• Elastomers and Composites
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• v.31 no.4
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• pp.247-255
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• 1996

금속이나 고분자 재료에 비하여 세라믹스는 우수한 내열성과 고온 물성을 가지고 있음에도 불구하고, 잘 깨지는 특성과 제조시 많은 열량을 필요로 하는 단점 때문에 그 동안 고온 구조용 부품으로서 광범위하게 사용되지 못하였다. 본 연구에서는 polycarbosilane을 이용하여 C/C 복합체를 포함한 산화물 및 비산화물 세라믹 복합체의 저온 치밀화 제조 공정을 확립하였다. polympr precursor를 열처리하여 얻은 $Al_2O_3$와 SiC 장섬유를 대표적인 산화물, 비산화물 세라믹스인 알루미나와 탄화규소에 각각 보강하여 파괴에너지가 기존의 단체 세라믹스에 비하여 10배 이상 향상된 세라믹 복합체를 제조하였다. 복합체 제조시 polycarbosilane을 결합제로 첨가하였으며 polycarbosilane이 SiC로 전이되는 $1150^{\circ}C$에서 열처리하여 이론 밀도의 73% 이상을 얻었다.

• Journal of Hydrogen and New Energy
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• v.18 no.3
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• pp.317-324
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• 2007

The conversion reaction of ortho to para hydrogen was studied. The percentage of ortho and para hydrogen is mainly dependent on the equilibrium temperature. Because this reaction is known to be accelerated by the catalyst such as nickel-silicate and ruthenium on silica, we focused in the test and development of the catalysts. We studied metal-silicates because they provide high metal dispersion on support. Nickel-silicate, ruthenium-silicate and mixed-silicate were prepared by the coprecipitation method and used in the reaction at the temperature of liquid nitrogen. The conversion was measured by the difference of thermal conductivity between reference gas and sample gas. The activation condition was important and it affected the activities of the catalysts. Nickel-silicate showed high activities. Ruthenium-silicate also showed relative high activities but mixed-silicate showed poor activities.

• Proceedings of the KAIS Fall Conference
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• 2000.10a
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• pp.42-42
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• 2000

반응소결 탄화규소는 소결체 내에 잔존 실리콘이 남아 있어 고온강도의 감소를 초래하는 단점이 있어 고온 구조재료로서의 사용이 제한되어 왔다. 따라서 이러한 문제점을 해결하기 위한 방법으로 Si 단독으로 용응침투시키는 대신 Si-MoSi₂를 침투시키는 방법이 시도되고 있으며, 이외에도 TiC 성형체에 Co, Ni 등의 금속, ZrB₂ 성형체에 Zr 금속 등을 용융, 침투시켜 성능향상을 유도하는 연구가 진행되고 있다. 본 연구에서는 반응소결에 대한 기본이론과 응용분야, 반응소결 비산화물계 세라믹스의 제조공정 및 이들 소결체의 미세구조와 기계적 특성 등을 소개하고자 한다.

• Journal of the Korean Crystal Growth and Crystal Technology
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• v.5 no.4
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• pp.358-369
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• 1995

Surface structure and adhesion by the reaction between thin metal films and SiC were studied at temperatures between 550 and $1450^{\circ}C$ for various times. The reaction with the formation of various silicides was initially observed above $850^{\circ}C$ for SiC/Co system and $650^{\circ}C$ for SiC/Ni system. The cobalt reacted with SiC and consumed completely at $1050^{\circ}C$ for 0.5 h and the nickel at $950^{\circ}C$ for 2 h. The observed CoSi phase in SiC/Co and Ni$_2$Si phase in SiC/Ni are thermodynamically stable in the reaction zone up to 125$0^{\circ}C$ and $1050^{\circ}C$ respectively. Carbon was crystallized as graphite above $1450^{\circ}C$ for SiC/Co reaction surface and $1250^{\circ}C$ for SiC/Ni. The critical loads of the thin metal films on SiC substrate were qualitatively compared in terms of the scratch test method. At temperatures between 850 and $1050^{\circ}C$, relatively higher values of 20~33 N were observed for SiC/Ni couples.

• Economic and Environmental Geology
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• v.49 no.1
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• pp.13-22
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• 2016

The objectives of this study were to recover silica and iron oxides and $CO_2$ sequestration using serpentine via various acid dissolution and pH swing processes. Serpentine collected from Guhang-myeon in S. Korea were mainly composed of antigorite and magnetite consisting of $SiO_2$ (45.3 wt.%), MgO (41.3 wt.%), $Fe_2O_3$ (12.2 wt.%). Serpentine pulverized ($${\leq_-}75{\mu}m$$) and then dissolved in 3 different acids, HCl, $H_2SO_4$, $HNO_3$. Residues treated with acidic solution were recovered from the solution (step 1). And then the residual solution containing dissolved serpentine was titrated using $NH_4OH$. And pH of the solution increased up to pH=8.6 to obtain reddish precipitates (step 2). After recovery of the precipitates, the residual solution reacted with $CO_2$ and then pH increased up to pH=9.5 to precipitate white materials (step 3). The mineralogical characteristics of the original sample and harvested precipitates were examined by XRD, and TEM-EDS analyses. ICP-AES analysis was also used to investigate solution chemistry. The dissolved ions were Mg, Si, and Fe. The antigorite became noncrystralline silica after acid treatment (step 1). The precipitate at pH=8.6 was mainly amorphous iron oxide, of which size ranged from 2 to 10 nm and mainly consisting of Fe, O, and Si (step 2). At pH=9.5, nesquehonite [$Mg(HCO_3)(OH){\cdot}2(H_2O)$] and lasfordite [$MgCO_3{\cdot}H_2O$] were formed after reaction with $CO_2$ (step 3). The size of carbonated minerals was ranged from 1 to $6{\mu}m$. These results indicated that the acid treatment of serpentine and pH swing processes for the serpentine can be used for synthesis of other materials such as silica, iron oxides and magnesium carbonate. Also, This process may be useful for the precursor synthesis and $CO_2$ sequestration via mineral carbonation.