• 한국광물학회지
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• 제5권1호
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• pp.42-47
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• 1992

해남 성산광산에서 산출되는 명반석에서 나타나는 진동누대구조를 back-scattered electron(BSE) 상과 전자현미분석기를 이용하여 연구하였다. 이런 누대구조는 편광현미경 하에서는 관찰되지 않자만, BSE상에서는 아주 명확히 관찰된다. 전자현미분석에 의하면 이런 누대구조는 명반석 구조 내 A 자리에서 칼륨을 치환하는 나트륨의 양적인 차이에 의하여 생긴다는 것을 지시한다. BSE상에서 밝기가 증가함에 따라 칼륨의 양은 증가하지만, 나트륨의 양은 감소한다. 섬세한 작은 규모의 누대구조와 인접한 zone사이의 명확한 경계는 이런 진동누대구조가 성장하는 명반석 결정주변의 열수용액의 성분의 변화에 기인하여 형성된 것임을 가리킨다. 이러한 변화를 초래한 요인은 1) 유입되는 유체 성분의 변화 및 2) 보다 안정한, 나트륨이 적은 명반석의 따른 침전에 의한 용액성분의 변화일 것으로 생각된다.

• 한국광물학회지
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• 제12권1호
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• pp.11-22
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• 1999

Thermal behavior of dickite was studied by thermal analysis, X-ray diffraction analysis, electron microprobe analysis, and scanning electron microscopy, Dickite has an endothermic peak at about$ 650^{\circ}C$ and an exothermic one at $960^{\circ}C$ in the differential thermal analysis. The endothermic reaction is assigned to the decomposition of dickite to meta-dickite. Hydroxyl radicals are removed from dickite structure by the reaction, resulting in the weight loss about 10.5~14.5% and appearance of a 14$\AA$ phase different from other kaolin minerals. The reaction slowly proceed in the range of $200^{\circ}C$. As the completion of decomposition, aciclular mullite forms at the expense of meta-dickite plates with random crystallographic relationship. Mullites have diverse silica versus alumina ratio. The exothermic reaction without weight loss seems to be due to the formation of spinel and amorphous silica. The spinel phase shows cryptocrystalline globular morphology accompanying a little amount of silica. From spinel phase shows cryptocrystalling globular morphology accompanying a little amount of silica. From this work, it is suggested that mullite is formed from meta-dickite much lower temperature than the reported one in the previous works.

• Transactions on Electrical and Electronic Materials
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• 제8권5호
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• pp.211-214
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• 2007

Chemical and morphological changes of phenol formaldehyde-based photoresist after $O_2$ radiofrequency(RF) plasma treatment depending on exposure time and source power were investigated. It was found that etch rate of photoresist sharply increased after discharge turn on and reached a limit with increase in plasma exposure time. Contact angle measurements and X-ray photoelectron spectroscopy(XPS) analysis showed that the surface chemical structure become nearly constant after 15 sec of the treatment. Atomic force microprobe(AFM) measurements were shown that surface roughness was increased with plasma exposure time.

• Journal of Korean Society for Atmospheric Environment
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• 제24권E1호
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• pp.44-53
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• 2008

This study was undertaken to measure the properties of individual mineral particles in an artificially saturated atmosphere at a vertical extinct mine with 430 m height. By synchrotron radiation X-ray fluorescence (SR-XRF) microprobe analysis, it was possible to determine the elemental composition of residual insoluble particles on individual cloud droplet replicas formed on the Collodion film. The XRF visualized elemental maps enabled us not only to presume the chemical mixing state of particles retained in cloud droplet, but also to estimate their source. Details about the individual mineral particles captured by artificial cloud droplets should be helpful to understand about the removal characteristics of dust particles such as interaction with clouds. Nearly all individual particles captured in cloud droplets are strongly enriched in Fe. Mass of Fe is ranged between 41 fg and 360 fg with average 112 fg. There is a good agreement between single particle analysis by SR-XRF and bulk particle analysis by PIXE.

• Mass Spectrometry Letters
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• 제7권3호
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• pp.64-68
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• 2016

Scanning electron microscopy combined with thermal ionization mass spectrometry (SEM-TIMS) was used to determine the precise isotope ratios of ultra-trace levels of uranium contained in individual microparticles. An advanced multiple ion counter system consisting of three secondary ion multipliers and two compact discrete dynodes was used for complete simultaneous ion detection. For verification purposes, using TIMS with complete simultaneous measurement, isotopes were analyzed in 5 pg of uranium of a certified reference material. A microprobe in the SEM was used to transfer individual particles from a NUSIMEP-7 sample to TIMS filaments, which were then subjected to SEM-TIMS and complete simultaneous measurement. The excellent agreement in the resulting uranium isotope ratios with the certified NUSIMEP-7 values shows the validity of SEM-TIMS with complete simultaneous measurement for the analysis of uranium isotopes in individual particles. Further experimental study required for investigation of simultaneous measurement using the advanced multiple ion counter system is presented.

• 암석학회지
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• 제10권3호
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• pp.222-232
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• 2001

이차이온질량분석기는 고속으로 가속된 일차이온을 고체 시료 표면에 충돌시켜, 이차이온을 발생시킨 후 질량분석 장치를 통해 분석하는 장치이다. 시료에 충돌하는 일차이온빔의 크기를 마이크론 단위까지 줄여 미세영역에 대한 분석이 가능하므로 이온현미분석기라고도 불린다. 이차이온질량분석기의 정밀도와 정확도는 고전적인 질량분석기에 비해 떨어진다. 하지만, 극소량의 시료로 분석이 가능하며, 화학적 전처리 과정 없이 연마편을 이용하여 매우 좁은 영역에서 동위원소의 분포를 연구할 수 있다는 장점이 있다. 지구화학/우주화학 분야에서 이차이온질량분석기의 활용은 최근 급속히 증가하고 있으며, 주로 (1) 수소, 탄소, 산소, 황 등의 안정동위원소 연구, (2) 함 우라늄/토륨 광물의 절대연령측정, (3) 광물 내 미량원소의 분포 연구, (4) 선태양계 광물 발견 및 이들의 동위원소 연구 등에 사용되고 있다.

• 암석학회지
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• 제2권2호
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• pp.63-73
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• 1993

The assemblage epidote and grandite garnet occurs in low-to medium-grade metabasites and calc schists of various geotectonic settings and in hydrothermally altered calcareous rocks in skarn deposits. The compositions of sixteen epidote-garnet paris have been analysed by means of electron microprobe. Al-Fe partitioning between coexisting grandite garnet and epidote is considered and measured at the grain boundaries on the supposition that the surface equilibrium was maintained in the following exchange reaction: 2$Ca_2Al_3Si_3O_12$(OH)+$Ca_3Fe_2Si_3O_12$=2$Ca_2A_l2FeSi_3O_12$(OH)+$Ca_3Al_2Si_3O_12$ Partition coefficients confirms the differences in thermal conditions between low-grade and medium-grade metamorphic rocks. $K_D$ values ($X_{$CO_2$}$=($Fe^{+3}$/Al)$^{Ep}$/($Fe^{+3}$/Al)$^{Gr}$, where Fe=$Fe^{+3}$) from greenschist facies rocks of the estimated metamorphic temperatures, 330~$390^{\circ}C$, range approximately between 0.02 and 0.17. Epidote-amphibolite facies rocks and calcareous skarns of the estimated temperatures, 400~$550^{\circ}C$, have $K_D$ values between 0.24 and 0.37. $K_D$ values from the rocks of the temperatures, 640~$700^{\circ}C$, range nearly between 0.58 and 0.75. The diagrams in Figs. 2 and 3 can serve as a mineralogic thermometer for relatively shallow rocks, assuming that the pressure dependence of partition coefficients for the iron-exchange reaction in the two minerals can be neglected.

• 한국광물학회지
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• 제8권1호
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• pp.13-22
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• 1995

Phase relations of the Pd-Sb system were investigated using the sealed-capsule technique; the quenched run products were studied by reflected light microscopy, X-ray diffraction, and electron microprobe analysis. Eight binary phases were confirmed to exist in the system: Pd20Sb7, Pd31Sb12, Pd8Sb3 (mertieite II), Pd5Sb2, Pd2Sb, Pd5Sb3, PdSb (sudburyite), and PdSb2, (unnamed PdSb2), The X-ray powder diffraction data of all the phases, except for Pd5Sb3, however, may be indexable on an orthorhombic cell, space group Cmc2, with a=3.362(1), b=17.484(7), c=6.934(2)$\AA$. Some physical properties as well as re-determined cell parameters are newly established. A revised phase relations of the Pd-Sb system are presented.

• 한국수소및신에너지학회논문집
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• 제7권1호
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• pp.111-115
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• 1996

Metal atom rearrangement has been shown to take place under the influence of hydrogen-induced atomic diffusion (HIAD) in initially homogeneous fee palladiumalloys by electron microprobe analysis, optical microscopy, mechanical property tests and hydrogen isotherms. HIAD takes place in palladium alloys at moderate to elevated temperatures leading to phase segregation under conditions where segregation does not normally occur, i.e., in the absence of H over the time scale of the experiments. From these results, it is confirmed that dissolved hydrogen plays a dual role in some of these alloys, i.e. it catalyzes metal atom diffusion. This research demonstrates the potential utility of employing H-induced changes for phase diagram determination of Pd alloys and possibly for other alloy system.

• 대한의용생체공학회:학술대회논문집
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• 대한의용생체공학회 1989년도 춘계학술대회
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• pp.9-12
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• 1989

A preliminary study has been conducted to demonstrate the effect of laser heat treatment on Ni Ti alloy dental arch wires ($0.016"\;{\times}\;0.022"$ and $0.018"\;{\times}\;0.026"$, rectangular shape). Changes in mechanical and thermal properties and surface morphologies are investigated by using optical and scanning electron microscope (SEM), energy dispersive x-ray microprobe analysis(EDX), differential scanning calorimeter (DSC), and micro hardness tester. The results indicate that the laser can affect the thermal equilibrium state of the localized surface. Titanium rich surface film is formed by the laser treatment. The surface film and rapidly resolidified underlying structures show better chemical resistance than the matrix material. Phase transition temperatures which are related to shape recovery temperatures are changed after laser treatment. Hardness of resolidified area and heat affected zone are lower than before treatment.