• Journal of the Mineralogical Society of Korea
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• v.20 no.3
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• pp.223-229
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• 2007

The mechanism of hydrothermally synthesizing Na-A zeolite from siliceous mudstone at a $Na_2O/SiO_2$ ratio of 0.6, a $SiO_2/Al_2O_3$ 2.0 and a $H_2O/Na_2O$ 119 has been observed by IR, DTA, XRD and SEM. This mudstone is a tertiary periodic sedimentary rock and widely spreads around the Pohang area. In the early hydrothermal synthesis at $80^{\circ}C$ in an autoclave, sodium silicate and sodium aluminate were found to be preferentially reacted to generate Na-A type zeolite. Gibbsite and bayerite were also formed due to the presence of extra aluminum oxide in the feedstock. As reaction time in-creased up to 50 h, residual sodium aluminatewas reacted with siliceous mudstone, causing the Na-A zeolite crystal to grow and the hydroxylsodalite to generate. Therefore, in the $14{\sim}50\;h$ synthetic time, Na-A zeolite and hydroxylsodalite were formed. Also, if reaction time passed over 50 h, a part of the Na-A zeolite was finally redissolved and reacted with hydroxylsodalite to synthesize Na-P zeolite, generating porous surface of Na-A zeolite and disappearing hydroxylsodalite.

• Journal of the Mineralogical Society of Korea
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• v.29 no.3
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• pp.89-101
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• 2016

This study investigated spectral characteristics of heavy metal contaminated soil samples in the vicinity of abandoned Boksu mine. Heavy metal concentrations including arsenic, lead, zinc, copper and cadmium were analyzed by XRF analysis. As a result, all of the soil samples excluding control sample were over-contaminated based on the counter measure standard. The XRD results revealed that quartz, kaolinite and smectite were detected for all of the soil samples and heavy metals in soil were adsorbed on clay minerals such as kaolinite and smectite. The spectral analyses confirmed that spectral reflectance of near-infrared and shorter portion of shortwave-infrared spectrum decreases as heavy metal concentration increases. Moreover, absorption depths at 2312 nm and 2380 nm, the absorption features of clay minerals, decreases with higher heavy metal concentration indicating adsorption of heavy metal ions with clay minerals. It indicates that spectral features and heavy metal contamination of soil samples have high correlations.

• Journal of the Mineralogical Society of Korea
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• v.6 no.1
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• pp.17-26
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• 1993

Mineralogical characteristics of tosudite from the Sungsan and Bubson mines were studied and correlated using X-ray diffraction analysis, chemical analysis and electron microscopy. Tosudite occurs as an alteration product of Cretaceous volcanoclastic rocks in both mines. It is associated with microcrystalline quartz, dickite, illite/smectite or mica/smectite mixed-layer mineral. It forms cryptocrystalline aggregates with flaky habit. XRD analysis suggests that tosudite is an 1:1regularly interstratified dioctahedral smetite/dioctahedral chlorite. Bubsoo tosudite has more(00ℓ ) reflections and more periodice stacking sequence than Syngsan tosudite. Chemical analysis shows that tosudite is a Li-bearing aluminous 1:1 regularly interstrattified mineral composed of K-bedellite and donbassite. Cookeite component may be present in the chlorite layer. Bubsoo tosudite is more Al in tetrahedral site and Ca in interlayer, but less Al in octahedral site than Sugsan tosudite. Tosudite may be formed as the intermediate alteration products, forming after muscovite and before illite/smectite or mica/s$^{\circ}C$mectite, with the range from 100 $^{\circ}C$ to 360 ~ 480 $^{\circ}C$. The hydrothermal solution forming tosudite may be acidic solution with high activities of Si and Al.

• Journal of the Mineralogical Society of Korea
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• v.30 no.1
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• pp.31-43
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• 2017

This study investigated mineralogy, spectral characteristics and heavy metal contamination including Cd, Ni, Al, Fe, Mn and S for white precipitation in Miin falls based on XRF, XRD, and spectrometer. As a result, Al concentration was abnormally high at all samples, and most of the samples showed high contamination level in Cd and Ni. XRD results detected quartz, kaolinite, rhomboclase, aluminocoquimbite, and gibbsite which infers that heavy metal elements are distributed by adsorption with clay minerals. Spectral characteristics of white precipitation can be described by increasing pattern of reflectance in visible spectrum and decreasing pattern of reflectance in longer wave length including near infrared and shortwave infrared spectrum. The absorption features reveals that spectral characteristics of white precipitation is mainly controlled by kaolinite, rhomboclase, aluminocoquimbite, and gibbsite. The relationship between heavy metal concentration and absorption depth showed high positive correlation for Al concentration and absorption feature at 2202 nm of Al-OH absorption. This spectral characteristics indicates that absorption depth could be effectively used for estimation of heavy metal concentration.

• Journal of the Korean Magnetics Society
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• v.2 no.3
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• pp.251-256
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• 1992

Artificial superlattices of Co/Pd were prepared by RF magnetron sputtering Multilayered structure and compositional modulation were analyzed with a side angle x-ray diffractometer. It has been found that expansion of Co lattice occured in this artificial superlattice due to the lattice mismatch between Co and Pd. Perpendicular magnetic anisotropy could be observed when the Co layer thickness became less than 8${\AA}$ and maximum coercivity of 2350 Oe could be obtained in [Co(2.5 ${\AA}$)/Pd(9.3 ${\AA})]_{50}$/Pd$(200\;{\AA})$ with a perfect squareness of magnetic hysteresis loop. Characteristic of perpendicular magnetic anisotropy in Co/Pd superlattices could be related to the expansion of Co lattice caused by Pd layer and it turned out that as the thickness of Pd layer increased, perpendicular magnetic anisotropy increased. The interface anisotropy energy and volume anisotropy energy were calculated to be 0.29 ergs/$cm^2$ and -$6.9{\times}10^6$ ergs/$cm^3$ respectively, which are consistent with the values reported elsewhere.

• Proceedings of the Korean Vacuum Society Conference
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• 2012.08a
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• pp.398-398
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• 2012

SnO2 나노세선은 n-형 전기적 성질과 화학적인 안정성 때문에 가스센서, 투명 전극 및 태양전지와 같은 전자소자와 광소자에 널리 사용되고 있다. 화학 기상 증착, 전자빔 증착과 전기화학증착법을 사용하여 SnO2 나노세선을 제작하고 있다. 여러 가지 증착 방법중에서 전기화학증착방법은 낮은 온도와 진공 공정이 필요하지 않으며 대면적 공정이 가능하고 빠른 성장 속도로 나노구조를 효과적으로 성장할 수 있는 장점을 가지고 있다. 본 연구에서는 전기화학증착법을 이용하여 Indium Tin Oxide (ITO) 기판 위에 SnO2 나노세선 성장하고 성장시간에 따라 형성한 SnO2 나노세선의 구조적 성질을 조사하였다. SnO2 나노세선을 성장하기 위하여 D.I. water와 Entanol을 7:3의 비율로 섞은 용액을 $65^{\circ}C$로 유지하였고, 0.015 M의 Tin chloride pentahydrate ($Cl4{\cdot}Sn{\cdot}5H2O$)를 타겟 물질로 이용하였고, 0.1 M의 Potassium chloride (KCl)를 완충 물질로 사용하였다. 전기화학증착 방법을 사용하여 제작한 ITO 기판위에 성장한 SnO2 나노세선 위에 전극을 제작하고 전류-전압 특성을 측정하였다. SnO2 나노세선이 성장되는 전기화학증착 전압을 1.2 V로 고정하고, 성장시간을 15분, 30분 및 1시간으로 변화하여 SnO2 나노세선의 구조적 특성을 분석하였다. X-선회절 (X-ray diffraction; XRD) 실험 결과는 $31^{\circ}$에서 (101) 성장방향을 갖는 SnO2 나노세선이 성장함을 확인하였고, 성장 시간이 길어짐에 따라(101) 성장방향의 XRD 피크의 intensity가 증가하였다. 전기화학증착 성장 시간이 길어짐에 따라 SnO2 나노세선의 지름이 60 nm에서 150 nm로 변화하는 것을 주사전자현미경으로 관측하였다. 이 실험 결과는 전기화학증착방법을 사용하여 제작한 SnO2 나노세선의 성장 시간에 따른 구조적 특성들을 최적화하여 소자제작에 응용하는데 도움이 된다.

• Korean Chemical Engineering Research
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• v.49 no.3
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• pp.301-305
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• 2011

ABS/silicate composites with different clay types and compositions were prepared by in situ emulsion polymerization. The chemical structure of ABS was confirmed by the change of C-H stretching peak(near 3000 $cm^{-1}$) in fourier transform-infrared(FT-IR) spectrum. The thermal properties of the ABS/silicate composites were investigated by differential scanning calorimetry(DSC) and thermogravimetric analyzer(TGA). There was no distinct change in glass transition temperature of the ABS/silicate composites with different clay types. TGA curve indicates a dramatic increase in degradation temperature in case of ABS/20A composite with 3 wt% 20A. The silicate dispersion in the composites was measured by X-ray diffraction(XRD). The silicate dispersion in ABS/20A composites depended on the 20A composition. XRD results showed that the diffraction peak of the ABS/20A composite appeared when the content of 20A was higher than 5 wt%.

• Journal of the Mineralogical Society of Korea
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• v.27 no.4
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• pp.293-299
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• 2014

The bentonite, a buffer material, is essential for the deep geological disposal of HLW (high-level radioactive waste), and it is important to know its characteristic long-term evolution in the underground environment. With an assumption that the concentration of aqueous copper ions will increase if copper-coated materials on a metal canister are corroded, we examined some characteristic ion-exchanges and cation release phenomena occurring in the bentonite clay (montmorillonite) interacted with aqueous Cu cations. During the interaction between dissolved copper and bentonite, Na rather than Ca cations in the expandable clay were preferentially replaced by Cu ions in the experiment. In addition, the Cu-exchanged montmorillonite was characterized by an asymmetric X-ray diffracted pattern with relatively collapsed interlayers compared to the raw sample. These results indicate that the gradual change of the original bentonite property may occur in a underground disposal condition. We are going to further study the characteristic chemical and mineralogical changes of the bentonite buffer to be used for the disposal site by conducting additional experiments.

• Korean Journal of Soil Science and Fertilizer
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• v.36 no.6
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• pp.357-366
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• 2003

This study was conducted to develop n convenient and efficient granular type absorbent with high CEC from powdery zeolite, which is a waste produced while crushing the natural zeolite of Korea to get a particular particle size. The change of mineralogical characteristics during hydrothermal alternation of natural zeolite to Na-P zeolite in alkaline solution at various reaction times was determined by X-ray diffraction (XRD), scanning electron microscopy (SEM), and total elemental analysis. The columnar aggregate of Na-P Zeolite was produced by calcinating the natural zeolite-charcoal extrudates of about 3 mm diameter. In 24 hours reaction, clinoptillonite, mordenite and feldspar in natural zeolite were disappeared by 3 N NaOH treatment, while Na-P Zeolite with spherical granular structure was newly detected by XRD. As increasing reaction time, Si/Al ratio in remaining solution was deceased. The CEC of the synthesized material increased more than 2 times compared with that of natural zeolite, although the diameter of Na-P zeolite were rather increased.

• Proceedings of the Korean Vacuum Society Conference
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• 2013.08a
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• pp.261.2-261.2
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• 2013

에너지 갭이 큰 ZnO 반도체는 빛 투과율이 우수하여 투명성이 좋으며 화학적으로 안정된 구조를 가지고 있어 전자소자 및 광소자 응용에 대단히 유용하다. 일반적으로 화학 기상증착, 전자빔증착과 전기화학증착법을 사용하여 ZnO 나노 구조를 제작하고 있다. 여러 가지 증착 방법 중에서 전기화학증착방법은 낮은 온도와 진공 공정이 필요하지 않으며 대면적 공정이 가능하고 빠른 성장 속도로 나노구조를 효과적으로 성장할 수 있는 장점을 가지고 있다. 본 연구에서는 전기화학증착법을 이용하여 Indium Tin Oxide (ITO) 기판위에 Al 도핑된 ZnO 나노세선 성장시키고 성장시간에 따라 형성한 ZnO 나노세선의 구조적 성질을 조사하였다. ZnO 나노세선을 성장하기 위하여 zinc nitrate와 potassium chloride를 각각 0.1 M을 용해한 용액을 사용하였다. 전기화학증착방법을 사용하여 제작한 ITO 기판 위에 성장시킨 ZnO 나노세선 위에 전극을 제작하고 전류-전압 특성을 측정하였다. Al-doped ZnO 나노세선의 성장되는 조건을 Al 농도별로 0 wt%, 1 wt%, 2 wt% 및 5 wt% 씩 증가시키면서 ZnO 나노세선의 구조적 특성을 분석하였다. X-선회절 (X-ray diffraction; XRD) 실험 결과를 통해 ZnO 나노세선이 성장함을 확인하였고, 성장 시간이 길어짐에 따라 (101) 성장방향의 XRD 피크의 세기가 증가하였다. 전기화학증착시 Al 도핑 농도 증가에 따라 ZnO 나노세선의 지름이 200 nm에서 300 nm로 변화하는 것을 주사전자현미경으로 관측하였다. 이 실험 결과는 전기화학증착방법을 사용하여 제작한 ZnO 나노세선의 Al 도핑 농도에 따른 구조적 특성들을 최적화하여 소자제작에 응용하는데 도움이 됨을 보여주고 있다.