• 한국광학회지
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• 제10권1호
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• pp.5-9
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• 1999

파장이 532nm인 선형 파극된 Nd:YAG 레이저 광속을 Gadolimium Gallium Garnet 프리즘 면에서 전반시킬 때 형성된 에바네슨트파 석에 위차한 Mie 입자 결합체들이 광압에 의해 회전하는 것을 관찰하였다. 가우스 광속에 의한 에바슨트파의 최대 강도 지점에서 벗어난 곳에 위치한 3~5$\mu\textrm{m}$ 크기의 라텍스 또는 효모 결합체들이 0.1~1 rpm의 속도로 회전하엿는데, 두입자의 결합체는 광속의 진행 방향과 나란해질 때 회전이 멈추었으나 세입자 이상의 결합체들은 계속 회전하는 것을 볼 수 있었다. 본 실험 결과는 근접장 영역에서 에바네슨트파의 광압에 의한 마이크로 모터의 제작 가능성을 보여준다.

• The Korean Journal of Ceramics
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• 제1권1호
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• pp.35-39
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• 1995

Yttrium aluminum garnet(YAG) powders were synthesized by spray-drying of the hydroxides coprecipitated from a mixture of aqueous solutions of $Al(NO_3)_3.9H_2O \;and\; Y(NO_3)_3.6H_2O$ Phase formation in the powders during heat treatments and their sintering charactristics were investigated. In the powder obtained by washing the hydroxides before spray-drying, a metastable yttrium aluminum hexagonal (YAH) phase was first crystallized and then transformed into YAG as temperature was increased. The formation of YAH was attributed to a deviation in compositions of the particles from the starting composition of YAG. However, the powder prepared without washing step contained a stable yttrium aluminum monoclinic(YAM) phase in addition to YAG due to a large deviation from the starting composition. A powder compact of a single phase YAG was pressureless-sintered for 4 hrs at $1700^{\circ}C$ and the density was 93% of the theoretical density.

• 한국세라믹학회지
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• 제35권4호
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• pp.413-419
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• 1998

${\beta}$-silicon carbides with yttrium aluminum garnet of 2,5,10 mol% were prepared by a liquid--phase sint-ering and the microstructural evolution and phase transformation were investigated during sintering as functions of liquid-phase amount and sintering time. The rate of grain growth decreases with the addition of the amount of yttrium aluminum garnet (YAG) in the SiC starting powder however the apparent density and the aspect ratio of grains in sintered body increase. The phase transformation from ${\beta}$-SiC to ${\alpha}$-SiC were dependent on the liquid-phase amount and sintering time.

• 한국콘크리트학회:학술대회논문집
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• 한국콘크리트학회 2003년도 가을 학술발표회 논문집
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• pp.36-39
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• 2003

In this study, we made the high strength light weight concrete which was composed of the garnet minute powder to be the industry by-product in the YoungJoo region and the artificial light weight aggregate which the high temperature(1100℃) plastic process. The characteristic of the autogenous shrinkage had been considered about strength characteristic and the age passage In the following addition: The concrete's each unit quantity was determined 145,160,175㎏f/㎥.w/b and s/a was determined 30%, 43%, 45%. the each garnet's substitution ratio was determined 0, 10%. In this results, the compressive strength appeared greatly as the unit joining discretion grew bigger. The autogenous shrinkage ratio was increased rapidly until 7th day but it was reduced after 7th day regardless of the mixed factor. The autogenous shrinkage ratio which follows the change of the unit quantity and s/a increased together as the unit quantity and the s/a increases.

• 자원환경지질
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• 제32권5호
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• pp.519-535
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• 1999

Precambrian metasedimetay rocks in the Sunchang Shear Zone (so-called Seologri and Yongamsan Formation) consist of black slate, phylite, mica schistm quartzite and rarely calc schist. The metamorphic rocks in the area have undergone at least three stages of metamorphism, which are two prograde (M1 and M2) and one contact metamorphism (M3). The metamorphism which made the most prevailing mineral assemblages in the area, is M2 stage metamorphism. The metamorphic grade of M2 methamorphism in metapelites increases from the Chlorite zone through Biotituzone, Garnet zone to Staurolite zone. The M1 stage metamorphism is recognized by kyanite and sillimanite pressure type regional metamorphism. The M3 stage methamorphism is represented in the contact boundary, which area is the chlorite zone and biotite zone near the Sunchang foliated granite and the namwon granite. The M3 stage methamorphism is characterized by andalusite bearing mineral assemblages. The peak temperature condition of M2 metamorphism estimated from coexising garnet and biotite (Kretz, 1990) is 518~598$^{\circ}C$.

• 한국전기전자재료학회논문지
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• 제14권3호
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• pp.257-262
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• 2001

Single crystalline films of La doped YIG(yttrium iron garnet) were grown by the liquid phase epitaxy. The lattice constants of films obtained by DCD(double crystalline diffractometer) measurement increased with increasing La contents in films. In particular, lattice constants of films grown wiht Y/La=20 solution were nearly same as those of GGG (gadolinium gallium garnet) substrate. The saturation magnetization measured with VSM (vibrating sample magnetometer) was about 1750Gauss which is the same as that of pure YIG irrespective of La contents in films. FMR(ferromagnetic resonance) linewidth of La doped YIG was smaller than that of pure YIG. Since appropriate La doping decreases the lattice mismatch between film and substrate, the FMR linewidth was Y/La=20 in this experiment.

• 한국광물학회지
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• 제14권1호
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• pp.1-11
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• 2001

미국 메사추세츠 북중부에 산출되는 데본기 리틀톤층(Littleton Formation)의 남정석-십자석-석류석대에서 채취한 석류석 반상변정의 화학적 누대구조는 여러 번의 성장 단계를 경험했음을 보여준다. 석류석 반상변정들은 비대칭적이고 불규칙적인 Mn, Mg, Ca의 누대구조를 보인다. 조직대 경계부에서 석류석 성분들은 단면선에 따라 그 형태가 다르게 나타나고, $X_{Mn}$ 과 Fe/(Fe+Mg)비의 역전 누대구조는 석류석내의 내부엽리의 발달과 밀접한 관계를 보여준다. 이런 관찰 사항들은 석류석 누대구조가 석류석을 형성/소모시키는 반응뿐만 아니라, 용해작용과 침전작용과 관련된 기존의 미세구조에 의해 변화되었음을 의미한다. 화학적 그리고 조직적 잘림구조의 관계 그리고 저자가 제안한 석류석 성장모델은 석류석 누대구조가 엽리의 발달 동안 전단 응력대에서 일어나는 선택적 용해작용과 압축 운동대에서 발생하는 침전작용에 의해 조절되었음을 지시한다.

• 자원환경지질
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• 제18권3호
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• pp.205-216
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• 1985

Fluid inclusion study reveals that the mineralogical zonal distribution of the Sangdong skarn orebody may be likely related to (homogenization) temperatures of fluids with time and spaces. Firstly limestone beds were replaced by hot boiling fluids ranging from 350 to $550^{\circ}C$ and formed the pyroxene-garnet skarn, which was replaced into the amphibole and the quartz-mica skarns by non-boiling fluids at 300 to $500^{\circ}C$, mainly penetrated the central part of the pyroxene-garnet skarn orebody. Freezing tests identify presence of $CaCl_2$ and $MaCl_2$ as brines in the fluids besides NaCl and KCL that are shown as daughter minerals and show that two or more fluids be involved in mineralization by showing a bimodal distribution of salinities. This study has contributed to find a new orebody and a granitic pluton as a source rock.

• 자원환경지질
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• 제26권4호
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• pp.473-487
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• 1993

The Janggun mine area is occupied by the Proterzoic and the Paleozoic meta-pelites, which are intruded by the Jurassic Chunyang granite. The metamorphic terrain is divided into four zones of progressive metamorphism on the basis of mineral assemblages. The zones are chlorite zone, staurolite zone, andalusite zone, sillimanite zone ascending order. Boundary lines between the zones resemble outline of the Chunyang granite mass. Isograd reactions are chlorite+chloritoid+muscovite=staurolite+biotite+quartz+water, staurolite+chlorite+muscovite+quartz=andalusite+biotite+water, and staurolite+muscovite+quartz=andalusite+biotite+garnet+water between the chlorite zone and the staurolite zone, the staurolite zone and the andalusite zone, and the andalusite zone and the sillimanite zone, repectively. They are univariant reactions in KFMASH component system. Metamorphic conditions estimated from garnet-biotite geothermometers and phase equlibria are $530^{\circ}C$ and lower than 4 kb.

• Journal of Magnetics
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• 제11권3호
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• pp.143-146
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• 2006

We attempted to fabricate a new type of magneto optic spatial light modulator (MO-SLM) for multiple-tone modulation by using in-plane magnetization. In the MO-SLM, magnetic property of magneto-optical layer was modified to be suitable for multiple-tone expression by substituting Al in Bi:YIG film. At a driving current to 28 mA in an electrode of the fabricated MO-SLM, changes in brightness of pixels were observed using a polarization microscope.