• The Korean Journal of Ceramics
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• 제2권3호
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• pp.152-156
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• 1996

Fine (~0.09 $\mu$m) $\beta$-SiC Powders with 3.3wt% of large (~0.44$\mu$m) $\alpha$-SiC of $\beta$-SiC particles (seeds) added were hotpressed at 175$0^{\circ}C$ using $Y_2O_3$, $Al_2O_3$ and CaO as sintering aids and then annealed at 185$0^{\circ}C$ for 4 h to enhance grain growth. The resultant microstructure and polytypes were analyzed by high resolution electron microscopy (HREM).Growth of $\beta$-SiC with high density of microtwins and formation of ${\alpha}/{\beta}$ composite grains consisting of $\alpha$-SiC domain sandwiched between $\beta$-SiC domains were found in both specimens. When large $\alpha$-SiC (mostly 6H) seeds were added, the $\beta$-SiC transformend preferentially to the 6H polytype. In contrast, when large $\beta$-SiC (3C) seeds were added, the fine $\beta$-SiC transformed preferentially to the 4H polytype. Such results suggested that the polytype formation in SiC was influenced by crystalline form of seeds added as well as the chemistry of sintering aids. The ${\alpha}/{\beta}$ interface played and important role in the formation of elongated grains as evidenced by presence of ${\alpha}/{\beta}$ composite grains with high aspect ratio.

• 한국세라믹학회지
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• 제27권6호
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• pp.799-807
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• 1990

In this study, effects of oxide additives on mechanical properties and microstructure of A1N and A1N polytype ceramics were investigated. Fine A1N powder was synthesized by nitriding alumiuim hydroxide prepared from Al-isopropoxide, at 1350$^{\circ}C$ for 10h in N2 atmosphere. By adding 3w/o Y2O3, 0.56w/o CaO, and 10w/o SiO2 to AlN powder, AlN and AlN polytype ceramics were prepared by hot-pressing under the pressure of 30 MPa at 1800$^{\circ}C$ for 1h. AlN ceramics with no additives formed considerable amount of AlON phase, while AlN ceramics doped with Y2O3 or CaO decreased AlON phase and formed Y-Al or Ca-Al oxide compound. AlN＋10w/o SiO2(＋3w/o Y2O3) composition produced AlON and AlN polytype compound having 21R as a major phase. Room temperature flexural strength of AlN ceramics with no additive was 246MPa, and room temperature flexural strength and critical temperature difference by thermal shock(ΔTc) of AlN ceramics dooped with Y2O3 or CaO were 532MPa/340$^{\circ}C$ and 423MPa/300$^{\circ}C$, respectively. Y2O3 and CaO used as sintering agent played roles of densification and oxygen removal of AlN ceramics, and affected grain growth/grain morphologies of AlN ceramics.

• 한국광물학회지
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• 제11권2호
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• pp.69-84
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• 1998

The Daehyun sericite deposit in socheon-myun, Bongwha-gun, Kyungsangbuk-do, Korea, has been formed by the hydrothermal alteration of the Hongjesa granite of Precambrian age, leaving the muscovite granite between ore body and the Hongjesa granite as the wall rock alteration zone. The process of sericitization of granitic rock as well as chemistry and structures of sericites were studied using polarizing microscope, X-ray diffractometer (XRD), electron probe microanalyzer (EPMA) and high resolution transmission electron microscope (HRTEM). There are two genetic types of sericites having different chemistry and structure. The early sericite is of 2M1 polytype and has octahedral composition close to muscovite. It has been formed from the primary muscovite, tourmaline and quartz under a relatively high temperature. The late sericite is of 1M, 2M1 and 3T polytypes and has phengitic composition. It has been formed form feldspar, biotite, muscovite and tourmaline under a relatively low temperature. Chemical analyses show t, the early sericite has less Mg+FeT content and lower Si/AlIV ratio in tetrahedral site than the late sericite.

• 한국전기전자재료학회논문지
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• 제26권12호
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• pp.863-866
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• 2013

SiC crystal ingots were grown on 6H-SiC dual-seed crystals with different surface roughness and different seed orientation by a PVT (Physical Vapor Transport) method. 4H and 15R-SiC were grown on seed crystal with high root-mean-square (rms) value. The polytype of grown crystal on the seed crystal with lower rms value was confirmed to be 6H-SiC. On the other hand, all SiC crystals grown on seed crystals with different seed orientation were proven to be 6H-SiC. The surface roughness of seed crystals had no effect on the crystal structure of the grown crystals. However, the crystal quality of 6H-SiC single crystals grown on the on-axis seed were revealed to be slightly better than that of 6H-SiC crystal grown on the off-axis seed.

• 한국광물학회지
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• 제4권2호
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• pp.129-140
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• 1991

Two illite polytypes, 2M1 and 1Md, have been identified from the sericite deposits of the Bobae mine, Kimhae, Kyungsangnam-do. Each polytype has characteristic grain size, chemical composition, and occurrence. 2M1 illite occurs predominantly in the sericitic alteration zone, while 1Md illite occurs predominantly in the propylitic alteration zone, implying that the former was formed in the higher temperature than the latter. Illites can be subdivided into two types based on their crystal sizes;(1) the $\mu\textrm{m}$-sized illite which is below 0.01mm(100$\mu\textrm{m}$) in size and consists of 2M1 and 1Md type, (2) the mm-sized illite which is above 0.01mm in size and consists only of 2M1 type. Especially illite below 1$\mu\textrm{m}$ is premominantly of 1Md type. Therefore, it seems likely that illite crystal size is to some extent related to the polytype. XRD data show that there is no interstratified layer in illites regardless of the crystal size and polytype. Activity of muscovite component of the $\mu\textrm{m}$-sized illite is 0.843 while that of the mm-sized illite is 0.790. However, the latter is more similar to muscovite in crystal structure than the former is. The mm-sized illite has less Al and more Kthan the $\mu\textrm{m}$-sized illite. In both illites, Si contents show a positive relation to octahedral Mg. Fluid inclusion study and mineral association show that the formation temperature of illite is $270-330^{\circ}C$. The major chemical processes leading to the formation of sericitic deposit as well as the alteration zones are the leaching of SiO2 from the country rock and the addition of Al2O3 and K2O into the sericitic ores.

• 한국광물학회지
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• 제23권4호
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• pp.305-313
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• 2010

콩고민주공화국의 중앙아프리카 구리광화대에서 수입하는 Cu-Co 광석의 광물학적 특성을 X-선 회절 분석, 2차원 X-선 회절 분석과 전자현미분석에 의하여 연구하였다. 검은색 광석은 코발트 광석광물인 헤테로제나이트와 구리 광석광물인 공작석, 초록색 광석은 공작석으로 주로 구성된다. 헤테로제나이트는 반사 현미경 하에서 매우 밝은 흰색을 나타내며 X-선 회절 분석에서는 $4.39{\AA}$과 $2.316{\AA}$ 피크를 가지는 3R 다형으로 확인된다. 그러나 전형적인 3R형에 비하여 낮은 NiO와 $Fe_20_3$의 함량으로 미루어 보아, 3R 다형 이외에 2H 다형도 일부 존재하는 것으로 판단된다. 공작석은 반사 현미경하에서 밝은 회색을 나타내며, 화학식은 $Cu_{1.97}Co_{0.02}Fe^{2+}{_{0.01}}CO_3(OH)_2$이다. 헤테로제나이트와 공작석은 중앙아프리카 구리광화대의 광화작용 중 최후기인 표성부화기에 형성되었으며, 코발트는 일차 광석보다는 표성작용에 의하여 형성된 (산)수산화 광석에 더 많이 부화되었을 것으로 추정된다.

• 자원환경지질
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• 제46권1호
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• pp.1-9
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• 2013

본 연구에서는 배경값 보정 및 크기보정을 포함하여 오차요인을 크게 줄이고, WILDFIRE(C)를 통해 최적화된 이론값과 실측값의 일치정도 (R%, (${\sum}$|이론값-측정값|/이론값)/$n{\times}100$)를 정량값으로 제시하고, 그 값을 최소화하는 반복과정을 통해 일라이트 폴리타입 함량을 정량하는 개선된 full-pattern-fitting법을 제안하여 일정 함량을 갖는 혼합시료를 대상으로 검증하고, 기존의 Grathoff and Moore법과 비교하였다. 개선된 full-pattern-fitting법은 대상시료 내 불순물로 인한 각 폴리타입 함량오차에도 불구하고, 기존의 full-pattern-fitting법 보다 개선된 최대 3.6% 이내의 오차를 보였다. Grathoff and Moore법과의 비교에서 대상시료 모두에서 Grathoff and Moore법 적용결과는 $2M_1$ 폴리타입의 상대함량이 고평가되어 나타났으며, 이용한 피크별 매우 큰 정량값 차이를 보이는 반면, 본 연구의 개선된 full-pattern-fitting법 적용 결과는 10% 이내의 낮은 R% 값을 갖는 폴리타입 상대함량값을 보이는 것으로 나타나, 높은 신뢰도의 정량결과를 제공할 수 있음을 확인하였다.

• 한국결정성장학회지
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• 제7권2호
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• pp.197-206
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• 1997

6H-SiC 위에 SiC 에피층이 화학 기상 증착(CVD)에 의하여 성장되었다. 성장된 SiC 에피층의 결정구조는 X-선 회절과 Raman 분광을 사용하여 조사되었으며, 이 에피층은 6H-SiC로서 성장되었음을 확인하였다. 수정된 Lely법으로 성장된 한 SiC 결정 분말의 결정구조를 확인하기 위하여 전형적인 SiC polytype들의 X-선 회절상을 계산하였으며, 측정된 X-선 회절상과 비교하여 이 SiC 결정에는 15R-SiC가 약간 혼재되어 있음을 확인하였다.

• 한국전기전자재료학회논문지
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• 제24권10호
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• pp.799-802
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• 2011

In this study, SiC single-crystal ingots were prepared on two seed crystals with different doping level by using the physical vapor transport (PVT) technique; then, SiC crystal wafers sliced from the grown SiC ingot were systematically investigated to find the effect of seed doping level on the doping concentration and crystal quality of the SiC. To exclude extra effects induced by adjustment of the process parameters, we simultaneously grew the SiC crystals on two seed crystals with different level, which were fabricated from previous two SiC crystal ingots.

• 자원환경지질
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• 제45권2호
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• pp.181-188
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• 2012

일라이트에서 적층방식을 달리하여 나타나는 폴리타입은 대부분 1M과 $2M_1$이며, 적층 Disordering에 따른 $1M_d$ 또한 흔히 관찰된다. 본 해설에서는 일라이트의 폴리타입을 구분하고 정량적으로 해석할 수 있는 광물학적 이론적 근거와 방법을 소개하고, 소규모 열수환경에 준하는 단층대 내 생성시기 및 조건을 달리하는 일라이트 폴리타입 혼합물에의 적용을 통한 단층 활동 및 재활동연대 결정에의 활용 가능성을 검토하였다. 단층연대해석의 정확도와 신빙도를 높이기 위해서는 단층암 대상시료 내 일라이트 폴리타입의 생성환경에 대한 정보, 동정 및 광물학적 특성에 대한 규명이 이루어져야 한다. 또한 WILDFIRE(C)시뮬레이션을 이용한 정량분석에서, $1M_d$ 폴리타입의 Disordering 정도 및 I/S 광물의 팽창도에 기인한 (hkl) 회절선들의 Broadening 효과 등 일라이트 폴리타입 정량분석법의 오차요인을 최소화시키는 하기 방법을 고려해야 할 것이다.