve of undersaturated alkaline series from alkaline basaltic composition through basanitic composition to tephritic composition. Layered cumulate rocks, which are distributed between basanitic composition and tephritic composition, reflect their cumulate character, slightly scattering away from the curve. The medium-grained rock shows higher contents in Ba, Sr and light rare earch elements than the coarse-grained and pegmatitic rock. The former shows two times higher contents of total rare earth elements than the latter, $while(La/Lu)_{cn}$ ratios maintain fairly constant values of 5.08~5.06 in these two rocks. This means that coarse-grained and pegmatitic rock, as compared with the medium-grained rock, was formed by the earlier differentiated magma but rare-earth element distribution pattern remained almost parallel during differentiation. From the data the above mentioned, these alkaline gabbros are considered to be comagmatic and to be formed by intrusions of differentiated magmas in its reservoir.