• Journal of Magnetics
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• 제11권1호
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• pp.16-19
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• 2006

$2-\mu{m}$ thick GaN epilayer was prepared, and 80 KeV $Co^{-}$ ions with a dose of $3X10^{16}\;cm^{-2}$ were implanted into GaN at $350^{\circ}C$. The implanted samples were post annealed at $700^{\circ}C$. We have investigated the magnetic and structural properties of Co ion-implanted GaN by various measurements. HRXRD results did not show any peaks associated with second phase formation and only the diffraction from the GaN layer and substrate structure were observed. SIMS profiles of Co implanted into GaN before and after annealing at $700^{\circ}C$ have shown a projected range of $\sim390\AA$ with 7.4% concentration and that there is little movement in Co. AFM measurement shows the form of surface craters for $700^{\circ}C$-annealed samples. The magnetization curve and temperature dependence of magnetization taken in zero-field-cooling (ZFC) and field-cooling (FC) conditions showed the features of superparamagnetic system in film. XPS measurement showed the metallic Co 2p core levels spectra for $700^{\circ}C$-annealed samples. From this, it could be explained that magnetic property of our films originated from Co magnetic clusters.

• 한국광물학회지
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• 제10권2호
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• pp.148-161
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• 1997

Based on the X-ray powder diffraction (XRD) and M ssbauer spectroscopy, the thermal behavior and phase transformations of two clays are investigated for raw and fired conditions, which are collected from Kwangryeongli and Ildo district in Cheju Island. M ssbauer spectra at room temperature and 20for two clays show that paramagnetic Fe3- is the structural iron of the layer silicate and ferrihydrite, and superparamagnetic goethite has about 50% of total iron contents. The XRD peaks of hematite for the fired clays appear from 80$0^{\circ}C$ in Kwangryeongli clay and from $600^{\circ}C$ in Ildo district clay, respectively. The structural Fe2+ was completely oxidized into Fe3- at 40$0^{\circ}C$ for Kwangryeongli clay and 50$0^{\circ}C$~$600^{\circ}C$ for Ildo district clay, respectively. The structural Fe2+ was completely oxidized into Fe3- at 40$0^{\circ}C$. For the temperature ranging from 40$0^{\circ}C$ to $700^{\circ}C$~80$0^{\circ}C$, two fired clays exhibit the dehydroxylation of the clay mineral. A disintegration of the clay mineral structure is observed from $700^{\circ}C$~80$0^{\circ}C$ to 110$0^{\circ}C$, followed by the onset and spread of vitrification process. It is also shown that well-crystallized hematite phase is formed at the temperature higher than 110$0^{\circ}C$ and the relative absorption area decreases, which might be related to the recrystallization of alluminosilicate matrix.

• 자원환경지질
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• 제31권4호
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• pp.311-324
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• 1998

Paleomagnetic study is carried out to investigate the possibility of remagnetization by dikes in the Cretaceous Gyeongsang Basin. We selected a site for a contact test as a preliminary study, and collected 41 core samples (7 from andesitic dike, 17 from sedimentary rock on the left side of dike and 17 from sedimentary rock on the right side). Magnetite was responsible for the remagnetization based on microscopic observation and demagnetization analysis. Although the increasement of magnetic susceptibility appears on both sides about 100 cm from the dike, the increment of NRM intensity was obtained from the specimens on the left side only. This is interpreted that the size of magnetite newly formed is dominated by superparamagnetic grains in the right side, but by larger than single-domain grains in the left. Reversed polarity component remagnetized by intrusion of dike was also found only for core samples from 116 cm left side of dike but abscent from right side indicating the remagnetization by the dike depends on the geometric shape and width of the dike, which is supported by field observations. The content of epidote is well correlated with remagnetization, and indicates the hydrothermal alteration/metameorphism was activated by the intrusion. We concluded that the above evidences in this study further support thermally-activated chemical origin of the remagnetization with meager contribution of contact metamorphism, and that any significant evidence of regional-scaled remagnetization was not found in the study area.

• 한국분말재료학회지
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• 제9권6호
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• pp.422-432
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• 2002

Mechanically driven decomposition of intermetallics during mechanical milling(MM 1 was investigated. This process for Fe-Ce and Fe-Sn system was studied using conventional XRD, DSC, magnetization and alternative current susceptibility measurements. Mechanical alloying and milling form products of the following composition (in sequence of increasing Gecontent): $\alpha$(${\alpha}_1$) bcc solid solution, $\alpha$+$\beta$-phase ($Fe_{2-x}Ge$), $\beta$-phase, $\beta$+FeGe(B20), FeGE(B20), FeGe(B20)+$FeGe_2$,$FeGe_2$,$FeGe_2$+Ge, Ge. Incongruently melting intermetallics $Fe_6Ge_5$ and $Fe_2Ge_3$ decompose under milling. $Fe_6Ge_5$ produces mixture of $\hat{a}$-phase and FeGe(B20), $Fe_2Ge_3$ produces mixture of FeGe(B20) and $FeGe_2$ phases. These facts are in good agreement with the model that implies local melting as a mechanism of new phase for-mation during medchanical alloying. Stability of FeGe(B20) phase, which is also incongruently melting compound, is explained as a result of highest density of this phase in Fe-Ge system. Under mechanical milling (MM) in planetary ball mill, FeSn intermetallic decomposes with formation $Fe_5Sn_3$ and $FeSn_2$ phases, which have the biggest density among the phases of Fe-Sn system. If decomposition degree of FeSn is relatively small(<60%), milled powder shows superparamagnetic behavior at room temperature. For this case, magnetization curves can be fitted by superposition of two Langevin functions. particle sizes for ferromagnetic $Fe_5Sn_3$ phase determined from fitting parameters are in good agreement with crystalline sizes determined from XRD data and remiain approximately chageless during MM. The decomposition of FeSn is attributed to the effects of local temperature and local pressure produced by ball collisions.

• Investigative Magnetic Resonance Imaging
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• 제19권1호
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• pp.37-46
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• 2015

Purpose: This report compared the diagnostic effectiveness between ultrasmall superparamagnetic iron oxide (USPIO) and gadolinium (Gd) based magnetic resonance imaging (MRI) for differentiation of axillary status in breast cancer patients. Materials and Methods: The present authors performed a meta-analysis of previous studies that compared USPIO or Gd based MRI with histological diagnosis after surgery or biopsy. We searched PubMed, EMBASE, Cochrane Library, ScienceDirect, SpringerLink, Ovid databases and references of articles to identify studies reporting data until December 2013. Pooled sensitivity and specificity were calculated for every study; summary receiver operating characteristic and subgroup analysis was done. Analyses of study quality and heterogeneity were also assessed. Results: There were 14 publications that met the criteria for inclusion in our meta-analysis. USPIO based MRI showed 0.83 (95% CI: 0.75-0.89) and 0.97 (95% CI: 0.94-0.98) for pooled sensitivity and specificity, respectively. Gd based MRI represented pooled sensitivity and specificity of 0.61 (95% CI: 0.55-0.67) and 0.90 (95% CI: 0.87-0.92) for each. Overall weighted area under the curve for USPIO and Gd based MRI were 0.9563 and 0.9051, respectively. Conclusion: USPIO based MRI had a tendency toward high pooled sensitivity and specificity in detection of axillary metastases for breast cancer. This result may mean that USPIO based MRI could be used as complementary modality to differentiate axillary status more precisely, and assist in the decision-making process regarding possible invasive procedures, such as sentinel node biopsy.

• 한국자기학회지
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• 제24권5호
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• pp.135-139
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• 2014

물리적 기상합성법인 전기선폭발법을 이용하여 챔버내 산소분압을 바꾸면서 철산화물을 제조하였다. 제조된 철산화물은 산소 분압에 따라 $Fe_2O_3$ 및 $Fe_3O_4$상으로 제조되었다. 산소분압이 30 %인 경우 ${\gamma}-Fe_2O_3$와 ${\alpha}-Fe_2O_3$와 같이 $Fe^{3+}$의 형성이 용이함을 확인 하였다. 산소 분압을 15 %로 줄이면 $Fe_3O_4$가 형성되어 $Fe^{2+}$ 이온을 확인할 수 있었다. 뫼스바우어분광분석을 활용하여 ${\gamma}-Fe_2O_3$와 $Fe_3O_4$상 분석을 수행하였다. 13 K에서 295 K까지의 뫼스바우어 스펙트럼으로부터 자기정렬구조가 사라진 면적비로부터 약 12 % 정도의 ${\gamma}-Fe_2O_3$상이 초상자성 특성을 보임을 확인하였다.

• 한국자기학회지
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• 제26권6호
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• pp.190-195
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• 2016

본 연구에서는 분산제 및 산화제를 전혀 첨가하지 않은 채 고압 균질기를 사용하여 $Fe(OH)_2$ 현탁액으로부터 합성된 마그네타이트 나노입자의 자기 특성에 미치는 공정 압력의 영향을 체계적으로 조사하였다. 관측된 X-선 회절 패턴으로부터 모든 나노입자가 마그네타이트의 역스피넬 구조를 가진다는 것을 알 수 있었다. X-선 회절 및 투과전자현미경 분석 결과로부터 마그네타이트 나노입자의 평균 입자 크기는 고압 균질화 과정의 공정 압력에 의해 조절될 수 있는 것으로 드러났다. 평균 입자 크기는 21에서 26 nm에 이르며, 공정 압력이 증가함에 따라 감소하는 것으로 밝혀졌다. 시료진동형 자화율 측정기를 사용하여 상온에서 측정된 자기 이력 곡선으로부터 1500 bar의 공정 압력 조건에서 합성된 마그네타이트 나노분말이 초상자성 거동을 나타내는 것을확인할 수 있었다.

• 한국자기학회지
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• 제5권1호
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• pp.48-53
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• 1995

동시 열진공증착한 Ag-Co 미세입상 합금박막의 구조, 자기적 성질 및 거대자기저항 현상에 관하여 연구하였다. 증착된 상태에서 합금박막은 과포화된 Ag 기지와 석출된 Co 입자들이 공존하는 준안정한 fcc 구조를 이루고 있다. Co의 양이 20에서 55 at.%로 증가함에 따라 Ag 기지의 입자크기는 평균 147에서 $67{\AA}$으로 감소하였고 Ag 기지에 Co의 고용량은 2.5에서 6.7%로 증가하였다. 25 at.% 이하의 조성을 갖는 합금박막은 주로 초상자성 특성을 보였으며 그 이상의 조성에서는 초상자성과 강자성이 혼합된 거동을 보였다. 증착된 상태의 30 at.% 합금 박막에서(상온, 10 kOe) 최대 19%의 자기저항비를 얻었다. 증착된 상태에서 대부분의 코발트가 석출되어 있기 때문에 Cu-Co계와는 달리 열처리에 의해 MR비의 증가는 보이 지 않았다.

• 폴리머
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• 제30권5호
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• pp.412-416
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• 2006

$FeCl_3$와 $Na_2SO_3,\;NH_4OH$에 의해 제조된 나노 자철광은 강자성체로 화학 흡착에 의해 형성된 표면의 수산기에 의해 표면전하가 변하는 특성이 있다. 본 연구는 이런 나노 자철광을 함유한 poly(acrylic acid) (PAAc) 수화젤의 물성에 대하여 연구하였다. 나노 자철광의 특성은 XRD, AFM, FTIR로 측정하였다. 나노 자철광 표면의 제타전위는 pH 변화에 의해 큰 영향을 받았으며, pH 4 이하에서는 높은(+)전위를 나타내었으며, 등전점은 pH 7에서 확인되었다. pH 4 이하에서 나노 자철광 콜로이드를 PAAc 수화젤에 함유시키면, 강력한 수소결합이 형성되어 젤의 인장강도는 증가하고, 신율 및 팽윤비는 감소하여 기계적인 물성이 증가하였다. 나노 자철광의 함량에 비례하여 나노 자철광을 함유한 PAAc 수화젤의 자기이력은 증가하였다.

• 접착 및 계면
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• 제14권2호
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• pp.82-87
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• 2013

본 연구에서는 레졸, 질산철 그리고 트리블럭 공중합체를 이용하여 직접 탄화과정에 의해 자성체 나노입자가 분산된 탄소나노세공체를 합성하였다. 나노세공 마그네타이트/카본($Fe_3O_4$/carbon) 나노복합체는 낮은 마그네타이트 함량(1 wt%)을 가지고 잘 배열된 이차원적 육방체 구조(p6mm)를 보이며, 균일한 세공크기(3.6 nm), 높은 표면적(635 $m^2/g$)과 세공부피(0.48 $cm^3/g$)를 가진다. 작은 입자크기(10.2 nm)를 가지는 마그네타이트 나노입자는 초상자기성(7.7 emu/g)을 보이고 탄소 세공벽 내에 잘 분산되었다. 나노세공 마그네타이트/카본 물질은 최대 995 mg/g의 아이부프로펜 흡착량을 보였다. 또한, 자석을 이용하여 용액과 나노세공 마그네타이트/카본 물질의 분리가 용이하였다. 본 연구에서 제조된 나노복합체는 우수한 아이부프로펜 흡착제로 작용하였다.