• 한국광물학회:학술대회논문집
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• 한국광물학회.한국암석학회 2003년도 공동학술발표회 논문집
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• pp.67-67
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• 2003

The chemical compositions and textural relationships of the Nb-Zr oxide minerals including pyrochlore [ideally (Ca,Na)$_2$Nb$_2$O$\sub$6/(OH,F), with up to 24% UO$_2$ and 16% Ta$_2$O$\sub$5/] and baddeleyite [ideally ZrO$_2$, with up to 6% Nb$_2$O$\sub$5/] in the Sokli carbonatite complex, Kola Peninsula, Arctic are described. These two minerals in carbonatites are the major hosts for the HFSEs such as U, Th, Ta, Nb, Zr and Hf and thus are interest both economically and petrologically. The Sokli carbonatite complex (360-370 Ma) in Northern Finland, which forms a part of the Paleozoic Kola Alkaline Province (KAP), is mainly composed of multi-stages of carbonatite and phoscorite associations (P1-C1 P2-C2, P3-C3, D4 and D5) surrounded by altered ultramafic rocks (olivinite and pyroxenite) and cut by numerous small dikes of ultramafic lamprophyre. The Sokli complex contains the highest concentration in niobium and probably in tantalum, which are economically very important to modern steel technology, among the ultramafic-alkaline complexes of the KAP. Pyrochlore and baddeleyite mostly concentrate in the phoscorites. Pyrochlores in the Sokli complex are generally rounded octahedra and cubes in shape, red brown to grey yellow in color, and 0.2 to 5 mm in size. They are found in all calcite carbonatites, phoscorites and dolomite carbonatites, except P1-C1 rocks. These pyrochlores display remarkable zonations which depend on host rock compositions, and have significant compositional variations with evolution of the Sokli complex. The common variation scheme is that (1) early pyrochlore is highly enriched in U and Ta; (2) these elements decrease abruptly in the intermediate stage, while Th and Ce increase, and (3) late stage pyrochlore is low in U, Ta, Th, and Ce, and correspondingly high in Nb. Baddeleyites in the Sokli complex occur in the early P1-C1 and P2-C2 rocks and rarely in P3. They crystallized earlier than pyrochlores, and occasionally show post-magmatic corrosion and replacement. The FeO and TiO$_2$ contents of baddeleyites are much lower than those of the other terrestrial and lunar baddeleyites, whereas Nb$_2$O$\sub$5/ and Ta$_2$O$\sub$5/ contents are the highest among the reported compositions. Ta/Nb and Zr/Nb ratios of pyrochlores and baddeleyites decrease towards later stage facies, which is in accordance with the whole rock compositions. The variation of Ta/Nb and Zr/Nb ratios of pyrochlores and baddeleyites is considered to be a good indicator to trace an evolution of the carbonatite complexes.

• 한국재료학회지
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• 제25권8호
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• pp.386-390
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• 2015

Fe-base superalloy powders with $Y_2O_3$ dispersion were prepared by high energy ball milling, followed by spark plasma sintering for consolidation. High-purity elemental powders with different Fe powder sizes of 24 and 50 mm were used for the preparation of $Fe-20Cr-4.5Al-0.5Ti-O.5Y_2O_3$ powder mixtures (wt%). The milling process of the powders was carried out in a horizontal rotary ball mill using a stainless steel vial and balls. The milling times of 1 to 5 h by constant operation (350 rpm, ball-to-powder ratio of 30:1 in weight) or cycle operation (1300 rpm for 4 min and 900 rpm for 1 min, 15:1) were applied. Microstructural observation revealed that the crystalline size of Fe decreased with an increase in milling time by cyclic operation and was about 15 nm after 3 h, forming a FeCr alloy phase. The cyclic operation had an advantage over constant milling in that a smaller-agglomerated structure was obtained. The milled powders were sintered at $1100^{\circ}C$ for 30 min in vacuum. With an increase in milling time, the sintered specimen showed a more homogeneous microstructure. In addition, a homogenous distribution of Y-compound particles in the grain boundary was confirmed by EDX analysis.

• 한국재료학회지
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• 제8권12호
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• pp.1165-1169
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• 1998

제1세대 니켈계 단결정 초합금인 CMSX 6를 사용하여 셀렉타법으로 진공 정밀주조하여 단결정을 제작하였다. 주형온도 약 150$0^{\circ}C$, 주입온도 약 163$0^{\circ}C$와 용탕 주입 직후 주형을 2.5mm/분 속도로 하강시켜 단결정을 성장시켰다. 단결정 주조조직에서 기지와 공정조직은 ${\gamma}$' 석출물(Ni$_3$(Al, Ti)) 모양과 크기에 따라 각각 모두 두영역으로 구분되었으며, 공정조직의 Ti함랗은 기지보다 높았다. 즉, EPMA 및 CBED 분석 등으로 ${\gamma}$' 석출물을 분석한 결과, 기지내의 ${\gamma}$'은 크기가 0.5~0.7$\mu\textrm{m}$ 이하이며 화학조성상 Ni$_3$Al에 가까웠으며 격자구조도 Ll$_2$를 나타내었다. 반면에 공정조직에 가까울수록 ${\gamma}$' 크기는 1.0$\mu\textrm{m}$보다 컸으며, 모양도 판상형의 거대한 모양으로 바뀌었다. 화학조성 또한 Ni$_3$Ti에 가까웠으며 격자구조도 D $O_{24}$를 나타내었으므로 수지상과 공정조직의 ${\gamma}$' 석출물은 화학조성 및 격자구조가 상이함을 알 수 있었다.

• 한국가금학회지
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• 제24권3호
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• pp.127-137
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• 1997

This study was conducted to estimate the laying performance and heterosis of Korean Native Chicken(KNC), Rhode Island Red(RIR), and KNC x RIR crossbreds A total of 1,274 female pullets were produced from KNC, RIR and RIR crossbreds in National Livestock Research Institute, Korea. The experiment was conducted for 2O~64 weeks from Jan 20. to Nov.25, 1996. The age at first egg of crossbreds were 144.1~148.7 days. The first egg weight of crossbreds was 39. 4~40.3 g, and body weights at first egg of KNC dark brown strain x RlR(DR), KNC light brown strain x RlR(LR) and KNC dark black strain x RlR(BR) were 1,943 g, 1,925 g and 2,044 g, respectively. During the laying period the average viability of crossbreds was 96.6~98.3%. The hen-day egg production of crossbreds were 111.1~113.O eggs at 40 weeks of age, and 223.5~227.5 eggs at 64 weeks of age, respectively. The hen-day egg production peaks were 78.2~80.1% in KNC, and 85.8~87.5% in crossbreds. The heterosis were estimated to be 3.61%, 9.21%, 4.78%, 2.97% and -1.63% for the first egg days, body weights at first egg, layer viability, hen-day egg production, and feed conversion ratio, respectively.

• Korea-Australia Rheology Journal
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• 제18권1호
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• pp.15-24
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• 2006

The first international inter-laboratory study, involving six laboratories, has been conducted to examine issues associated with yield stress measurements in suspensions. The initial focus of the project was to evaluate the reliability and reproducibility of several common yield stress measuring techniques employed in different laboratories and with different instruments. Aqueous suspensions of colloidal $TiO_2$ at concentrations of 40-70 wt% solids were used as the test fluids. A wide range of instruments and techniques employing both direct and indirect methods were used to determine the yield stress of the samples prepared according to a prescribed procedure. The results obtained indicated that although variations of results existed among different techniques, direct yield stress measurements using static methods produced more reliable and repeatable results than other methods. Variability of the yield stress measured using different techniques within any laboratory however was less significant than variability of the results among different laboratories. The nature and condition of the test suspensions was identified as the most likely factor responsible for the poor reproducibility of yield stress measurements from different laboratories.

• 보존과학회지
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• 제37권1호
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• pp.34-42
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• 2021

This study analyzes six slags excavated from the iron making site in Gogi-ri, Namwon, Korea to understand the characteristics of the ruins, and to confirm the iron making process performed at the time. The chemical components of the iron making by-products from the Gogi-ri site were analyzed, and the findings indicate total Fe contents between 23.24% and 37.56%, which are lower than the typical total Fe content found in ancient iron making processes. The deoxidation agent contents of the slags ranged from 43.88% to 58.13%, which are higher than the typical deoxidation agent content of ancient iron making processes. The high content suggests smooth separation between iron and slags, and TiO₂ detected from the site suggests the use of materials with high titanium content in the iron making in the region. As for the microstructures of the slags, some slags have long pillar-shaped fayalites, while others have pillar-shaped wüstite along with ulvöspinel. Slags from the forging furnace show hammer scales created by both the earlier stages and later stages of forging work. The findings suggest that the iron making site in Gogi-ri, Namwon, Korea used to be an iron making facility where a full range of iron making process was carried out ranging from smelting to forging, and the ironmakers used a wide array of technologies to manufacture iron products.

• 자원환경지질
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• 제56권3호
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• pp.259-275
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• 2023

Pan African granitoids of Kaiama is comprised of K-feldspar rich granites, porphyritic granites, and granitic gneiss that are intruded by quartz veins and aplitic veins and dykes which trend NE-SW. In order to establish the geochemical signatures, petrogenesis, and tectonic settings of the lithological units, petrological, petrographical, and geochemical studies was carried out. Petrographic analysis reveals that the granitoids are dominantly composed of quartz, plagioclase feldspar, biotite, and k-feldspar with occasional muscovites, sericite, and opaque minerals that constitute very low proportion. Major, trace, and rare earth elements geochemical data reveal that the rocks have moderate to high silica (SiO₂=63-79.7%) and alumina (Al₂O₃=11.85-16.15) contents that correlate with the abundance of quartz, feldspars, and biotite. The rocks are calc-alkaline, peraluminous (ASI=1.0-<1.2), and S-type granitoids sourced by melting of pre-existing metasedimentary or sedimentary rocks containing Al, Na, and K oxides. They plot dominantly in the WPG and VAG fields suggesting emplacement in a post-collisional tectonic setting. On a multi-element variation diagram, the granitoids show depletion in Ba, K, P, Rb, and Ti while enrichment was observed for Th, U, Nd, Pb and Sm. Their rare-earth elements pattern is characterized by moderate fractionation ((La/Yb)_N=0.52-38.24) and pronounced negative Eu-anomaly (Eu/Eu^*=0.02-1.22) that points to the preservation of plagioclase from the source magma. Generally, the geochemical features of the granitoids show that they were derived by the partial melting of crustal rocks with some input from greywacke and pelitic materials in a typical post-collisional tectonic setting.

• 한국작물학회지
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• 제40권4호
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• pp.494-503
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• 1995

벼 품종의 효율적인 내염성 검정방법을 확립하기 위하여 호남농업시험장 개화도출장소 내염성 검정포에서 45개 벼 품종을 공시하여 유묘기, 분벽기, 유수형성기에 각각 염수처리를 하여 내염성을 검정하였다. 1. 분벽기 염수처리는 무처리와 비교하여 초장의 신장율은 조생종군 77.4%로 단축되었고, 경수는 조생종군 88.8%, 중생종군 63.8%, 중만생종군 64.0%로 각각 줄어들었다. 2. 유수형성기의 염수처리 결과는 처리 전보다 초장의 신장율은 조생종군 7.4%, 중생종군 4.5%, 중만생종군 4.0%로 생육시기이 짧은 품종들이 신장율이 높은 경향이었고, 경수의 감소율은 조생종군 15.4%, 중생종군 17.3%, 중만생종군 24.6%로 만생종일수록 많이 줄어 들었다. 3. 유수형성기 염수처리에서 고염율은 조생종군 62.2%, 중생종군 60.6%, 중만생종군 65.1%로 중만생종군이 심한 편이었으며, 건물중은 중생종 > 중생종 > 중만생종 순으로 무거웠다. 4. 생육단계별 단관조사한 내염성 정도는 대관벼, 조령벼, 남원벼, 간척벼, 신선찰벼, 개화벼, 대야벼 등은 강하게 나타났고, 진부올벼, 둔내벼, 탐진벼, 대청벼 추정벼 등은 약하게 나타났다. 5. 무처리재배에 대한 염수처리재배의 수량지수는 조생종군 > 중생종군 > 중만생종군 순으로 높았고, 진부벼, 남원벼, 화성벼, 팔공벼, 화청벼, 개화벼 등은 수량 감소가 적게 나타난 품종들이었다. 6. 수량감소율에 대한 염수처리의 각종 특성과의 상관에서 조, 중생종군은 분벽기와 유수형성기의 내염성 정도와는 부의 상관을 보였고, 분벽기의 초장감소율과는 정의 상관을 보였으며, 조생종군에서는 고엽율과의 부의 상관을 보였고, 중만생종군에서는 유수형성기의 경수감소율과 고엽율 등에서 부의 상관관계를 보였다. 있어서 다른 조건이 좋은 경우 등숙에 적당한 온도범위는 21~26$^{\circ}C$로 나타났다.다. 6. 파종 10일후 묘의 생육에 있어서도 1대잡종벼가 양친이나 비교품종보다 건물중, 초장 등에서 잡종강세를 나타내었으며 묘의 생육과 a-amylase 활성간에는 유의한 정의상관이 있었다./TEX>, RH 50%)한 벼는 2년반 저장한 벼도 밥맛의 변화가 거의 없었다. 5. 1988년산 및 1989년산 일반계를 10분도와 12분도로 도정하였을 때 도정도에 따른 밥맛의 차이는 없었다.X>$CoO_x$는 $Co_3O_4$로 존재하고, 반응 전의 경우에는 이와는 다른 chemical state를 보여주었다. XRD 및 XPS 결과를 바탕으로, 촉매표면에 존재하는 $Co_3O_4$의 외부표면이 $Co_2TiO_4$와 $CoTiO_3$ 같은 $CoTiO_x$로 encapsulation되어 있는 모델구조를 제안할 수 있고, 이는 반응시간의 함수로 나타나는 촉매활성에 있어서 전이영역의 존재를 잘 설명할 수 있을 뿐만 아니라, XRD와 XPS에서 얻어진 촉매의 물리화학적인 특성을 잘 반영할 수 있다. 나타냈고, 골격근과 눈 조직에서 피루브산에 대한 LDH의 친화력이 상당히 크므로 LDH가 혐기적 조건에서 효율적으로 기능을 하는 것으로 사료된다.5) and "Cleanliness of clothes ＆ features" (p ＜0.05) of VIP ward were significantly higher than those of a general ward.tive to apply.아울러 고려(考慮)해야 한다. 이것은 고무기술자(技術者)가 당면(當面)해야할

• 자원환경지질
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• 제8권3호
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• pp.147-164
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• 1975

소백산(小白山) 변성대내(變成帶內)의 옥방(玉房), 선산(善山), 지례(知禮) 및 단성(丹城)일대에 분포하는 각섬석질암(角閃石質岩) 중 옥방지역(玉房地域)의 것은 주변 변성암류(變成岩類)에 상합적(相合的)이며 엽이(葉理)가 잘 발달되어 있고 그외 지역의 것은 심한 화강암화작용(花岡岩化作用)의 영향을 받아 편마암(片磨岩)및 화강암질암내(岡岩質岩內)에 lense 상(狀)의 잔류체(殘留體)로 산출(産出)된다. 본 연구에서는 주로 소백산(小白山) 변성대내(變成帶內)의 각섬석질암(角閃石質岩)옥방중석광상((玉房重石鑛床) 포함)과 그의 경계부에 위치한 옥천지향사대내(沃川地向斜帶內)의 상동광상(上東鑛床)의 염기성변성암(鹽基性變成岩)의 시료를 대상으로 습식(濕式) 및 방출분광분석(方出分光分析)을 수행하여, 24개 주성분(主成分) 및 희유원소(稀有元素)의 정성(定性) 정량적(定量的)인 값을 variation trend와 discriminant function analysis 를 통하여 비교검토함으로써 이들의 성인(成因)을 밝혀보려 하였다. 주성분원소(主成分元素)의 Niggli value를 사용한 각종 도면에서는 화강암화작용(花岡岩化作用)으로 인한 alkali, alumina, 및 silica 등의 증가로 인하여 충분한 data를 얻지못했으나, 연구(硏究) 대상 시료(試料)의 희유원소(稀有元素)들은 alkli, alumina, silica의 증감(增減)에 영향을 받지않아 (도면 12, 13) 성인규명(成因規明)에 만족한 결과를 얻을 수 있었다. 옥방(玉房), 선산(善山), 지례(知禮) 및 단성지역(丹城地域)의 각섬석질암(角閃石質岩)은 각 도표에서 높은 비율의 Cr, Ni, Co, Ti, Sr 및 V의 값을 가지며 염기성(鹽基性) 화성암(火成岩)의 variation trend를 잘 보여주고, 상동지역(上東地域)의 염기성변성암(鹽基性變成岩)은 낮은 Cr, Ni, Co, Ti, Sr 및 V의 값과 낮은 Niggli mg 값을 가져서 화성(火成), 퇴적(堆積)의 두 특징을 동시에 나타내고 있으나 화성기원의 특징을 더욱 강조하여 준다. 한편 Discriminant function test ($X_1$, $X_2$, $X_3$)에서도 옥방(玉房), 선산(善山), 지체(知體), 단성(丹城)지역의 각섬석질암(角閃石質岩)은 한 개의 시료(試料)를 제외하고는 모두 $X_1$, $X_2$, $X_3$ 중 둘이상이 positive값을 가져 화성기원(火成起源)을 지시해주며 상동광상(上東鑛床)의 것은 하나의 시료는 둘이상의 positive 값 ($X_1$=7.08, $X_2$=0.43, $X_3$=-4.42) 을 나타내고 두 개의 시료는 둘 이상의 negative 값($X_1$=7.66, -8.60, $X_2$=-0.78, -2.13, $X_3$=4.62, -1.00) 을 나타낸다. 또한 기원암(起源岩)의 규명에서 본 연구의 대상이 된 모든 염기성(鹽基性) 변성암(變成岩)이 분출암(憤出岩)및 퇴적암(堆積岩)의 특징인 높은 oxidation ratio (2 $Fe_2O_3{\times}100/2$ $Fe_2O_3+FeO$, in mols)를 가지는 것으로 보아 주성분(主成分) 및 희유원소(稀有元素) 연구(硏究)결과와 비교하여 보면 분출암(憤出岩)에서 유래된 것으로 결론 될 수 있으나 소백산변성암(小白山變成帶)의 경우는 oxidation ratio의 증가가 심한 화강암화작용(花岡岩化作用)의 영향 일수도 있으며 야외산출상태와 현미경기재에서도 분출암(憤出岩)의 잔류증거를 찾지못하였다. 결론적으로 소백산변성대내의 옥방(玉房), 선산(善山), 지체(知體), 단성(丹城)일대의 각섬석질암(角閃石質岩)은 염기성(鹽基性) 관입암(慣入岩)으로부터 유래된 것으로 사료되고, 옥천지향사대내(沃川地向斜帶內)의 상동광상(上東鑛床)일대의 염기성변성암(鹽基性變成岩)은 Kamp (1968)와 Orville (1969)가 취급한 연구 결과에서와 같이 탄산염퇴적물(炭酸鹽堆積物)의 퇴적환경에서 침천한 염기성(鹽基性) tuff로부터 유래된 가능성이 많다.

• 대한치과기공학회지
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• 제30권2호
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• pp.39-45
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• 2008

Titanium and its alloys are widely used as dental implants materials because of their excellent mechanical properties. However, the alumina and zirconia ceramics are preferred to use as the substitute of Ti implants because there is a problems in esthetics and biocompatibility in Ti implant. The the glass infiltrated alumina ceramics are studied to increase the toughness and biocompatibility. The 45S5 and soda-lime glass powder was mixed with ethanol at ratio of 1:1 and brushed on the surface of alumina. Then it was heat treated in the electric furnace at $1400^{\circ}C$ from 30 min. to 5 hours. The glass powder was controlled from 200 to $350{\mu}m$ using ball milling. After heat treatment, the glass infiltrated specimen was tested in universal testing machine to measure the bending strength. The surface microstructure of each specimen was observed with SEM. The biocompatibility of 45S5 and soda-lime glass coated alumina was investigated using PBS at $36.5^{\circ}C$ incubator. The specimen was immersed in PBS for 3, 5, 7, 10 days. After that, the surface morphology was investigated with SEM. As the results of experiment, the 45S5 bioglass infiltrated alumina show the increase of bending strength according to the increasing of heat treatment time from 30 min. to 5 hours at $1400^{\circ}C$ Finally the 1370N bending strength of alumina increased to 1958N at 5 hours heat treatment, which shows 1.4 times higher. In contrast to this, the soda lime glass infiltrated alumina ceramics shows the convex curve according to heat treatment time. Thus it shows maximum bending strength of 1820N at 1 hour heat treatment of $1400^{\circ}C$ It gives 1.3 times higher. However, the bending strength of soda lime glass infiltrated alumina is decreasing with increasing heat treatment time after 1 hour. The precipitation on the surface of 45S5 glass infiltrated alumina was revealed as a sodium phosphate ($Na_{6}P_{6}O_{24}6H_{2}O$) and the amount of precipitation is increasing with increasing of immersion time in PBS. In contrast to this, there is no precipitation are observed on the surface of soda lime glass infiltrated alumina. This implies that 45S5 glass infiltrated alumina brings more biocompatible when it is implanted in human body.