• Title/Summary/Keyword: 저온 석영

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Local Electronic Structures of $SiO_2$ Polymorph Crystals: Insights from O K-edge Energy-Loss Near-Edge Spectroscopy (산소 K-전자껍질 에너지-손실 흡수끝-부근 구조 양자계산을 이용한 $SiO_2$ 동질이상 광물의 전자구조 연구)

  • Yi, Yoo-Soo;Lee, Sung-Keun
    • Journal of the Mineralogical Society of Korea
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    • v.23 no.4
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    • pp.403-411
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    • 2010
  • Essentials of understanding the geochemical evolution and geophysical processes in Earth's system are macroscopic properties and atomistic (and electronic) structures of Earth materials. Recent advances in quantum calculations based on the density functional theory allow us to unveil the previously unknown details of local atomic structures in diverse silicates in Earth's interior. Here, we report the O K-edge ELNES (energy-loss near-edge structure; ELNES) spectra and PLDOS (partial local density of states) for oxygen atoms in ${\alpha}$-quartz and stishovite using the quantum calculations based on FP-LAPW (full potential linearized augmented plane wave). The calculated O K-edge ELNES spectrum of ${\alpha}$-quartz shows a strong peak at ~538 eV due to comer-sharing oxygen linking two $SiO_4$ tetrahedra and that for stishovite shows two distinct peaks at ~537 and ~543 eV corresponding to edge-sharing oxygen linking $SiO_6$ octahedra. The significant differences in spectral features of O K-edge ELNES spectra suggest that the O K-edge features can be useful indicator to distinguish various oxygen sites in diverse crystal and amorphous silicates in the Earth's interior.

On the Growth of GaN Single Crystal from GaOOH Powders (GaOOH 분말로부터 GaN 단결정 성장에 관하여)

  • 이재범;이종원;박인용;김선태
    • Proceedings of the Materials Research Society of Korea Conference
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    • 2003.03a
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    • pp.96-96
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    • 2003
  • 벌크 형태의 CaN 단결정 성장은 매우 곤란한 관계로 아직까지 관련 기술의 개발이 미흡한 실정이다 오랜 기간동안 승화 (sublimation)법으로 대구경 벌크 GaN 단결정을 성장시키고자 하는 노력이 지속되었지만 최근까지도 만족할 만한 결과가 보고되지 않고 있다. 본 논문에서는 종래의 방법과는 달리 출발물질로서 GaOOH 분말을 채택하고, 이를 NH$_3$ 분위기에서 가열 반응시켜 GaN 결정을 성장시켰다. 반응온도와 반응시간 및 NH$_3$ 유량 등의 성장조건에 따른 GaN 결정의 성장거동과 광학적 특성을 조사하였다. 원료인 GaOOH 분말 1g을 석영 용기에 담아 직경이 35mm인 석영 보호관에 위치시키고, 1000~l17$0^{\circ}C$의 온도에서 NH$_3$ 가스를 100~1000 sccm으로 공급하면서 96시간 동안 반응시켰다. 실험이 종료되면 전기로의 온도를 상온까지 냉각시킨 후 석영 보호관 내벽에 성장된 Ga 결정을 채집하였다. 이와 같이 채집된 결정의 형태와 크기를 광학현미경을 사용하여 조사하였고, 결정표면의 상태를 전자현미경을 사용하여 관찰하였다. 시료의 결정성을 알아보기 위하여 X선 회절 분석을 하였고, 저온에서의 광루미네센스 (PL; photoluminescence) 특성을 조사하였다.

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The Scientific Analysis of Floor Tile Excavated from the Beobgwangsa Temple Site in the Pohang (포항 법광사지 출토 녹유전의 자연 과학적 조사)

  • Moon Whan-Suk;Han Min-Su;Hwang Jin-Ju;Kim Ho-Sang
    • KOMUNHWA
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    • no.60
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    • pp.101-120
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    • 2002
  • The floor tile on a coated green-glass was excavated from the Beobgwangsa Temple Site in the Pohang City. We analyzed using the MXRD, ICP-AES, EDXRF, TG/DTA and TIMS. As a result of microscope analysis, it was composed of quartz, feldspar and clay particl

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Comparative Anatomy of the Hydrothermal Alteration of Chonnam and Kyongsang Hydrothermal Clay Alteration Areas in Korea (전남 및 경상 열수변질 점토광상의 생성환경 비교)

  • Koh, Sang Mo;Chang, Ho Wan
    • Economic and Environmental Geology
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    • v.30 no.2
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    • pp.81-87
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    • 1997
  • Chonnam and Kyongsang clay alteration areas are distributed in volcanic fields of the Yuchon Group in late Cretaceous period. The host rock of the Chonnam alteration area is generally acidic and that of the Kyongsang alteration area is acidic to dominantly intermediate volcanics. The important difference of two alteration areas is source of fluid; the Chonnam alteration area is characterized by dominantly meteoric water and the Kyongsang alteration area is characterized by dominantly magmatic water. Accordingly, the high temperature minerals such as pyrophyllite and andalusite, and boron bearing minerals such as dumortierite and tourmaline are common in the Kyongsang alteration area. In contrast to this, the lower temperature minerals such as kaolin and alunite are common in the Chonnam alteration area. The mineralogical difference of two alteration areas were depended on the difference of the formation temperature of clay deposits. The other important geochemical difference is the chemistry of hydrothermal solution such as pH. The alteration of "acid-sulfate type" with alteration mineral assemblage of alunite-kaolin-quartz is dominant in the Chonnam alteration area, which was caused by the attack of strong acid and acid solution. In contrast to this, the that of "quartz-sericite type" with the mineral assemblage of sericite-quartz is dominant in the Kyongsang alteration area, which was caused by the attack of neutral or weak acid solution. Also, the Kyongsang and Chonnam alteration areas show the difference in structural setting; the Chonnam alteration area is commonly associated with silicic domes and the Kyongsang alteration area is commonly associated with calderas.

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Behavior of Solid Phase Crystallizations in Mechanical Damage Induced Hydrogenated and Non-Hydrogenated Amorphous Amorphous Silicon Thin Films (기계적 Damage 활성화 효과에 대한 수소화 및 비수소화 비정질 규소 박막의 고상 결정화 거동)

  • Kim, Hyeong-Taek;Kim, Yeong-Gwan
    • Korean Journal of Materials Research
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    • v.6 no.4
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    • pp.436-445
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    • 1996
  • 비정질 실리콘박막의 고상결정화 특성에 대한 비정질 박막의 증착방법, 수소화 정도, 표면결정 활성화 에너지 변화 및 열처리 환경 영향을 X선 회절, EDAX, Raman 분광 분석으로 조사하였다. 저온(58$0^{\circ}C$)열처리 corning 시료에서 기판 barium(Ba), aluminum(AI) 성분의 막내 확산 임계열처리시간 및 확산에 기인 한 불안정 결정화 특성을 관찰하였다. 화학기상증착 석영 수소화 시료에서 hard damage 기계적 활성화 효과로 얻어진 조대결정립 결정화 특성을 X선 회절의 (111) 배향 상대강도 변화로 관찰 할 수 있었으며, 이는 활성화 효과에 의한 고상 결정화 시 핵생성과 성장속도변화로 다결정 실리콘의 전기적물성 향상 가능성을 보여주었다. Soft damage, bare 활성화 처리 수소화막의 결정화는 비정질 상의 혼재, 박막 응력등의 저품위 입계특성 및 미세결정립 성장 특성으로 관찰되었으나, 활성화 전처리에 의한 저온 및 고온(875$^{\circ}C$)단시간(30분) 결정화는 확인 되었다. 스퍼터링 비수소화 막의 결정화는 상변태 상태의 Raman 결정피크로 분석 되었으며, 결정화 거동에 선행막의 스퍼터링 및 비수소화 영향은 활성화효과에 관계없이 불완전 저품위 결정특성으로 확인되었다. AFM 표면형상은 3차원 island 성막특성을 보여주었고 표면거칠기정도는 높은 것으로 관찰되었다.

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Searching and Prediction of Cutting Characteristics Using Cryogenic Tool (극저온 절삭공구에 의한 가공특성의 규명과 예측)

  • 오석영;정우섭;김칠수;이소영
    • Journal of the Korean Society for Precision Engineering
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    • v.15 no.4
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    • pp.36-43
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    • 1998
  • We experimented turning SCM440, called difficult-to-cut materials in general, using tungsten carbon tool(PIO) in order to elevate machinability by a new cutting method. The cutting tool designed and made to study was cooled to -17$0^{\circ}C$ in about 1 minute by liquid nitrogen. Then, we operated cryogenic cutting by cooling tool with liquid nitrogen and stuided the effect about cutting force, chip thickness, surface roughness, behavior of tool wear and cutting temperature. In addition, we investigated the possibility that sur face roughness of workpiece can be predicted analyzing cutting characteristics.

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The Prediction of the Cutting Characteristics in Cryogenic Cutting Using Neural Network (신경회로망을 이용한 극저온 절삭특성의 예측)

  • Kim, Chill-Su;Oh, Sueg-Young;Oh, Sun-Sae
    • Journal of the Korean Society for Precision Engineering
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    • v.13 no.10
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    • pp.62-70
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    • 1996
  • We experimented on cutting characteristics-cutting force, behavior of cutting temperature, surface roughness. chip thickness under low temperature, which generated by liquid nitrogen(77K). The work-pieces were freezed to-195 .deg. C and liquid nitrogen was also sprinkled on cutting area in order to decrease an experimental error of machining in low temperature. The workpiece was became to -195 .deg. C in5 minutes. In cooled condition surface roughness of workpiece was better than normal condition. In addition, we investigated the possibility that surface roughness of workpiece and cutting force can be predicted analyzing cutting conditions by the trained neural network.

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Alteration Zoning, Mineral Assemblage and Geochemistry of the Hydrothermal Clay Deposits Related to Cretaceous Felsic Magmatism in the Haenam Area, Southwest Korea (한국 서남부, 해남지역에서 백악기 산성마그마티즘에 관련된 열수점토광상의 누대분배, 광물조합의 지구화학적 연구)

  • Kim, In Joon
    • Economic and Environmental Geology
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    • v.25 no.4
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    • pp.397-416
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    • 1992
  • In the present study, three clay deposits, named the Seongsan, Ogmaesan and Haenam deposits, were investigated. The altered zones are recognized in the hydrothermally altered rocks of the clay deposits from the center of the alteration to the margin: Kaolin, Kaolin-Quartz, Quartz, Sericite and Chlorite zones in the Seongsan deposits; Quartz zone, Alunite zone, Kaolin zone, Sericite zone and Chlorite zone in the Ogmaesan deposits; Quartz zone, Pyrophyllite zone, Sericite zone and Chlorite zone in the Haenam deposits. These zones can be grouped into two types of alteration: Acidic alteration such as Pyrophyllite zone, Alunite zone, Quartz zone, Kaolin zone, Kaolin-Quartz zone and a part of Sericite zone; Propylitic alteration such as Chlorite zone and a part of Sericite zone. All clay deposits belong to high-sulfidation (acid-sulfate) system. The rocks of the acidic alterations are composed of pyrophyllite, alunite, kaolin minerals, sericite, quartz and pyrite. On the basis of bulk chemical compositions, it was found that some components such as $SiO_2$, $TiO_2$, $Fe_2O_3$, FeO, MgO, CaO, $K_2O$ and $Na_2O$ were mobilized considerably from the original rocks. The mobility of these major elements is related to, and controls, mineral assemblages in each altered zone. Polytypes of sericite are determined as $2M_1$ and 1M by X-ray diffraction method. The amount of $2M_1$ is nearly equal to that of 1M in the Seongsan deposits whereas $2M_1$ is less and higher than that of 1M in the Ogmaesan and the Haenam deposits. These facts indicate that formation temperature of sericite is relatively high in the Haenam deposits, moderate in the Seongsan deposits, and low in the Ogmaesan deposits. The ratios of Na/(K+Na) for alunite in the Ogmaesan deposits determined by electron microprobe analyzer (EPMA) are higher than those in the Seongsan deposits. Thus, the alunite of the Ogmaesan deposits must have been formed from the solutions with relatively high aqueous Na/(K+Na) ratios and low pH at a high temperature rather than that of the Seongsan deposits. From all data, it is clarified that alunite is hypogene in origin, and has been formed by oxidation of hydrogen sulfide in the steam-heated environment, and that alunite has been produced by the spectacular solfataric alteration observed at the surface of some present-day hydrothermal systems.

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Distribution of Indicator Organisms and Influence of Storage Temperature and Period in Commercial Animal Foods (시판 동물성 식품의 오염지표세균 분포 및 저장온도, 기간별 오염지표세균의 변화)

  • 이용욱;박석기
    • Journal of Food Hygiene and Safety
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    • v.13 no.4
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    • pp.430-440
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    • 1998
  • The average number of total viable counts for the commercial pork tested was 19/g, coliform 1.8/g, psychrophilic bacteria 15/g, heterotrophic bacteria 12/g, fecal streptococcus 6.2/100 g, Pseudomonas aeruginosa 13/100 g and none of heat-resistant bacteria and Staphylococcus was detected. That for the commercial beef tested was 130/g, coliform 5.2/g, psychrophile 140/g, heterotroph 28/g, Staphylococcus 1.2/g, fecal streptococcus 9.5/100 g, Pseud. aeruginosa 1.9/100 g and heat-resistant bacteria was not detected. That for the commercial chicken tested was 8800/g, coliform 53/g, psychrophile 4600/g, heterotroph 4700/g, fecal streptococcus 9.9/100 g, Pseudo aeruginosa 2.5/100 g. That for milk was 4700/ml, psychrophile 120/ml, heterotroph 420/ml and the others were not detected. That for the commercial cheese was 3.2/g, psychrophile 2.3/g, heterotroph 1.6/g, Staphylococcus l/g, fecal streptococcus 9.1/g. That for fermented milk was $10^{7}/ml$, heatresistant bacteria $10^{6}/ml$, fecal streptococcus 2400/100 ml, lactobacillus $3.2{\times}10^{15}/ml$, in accordance with lactic acid bacteria and the others were not detected. There was not detected any indicator organisms from ham, sausage, butter, eggs and quails in the commercial fooods tested. SPC, coliform, psychrophile and heterotroph in commercial meats stored at $10^{\circ}C$ were increased rapidly as time goes on but heat-resistant bacteria, staphylococcus, fecal streptococcus and Pseudo aeruginosa were constant. At $20^{\circ}C$, SPC, coliform, psychrophile, heterotroph and fecal streptococcus were the highest at 7 days and heat-resistant bacteria, staphylococcus and Pseudo aeruginosa were increased a little. At $30^{\circ}C$, all indicators were increased rapidly for 3 and 7 days and then decreased rapidly. All indicator organisms were increased at the level of 10/g for 14 days in meat products stored at $10^{\circ}C$, but SPC, psychrophile and heterotroph in meat products stored at $20^{\circ}C$ were increased at the level of $lO^5/g$. It showed that the indicators in meat products stored at $30^{\circ}C$ had a tendency to increase at the level of $10^{2}/g$ relative to those stored at $20^{\circ}C$. SPC, psychrophile and heterotroph in milk stored at $10^{\circ}C$ increased up to the level of $10^4/ml$, but coliform, staphylococcus, fecal streptococcus and Pseudo aeruginosa were not detected. As stored at $20^{\circ}C$ and $30^{\circ}C$, they were increased rapidly for 1 or 3 days and then constant for a long time.

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Hydrothermal Antimony Deposits of the Hyundong Mine : Geochemical Study (현동 광산의 열수 안티모니 광화작용 : 지화학적 연구)

  • Seong-Taek Yun
    • Economic and Environmental Geology
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    • v.32 no.5
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    • pp.435-444
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    • 1999
  • The antimony deposits of the Hyundong mine, located in the northeastern part of the Sobaegsan massif, occur as hydrothermal quartz+carbonate veins and stockworks which fill the fault fractures developed in Precambrian metamOlphic rocks (mainly, granitic gneiss). Hydrothermal alteration occurs commonly in the vicinity of mineralized veins and is characterized by sericitization and silicification. A K-Ar age of alteration sericite is 139.2$\pm$ 4.4 Ma, implying the early Cretaceous age of mineralization, possibly in association with intrusion of nearby acidic dikes (mainly, quartz porphyry). The hydrothermal mineralization occurred in five mineralization stages. These are: (I) stage I, characterized by deposition of chalcedonic quartz; (2) stage II, deposition of quartz with base-metal sulfides and stibnite; (3) stage III, deposition of quartz and carbonates (calcite, dolomite, ankerite, rhodochrosite) with various antimony-bearing minerals such as stibnite, polybasite, berthierite, native antimony, gudmundite and ullmannite; (4) stage IV, deposition of calcite with stibnite; and (5) stage V, deposition of barren calcite. Antimony occurs mostly as stibnite within stages II to IV veins, which has various habits including disseminated, veinlets and euhedral coarse crystals. Fluid inclusion studies indicate that hydrothermal mineralization at Hyundong occurred from the fluids with temperature and salinity of $330^{\circ}$C to 120 and 5.3 wI. % equiv. NaCI. The temperature and salinity of ore fluids systematically decreased with elapsed time in the course of mineralization, possibly due to the influx of larger amounts of meteoric groundwater. The deposition of antimony-bearing minerals occurred at low temperatures «$250^{\circ}$C), mainly due to the cooling and dilution of fluids. Based on the evidence of fluid boiling during the early stage II mineralization, the mineralization occurred under low pressure conditions (about 80 bars, corresponding to depths of about 350 m under hydrostatic pressure regime). Thermodynamic considerations of ore . mineral assemblages indicate that antimony deposition also occurred as the results of decreases in temperature and sulfur fugacity of hydrothermal fluids. Calculated sulfur isotope composition of ore fluids ($\delta^{34}S_{\Sigma s}$=5.4 to 7.8$\textperthousand$) indicates an igneous source of sulfur.

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