• 분석과학
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• 제19권5호
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• pp.376-382
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• 2006

In this work, pitch/activated carbon/$TiO_2$ composite were prepared by $CCl_4$ solvent method with different mixing ratios. The BET surface area of pitch/activated carbon/$TiO_2$ composite has a significantly increase with increasing activated carbon content in pitch/activated carbon/$TiO_2$ composite. The surface structure and elemental compositions of the composite were studied by SEM and EDX, respectively. The SEM results were presented to the characterization of porous texture on the pitch/activated carbon/$TiO_2$ composite. And EDX data was shown the presence of C, O, S, Ti and other elements. The structural properties of the composite were studied in XRD measurements. The $TiO_2$ crystal phases of the pitch/activated carbon/$TiO_2$ composite had lots of rutile-type structure which transforms from anatase-type with a little of anatase-type structure. The photocatalytic activities of the composite were evaluated using a photo-decomposition method under UV lamp. The pitch/activated carbon/$TiO_2$ composites were observed better photocatalytic activity than that of pristine $TiO_2$.

• 한국표면공학회지
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• 제57권3호
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• pp.179-191
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• 2024

This study focuses on improving the photocatalytic degradation efficiency by synthesizing a TiO₂/WO₃ composite. Given the environmental significance of photocatalysis and the limitations posed by TiO₂'s large bandgap and high electron recombination rate, we explored doping, surface modification, and synthesis strategies. The composite was created using a ball mill process and heat treatment, analyzed with field emission scanning electron microscope, high resolution X-ray diffraction, Raman microscope, and UV-Vis/NIR spectrometer to examine its morphology, composition and absorbance. We found that incorporating WO₃ into the TiO₂ lattice forms a W_x-Ti_1-x-O₂ solution, with optimal WO₃ content reducing the band gap and enhancing sterilization efficiency by inhibiting the anatasese to rutile transition. This contributes to the field by offering a way to overcome TiO₂'s limitations and improve photocatalytic performance.

• 한국광학회지
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• 제17권3호
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• pp.296-302
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• 2006

졸-겔법으로 촉매농도에 따라 저온 $TiO_2$ 졸을 제조한 후, 침지코팅법을 이용하여 $TiO_2$ 박막을 제작하였다. 제작된 저온 $TiO_2$ 박막의 광학적, 구조적, 광활성 특성을 조사하였다. 0.10 mol, 0.25 mol, 0.50 mol과 0.75 mol의 촉매농도로 제작된 저온 $TiO_2$ 박막은 가시광 영역에서 높은 투과율 특성을 나타내었다. XRD 스펙트럼 결과에 의하면 촉매농도가 증가함에 따라 아나타제 결정구조에서 루타일 결정구조로의 상전이가 촉진되고 결정크기는 촉매농도가 증가함에 따라 아나타제 결정크기가 감소하였다. SEM 결과로부터 $TiO_2$ 박막의 표면입자크기가 0.25 mol의 측매농도에서 가장 작았다. 아나타제 결정구조를 가지는 0.10 mol, 0.25 mol과 0.50 mol의 $TiO_2$ 박막 존재 하에서 메틸렌블루가 완전히 광분해 되는 것을 확인하였다.

• 한국세라믹학회지
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• 제40권4호
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• pp.346-349
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• 2003

Microwave dielectric characteristics and physical properties of the new Zr$_{1-x}$ (Bn$_{1}$3/Nb$_{2/3}$)xTi $O_4$ (0.2$\leq$x$\geq$ 1.0) system have been investigated as a function of the amount of Bn$_{1}$3/Nb$_{2/3}$ $O_2$substitution. With increasing Bn$_{1}$3/Nb$_{2/3}$ $O_2$ content (x), two phase regions were observed: $\alpha$-Pb $O_2$ solid solution (x<0.4), mixture of the rutile type Zn$_{1}$3/Nb$_{2/3}$Ti $O_4$ and the $\alpha$-Pb $O_2$ solid solution (x$\geq$0.4). In the$\alpha$-Pb $O_2$solid solution region below x<0.4, the Q.f$_{0}$ value sharply increased and the Temperature Coefficient of the Resonant Frequency(TCF) decreased with increasing Bn$_{1}$3/Nb$_{2/3}$ $O_2$ contents while dielectric constant (K) showed nearly same value. In the mixture region above x$\geq$4, the dielectric constant and TCF increased with increasing Bn$_{1}$3/Nb$_{2/3}$ $O_2$ content. Zr$_{1-x}$ (Zn$_{1}$3/Nb$_{2/3}$)xTi $O_4$ materials have excellent microwave dielectric properties with K=44.0, Q.f$_{0}$ : 41000 GHz and TCF =-3.0 ppm/$^{\circ}C$ at x=0.35.=0.35. x=0.35.=0.35.

• 자원환경지질
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• 제29권6호
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• pp.689-698
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• 1996

The coal-bearing metapelites from the Hoenam area are interbedded within the Ogcheon Supergroup, which are composed mainly of graphite, quartz, muscovite and associated with trace amount of biotite, chlorite, pyrite, rutile and barite. Although the formation was mined for coal, and the contents of V, U and Mo are a higher grade in coal formations than the host metapelites. The ratios of Al/Na and K/Na in coal formation are very heterogeneous and wide range from 10.28 to 90.91 and from 3.73 to 36.60, respectively. The V content increase with increasing Al and Ba contents, but the U and Mo are not related with other elements. Those are suggested that controlled of mineral compositions in coaly metapelites due to substitution, migration and reequilibrium of elements by regional metamorphism. These coal formation were deposited in basin of marine environments and the REE of these rocks are not influenced with metamorphism and hydrothermal alterations on the basis of Al content versus La, La against Ce, the ratios of La/Ce (0.23 to 0.73) and Th/U (0.03 to 16.6). These rocks also show much variation in $La_N/Yb_N$ (0.53 to 14.19), Th/Yb (0.51 to 6.00) and La/Th (0.15 to 18.92), and their origin is explained by derivation from a mixture of sedimentary and metasedimentary rocks. The wide range in trace and REE element characteristics as Co/Th (0.07 to 3.00), La/Sc (0.04 to 23.48), Sc/Th (0.06 to 7.57), V/Ni (2 to 3319), Cr/V (0.03 to 1.06) and Ni/Co (1.00 to 79.85) of these coaly metapelites argues for inefficient mixing of the various source lithologies during sedimentation.

• Korean Chemical Engineering Research
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• 제44권4호
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• pp.375-381
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• 2006

티타늄 담지 구형활성탄(spherical activated carbon, SPAC)을 제조하여 유동상 광촉매 반응에 적용하고 그 특성을 평가하였다. 티타늄을 담지하기 위하여 염화티타늄용액으로 이온교환 처리된 이온교환수지를 열처리 과정을 통하여 구형활성탄으로 변환시켜 주었다. 열처리 과정 중 감량되는 성분 및 무게 변화는 TGA/MS 분석을 통하여 알아보았으며,Ti을 함유한 구형활성탄의 물리화학적 성질은 SEM, XRD, EPMA, ESR, EDS, BET와 같은 분석을 통하여 그 특성을 알아보았다. 그 결과 Ti-구형활성탄의 입자 크기는 $350{\mu}m{\sim}400{\mu}m$, 비표면적은 $617m^2/g$ 이였으며, 담지 된 티타늄은 $TiO_2$ anatase 형태와 rutile 형태가 주를 이루고 있음을 알 수 있었다. 구형활성탄에 담지 된 $TiO_2$는 약 6 wt%로 균일한 분산도로 구형활성탄 표면에 담지 된 것을 EPMA 분석을 통해 알 수 있었다. 더욱이 ESR 분석을 통하여 간접적인 광촉매 활성을 확인할 수 있었으며, 따라서 이러한 결과들을 바탕으로 유동상 광반응조를 이용한 HA(humic acid) 광분해 반응에 적용하였다. 그 결과, 제거 효율이 약 70％ 정도로 높게 나타났을 뿐만 아니라 반응 중에도 Ti-구형활성탄의 강도가 계속 유지되어 유동상 반응에서의 광분해 촉매로서 활용가능성을 보여주었다.

• 한국해양학회지
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• 제24권1호
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• pp.39-51
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• 1989

한국 동남해역의 대륙붕과 대륙사면에서 채취된 139개의 표면퇴적물 시료의 입도특성과 광물성분 및 유기탄소 함량이 분석되었다. 퇴적물의 입도특성에 의하여 사질퇴적상, 점토질퇴적상, 이토질퇴적상, 사니혼합퇴적상 빚 사점토혼합퇴적상 등 5개의 퇴적상이 구분될 수 있었고, 이들의 지역적인 분포 양상이 해석되었다. 한편, 본 연구지역의 퇴적물은 한반도 주변의 다른 해역환경에 비하여 전반적으로 점토의 함량이 높은 반면 상대적으로 실트의 함량이 빈약한 것이 특징적이다. 사립의 광물성분은 주로 석영, 장석 및 암편으로 구성된다. 중광물의 조성은 지역적 특징을 나타내어, 연구지역의 남부에서 ZTR 광물(zircon, tourmaline, rutile)이, 북부에서 변성기원 광물이, 그리고 후포뱅크에서 석류석이 각각 타 지역에 비하여 풍부했다. 한편, 점토광물 중에서는 일라이트가 가장 우세하였으며(평균 64%), 클로라이트(20%), 카올리나이트(13%), 스멕타이트(4%) 순으로 그 함량이 감소하였다. 퇴적물의 유기탄소 함량은 평균 1.94%로서, 한반도 주변의 다른 해역들에 비하여 높았다. 유기탄소의 함량은 주로 퇴적물 입도에 의해 조절되며, 지역적으로는 대륙사면의 퇴적물에서 특히 높았다. 퇴적물의 입도와 광물성분의 지역적인 분포양상은 연구지역의 북부와 남부가 세립퇴적물의 공급 및 이동경로에 있어 서로 다르다는 사실을 시사한다. 이 해역에서 보고된 수온이나 해류에 관한 연구결과들은 이렇게 서로 다른 세립질 퇴적물의 이동 양상을 뒷받침해 주는 것으로 보인다.

• 한국재료학회지
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• 제18권11호
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• pp.583-591
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• 2008

In this study, two series of CNT/$TiO_2$ electrodes were prepared. The decrease of surface area compared with that of the pristine carbon nanotubes (CNTs) indicated the blocking of micropores on the surface of the CNTs; was further supported by scanning electron microscopy (SEM) and field emission SEM (FE-SEM) observations. The X-ray diffraction (XRD) results showed that the CNT/$TiO_2$ composites contained a mix of anatase and rutile forms of $TiO_2$ particles when the precursor was $TiO_2$ powder, whereas when the precursor was Ti ($OC_4H_7$) (TNB), the composites contained only the typical single and clear anatase $TiO_2$ particles. The energy dispersive X-ray spectroscopy (EDX) spectra showed the presence of C, O and Ti peaks for all samples. It was found that catalytic decomposition of methylene blue (MB) solution could be attributed to synthetic effects between the $TiO_2$ photocatalysis and electro-assisted CNTs network, and that photoelectrocatalytic oxidation increased with an increase of CNT composition. It was also found that the photoelectrocatalytic oxidation efficiency for MB is higher than that of photocatalytic oxidation. Moreover, the CNT/$TiO_2$ composites catalyst prepared by the impregnation method demonstrates higher photoelectrocatalytic activity than the mechanical mixture with the same CNT content.

• 자원환경지질
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• 제16권2호
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• pp.65-78
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• 1983

This report deals with the sedimentological study of the littoral sand of beaches in the Busan area. The purpose of this report is to know the grain size, mineralogical composition, heavy mineral and clay mineral of the beach sands, and gravity measurements of the Nagdong River Deltas. 1) As a whole, the littoral sand of the beaches are composed of uniformly medium grained, moderately sorted and nearly symmetrical. The barrier sand of the Nagdong Estuary is composed of fine grained, well sorted and nearly symmetrical. 2) The littoral sand of the beaches is transported by saltation and rolling. The barrier sand of the Nagdong Estuary is transported by suspension and saltation. 3) In the littoral sand of the beaches, the ratio of feldspar to quartz is 1 :2.31 and in the barrier sand of the Nagdong Estuary 1:1.40. 4) The content of heavy mineral of samples ranges from 0.54 to 3.87 %. The principal heavy minerals are hornblende, pyroxene, epidote, garnet, leucoxene, zircon, apatite, magnetite, hematite and ilmenite with minor accessories of rutile and olivine. 5) The x-ray diffraction analysis of the clay mineral informs the existence of quartz, feldspar, kaolinite and montmorillonite. The montmorillonite is considered to have been derived from the alteration of acidic volcanic rocks. 6) To determine the depositional structure of the Nagdong Estuary, Gravity measurements were made. Free air anomaly ranges from 14.5 mgal to 33.5 mgal and Bouguer anomaly ranges from 14.3 to 23.5 mgal and both are closely related to the topography. According to the interpreted layer structure, the upper layer composing sand, silt and clay, the intermediate layer composing sand with gravel, the lower layer composing weathered and soft rock, and bed rock composing hornfels or andesite. 7) The depositional environments of the study, the littoral area is dominated by the marine environment and the Nagdong Estuary by the mixed environment.

• 자원환경지질
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• 제25권3호
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• pp.283-296
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• 1992

The Keumryeong deposits is a low grade copper deposits in which copper minerals form disseminated grains and thin veinlets in felsic volcanics seem to be dacite. Alteration of the volcanics consists mainly pervasive propylitization and silicification. Potassic alteration characterized by biotite developed locally adjacent to southwestern contact of granodiorite body. Principal sulfide minerals in altered zone are mainly pyrite and lesser chalcopyrite. Chalcopyrite content in potassic zone is relatively higher than that of surrounding propylitized zone. Pyrite and chalcopyrite accompanies magnetite, molybdenite, sphalerite, pyrrhotite, arsenopyrite, pentlandite, marcasite, hematite, ilmenite, rutile, bismuthinite and native Bi as disseminations, veinlets and knots. Granodiorite body is propylitized and contains veinlets of pyrite, chalcopyrite and molybdenite. Fluid inclusions in sulfide-bearing quartz veinlets and quartz grains of felsic volcanics and granodiorite in altered zone consist of liquid-rich, vapor-rich, $CO_2-bearing$ and halite-bearing inclusions. These four types of inclusion intimately associated on a microscopic scale and indicate condensing or boiling of ore fluid during mineralization. Homogenization temperature of coexisting fluid inclusions are mostly in the range of 350 to $450^{\circ}C$. High salinity fluid contains 28.6 to 48.4 weight percent NaCI equivalent and moderate salinity fluid cotains 0.5 to 12.5 weight percent NaCl equivalent. Pressure estimated from $CO_2$ mole fraction of $CO_2-bearing$ inclusion range 160 to 375 bars. The Kigu copper deposits is a fissure filling copper vein developed 500 m south from the Keumryong deposits. Mineralogy and fluid inclusion data of the Kigu deposits are similar to that of the Keumryeong deposits. Homogenization temperature of fluid inclusions from the Kigu deposits are reasonable agreement with temperature estimated from sulfidation curve of cubanite-chalcopyrite-pyrite-pyrrhotite and pyrite-pyrrhotite mineral assemblages. Not only mineral occurrence and wall rock alteration in the Keumryeong deposits but also fluid inclusion data such as temperature, salinity, pressure and boiling evidences are similar to those of porphyry copper deposits.