• Title/Summary/Keyword: long-range ordering parameter

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Cation Ordering and Microwave Dielectric Properties of $Ba(Mg_{1/3}Nb_{2/3})O_3$Ceramics: I. Long-Range Order Parameter ($Ba(Mg_{1/3}Nb_{2/3})O_3$ 세라믹스의 양이온 규칙구조와 유전특성: I. 장거리 규칙도)

  • 김영웅;박재환;김윤호;박재관
    • Korean Journal of Crystallography
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    • v.12 no.2
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    • pp.76-80
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    • 2001
  • We have studied the effect of sintering conditions on the long-range order parameter of the 1 : 2 cation ordering in Ba(Mg/sub 1/3/Nb/sub 2/3/)O₃microwave dielectrics prepared through a columbite precursor method. It is found that the order parameter depends strongly on the sintering conditions. As the heat-treatment time increases at 1350℃, the long-range order parameter decreases. When sintered at 1500℃ for 4 hours, BMN shows a high long-range order parameter of 0.94.

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Nano-structure and Magnetic Properties of FePd Superlattice Thin Film (FePd 인공격자박막의 나노구조 및 자기적 특성)

  • Kang, J.G.;Chung, I.S.;Koo, J.W.;Koh, J.H.;Koo, S.M.;Nam, S.M.;Ha, J.G.
    • Journal of the Korean Magnetics Society
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    • v.18 no.5
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    • pp.190-194
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    • 2008
  • Epitaxial $L1_0$ FePd (001) thin films were successfully manufactured by sputtering deposition method. The structure and magnetic properties of FePd thin films were characterized as a function of Fe compositions. It was found that the long-range ordering parameter had a maximum for the stoichiometric composition, whereas the magnetic anisotropy had a maximum as the Fe content is decreased to slightly above the stoichiometric composition. This indicates that the stoichiometry is directly contributed to the chemical ordering and the magnetic anisotropy. These results imply that nonstoichiometric FePd compositions, with a slight excess of Pd, may in fact be preferred for applications that require high magnetic anisotropy.

High-resolution Transmission Electron Microscopy of Ordered Structure for Lead Magnesium Niobate Solid Solutions ($Pb(Mg_{1/3}Nb_{2/3})O_3$ 고용체에서 고분해능 투과전자현미경을 이용한 구조 규칙화에 대한 연구)

  • Park, Kyeong-Soon
    • Applied Microscopy
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    • v.27 no.1
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    • pp.101-109
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    • 1997
  • The nonstoichiometric ordering of Mg and Nb cations in undoped and La-doped lead magnesium niobate solid solutions has been investigated by means of high-resolution transmission electron microscopy and computer image simulation. High-resolution lattice images were obtained under various microscope imaging conditions and objective apertures. Computer image simulations were performed for a wide range of sample thickness, defocusing value, and long-range order parameter. The simulated images revealed that the lattice images of the ordered regions were predominantly dependent on the long-range order parameter. From the comparisons of the experimental and simulated images for the ordered regions, the long-range order parameter approximately ranged 0.2 to 0 7. It was also found that the ordered structure has a $(NH_4)_3-FeF_6$ structure, which consists of alternating Mg- and Nb-preferred sublattices along the (111) directions.

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FTIR and M ssbauer Spectroscopic Studies on the Hydrothermal Epidote from the Bobae Clay Deposit, Pusan, Korea (보배광산에서 산출하는 열수변질 기원 녹염석의 분광학적 특성: 적외선 및 뫼스바우어 연구)

  • 추창오;김수진
    • Journal of the Mineralogical Society of Korea
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    • v.9 no.2
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    • pp.55-63
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    • 1996
  • Epidote occurs as veinlets in the propylitic alteration zone of the Bobae clay deposit, Pusan, Korea. Its cell parameters apparently decrease with the contents of Al, Fe, and Ca. Fourier transform infrared (FTIR) spectra show one hydrosyl environment related to AlM2 at 3357-3358 cm-1. In the mid-infrared region, the peaks at 950 and 1030 cm-1 sharper with increasing Al shifting to higher energy region. The peak at 885 cm-1 shifts slightly to a lower energy region with a decreasing intensity as the Fe content increases. In the far-IR region, epidote exhibits absorption bands at 120 and 140 cm-1, which are related to the Ca-O bonds in A-sites.M ssbauer spectra of epidote show that the isomer shifts of Fe3+ range from 0.36-0.37 at the M3 site and from 0.35-0.44 at M1 site. Fe2+ shows the isomer shift ranging from 1.11 to 1.13. Quadrupole splitting is 2.04 for Fe3+M3, 0.52-0.70 for Fe3+M1, and 2.61-2.70 for Fe2+M3. Calculation shows Fe3+M386-90.7%, Fe3+M12.5-3.6%, and Fe2+M35.8-11.4% of total iron, showing preferential distribution of Fe3+ in the M3 site. The Fe3+M3 content is between 0.486 and 0.513 per formula unit. in the Fe-rich epidote, less Fe3+ and more Fe2+ are accommodated in the M1 and M3 sites. Hence, the overall disorder increases as total Fe content increase. The ordering parameter of the Bobae epidote is 0.93-0.95, suggesting a disequilibrium state below 200$^{\circ}C$. The constant temperature over a long period may be essential for the transition from disordered state to equilibrium state, despite the possible variation in flux and composition of the hydrothermal fluid.

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