• 대한전기학회논문지:전기물성ㆍ응용부문C
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• 제50권8호
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• pp.376-381
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• 2001

The(1-x) MgTiO$_3$-xSrTiO$_3$(x=0.03~0.04) ceramics were fabricated by the conventional mixed oxide method. The structural and microwave dielectric properties were investigated by XRD, SEM, EDS and network analyzer. The sintering temperature and time were 1275$^{\circ}C$~135$0^{\circ}C$ and 2hours, respectively. In the XRD results of 0.96MgTiO$_3$-0.04SrTiO$_3$ceramics, the perovskite structure of SrTiO$_3$and ilmenite structure of MgTiO$_3$phase were coexisted. The dielectric constant($\varepsilon$(sub)${\gamma}$) and temperature coefficient of resonant frequency($\tau$(sub)f) were increased with addition of SrTiO$_3$. In thie case of 0.96MgTiO$_3$-0.04SrTiO$_3$ ceramics sintered at 13$25^{\circ}C$, the dielectric constant, quality factor(Q) and temperature coefficient of resonant frequency($\tau$(sub)f) were 20.13, 7956(at 7.27GHz), and +1.76ppm/$^{\circ}C$, respectively.

• 한국진공학회:학술대회논문집
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• 한국진공학회 1999년도 제17회 학술발표회 논문개요집
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• pp.86-86
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• 1999

본 연구에서는 마이크로파 유전체 소자로서의 응용 및 절연 산화막으로의 응용을 위해 마이크로파 유전체 세라믹으로 사용되어 온 MgTiO3 물질을 펄스 레이저로 박막을 제조하였다. MgTiO3 는 주로 고주파에서 높은 유전율을 갖고 높은 품질계수 (22.000 at 5 GHz) 혹은 낮은 유전손실을 갖으며 유전특성의 온도 안정성이 우수하여 유전체 세라믹 재료로 응용된다. MgTiO3 박막의 성장은 KrF(파장:248nm) 엑시머 레이저를 이용했으며 공정조건으로 박막의 성장온도는 500-75$0^{\circ}C$, 산소 압력은 10-5-200mTorr, 성장 후 냉각시 산소분위기는 200Torr, 레이저 에너지 밀도는 1.5-5J/cm2 등의 조건으로 박막을 성장하였다. MgTiO3 박막을 여러 가지 기판, 즉 Al2O3(r-plane), Si, Pt 위에 성장시켰으며 기판에 따라 에픽텍셜 혹은 다결정 상태를 갖는 ilmenite 구조로 성장되었다. PLD(Pulsed laser deposition)법에 의해 형성된 MgTiO3 박막을 보면, 우선 Al2O3(r-plane) 기판위에 성장된 경우 $700^{\circ}C$에서 에픽텍셜하게 성장하였으며, Si 기판 위에 성장된 경우 $650^{\circ}C$에서부터 (003)면으로 우선 배향된 단일상의 ilmenite 구조가 형성된다. Ptdnl에 성장된 경우 $600^{\circ}C$에서부터 (003)면으로 우선배향성을 가지며 $650^{\circ}C$에서 결정의 안정화를 이루었으나, MgTiO3 박막은 전기적 특성으로 유전특성 및 유전분산 특성 등이 측정 분석되어 MgTiO3 박막의 고주파 유전체로의 응용에 관한 가능성을 토의하였다.

• 한국자기학회지
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• 제13권6호
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• pp.226-230
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• 2003

제주도 지역의 특정위치를 선정하여 그 위치에서 채취한 화산암과 송이시료를 대상으로 상온에서 X-선형광법을 이용하여 시료의 화학조성을, X-선회절법과 Mossbauer분광법을 이용하여 시료에 함유된 광물, 산화철의 종류, 원자가상태와 자기적 성질을 분석하였다. 화산암과 송이시료는 SiO$_2$와 같은 규산염 광물이 주성분을 이루고 있고, olivine, pyroxene, ilmenite, hematite와 magnetite 등의 광물도 포함되어 있음을 확인하였다. 또한 화산암에 존재하는 철의 원자가 상태의 대부분은 Fe$^{2+}$이었고, 송이는 Fe$^{3+}$ 임을 알 수 있었다.

• 자원환경지질
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• 제20권2호
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• pp.85-95
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• 1987

The host rocks of titaniferous magnetite deposits in Gonamsan are alkaline gabbros, which are typical of undersaturated alkaline rocks in terms of the lack of normative quartz. According to field occurrences and petrographic features, these alkaline gabbros are divided into 3 rock types: coarse-grained and pegmatitic rock, medium-grained rock with equigranular texture, and layered cumulate rock. All these rocks mainly contain clinopyroxene(salite), plagioclase(An 43-66), pargasite, and ilmenite. The accessory minerals are apatite, sphene, quartz, and sometimes titaniferous magnetite. Pargasite, sphene, and quartz are considered to be secondary minerals formed by the reaction among clinopyroxene, plagioclase and Fe-Ti oxide at deuteric stage. Fe-Ti oxides generally occur as ilmenite in the alkaline rocks, and titaniferous magnetite in the ore deposits. Layered cumulate rocks are characterized by a recurrence of discontinuous thin mesolayer of clinopyroxene-pargasite within leucolayer mainly composed of plagioclase. Clinopyroxene is cumulus mineral whereas plagioclase, ilmenite and apatite occur as intercumulus minerals. According to the variation diagrams of oxide and trace element contents against the differentiation index, incompatible elements, such as Na, Ba and Sr, show positive correlations whereas compatible elements, such as Mg and Cr, show negative correlations. However some compatible elements, such as Co, Ni and V show irregular variations, reflecting relative cumulate status of cumulus and intercumulus minerals. On the de la Roche multicationic diagram, these alkaline gabbros are distributed along the differentiation curve of undersaturated alkaline series from alkaline basaltic composition through basanitic composition to tephritic composition. Layered cumulate rocks, which are distributed between basanitic composition and tephritic composition, reflect their cumulate character, slightly scattering away from the curve. The medium-grained rock shows higher contents in Ba, Sr and light rare earch elements than the coarse-grained and pegmatitic rock. The former shows two times higher contents of total rare earth elements than the latter, $while(La/Lu)_{cn}$ ratios maintain fairly constant values of 5.08~5.06 in these two rocks. This means that coarse-grained and pegmatitic rock, as compared with the medium-grained rock, was formed by the earlier differentiated magma but rare-earth element distribution pattern remained almost parallel during differentiation. From the data the above mentioned, these alkaline gabbros are considered to be comagmatic and to be formed by intrusions of differentiated magmas in its reservoir.

• 자원환경지질
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• 제27권4호
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• pp.345-361
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• 1994

Lens shaped titanomagnetite ore bodies in the Soyeonpyeong iron mine are embedded in amphibolites, which were intruded into Precambrian metasediments such as garnet-mica schist, marble, mica schist, and quartz schist. Mineral chemistry, K-Ar dating and hydrogen and oxygen stable isotopic analysis for the amphibolites and titanomagnetite ores were conducted to interpret petrogenesis of amphibolite and ore genesis of titanomagnetite iron ore deposits. Amphibolites of igneous origin have unusually high content of $TiO_2$, ranging from 0.94 to 6.39 wt.% with an average value of 4.05 wt.%. REE patterns of the different lithology of the amphibolite show the similar trend with an enrichment of LREE. Amphiboles of amphibolites are consist mainly of calcic amphiboles such as ferro-hornblende, tschermakite, ferroan pargasite, and ferroan pargasitic hornblende. K-Ar ages of hornblende from amphibolite and gneissic amphibolite were determined as $440.04{\pm}6.39Ma$ and $351.03{\pm}5.21Ma$, respectively. This indicates two metamorphic events of Paleozoic age in the Korean peninsula which are correlated with Altin orogeny in China. The titanomagnetite mineralization seems to have occurred before Cambrian age based on occurrence of orebodies and ages of host amphibolites. The Soyeonpyeong iron ores are composed mainly of titanomagnetite, ilmenite, and secondary minerals such as ilmenite and hercynite exsolved in titanomagnetite. The temperature and the oxygen fugacity estimated by the titanomagnetite-ilmenite geothermometer are $500{\sim}600^{\circ}C$ (ave. $550^{\circ}C$) and about $2{\pm}10^{-23}bar$, respectively. Hornblendes from ores and amphibolites which responsible for magnetite ore mineralization, have a relatively homogeneous isotopic composition ranging from +0.8 to +3.9 ‰ in ${\delta}^{18}O$ and from -87.8 to -113.3 ‰ in ${\delta}D$. The calculated oxygen and hydrogen isotopic compositions of the fluids which were in equilibrium with hornblende at $550^{\circ}C$, range from 2.8 to 5.9‰ in ${\delta}^{18}O_{H2O}$ and from -60.41 to -81.31 ‰ in ${\delta}D_{H2O}$. The ${\delta}^{18}O_{H2O}$ value of magnetite ore fluids are in between +6.4 to + 7.9 ‰. All of these values fall in the range of primary magmatic water. A slight oxygen shift means that $^{18}O$-depleted meteoric water be acted with basic fluids during immiscible processes between silicate and titaniferous oxide melt. Mineral chemistry, isotopic compositions, and occurences of amphibolites and orebodies, suggest that the titanomagnetite melt be separated immisciblely from the titaniferous basic magma.

• 보존과학회지
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• 제16권
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• pp.64-76
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• 2004

지사동 출토 슬래그에 대하여 화학적인 분석과 현미경 조직관찰에 의하여 금속학적인 조사연구를 수행하였다. 화학적인 분석은 ICP, XRD, SEM-EDS로 실행하였으며 슬래그 조직은 금속현미경 및 SEM으로 관찰하였다. 화학적 분석 결과, A 및 C 지구 슬래그의 전철량(Total Fe)은 $39\~45\%$ 로 고대 제철과정에서 발생했던 철분의 평균치에 해당하였다. 또한 CaO 성분은 $3\~8\%$로 많은 양은 아니지만 조재제로 Ca성분을 함유한 재료를 소량 사용한 것으로 사료되었다. A지구에서는 Ti성분이 미량 검출되었으며 C지구에선 Ti 성분과 V 성분이 다량 검출되었다. XRD 분석 결과 Fayalite, Wustite, Magnetite, Ilmenite, Pseudo - brookite, Ulvospinel, Forsterite, Fephroite, Olivine 같은 화합물이 검출되었다. 이는 금속현미경 및 SEM에 의한 관찰에서도 위와 같은 조직을 확인하였다. 따라서 A지구의 로에서는 주로 철광석을 이용한 제련작업을 하였고 C지구의 제철로에서는 철광석을 원료로 하는 제련작업과 사철을 원료로 하는 제련작업이 병행되었던 것으로 추정되었다.

• 대한기계학회논문집
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• 제7권3호
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• pp.263-269
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• 1983

Underwater welding by a gravity arc welding process was investigated by using six types of coated electrodes and SM41A steel plates of 10 mm thickness as base metal and it was ascertained that this process may be put to practical use. Main results obtained are summarized as follows: 1. Angle of electrode affects no influence on bead appearance and the proper range of welding current and diameter of electrode for the high titanium oxide type is relatively wider than that for the ilmenite type. And the lime titania type, high titanium oxide type and ilmenite type of domestic coated arc welding electrodes of .phi.4 mm could attain the soundest underwater welded joints which contain no welding imperfection. 2. According to macro-structure, micro-structure and hardness distribution inspectionson underwater welded joint, the area between the HAZ and the surface of the weld in neighbourhood of the bond has the maximum hardness value. The structure of these parts is martensite and bainite. Other parts contain mocro-ferrite, micro-pearlite structure, which contain soundness of welded joint free from weld imperfection. 3. On consideration of both tensile strength of more than 100% joint efficiency and sufficient impact value, the welding condition which can get optimal welding strength is heat input of 1,400-1,500 J/mm, current of 200-215 ampere (voltage of 32-33 volts) in the case of lime titania type electrode. 4. Underwater welding strength (tensile strength, impact strength) depends on heat input (or current) quantitatively and they have the relationship of parabolic function. Each experimental equation has a high reliability and its percent of mean error is 4.14%. 5. It is suggested that the optimal design of weld strength by welding condition (current, heat input) could be utilized for a quality control of underwater welding.

• 암석학회지
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• 제10권3호
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• pp.133-147
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• 2001

최근 기존 연대측정법의 한계를 극복하여 절대연령 측정 대상을 획기적으로 넓힐 수 있는 방법으로 개발되고 있는 단계적 용해에 의한 연대측정법을 국내 시료에 적용하여 이 방법에 의한 연대측정의 성공가능성에 대해 평가하여 보았다. 대상 시료는 옥천변성대 대전 남부지역 창리층의 함우라늄 흑색 점판암, 영남육괴 북동부의 선캠브리아 내덕리 화강암에서 분리한 전기석 및 옥방광산의 회중석 등을 선정하였다. 이들에 대한 단계적 용해를 위해 산의 종류와 시간을 달리하여 점차 그 세기를 늘려가며 납을 용출시켰으며, 각 단계에서 얻은 용액들에 대해 납 등위원소 비율과 함께 납과 우라늄 함량을 열이온화 질량분석기로 측정하였 다. 그 결과 창리층 혹색 점판암과 내덕리 화강암으로부터는 상당한 Pb 동위원소 값의 분산을 얻을 수 있었으며 단계적 용해에 의한 Pb-Pb 연대측정이 성공적일 수 있음을 보여준다. 단계적 용해 과정에서 시료의 종류마다 우라늄과 납의 거동이 다르며 이는 구성 광물의 종류에 따라 우라늄과 납이 차지하는 결정 내에서의 위치에 지배되는 것으로 판단된다.

• 한국광물학회지
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• 제25권4호
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• pp.295-304
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• 2012

하동군 옥종면 월횡리에는 과거 개발하던 티탄철석 광산이 위치하며, 주변 지질은 선캄브리아기 지리산 편마암 복합체가 광범위하게 분포하고 이를 회장암이 관입하고 있다. 간극누적형 회장암체 내 티탄철 광체가 발달하고 있으며, Ti-광체 내 희토류원소를 포함하는 갈렴석이 맥상으로 발달하고 있다. 갈렴석의 CaO 함량은 11.02~12.81 wt%로 낮은 반면, ${\Sigma}R_2O_3$는 상대적으로 높은 17.21~21.58 wt% (R=Ce, La, Nd)의 범위를 보여준다. 갈렴석이 높은 방사능 이상치를 보여주는 이유는 갈렴석 내에 미립의 광물상으로 존재하는 토륨 광물인 톨라이트(thorite, $ThSiO_4$) 때문인 것으로 밝혀졌다. 톨라이트는 $3{\sim}6{\mu}m$ 크기의 입상으로 누대구조를 보여주며, 화학분석 결과 $ThO_2$는 65~72.78 wt%, $UO_2$는 5.49~12.78 wt%의 함량을 보였다. 이러한 광물학적 특성은 톨라이트를 함 REE 갈렴석을 찾는 방사능 탐사를 함에 있어 좋은 지시자로 이용할 수 있을 것으로 사료된다.

• Journal of Welding and Joining
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• 제2권1호
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• pp.30-40
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• 1984

Moisture content in the coating of an electrode is known to cause defects such as porosities, fish eyes and cracks in the weld metal, however, quantitative relationship between them is not clearly understood. In this study widely consumed and the most common type of arc welding rods such as ilmenite and low hydrogen type were chosen for the investigation, and attempts were made to correlate the relationship between the mechanical properties and gas contents when welding was carried out with electrodes of various moisture contents. As the relative humidity changed from 70% to 92%, it was determined that moisture content to reach saturation was in the range of 0.6~6.8%. As the moisture content in the electrode coating was increased, the amount of gaseous components (H, O, N) in the weld metal was accordingly increased, especially diffusible hydrogen showed prominent effect, i.e. it increased proportionally to the increase of the moisture content. The mechanical properties of the weld metal was observed to become more inferior as the diffusible hydrogen was greater. It was determined for ilmenite type of electrode that the increase of hydrogen content was approximately 1.8ml per unit weight percent increase of moisture and also tensile strength resulted lowering from $45.3kg/\textrm{mm}^2$ to $42.7kg/\textrm{mm}^2$ as moisture content increased from 0.7% to 6.8%. For low hydrogen type the increase of the hyrogen was about 2.4ml per unit percent of moisture and tensile strength decreased from $63.0kg/\textrm{mm}^2$ to $53.8kg/\textrm{mm}^2$ particularly in the region of moisture content 0.1~4.2%.