• 한국결정성장학회지
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• 제12권3호
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• pp.157-160
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• 2002

The ferroelectric domain variation and electrical performance of $Pb(Zr,Ti)O_{3}$ (PZT) based capacitors through La additions were systematically studied. La substitution up to 10 % was performed to lower the coercive and saturation voltages of epitaxial ferroelectric capacitors grown on Si using a (Ti_{0.9}Al_{0.1})N/Pt$ conducting barrier composite. Ferroelectric capacitors substituted with 10 % La show significantly lower coercive voltage compared to capacitors with 0 % and 3 % La. This is attributed to a systematic microstructure change into $180^{\circ}C$ domain and decrease in the tetragonality (i.e., c/a ratio) of the ferroelectric phase. These capacitors show promise as storage elements in low power memory architectures.

• 한국광물학회지
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• 제2권1호
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• pp.11-17
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• 1989

The kaolin deposits in Hadong-Sancheong area, have been formed by supergene weathering of anorthositic rocks including anorthosite, leucogabbro, and gabbro. Kaolin consists chiefly of halloysite(10$\AA$) and kaolinite with other minerals such as illite, vermiculite, plagioclase, hornblende, quartz amorphous materials(allophane and siica), goethite, and hematite. Goethite and hematite are the major coloring agents of the reddish brown and other colored kaolins. Other common accessory minerals are magnetite, ilmentite, anatase, gibbsite, I/S, C/V, chlorite, lithiophorite, and birnessite. Paragonite, dravite, laumontite, clinozoisite, muscovite, scolecite, stellerite are locally found. Al substitution of Fe in goethite and hematite decreases from the surface zone toward the deeper zone. The kaolin deposits show three horizontal zoning; the upper reddish brown, middle pink, and lower white zones. All the zones are characterized by somewhat different mineralogy. The factors for the formation of kaolin deposits in Hadong-Sancheong area are 1) the presence of anorthositic rocks, 2) the low flat or gentle topography, 3) the favorable climate, and 4) the long-continued preservation of kaolins with-out erosion.

• 한국자기학회:학술대회 개요집
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• 한국자기학회 2000년도 International Symposium on Magnetics The 2000 Fall Conference
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• pp.413-420
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• 2000

Cheju Island has nature of typical trass through volcanic activities in many times. The soil in Cheju Island has principally sprung from basalt and partially made up of trachyte, trachyte's nature and site. Also ancient relics, plain coarse pottery's kilns and pantiles kilns are homogeneously distributed all over the Cheju Island. In this study, as a result of X-ray fluorescence spectrometer and Mossbauer spectroscopy of a sample are from plain coarse pottery and pantiles in 5 regions of Cheju Island. It is thought that these samples are partially formed from neutral volcanic rock like trachyte and Atomicity state of iron is almost Fe$\^$3+/. Also the magnetic hyperfine field length of goethite, contained these samples is less than synthetic goethite magnetic hyperfine field length and this result shows that disintegration of inner magnetic order, created by partial substitution of diamagnetic positive ion containing Fe$\^$3+/ and Al$\^$3+/ in goethite lattice.

• Bulletin of the Korean Chemical Society
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• 제13권6호
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• pp.689-695
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• 1992

Methods for the selective functionalization of calix[4]arene at the upper rim are described. The diametrically substituted calix[4]arene dimethyl ether 2, obtained from the treatment of calix[4]arene 1 with methyl iodide in the presence of $K_2CO_3$, is converted to the two isomeric p-diacetylcalix[4]arene dimethyl ether 3 and 6 by direct substitution and by Fries rearrangement of corresponding diacetyloxycalix[4]arene dimethyl ether 5 respectively. Diametrically substituted p-diacetylcalix[4]arene 8 was also prepared by Fries rearrangement of calix[4]arene tetraacetate 7 using a limited amount of $AlCl_3$.

• Bulletin of the Korean Chemical Society
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• 제15권12호
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• pp.1084-1088
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• 1994

Electrical characteristics of Fe-substituted sodalites were analyzed and equivalent circuits of samples were designed using impedance and admittance data. Internal components of resistances (R$_e$, R$_b$, and R$_{gb}$) and capacitances (C$_b$, C$_dl$ and C$_D$) could be extracted by changing the frequency of measurement at three different temperatures. Upon increasing the temperature, electrical properties of the samples could be elucidated in detail by equivalent circuit. The substitution of Fe on Al site was indirectly confirmed by ESCA and the results explain the lower polarity in Na-O bond of Fe 10 mole ${\%}$-substituted sodalite.

• Bulletin of the Korean Chemical Society
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• 제24권8호
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• pp.1181-1187
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• 2003

Condensation of 4-cyano-5,6-dimethyl-3-pyridazinone 1 with aromatic aldehydes gave the novel styryl derivatives 2a-c. Refluxing of compound 2a with phosphorus oxychloride furnished 3-chloropyridazine derivative 3. Compound 3 was reacted with thiourea and produced pyridazine-3(2H)thione 4. Thieno[2,3-c]- pyridazines 5a-e were achieved by cycloalkylation of compound 4 with halocompounds in methanol under reflux and in the presence of sodium methoxide. Also, refluxing of compound 4 with N-substituted chloroacetamide in the presence of potassium carbonate afforded thienopyridazines 6a-e. Cyclization of compound 6 with some electrophilic reagents as carbon disulfide and triethyl orthoformate furnished the novel pyrimido[4',5':4,5]thieno[2,3-c]pyridazines 12 and 13a-c, respectively. Diazotisation of compound 6 with sodium nitrite in acetic acid produced the pyridazino[4',3':4,5]thieno[3,2-d][1,2,3]triazines 14a-c. Ternary condensation of compound 1, aromatic aldehydes and malononitrile in ethanol containing piperidine under reflux afforded the novel phthalazines 16a-c. Compound 3 was subjected to some nucleophilic substitution reactions with amines and sodium azide and formed the aminopyridazines 17a, b and tetrazolo[1,5-b]-pyridazine 19, respectively. The structures of the synthesized compounds were established by elemental and spectral analyses.

• 한국재료학회지
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• 제4권1호
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• pp.117-124
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• 1994

마이크로웨이브 Mg-Mn훼라이트에서 비자성 이온인 알루미늄으로 Fe 이온을 치환하여 포화자화를 낮출 수 있다. 이것은 마이크로웨이브 훼라이트의 사용 주파수 영역의 확장을 위해 필요하다. 이때 다른 특성의 변화가 수반되는 것은 검토해 봐야 할 점중의 하나이다. 본 연구에서는 MgO: MnO : $Fe_2O_3$를 1.0:0.1:0.95몰비로 제조한 마이크로 웨이브 훼라이트[화학식:$(MgO)_{1.0}(MnO)_{0.1}(Al_xFe_{1.9-x}O_{2.85}$]에서 AI을 0.1에서 0.4까지 첨가한 경우의 전기적.자기적 특성을 미세조직과 아울러 조사하였다. 포화자화 값은 첨가량에 따라 감소하였으며 강자성공명 선폭도 마찬가지였다. $H_c$ 값은 첨가량 0.2이상에서 103.48A/m(1.3Oe)이하로 나타났으며 각형비는 모두 우수하였다. 공명자기장은 첨가량에 따라 거의 변화가 없었다. 이상고 같은 실험결과로부터 적절한 조성범위에서 각각의 물성을 조합하여 넓은 범위의 마이크로웨이브 소자에 응용할 수 있는 제반 물성을 얻을 수 있었다.

• 한국산학기술학회논문지
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• 제15권11호
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• pp.6890-6897
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• 2014

본 전기로 환원슬래그는 팽창성 물질이 함유되어 불안정한 상태이므로 건설용 재료로 그대로 사용하기에는 다소 무리가 있다. 그러나 전기로 환원슬래그에는 $11CaO{\cdot}7Al_2O_3{\cdot}CaF_2$와 ${\beta}-C_2S$ (calcium aluminate compounds) 물질이 함유되어 있으므로 적절한 성분 보조제를 혼합하여 사용한다면 콘크리트용 혼화재료로서 사용이 가능할 것으로 판단된다. 이에 본 연구에서는 콘크리트 혼화재료서 전기로환원슬래그 미분말의 사용 가능성을 검토하고자 한다. 전기로 환원슬래그 미분말의 치환율별 모르타르 강도특성과 응결특성을 검토 결과, 최적 치환율은 30% 수준으로 나타났다. 최적 치환율에 석고 첨가에 따른 응결시간 및 강도특성을 파악한 결과, 전기로환원슬래그 미분말 치환율 30%인 배합에 이수석고를 8% 혼입하였을 경우 압축강도 발현 성상 및 응결특성이 OPC와 유사한 결과를 나타내었다.

• 한국분말재료학회지
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• 제9권6호
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• pp.381-393
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• 2002

Recent developments in nanocrystalline and nanocomposite rare earth-transition metal magnets are reviewed and emphasis is placed on research work at IFW Dresden. Principal synthesis methods include high energy ball milling, melt spinning, mold casting and hydrogen assisted methods such as reactive milling and hydrogenation-disproportionation-desorption-recombination. These techniques are applied to NdFeB-, PrFeB- and SmCo-type systems with the aim to produce high remanence magnets with high coercivity. Concepts of maximizing the energy density in nanostructured magnets by either inducing a texture via anisotropic HDDR or hot deformation or enhancing the remanence via magnetic exchange coupling are evaluated. With respect to high temperature applications melt spun $Sm(Co_{0.74}Fe_{0.1}Cu_{0.12}Zr_{0.04})_{7.5}$ ribbons were prepared, which showed coercivities of up to 0.53 T at 50$0^{\circ}C$. Partially amorphous $Nd_{60}Fe_xCo_{30-x}Al_{10}(0{\leq}x{\leq}30)$ alloys were prepared by copper mold casting. The effect of transition metal content on the glass-forming ability and the magnetic properties was investigated. The $Nd_{60}Co_{30}Al_{10}$ alloy exhibits an amorphous structure shown by the corresponding diffraction pattern. A small substitution of Co by 2.5 at.% Fe results In the formation of Fe-rich crystallites embedded in the Nd-rich amorphous matrix. The Fe-rich crystallites show hard magnetic behaviour at room temperature with a coercivity value of about 0.4 T, relatively low saturation magnetization and a Curie temperature of 500 K.

• 한국광물학회지
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• 제12권2호
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• pp.55-65
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• 1999

Spotted cordierite occurs as the result of intrusion of Wolaksan Granite of Cretaceous age in the northern part of the Ogcheon Metamorphic Belt, forming a contact metamorphic zoning in accordance with the distance from the granite body: a cordierite-muscovite-biotite-quartz assemblage and the higher-temperature cordierite-biotite-quartz-(cummingtonite). These quartz-ubiquitous mineral assemblages identified in the cordierite spot seem to reflect Al-deficient condition of the protolith. TEM observations of textural relations between the cordierite and mica within the cordierite spot clearly reflect that cordierite was formed at the expense of micaceous matrix. A structure refinement of the poikiloblastic cordierite was performed by the Rietveld refinement method. Unit cell of the cordierite was determined to be as follows : lower-temperature type: a=17.1480(9)${\AA}$, b=9.7743(6)${\AA}$, c=9.3184(5)${\AA}$, V=1561.9(4)${\AA}$3, higher-temperature type: a=17.136(2)${\AA}$, b=9.751(1)${\AA}$, c=9.322(1)${\AA}$, V=1557.7(4)${\AA}$3. They show a remarkable difference in the unit cell dimension. The refinement results indicate that structural sites of lower-temperature cordierite are wholly occupied by appropriating ions. Compared to this, tetrahedral sites of the higher-temperature type exhibit an order/disorder ranging about 5-8% as the result of substitution between Si4+ and Al3+, except for T26 site occupied wholly by Al3+. These structural differences seem to be related to the formation temperatures of both cordierite types.