• 제목/요약/키워드: Reduced atmosphere

검색결과 469건 처리시간 0.027초

Improved Luminescence Properties of Polycrystalline ZnO Annealed in Reduction Atmosphere

  • Chang, Sung-Sik
    • 한국세라믹학회지
    • /
    • 제48권3호
    • /
    • pp.251-256
    • /
    • 2011
  • The luminescence properties of polycrystalline ZnO annealed in reducing ambience ($H_2/N_2$) have been studied. An effective quenching of green luminescence with enhanced UV emission from polycrystalline ZnO is observed for the reduced ZnO. The variations of the UV and green luminescence band upon reduction treatment are investigated as a function of temperature in the range between 20 and 300 K. Upon annealing treatment in reducing ambience, the optical quality of polycrystalline ZnO is improved. The UV to green intensity ratio of sintered ZnO approaches close to zero (~0.05). However, this ratio reaches more than 13 at room temperature for polycrystalline ZnO annealed at $800^{\circ}C$ in reducing ambience. Furthermore, the full width at half maximum (FWHM) of the UV band of polycrystalline ZnO is reduced compared to unannealed polycrystalline ZnO. Electron paramagnetic resonance (EPR) measurements clearly show that there is no direct correlation between the green luminescence and oxygen vacancy concentration for reduced polycrystalline ZnO.

ISFET용 SiO2 감응박막에 관한 연구 (A Study on the SiO2Sensing Layer Used in ISFET)

  • 최두진;임공진;정형진;김창은
    • 한국세라믹학회지
    • /
    • 제27권1호
    • /
    • pp.79-85
    • /
    • 1990
  • A study on the oxidation of SiO2 sensing layer was done at 950, 1000, 105$0^{\circ}C$ under dry O2 atmosphere. The rate determining step around the oxide layer thickness, 1000$\AA$ was different with the oxidation temperature, as follows ; ⅰ) linear growth at 95$0^{\circ}C$ and ⅱ) parabolic growth at 100$0^{\circ}C$ and 105$0^{\circ}C$. The flatness of SiO2 film was observed within $\pm$1% and surface state charge density was reduced by annealing in N2 atmosphere. Finally, pH sensitivity of SiO2 film, in the range of pH 3-9, was 20mV/pH.

  • PDF

VARIABILITY OF BOW SHOCK LOCATION AT MARS

  • Yi, Yu;Kim, Eo-Jin;Kim, Yong-Ha;Kim, Jhoon
    • Journal of Astronomy and Space Sciences
    • /
    • 제16권2호
    • /
    • pp.139-148
    • /
    • 1999
  • Bow shock formation, in case the supersonic solar wind flow is hindered by the atmosphere of Mars, is investigated. The atoms newly ionized from the extensive neutral atmosphere of Mars are loaded to the solar wind. By the conservation of momentum, the solar wind velocity is decreased. Then the supersonic flow velocity drops to the subsonic flow velocity in front of Mars at certain region, which is called the bow shock. The location of Mars subsolar bow shock is highly varying in the range of 1.3 to 2.5 Rm. Martian bow shock location is estimated by one-dimensional flux tube equations reduced from full three-dimensional MHD equations. The variability of Mars bow shock location effected by the solar wind conditions is studied. It is evident that the solar wind dynamic pressure change is able to make the Mars bow shock location variable.

  • PDF

The influence of atomosphere on high temperature crystal growth

  • Klimm, D.;Schroder, W.
    • 한국결정성장학회지
    • /
    • 제9권4호
    • /
    • pp.360-364
    • /
    • 1999
  • The growth of crystals with high melting point$t_{fus}$$\geq$$1600^{\circ}C$ faces the researcher with experimental problems, as the choice of materials that withstand such high t is rather limited. Many metallic construction materials are in this high t range already molten or exhibit at least a drastically reduced mechanical strength. The very few materials with$t_{fus}$$1600^{\circ}C$ as e.g. W, Mo, and partially even Ir are more or less sensitive against oxygen upon heating. Whenever possible, high t crystal growth is performed under inert atmosphere (noble gases). Unfortunately, many oxides are not thermodynamically stable under such conditions, as reduction takes place within such atmosphere. A thoroughly search for suitable growth conditions has to be performed, that are on the one side "oxidative enough" to keep the oxides stable and on the other side "reductive enough" to avoid destruction of constructive parts of the crystal growth assembly. The relevant parameters are t and the oxygen partial pressure${po}_{2}$. The paper discusses quantitatively relevant properties of interesting oxides and construction materials and wasy to forecast theri behavior under growth conditions.

  • PDF

환원시약인 테트라카르보닐철산염(O)을 이용한 유기아지드화물의 아미노화 (제1보) (Amination of Organic Azides using Tetracarbonylhydridoferrate(O) as a Reducing Agent(I))

  • 심상철;최귀남
    • 대한화학회지
    • /
    • 제29권4호
    • /
    • pp.437-440
    • /
    • 1985
  • 유기아지드화물은 일산화탄소대기압하, 실온에서 높은 선택적 환원시약인 테트라카르 보닐철산염의 존재하에서 높은 수득율의 아민으로 환원되었다. 특히 벤조일아지드는 동일시약내 일산화탄소 대기압 실온에서는 에틸페닐카바메이트를 주나, -40$^{\circ}$에서는 정량적으로 벤즈아미드가 얻어졌다.

  • PDF

Pechini법에 의한 Y-doped SrTiO3 분말의 합성 (Synthesis and Characterization of Y-doped SrTiO3 Powder by Pechini Method)

  • 윤미영;송락현;신동열;황해진
    • 한국분말재료학회지
    • /
    • 제17권1호
    • /
    • pp.59-64
    • /
    • 2010
  • 8 mol% Y-doped $SrTiO_3$ powder was synthesized by Pechini method from titanium isopropoxide, strontium nitrate, yttrium nitrate, citric acid and ethylene glycol. A $Y_2Ti_2O_7$ pyrochlore phase-free perovskite powder was obtained by calcining a polymeric resin, which was prepared from a precursor solution, at $500^{\circ}C$ in an air atmosphere. Low temperature calcination could lead to a fine-grained microstructure. In the case of a solid-state reaction, an extended heat-treatment at high temperature in a reduced atmosphere needed to obtain a single phase perovskite $SrTiO_3$.

The Influence of Atmostphere on High Temperature Crystal Growth

  • Klimm, D.;Schroder, W.
    • 한국결정성장학회:학술대회논문집
    • /
    • 한국결정성장학회 1999년도 PROCEEDINGS OF 99 INTERNATIONAL CONFERENCE OF THE KACG AND 6TH KOREA·JAPAN EMG SYMPOSIUM (ELECTRONIC MATERIALS GROWTH SYMPOSIUM), HANYANG UNIVERSITY, SEOUL, 06월 09일 JUNE 1999
    • /
    • pp.51-67
    • /
    • 1999
  • The growth of crystals with high melting points tfus$\geq$1$600^{\circ}C$ faces the researcher with experimental problems, as the choice of materials that withstand such high t is rather limited. Many metallic construction materials are in this high t range already molten or exhibit at least a drastically reduced mechanical strength. The very few materials with tfus》1$600^{\circ}C$ as e.g. W, Mo, and partially even Ir are more or less sensitive against oxygen upon heating. Whenever possible, high t crystal growth is performed under inert atmosphere (noble gases). Unfortunately, any oxides are not thermodynamically stable under such conditions, as reduction takes place within such atmosphere. A thoroughly search for suitable growth conditions has to be performed, that are on the one side "oxidative enough" to keep the oxides stable and on the other side "reductive enough" to avoid destruction of constructive parts of the crystal growth assembly. The relevant parameters are t and the oxygen partial pressure pO2. The paper discusses quantitatively relevant properties of interesting oxides and construction materials and ways to forecast their behavior under growth conditions.r growth conditions.

  • PDF

Luminescence property of Eu2+ in SiO2-Al2O3 glass phosphor

  • Chae, Ki Woong;Lee, Kyoung-Ho;Cheon, Chae Il;Cho, Nam In;Kim, Jeong Seog
    • Journal of Ceramic Processing Research
    • /
    • 제13권spc2호
    • /
    • pp.189-192
    • /
    • 2012
  • Manufacturing process for silicate glass phosphors containing Eu2+ activator and their photoluminescence property have been studied. We adopted powder sintering process instead of traditional glass melting process for making glass phosphor. At first, phosphor powders were synthesized at 1200 ℃ for 2-3 hours under a reducing atmosphere with 10% H2-90% N2 gas mixture. The reduced powders were compacted into discs and then the discs weresintered at 1400 ~ 1500 ℃ for 1 hr under a reducing atmosphere of 5H2-95% N2. The enhancement of PL intensity by Al2O3 addition, XPS binding energy shift of Si 2p and O 1s, sintering shrinkage, and crystallization were characterized.

P2O5-SnO2계 유리에서 용융분위기에 따른 구조와 물성에 미치는 영향 (Effect of Melting Atmospheres on the Structure and Properties of P2O5-SnO2 Glass Systems)

  • 안용태;최병현;지미정;권용진;배현;황해진
    • 한국세라믹학회지
    • /
    • 제49권2호
    • /
    • pp.191-196
    • /
    • 2012
  • In this study, tin phosphate glass system($SnO_2-(1-x)P_2O_5-xB_2O_3$) that occur during the melting of the metal oxide inhibition of the oxidation reaction, and to reduce oxides of high melting temperature in the following three methods were melting. The first is the general way in the atmosphere, and the second by injecting $N_2$ gas under a neutral atmosphere, and finally in the air were melted by the addition of a reducing agent Melt in the atmosphere when the oxidation of the metal oxide is inhibited by low temperatures were melting. In addition, the deposition of crystals within glassy or inhibit devitrification phenomenon is also improved over 80% transmittance. This phenomenon, when the melting of glass, many of $Sn^{4+}$ ions are reduced to the $Sn^{2+}$ was forming oxides SnO, because it acts as a modifier oxide.

20세기 재분석 자료(20CR)를 이용한 남극대륙의 기온 변화 (Change of Temperature using the Twentieth Century Reanalysis Data (20CR) on Antarctica)

  • 조일성;지준범;이규태;채남이;윤영준
    • Ocean and Polar Research
    • /
    • 제34권1호
    • /
    • pp.73-83
    • /
    • 2012
  • Antarctica is very sensitive to climate change but the number of stations is not sufficient to accurately analyze climate change in this regoin. Model reanalysis data supplements the lack of observation and can be used as long term data to verify climate change. In this study, the 20CR (Twentieth Century Reanalysis) Project data from NCEP/NCAR and monthly mean data (temperature, solar radiation and longwave radiation) from 1871 to 2008, was used to analyze the temperature trend and change in radiation. The 20CR data was used to validate the observation data from Antarctica since 1950 and the correlation coefficients between these data were determined to be over 0.95 at all stations. The temperature increased by approximately $0.23^{\circ}C$/decade during the study period and over $0.20^{\circ}C$/decade over all of the months. This increasing trend was observed throughout the Antarctica and a slight increase was observed in the Antarctic Peninsula. In addition, solar radiation (surface) and longwave radiation (surface and top of atmosphere) trends correlated with the increase in temperature. As a result, outgoing longwave radiation at the surface is attenuated by atmospheric water vapor or clouds and radiation at the top of the atmosphere was reduced. In addition, the absorbed energy in the atmosphere increases the temperature of the atmosphere and surface, and then the heated surface emits more longwave radiation. Eventually these processes are repeated in a positive feedback loop, which results in a continuous rise in temperature.