• Journal of the Korean Magnetics Society
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• v.10 no.1
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• pp.16-21
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• 2000

Magnetic properties and crystallographic properties of $Cu_{0.95}Ge_{0.95}Fe_{0.1}O_3$ were studied by using x-ray diffraction, superconducting quantum interference device (SQUID) and Mossbauer spectroscopy. Our sample has orthorhombic structure and the lattice constants are a = 4.795 $\AA$, b = 8.472 $\AA$, c = 2.932 $\AA$. The spin-Peierls (SP) transition temperatures of our sample is 13 K. The Mossbauer spectra consisted with two Zeeman sextets and one doublet due to $Fe^{3+}$ions. The Zeeman sextets come from tetrahedral $Fe^{3+}$ions and the doublets come from octahedral $Fe^{3+}$ions. The jump up of magnetic hyperfine field of 2nd Zeeman sextet and the increasing of the values of quadrupole splitting and isomer shift of doublet below SP transition temperature could be interpreted related with the atomic displacements. The N el temperature is 715 K, the Debye temperature are 540 K for octahedral site and 380 K for tetrahedral site, respectively.

• Journal of the Korean Magnetics Society
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• v.7 no.5
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• pp.232-236
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• 1997

We have gone into details about the velocity calibration of sinusoidal mode for Mossbauer spectrometer. Since sinusoidal Mossbauer spectrometer has a ${\gamma}$-ray source that oscillates at the end of loudspeaker with the natural frequency. Doppler velocity is accurate and stable. From the analyzing Mossbauer spectra of $Fe_3O_4$ and U $Fe_3O_4$ (unbalanced $Fe_3O_4$), we have shown the power of correct velocity for sinusoidal mode.

• Korean Journal of Materials Research
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• v.6 no.11
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• pp.1107-1112
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• 1996

Ni를 Cd로 대치시켜 세라믹 소결법으로 합성한 Ni0.8Cd0.2Fe2O4 의 X-ray 회절선을 측정하여 구조를 확인하고, 형성된 결정체의 격자 상수를 조사하였다. 이 시료의 Mossbauer 스펙트럼을 80K-900K의 온도 영역에서 측정 분석하여 Mossbauer parameter의 온도 의존성과 Fe 이온에 대한 자료를 얻고, 이 자료를 토대로 Ni0.8Cd0.2Fe2O4 의 자기 전이 현상과 Curied 온도 Tc와 격자 비열 및 Debye 온도와 같은 물성을 조사하였다.

• Journal of the Korean Magnetics Society
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• v.8 no.3
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• pp.118-124
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• 1998

$Ni_{0.65}Zn_{0.35}Cu_{0.1}Fe{1.9}O_4$ has been studied with Mossbauer spectroscopy and X-ray diffraction. The crystal structure is found to be a cubic spinel with the lattice constant $a_0=8.390{\AA}$. Mossbauer spectra of $Ni_{0.65}Zn_{0.35}Cu_{0.1}Fe{1.9}O_4$ has been taken at various temperatures ranging from 12 K to 705 K. The isomer shift indicates that iron ions are ferric at tetrahedral [A] and octahedral sites [B], respectively. The Neel temperature is determined to be $T_N=705\;K$. As the temperature increases toward $T_N$ a systematic line broadening effect in the Mossbauer spectrum is observed and interpreted to originate from different temperature dependencies of the magnetic hyperfine fields at various iron sites. The quadrupole splitting just on $T_N$ is 0.41 mm/s whereas the quadrupole shift below $T_N$ vanishes. This implies that the orientation of the magnetic hyperfine field with respect to be principal axes of the electric field gradient is random.

• Journal of the Korean Magnetics Society
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• v.9 no.3
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• pp.143-148
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• 1999

Magnetic properties and crystallographic properties of $Cu_{1-x}Ge_{1-y}Fe_{x+y}O_3$ system were studied by using x-ray diffraction, superconducting quantum interference device (SQUID) and Mossbauer spectroscopy. All the samples have orthorhombic structure and the lattice constants some decreased as the substituted iron contents increasing. The spin-Peierls (SP) transition temperature of our samples are about 12.5 K and these temperatures lowered as increasing substituted iron contents. The Mossbauer spectra consisted with two Zeeman sextets and one doublet due to $Fe^{3+}$ ions. The jump up of magnetic hyperfine field of 2nd Zeeman sextet and the increasing of the values of quadrapole splitting and isomer shift of doublet below SP transition temperature could be interpreted with the variation of the superexchange interaction, the symmetry of lattice sites and the covalency of bonds due to the atomic displacements.

• Korean Journal of Materials Research
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• v.7 no.7
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• pp.618-622
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• 1997

상온에서 측정한 Cd$_{x}$Ni$_{1-x}$Fe$_{2}$O$_{4}$의 Mossbauer 스펙트럼은 조성비에 따라 x값이 0.4이하인 시료에서는 준강자성에 의한 여섯개의 공명 흡수선, x값이 0.5인 시료에서는 이완된 형태의 공명흡수선, 그리고 x값이 0.6시료인 상자성에 의한 두개의 공명 흡수선이 나타났다. Cd$_{x}$Ni$_{1-x}$Fe$_{2}$O$_{4}$의 x값이 0.4이하인 시료의 초미세 자기장(H$_{hf}$)과 x값이 0.6 이상인 시료의 사중극자 분열치 (Q.S.)는 Cd농도가 증가함에 따라 감소한다. 시료의자기적 성질에 따른 이성질체 이동치(I.S.)의 차이는 있으나, Ni와 Cd이온의 농도에 따른 뚜렷한 의존성은 나타나지 않았다.다.

• Journal of the Korean Magnetics Society
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• v.8 no.4
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• pp.192-197
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• 1998

The Mossbauer spectra of the $Ni_{1-x}Cd_xFeAlO_4$ system were investigated with the Cd content x at room temperature. The spectra of the samples exhibit various patterns as follows 1) superparmagnetic relaxation for 0$\leq$x$\leq$0.2, 2) ferrimagnetic sextet for 0.3$\leq$x$\leq$0.5, 3) ferromagnetic relaxation for x=0.6, 0.7, 4) paramagnetic doublet for 0.8$\leq$x$\leq$1, with the Cd content x. In the samples with x values from 0 to 0.2, the substituted $Cd^{2+}$ ions transfer the $Al^{3+}$ ions from A-site to B-site mainly. The superparamagnetic relaxation effect and the ferromagnetic relaxation effect are derived from the $Al^{3+}$, $Cd^{2+}$ respectively. The magnetic structure of the $Ni_{1-x}Cd_xFeAlO_4$ system was explained by the Yafet-Kittel model.

• Journal of the Korean Magnetics Society
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• v.10 no.4
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• pp.183-190
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• 2000

This study aims at making a research into the physical and chemical properties of the neolithic era potterys, which are unearthed from Gosanli, Sagaeli, Bukchonli, Samyangdong and Gonaili districts in Cheju Island, by using X-ray diffraction, X-ray fluorescence spectrometer and Mossbauer spectroscopy. This results are as follows. The principal component of five plain coarse pottery sherds by X-ray fluorescence spectrometer and X-ray diffraction spectrum at the room temperature is silicate mineral which is equal to SiO$_2$, and they also have a little magetite, hematite and goethite. The most existent Fe is Fe$\^$+3/ through Mossbauer spectroscopy analysis of plain coarse pottery sherds and it is presumed that the magnetic hyperfine splitting caused this result. The ratio of Fe$\^$2+//(Fe$\^$2+/+Fe$\^$3+/) is mostly zero by Mossbauer spectrum at the room temperature of plain coarse pottery sherds and it is thought because they were fired in the atmosphere.

• Journal of the Korean Magnetics Society
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• v.14 no.6
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• pp.219-223
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• 2004

L $i_{0.5}$F $e_{2.5-{\chi}}$R $h_{\chi}$ $O_4$ ($\chi$ = 0.25, 0.50, 0.75, 1.00) has been prepared by solid state reaction. Crystallographic and magnetic properties were investigated by Mossbauer spectroscopy, SQUID magnetometry, and x-ray diffraction. The crystal structure is found to be a cubic spinel structure with space group Fd3m for all the samples. The lattice constant $a_{0}$ increases from 8.3365 $\AA$ to 8.3932 $\AA$ with increasing Rh concentration $\chi$. The migration of Li ion has been confirmed by x-ray patterns and the results of applied field Mossbauer analysis. The temperature dependence of the absorption area of each site was analyzed with the Debye model for the recoil-free fraction. The Debye temperature for the octahedral sites is almost as large as for the tetrahedral sites, thereby suggesting similar inter-atomic binding forces for the octahedral and the tetrahedral sites. The saturated magnetic moment and the Mossbauer spectra taken at 4.2 K under the applied field (6 T) show that the spin structure of L $i_{0.5}$F $e_{2.5-{\chi}}$R $h_{\chi}$ $O_4$ is compatible with the collinear Neel Model.

• Journal of the Korean Magnetics Society
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• v.13 no.6
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• pp.226-230
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• 2003

In this study, we analyzed the volcanic rock and scoria samples taken from special sites of Jeju island in two ways at the room temperature. One is the analysis of the chemical composition using X-ray fluorescence spectrometer, the other is the analysis of minerals in the samples, oxidized iron's genus, valence state and magnetic properties using X-ray diffractometry and Mossbauer spectroscopy. We believe that the volcanic rock and scoria samples are chiefly made of silicate minerals, like SiO$_2$, and they also have olivine, pyroxene, ilmenite, hematite and magnetite. The major Fe fractions of the volcanic rock samples are 2+ charge state and those of the scoria samples are 3+ charge state.