• Title/Summary/Keyword: OOH

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On the Synthesis of Zn-doped GaN Fine-Powders (Zn가 첨가된 GaN 미세 분말의 합성에 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.95-95
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    • 2003
  • 최근, 대면적 평판표시소자 제작을 위한 전기발광 (EL; electroluminescence)소자용 소재로서 GaN 분말을 적용하고자 하는 연구가 진행되고 있다. 이와 같이 GaN 분말을 EL 소재로 사용하기 위해서는 원하는 파장의 빛을 발광할 수 있도록 특정의 불순물을 첨가하여야 할 필요가 있다. Mg이 첨가된 GaN 분말의 합성과 특성에 대한 연구가 있었으며, 희토류 원소가 첨가된 GaN 분말의 특성이 보고된바 있다. 본 논문에서는 GaOOH 분말을 출발물질로 채택하여 Zn가 첨가된 GaN 분말을 합성하고 광학적인 특성을 조사하였다. Zn가 첨가된 GaN 분말을 합성하기 위하여, 우선 CaOOH 분말 1g과 일정량의 ZnO 또는 Zn(NO$_3$)$_3$를 함께 섞어 유발에서 습식 혼합한 후 건조시켰다. Ga에 대한 Zn의 몰 비는 0.1부터 30 까지 변화시켰다. 반응온도는 900~110$0^{\circ}C$의 범위에서 변화시켰고, 반응시간은 1~4시간 범위에서 변화시켰으며, NH$_3$의 유량은 400 sccm으로 하였다. X선 회절분석장치를 사용하여 결정구조를 확인하였고, Zn의 첨가에 따른 광학적 특성은 10 K의 온도에서 광루미네센스(PL; photoluminescence)를 측정하여 평가하였다.

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Formation Reaction of Mn-Zn Ferrite by Wet Process (습식합성에 의한 Mn-Zn Ferrite의 생성반응에 관한 연구)

  • 이경희;이병하;허원도;황우연
    • Journal of the Korean Ceramic Society
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    • v.30 no.1
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    • pp.25-33
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    • 1993
  • Formation reaction of Mn-Zn ferrite depending on various synthetic conditions of wet process was investigated using FeCl2.nH2O(n≒4), MnCl2.4H2O, ZnCl2 as starting materials. A stable intermediate precipitate was formed by the addition of H2O2. And the precipitate was hard to transform to spinel phase of Mn-Zn Fe2O4. Single phase of Mn-Zn Fe2O4 spinel was obtained above 8$0^{\circ}C$ reaction temperature. The powder had spherical particle shape and 0.02~0.05${\mu}{\textrm}{m}$ particle size. Fe(OH)2 solid solution, -FeO(OH) solid solution, -FeOOH, Mn-Zn Fe2O4 spinel were formed with air flow rate 180$\ell$/hr. However, single phase of Mn-Zn Fe2O4 spinel with cubic particle shape and 0.1~0.2${\mu}{\textrm}{m}$ particle size was formed with synthetic conditions of 8$0^{\circ}C$ and 90 munutes. The particle shape of the -FeOOH was needle-like.

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Characteristic Distributions of $H_2O$$_2$ and $CH_3$OOH in Seoul (서울에서 $H_2O$$_2$$CH_3$OOH의 특징적 분포)

  • 김주애;배성연;김영미;이미혜;박정후
    • Proceedings of the Korea Air Pollution Research Association Conference
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    • 2003.11a
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    • pp.171-172
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    • 2003
  • Hydrogen peroxide($H_2O$$_2$)는 오존의 생성과 소멸에 관여할 뿐 아니라 용해도가 높아 액상에서도 중요한 산화제의 역할을 한다. 특히 도시의 오존농도가 증가하며 이를 제어하기 위한 연구가 활발히 진행되고 있는데 이때 $H_2O$$_2$는 오존 화학을 이해하고 저감대책을 세우는데 필요한 지시자의 역할을 한다. 따라서 $H_2O$$_2$의 시ㆍ공간적 분포의 이해는 대기 환경 연구에 필수적이다. (중략)

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Protective Effect of Some Medicinal Plants on tert-Butyl Hydroperoxide-Induced Oxidative Stress in Human Keratinocytes

  • Na, Min-Kyun;Jang, Tae-Su;Choi, Ji-Young;Lee, Seung-Ho;Bae, Ki-Hwan
    • Natural Product Sciences
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    • v.14 no.4
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    • pp.244-248
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    • 2008
  • It is well known that excessive production of reactive oxygen species (ROS) leads to oxidative stress, loss of cell function, and ultimately apoptosis or necrosis. To search for natural antioxidants able to modulate cellular oxidative stress, we investigated the protective effect of ethanol extracts of 17 medicinal plants selected from the preliminary antioxidant screening on tert-butyl hydroperoxide (t-BuOOH)-induced oxidative stress in human keratinocytes. The result showed that extracts of the four plants, Distylium racemosum, Astilbe chinensis, Cercis chinensis and Sapium japonicum, exhibited significant cytoprotective activity (over 50% protection) against t-BuOOH-induced cellular injury.

Characteristic Distributions of Hydrogen Peroxide and Methyl Hydroperoxide and over the North Pacific Ocean

  • Lee, Meehye;Brian G. Heikes
    • Journal of Korean Society for Atmospheric Environment
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    • v.18 no.E2
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    • pp.85-95
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    • 2002
  • Hydrogen peroxide and methyl hydroperoxide were measured over the northwestern Pacific Ocean during NASA's PEM (Pacific Exploratory Mission) -West. The first experiment (PEM -West A) was conducted in the fall of 1991 and PEM-West B in the early spring of 1994. Hydroperoxide data were obtained on board the NASA DC -8 aircraft through the entire depth of the troposphere. Average concentrations of both H$_2$O$_2$and CH$_3$OOH were higher during PEM -West A than B. The seasonal difference in hydroperoxide distribution was determined by the degree of photochemical activities and the strength and location of jetstream, which led to extensive and rapid continental outflow during the PEM-West B. While for H$_2$O$_2$distribution, a longitudinal gradient was more apparent than a latitudinal gradient, it was opposite for the CH$_3$OOH distribution. The longitudinal gradient indicates the proximity to the anthropogenic sources from the Asian continent, but the latitudinal gradient reflects photochemical activity. During PEM -West B, the ratio of C$_2$H$_2$/CO, a tracer for continental emission was raised and high concentrations of H$_2$O$_2$were associated with high ratios. The flux of hydroperoxide toward the North Pacific was also enhanced in the early spring. The eastward fluxes of H$_2$O$_2$ were 9% and 17% of the average photochemical production over the Pacific Basin between 140°E and 130°W during PEM-West A and B, respectively. For CH$_3$OOH, these ratios were 8% and 13%. Considering the lifetime of hydroperoxide and the rapid transport of pollutants, the export of hydroperoxide with other oxidants would have a significant influence on oxidant cycles over the North Pacific during winter/spring.

Preparation of $Ga_2O_3:Eu^{3+}$ phosphors by homogeneous precipitation (균일침전법에 의한 $Ga_2O_3:Eu^{3+}$ 형광체의 제조)

  • 천민호;박인용;이종원;김선태
    • Journal of the Korean Crystal Growth and Crystal Technology
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    • v.12 no.3
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    • pp.149-156
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    • 2002
  • Europium-activated $Ga_2O_3$ phosphor powders were prepared by homogeneous precipitation method. The resulting powders were characterized by means of TG/DTA, XRD, FT-IR and SEM, Two kinds of powders formed were the crystalline GaOOH and the amorphous-like $\gamma$-$Ga_2O_3$ phases. When the urea concentration was below 0,5 M, rod-like micrometer-sized GaOOH powders were formed. They were transformed via $\alpha$-$Ga_2O_3$ to $\beta$-$Ga_2O_3$ phases under heat treatment. On the other hand, the nanometer-sized $\gamma$-$Ga_2O_3$ powders were formed with urea concentrations higher than 1.0 M, and they were directly changed into $\beta$-$Ga_2O_3$.Photoluminescence (PL) spectra were observed at room temperature, and PL intensities of nanometer-sized $Ga_2O_3$ : $Eu^{3+}$ powders around 610 nm were higher than those of micrometer-sized ones.

Synthesis of boehmite powder from aluminum etching solution (알루미늄 에칭액으로부터 베마이트 분말 합성)

  • Park, Young-Soo;Wui, In-Hee;Cho, Woo-Seok;Kim, Jin-Ho;Hwang, Kwang-Taek
    • Journal of the Korean Crystal Growth and Crystal Technology
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    • v.22 no.6
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    • pp.286-290
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    • 2012
  • Boehmite (AlOOH) powder was synthesized using waste aluminium etching solution. In waste solution, precipitated phase was gibbsite ($Al(OH)_3$), and boehmite (AlOOH) phase was obtained at pH of 7 and 8 controlled by addition of acid. Boehmite powder was obtained by washing process to remove the Na ion in precipitated solution. Mean particle size of obtained powder was 40 nm. Boehmite phase transformed to ${\alpha}-Al_2O_3$ phase via ${\gamma}-Al_2O_3$, ${\delta}-Al_2O_3$, and ${\Theta}-Al_2O_3$.

Biotic and Abiotic Reduction of Goethite (α-FeOOH) by Subsurface Microorganisms in the Presence of Electron Donor and Sulfate (전자공여체와 황산염 이용 토착미생물에 의한 침철석(α-FeOOH) 환원 연구)

  • Kwon, Man Jae;Yang, Jung-Seok;Shim, Moo Joon;Lee, Seunghak;Boyanov, Maxim;Kemner, Kenneth;O'Loughlin, Edward
    • Journal of Soil and Groundwater Environment
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    • v.19 no.1
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    • pp.54-62
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    • 2014
  • To better understand dissimilatory iron and sulfate reduction (DIR and DSR) by subsurface microorganisms, we investigated the effects of sulfate and electron donors on the microbial goethite (${\alpha}$-FeOOH) reduction. Batch systems were created 1) with acetate or glucose (donor), 2) with goethite and sulfate (acceptor), and 3) with aquifer sediment (microbial source). With 0.2 mM sulfate, goethite reduction coupled with acetate oxidation was limited. However, with 10 mM sulfate, 8 mM goethite reduction occurred with complete sulfate reduction and x-ray absorption fine-structure analysis indicated the formation of iron sulfide. This suggests that goethite reduction was due to the sulfide species produced by DSR bacteria rather than direct microbial reaction by DIR bacteria. Both acetate and glucose promoted goethite reduction. The rate of goethite reduction was faster with glucose, while the extent of goethite reduction was higher with acetate. Sulfate reduction (10 mM) occurred only with acetate. The results suggest that glucose-fermenting bacteria rapidly stimulated goethite reduction, but acetate-oxidizing DSR bacteria reduced goethite indirectly by producing sulfides. This study suggests that the availability of specific electron donor and sulfate significantly influence microbial community activities as well as goethite transformation, which should be considered for the bioremediation of contaminated environments.