• 한국결정성장학회지
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• 제21권5호
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• pp.210-213
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• 2011

$P_2O_5$ 함량에 따른 $5Na_2O-36CaO-10TiO_2-xP_2O_5$으로 구성된 glass-ceramic을 다음과 같은 방법으로 제조하였다: 1) 1 N HCl 용액 내에서 $Ca_3(PO_4)_2$와 $NaTi_2(PO_4)_3$ 간의 $Ca_3(PO_4)_2$ 결정을 2일간 추출하여 제거함. 2) Ag($NO_3$) 용액에서 1일간 $Na^+$ 이온을 $Ag^+$ 이온으로 이온 교환시킴. Glass-ceramic의 합성 여부를 SEM 및 XRD를 이용하여 확인하였다. Staphylococus aureus를 이용한 박테리아 실험 결과 3시간 이후에는 완전하게 박테리아가 제거됨을 확인할 수 있었다.

• 한국산학기술학회:학술대회논문집
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• 한국산학기술학회 2008년도 추계학술발표논문집
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• pp.90-92
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• 2008

본 논문에서는$xAg_2O$-(5-x)$Na_2O$-36CaO-$10TiO_2$-$19.5P_2O_5$ (mol ratio)의 유리조성으로부터 $Ag_2O$의 함량을 변화시켜 유리의 제조 및 특성평가를 하였다. 제조된 유리는 TG-DSC를 통하여 열적특성을 관찰하였으며, 항균특성은 staphylococcus aureus균주에 대하여 항균특성을 평가하였다. 평가결과 열적특성은 $Ag_2O$함량이 증가할수록 결정화온도가 낮아짐이 관찰되었고, 항균특성 역시 $Ag_2O$성분의 함량이 증가 할수록 항균특성이 증가하는 것으로 관찰되었다.

• 동굴
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• 제74호
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• pp.23-31
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• 2006

(1) Kaeusetgul Cave in Kimnyong-Ri, Jeju-Do, Korea. Kaeuset-gul Cave (KC) is situated in NNE area of the Manjang-gul cave (125m a.s.l.). Kaeuset-gul Cave lies at $126^{\circ}45'22"$ E in longitude and $33^{\circ}33'09"$ N in latitude. The coast belong Kimnyeong-Ri, Kujwa-eup, Jeju-Do. Altitude of the cave-entrance is 10m and length of the cave is 90m. Lava hand-specimens of KC are studied by X-ray fluorescence analysis (XRF). Average major chemical components of specimens from KC is as follows (wt.%); $SiO_2=47.03$, $TiO_2=3.16$, $Al_2O_3=18.41$, FeO*=13.53, MnO=0.14, MgO=5.05, CaO=8.66, $Na_2O=2.81$, $K_2O=0.67$, $P_2O_5=0.55$ in KC. Polarizing microscopic studyindicates that these specimens are described of alkali-basalt. (2) Tachibori Fuketsu (Cave) in Shizuoka Prefecture, Fuji Volcano, Japan Tachibori Fuketsu lies attoward the south in skirt of the Fuji volcano, $138^{\circ}42'04"$ east longitude and $35^{\circ}18'00"$ north latitude. The location of cave entrance is 2745, Awakura, Fujinomiya-shi, Shizuoka Prefecture. The above sea level and length of Tachibori Fuketsu are 1,170m and 82m. Average major chemical components of specimens from cave areas follows (Total 100 wt.%) ; ($SiO_2$=50.52, $TiO_2$=1.69, $Al_2O_3$=15.47, FeO*=13.13, MnO=0.20, MgO=5.97, CaO=9.17, $Na_2O$=2.52, $K_2O$=0.94 and $P_2O_5=0.40).$ Polarizing microscopic study indicates that these specimens may belong to tholeiite-basalt series. According to polarizing microscopic study, Au (Augite), P1 (Plagioclase), and O1 (Olivine) are contained as phenocryst minerals. (3) Gorely Cave in Kamchatka Peninsula, Russia Gorely caldera is located at the southeastern part of Kamchatka Peninsula, about 75km southwest of Petropavlovsk-Kamchatskiy.. Gorely lava caves are situated in NHE area of Mt. Gorely volcano (1829m a.s.1.). One of lava cave (Go-9612=K-1) lies at $158^{\circ}00'22"$ east longitude and $52^{\circ}36'18"$ north latitude. The elevation of cave entrance is about 990m a.s.1. and the main cave extends in the NNW direction for about 50m by 15m wide and 5m in depth. The cave of K-3is near the K-1 cave. "@Lava hand-specimens K-1 and K-3 caves are studied by X-ray fluorescence analysis and polarizing microscopic observation. Average major chemical components of specimens from these caves are as follows (wt.%) ;($SiO_2$=55.12, $TiO_2$=1.25, $Al_2O_3$=16.07, T-FeO* =9.41, MnO=0.16, MgO=5.01, CaO=7.21, $Na_2O$=3.39, $K_2O$=1.92, $P_2O_5$=0.45) and these values indicate that the Gorely basaltic andesite belong to high alumina basalt. Polarizing microscopic study indicates that these specimens are described of Augite andesite.

• 자원환경지질
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• 제56권6호
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• pp.799-816
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• 2023

Mineralogical and geochemical studies of shales within the Lower Anambra Basin was conducted to unravel the depositional environment, provenance, maturity, paleo-weathering conditions, and tectonic settings. Mineralogical studies conducted using X-ray diffraction analysis revealed that the samples were composed of kaolinite, montmorillonite, chlorite, and illite. KaolinIite is the dominant mineral, constituting approximately 41.5% of the bulk composition, whereas the non-clay minerals are quartz, ilmenite, and sillimanite. Geochemical analysis showed a predominance of SiO₂, Al₂O₃, and Fe₂O₃ contents of the shale samples with mean values of 52.29%, 14.09%, and 6.15% for Imo Shale (IS); 52.31%, 16.70%, and 7.39% for Mamu Shale (MS); 43.21%, 21.33%, and 10.36% for Enugu Shale (ES); 53.35%, 15.64%, and 7.17% for Nkporo Shale (NS); and 51.24%, 17.25%, and 7.78% for Agwu Shale (AS). However, the shales were depleted in Na₂O, MgO, K₂O, MnO, TiO₂, CaO, and P₂O₅. The trace element ratios of Ni/Co and Cu/Zn of the shale suggest an oxic depositional environment. The average SiO₂ vs. Al₂O₃ ratio of the shales indicated textural maturity. Compared to the PAAS standard, the shales plot below the PAAS value of 0.85, suggesting a high degree of maturity and intensive chemical weathering, further confirmed on a CIA vs. PIA plot. On log (K₂O/Na₂O) against SiO₂ and tectonic setting discriminant function diagrams, the shales plot mostly in the field of passive continental margin tectonic setting. The discriminant function diagrams as well as Al₂O₃/TiO₂ ratio of the shales showed that they were derived from a mixed source (mafic and intermediate igneous rocks).

• 헤리티지:역사와 과학
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• 제46권4호
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• pp.108-125
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• 2013

경주 동천동 출토 토제범(土製范)에 대한 실측복원도, 조성광물 분석, 입도 및 물성시험, 미세조직관찰, 색도차 및 주성분 분석결과를 알아보았다. 연구대상 내범과 외범의 단면은 내측(제1층위)과 외측(제2층위)으로 구분되고 외측에는 유기물이 혼합되어 있다. 단면에는 열적 경험과 탈형제로 인한 변화 양상이 확인되며, X-선 촬영에서는 내측인 제1층위가 투과율이 높은 광물로 구성되었고 편광현미경에서 석영만이 관찰되었다. SEM 관찰에서 단면의 내측은 공극이 확대된 양상을 나타내고 중앙은 균열이 발달하였으며 외측에서는 변화를 관찰할 수 없었다. 구성입자의 입도는 내범과 외범이 거의 유사하며 미사질식양토로 구분되고, 미사질과 점토의 구성비는 약 2.7 : 1과 약 2.9 : 1이었다. 물성시험에서 내범과 외범의 밀도와 흡수율은 유사하고 공극률만이 내범이 27.36%와 외범은 31.09%로 다소 차이가 있었다. 단면의 색도차는 제1층위의 표면에 탈형을 위해 그을음을 입히거나 제1층위를 먹물로 수비하였을 가능성이 있다. 조성광물 분석에서는 내범과 외범의 조성광물이 동일하나 내범에서만 자철석이 동정되었다. 주성분 분석에서는 $SiO_2$의 평균함량이 71.64%, $Al_2O_3$는 14.59%이고, 부성분 중 $Fe_2O_3$는 4.51%, $K_2O$는 3.06%이며, $Na_2O$, MgO, CaO, $TiO_2$, $P_2O_5$, MnO는 2% 이하를 나타내었다.

• Journal of Korean Dental Science
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• 제11권2호
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• pp.71-81
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• 2018

Purpose: The purpose of this study was to investigate the corrosion behaviors of dental implant alloy after microsized surface modification in electrolytes containing Mn ion. Materials and Methods: $Mn-TiO_2$ coatings were prepared on the Ti-6Al-4V alloy for dental implants using a plasma electrolytic oxidation (PEO) method carried out in electrolytes containing different concentrations of Mn, namely, 0%, 5%, and 20%. Potentiodynamic method was employed to examine the corrosion behaviors, and the alternatingcurrent (AC) impedance behaviors were examined in 0.9% NaCl solution at $36.5^{\circ}C{\pm}1.0^{\circ}C$ using a potentiostat and an electrochemical impedance spectroscope. The potentiodynamic test was performed with a scanning rate of $1.667mV\;s^{-1}$ from -1,500 to 2,000 mV. A frequency range of $10^{-1}$ to $10^5Hz$ was used for the electrochemical impedance spectroscopy (EIS) measurements. The amplitude of the AC signal was 10 mV, and 5 points per decade were used. The morphology and structure of the samples were examined using field-emission scanning electron microscopy and thin-film X-ray diffraction. The elemental analysis was performed using energy-dispersive X-ray spectroscopy. Result: The PEO-treated surface exhibited an irregular pore shape, and the pore size and number of the pores increased with an increase in the Mn concentration. For the PEO-treated surface, a higher corrosion current density ($I_{corr}$) and a lower corrosion potential ($E_{corr}$) was obtained as compared to that of the bulk surface. However, the current density in the passive regions ($I_{pass}$) was found to be more stable for the PEO-treated surface than that of the bulk surface. As the Mn concentration increased, the capacitance values of the outer porous layer and the barrier layer decreased, and the polarization resistance of the barrier layers increased. In the case of the Mn/Ca-P coatings, the corroded surface was found to be covered with corrosion products. Conclusion: It is confirmed that corrosion resistance and polarization resistance of PEO-treated alloy increased as Mn content increased, and PEO-treated surface showed lower current density in the passive region.