• 대한화학회지
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• 제31권1호
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• pp.102-109
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• 1987

화학증착방법에 의해 dibutyl tin diacetate를 산소와 반응시켜 $SnO_2$박막을 slide glass에 증착시켜 각 조건에 형성된 $SnO_2$박막의 특성을 조사하였다. 본 연구에서 최적증착조건은 기판온도 420$^{\circ}C$, 증착시간 20분으로 나타났으며 증착속도는 증착시간이 증가함에 따라 증가하며 증착시간 25분이후에는 일정해졌으며 판저항의 값도 증착초기에는 감소하나 증착시간 20분이 지나면서 증가하였다. 증착온도 420$^{\circ}C$, 증착시간 20분에 형성된 박막은 두께 4000${\AA}$이며 가시광선 투과율이 90%이며 5800 ohms/${\square}$의 판저항을 가졌다. 그리고 산세척방법에 의해 표면처리한 기판과 반응기체중 수증기의 첨가는 더 좋은 특성의 투명전도성 $SnO_2$박막을 제조하는데 도움이됨을 알았다. 또한 증착막은 작은 구형의 입자들로 이루어져 있다는 것을 주사전자현미경으로 확인하였으며 X-선 회절 실험에 의해 rutile structure(tetragonal)를 갖는다는 것을 알 수 있었다.

• 한국재료학회지
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• 제12권5호
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• pp.334-340
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• 2002

$TiO_2$-coated fly ash was synthesized by dropping method of coating agent in order to get $TiO_2$ coating layer with high photocatalytic activity on the surface of coal fly ash. The properties of the $TiO_2$ coating layer such as morphology, crystal structure, crystal size and photocatalytic activity were compared with those of the $TiO_2$-coated fly ash prepared by the traditional method of precipitation. $TiCl_4$ aqueous solution was used as a titanium stock solution and $NH_4HCO_3$ was used as a precipitant. The $TiO_2$ coating layer obtained by dropping method of coating agent was more uniform than that coated by precipitation. However, the crystal of $TiO_2$ coated by dropping method of coating agent was easy to grow by heat treatment because of the small primary particle size and bulky morphology, and its photocatalytic activity was consequently lower than that of the $TiO_2$ coated by precipitation. The $TiO_2$ coating layer obtained by both methods had a crystal structure of anatase, and the temperature of phase transformation into rutile was 90$0^{\circ}C$. The minimum crystal size of $TiO_2$ for the highest photocatalytic activity was found to be about 10nm.

• 한국표면공학회지
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• 제37권6호
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• pp.307-312
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• 2004

Extensive efforts have been made in an attempt to utilize photocatalytic properties of $TiO_2$ in visible range. $TiO_2$ and TiO-N thin films were made by the DC reactive magnetron sputtering method at $300^{\circ}C$. Various gases (Ar, $O_2$ and $N_2$) were used and Ti target was impressed by 0.6 kW-5.8 kW power range. The hysteresis phenomenon of the $TiO_2$ thin film as a function of the discharge voltage characteristic was observed to be higher as applied power increases. That of TiO-N thin film was occurred at the 5.8 kW power. The cross section and surface roughness of thin films were observed by FE-SEM and AFM. Average surface roughness of TiO-N thin film was observed as $15.9\AA$ and that of $TiO_2$ as $13.2\AA$. The crystal phases of both $TiO_2$ and TiO-N thin films were found to be anatase structure. The atomic $\beta$-N (396 eV peak in N 1s XPS) was shown in the rutile crystal of TiO-N and was considered acting as the origin of wavelength shift to the visible light.

• 한국재료학회지
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• 제19권6호
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• pp.325-329
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• 2009

Titanium dioxide thin films were fabricated as hydrogen sensors and its sensing properties were tested. The titanium was deposited on a $SiO_2$/Si substrate by the DC magnetron sputtering method and was oxidized at an optimized temperature of $850^{\circ}C$ in air. The titanium film originally had smooth surface morphology, but the film agglomerated to nano-size grains when the temperature reached oxidation temperature where it formed titanium oxide with a rutile structure. The oxide thin film formed by grains of tens of nanometers size also showed many short cracks and voids between the grains. The response to 1% hydrogen gas was ${\sim}2{\times}10^6$ at the optimum sensing temperature of $200^{\circ}C$, and ${\sim}10^3$ at room temperature. This extremely high sensitivity of the thin film to hydrogen was due partly to the porous structure of the nano-sized sensing particles. Other sensor properties were also examined.

• 한국재료학회지
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• 제20권3호
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• pp.167-173
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• 2010

In this study, we used activated carbon (AC) and titanium oxysulfate as a titanium precursor to prepare carbon/titania composites. We then mixed it with bentonite in different ratios to make a carbon/titania/bentonite monolith for use in architecture bricks by using Phenolic rosin (PR) as a bonding agent. The physicochemical properties of the prepared composites were analyzed by BET surface area, scanning electron microscopy (SEM), X-ray diffraction (XRD), energy dispersive X-ray analysis (EDX), self-cleaning effect and bactericidal tests. The BET surface areas increased as the ratio of carbon/titania composites increased. The SEM microscopy showed that the $TiO_2$ and bentonite were coated on the surface of the AC. The XRD patterns showed a mixture structure of anatase and rutile of $TiO_2$ with a clear $SiO_2$ structure. The EDX spectra of the carbon/titania/bentonite monolith confirmed the presence of various elements, namely C, O, Ti and Si, as well as other, impure elements. Moreover, to determine the self-cleaning effect of the carbon/titania/bentonite monolith, we used methylene blue (MB, $C_{16}H_{18}N_3S{\cdot}Cl{\cdot}3H_2O$) in an aqueous solution under the irradiation of visible light. Accordingly, all of the samples had excellent degradation of the MB solution. Furthermore, it was observed that the composites with sunlight irradiation had a greater effect on E. coli than any other experimental conditions.

• Nano
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• 제13권10호
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• pp.1850124.1-1850124.12
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• 2018

$TiO_2$ films were deposited from oxygen/titanium tetraisopropoxide (TTIP) plasmas at low temperature by Helicon-PECVD at floating potential ($V_f$) or substrate self-bias of -50 V. The influence of titanium precursor partial pressure on the morphology, nanostructure and optical properties was investigated. Low titanium partial pressure ([TTIP] < 0.013 Pa) was applied by controlling the TTIP flow rate which is introduced by its own vapor pressure, whereas higher titanium partial pressure was formed through increasing the flow rate by using a carrier gas (CG). Then the precursor partial pressures [TTIP+CG] = 0:027 Pa and 0.093 Pa were obtained. At $V_f$, all the films exhibit a columnar structure, but the degree of inhomogeneity is decreased with the precursor partial pressure. Phase transformation from anatase ([TTIP] < 0.013 Pa) to amorphous ([TTIP+CG] = 0:093 Pa) has been evidenced since the $O^+_2$ ion to neutral flux ratio in the plasma was decreased and more carbon contained in the film. However, in the case of -50 V, the related growth rate for different precursor partial pressures is slightly (~15%) decreased. The columnar morphology at [TTIP] < 0.013 Pa has been changed into a granular structure, but still homogeneous columns are observed for [TTIP+CG] = 0:027 Pa and 0.093 Pa. Rutile phase has been generated at [TTIP] < 0:013 Pa. Ellipsometry measurements were performed on the films deposited at -50 V; results show that the precursor addition from low to high levels leads to a decrease in refractive index.

• 한국광물학회지
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• 제14권2호
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• pp.128-136
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• 2001

흘란다이트 터널 구조내의 A자리 양이온인 $Ba^{2+}$ 이온을 $K^{+ }$ 이온이 치환하면서 결정의 구조에 어떠한 변화가 있는지 알아보기 위해 K-Ba 전구간 완전고용체로 치환된 7개의 합성 흘란다이트형 광물($K_{2x}$ $Ba_{1}$ -x/$Cr_2$$Ti_{6}$ $O_{16}$ , x=0, 0.1, 0.3, 0.5, 0.7, 0.9, 1.0)에 대하여 X선 회절분석과 리트벨트 구조분석법을 실시하였다. 리트벨트 계산 결과, 구조의 정밀도를 나타내는 R 지수값을 보면$ R_{exp}$에 대한 $R_{wp}$ 값($R_{wp}$ /$R_{exp}$ )은 15.77%/20.90%~14.74%/l9.37%의 범위를 보여주며, $R_{B}$ 값은 6.45~8.97%, S (GofF)값은 1.45~l.63으로 각각 계산되었다. 합성 홀란다이트는 K-Ba 전구간에서 Ba의 함량에 관계없이 모두 공간군 14/m을 가지며, 단위포의 크기는 a=10.1194(2) ~ 10.0599(2)$\AA$, c=2.9572(6)~2.9512(7)$\AA$, V=302.75~298.66$\AA^{3}$의 범위를 보여주며, K 함량이 50% 이상에서는 금홍석이 부산물로 합성되었다. 그 결과 A자리의 Ba와 K의 치환관계에서는 비록 단위포의 크기에 일정한 변화를 보여주었으나 구조적 변이에 영향을 주기에는 충분치 않은 것으로 밝혀졌다. 따라서 정방정계에서 대칭성이 낮은 단사정계로의 구조적 변이는 A자리에 대한 K-Ba 치환보다는 다른 양이온의 치환이나 B자리의 치환 등 다른 요인에 의할 것으로 생각된다.다.

• 대한치과보철학회지
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• 제46권5호
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• pp.490-499
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• 2008

생체 활성 재료는 생체 내에서 자가적으로 인회석 층 (apatite layer)을 형성하여, 골과의 생화학적 결합이 가능해야 한다. 알칼리와 열처리를 통하여 생체 활성 표면을 얻을 수 있는 것으로 보고되고 있다. 본 실험에서는 알칼리 및 열처리를 시행한 임플란트들의 안정성을 평가하고자 하였다. 실험군의 분류로 1군은 대조군인 선반 가공 임플란트군, 2, 3군은 $60^{\circ}C$, 5 M의 NaOH 용액에 24시간 처리한 후, 각각 대기 중 및 진공 상태 $600^{\circ}C$에서 1시간 동안 열처리하였다. 처리된 시편은 FESEM, XPS, TF-XRD 및 AFM을 이용하여 표면 특성을 관찰하고, 임플란트의 안정성을 위해 공진 주파수와 페리오테스트 및 역 토오크를 측정하고, 골유착 안정성에 관한 차이를 비교 분석하여 다음과 같은 결과를 얻었다. 1. 표면 특성: 알칼리 및 열처리를 시행한 2, 3군은 비슷한 양상의 거친 표면을 보여주었다. 알칼리 처리를 시행한 2군과 3군에서 1군과는 달리 높은 함량의 나트륨 이온이 검출되었으며, 결정구조 분석 결과 2군에서 예추석 (antase)과 금홍석 (rutile)이 혼재된 상태로 금홍석이 우세한 양상을 보여주었다. 2. 공진 주파수 분석: 군간 비교에서 12주에 2군이 1, 3군에 비해 통계적으로 유의하게 높은 측정치를 보였다. 주간 비교시, 1, 2군은 4주 이후에 유의한 증가를 보여주었고, 3군은 2주와 4주에서 각각 유의한 증가를 보여주었다 (P < .05). 3. 페리오테스트 분석: 주간 비교에서 1, 2군은 4주 이후에 유의하게 감소를, 3군은 2주와 4주에서 각각 유의한 감소를 보여주었다 (P< .05). 4. 역 토오크 분석: 군간 비교에서는 2, 4, 8주에서는 2군이 1, 3군에 비해 유의하게 높은 측정값을 보여주었다. 주간 비교에서는 1, 3군은 4주, 12주에서 유의한 증가를 보여주었고, 2군은 4주부터 유의한 증가를 보여주었다 (P < .05). 이상의 결과로 볼 때, 알칼리 및 대기 중 열처리를 통해서 적절한 결정 구조의 산화막을 가진 생체 활성화된 무정형의 나트륨 티탄산염 층을 얻을 수 있었고, 알칼리 및 진공 상태 열처리만으로도 나트륨이 함유된 생체 활성화된 표면을 얻을 수 있었다고 사료된다. 또한 이런 처리 과정으로 형성된 표면층들은 임플란트의 초기 골유착에 도움을 줄 수 있는 유용한 방법 중 하나라고 사료된다.

• 한국세라믹학회지
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• 제31권12호
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• pp.1577-1587
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• 1994

TiO2 thin films with the substitution of oxygen with nitrogen were deposited on silicon substrate by metalorganic chemical vapor deposition (MOCVD) using Ti(OCH(CH3)2)4 (titanium tetraisopropoxide, TTIP) and N2O as source materials. X-ray diffraction (XRD) results indicated that the crystal structure of the deposited thin films was anatase TiO2 with only (101) plane observed at the deposition temperatures of 36$0^{\circ}C$ and 38$0^{\circ}C$, and with (101) and (200) plane at above 40$0^{\circ}C$. Raman spectroscopic results indicated that the crystal structure was anatase TiO2 in accordance with the XRD results without any rutile, fcc TiN, or hcp TiN structure. No fundamental difference was observed with temperature increase, but the peak intensity at 194.5 cm-1 increased with strong intensity at 143.0 cm-1 for all samples. The crystalline size of the films varied from 49.2 nm to 63.9 nm with increasing temperature as determined by slow-scan XRD experiments. The refractive index of the films increased from 2.40 to 2.55 as temperature increased. X-ray photoelectron spectroscopy (XPS) study showed only Ti 2s, Ti 2p, C 1s, O 1s and O 2s peaks at the surface of the film. The composition of the surface was estimated to be TiO1.98 from the quatitative analysis. In the bulk of the film Ti 2s, Ti 2p, O 1s, O 2s, N 1s and N 2s were detected, and Ti-N bonding was observed due to the substitution of oxygen with nitrogen. A satellite structure was observed in the Ti 2p due to the Ti-N bonding, and the composition of titanium nitride was determined to be about TiN1.0 from the position of the binding energy of Ti-N 2p3/2 and the quatitative analysis. The spectrum of Ti 2p energy level could be the sum of a 4, 5, or 6 Gaussian curve reconstruction, and the case of the sum of the 6 Gaussian curve reconstruction was physically most meaningful. From the results of Auger electron spectroscopy (AES), it was known that the composition was not varied significantly throughout the whole thickness of the film, and silicon oxide was not observed at the interface between the film and the substrate. The composition of the film was possible (TiO2)1-x.(TiN)x or TiO2-2xNx and in this experimental condition x was found to be about 0.21-0.16.

• 자원환경지질
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• 제28권6호
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• pp.541-551
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• 1995

The Yeongdeog gold-silver deposits at Jipum, Gyeongsangbugdo, is of a middle Paleogene $(45.52{\pm}1.02Ma)$ vein type, and is hosted in shale and sandstone of Cretaceous age. Based on mineral paragenesis, vein structure and mineral assemblages, the ore mineralization can be divided into two distinct depositional stages. The early stage is associated with base-metals such as pyrite, arsenopyrite (27.99~30.99 at%), hematite, rutile, pyrrhotite, sphalerite (10.53~18.42 FeS mole%), chalcopyrite and galena with wallrock alteration such as chlorite, sericite and pyrite. The late stage is characterized by the Au-Ag mineralization such as electrum, Ag-bearing tetrahedrite, freibergite, pyrargyrite, unidentified mineral, pyrite, sphalerite (1.08~5.57 FeS mole%), chalcopyrite and galena. Fluid inclusion data indicate that fluid temperatures and salinities range from 343 to $227^{\circ}C$ and from 8.3 to 5.7 wt% eq. NaCl in early stage, respectively. Temperatures and salinities of NaCl eq. wt% range from 299 to $225^{\circ}C$ and from 12.9 to 4.3 in late stage, respectively. They suggest that complex cooling histories were occured by the mixing of the fluids. Sulfur fugacity $(-logfs_2)$ deduced by mineral assemblages and composition ranges from 8.3 to 14.7 atm. in early stage, and from 8.8 to 14.5 atm. in late stage. It suggests that the mineralization was related to decrease of temperature in early stage and fluctuations of $fS_2$ with decrease of temperature in late stage. Sulfur and oxygen isotope compositions are 4.48~5.60‰ and 9.25~10.8% in early stage, and late stage is 4.84~7.00‰ and 5.7‰, respectively. It indicated that hydrothermal fluids may be magmatic origin with some degree of mixing of another water during paragenetic time.