• Korean Journal of Mineralogy and Petrology
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• v.35 no.3
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• pp.173-182
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• 2022

Dongsuak crater, located in the mid-mountainous region of Jeju Island, is located at an altitude of about 700 m, and the newly discovered Dongsuak spinel peridotites was enclosed in Dongsuak alkaline basalt. The Dongsuak spinel peridotites are composed of olivine, orthopyroxene, clinopyroxene, and spinel with porphyroclastic texture under the an equilibrium state. The variations of mineral major and trace compositions indicates that the Dongsuak spinel peridotites originate at depth from 66 to 88 km under an equilibrium temperature of about 960℃~1068℃. The Dongsuak spinel peridotites have been undergone about 1~3% fractional melting. The LREE-enriched characteristics indicate that the Dongsuak spinel peridotites have been undergone cryptic metasomatism by silicate melt without new minerals.

• Korean Journal of Mineralogy and Petrology
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• v.36 no.4
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• pp.365-376
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• 2023

Songaksan, formed about 3800 year ago, is one of the tuff rings in the Jeju Island. Mantle xenoliths, spinel peridotites, are enclosed in the Songaksan Trachybasalt. The spinel peridotites are less than 2 cm in size and are composed of olivine, orthopyroxene, clinopyroxene, and spinel. The uniform compositions of the minerals from core to rim indicate that equilibrium was reached in the spinel peridotites before these were enclosed in the host magma. The spinel peridotites originated at depths between 55 and 60 km with equilibrium temperatures ranging from 915 to 968℃. The spinel peridotites from Songaksan reveal porphyroclastic texture with a lot of neoblast minerals. Olivines display strong kink banding, indicating that the upper mantle of Songaksan has been deformed. The spinel peridotites from Songaksan have undergone about 5~7% fractional melting, and cryptic metasomatism by an silicate melt. The period of entrainment and transport of the spinel peridotites in the host magma is about 15 days.

• Journal of the Korean Ceramic Society
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• v.37 no.10
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• pp.994-1000
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• 2000

Mn-Ni-Co계 스피넬을 모재로 선택하여 상업용 페라이트 등 다양한 종류의 Fe-스피넬과 동시 소결 가능성을 검토할 목적으로 각 소재의 소결 거동, 서미스터와의 계면 반응이나, 2차상의 형성 등에 대해 알아보았다. 대부분의 페라이트 조성이 Mn 스피넬과 새로운 2차상을 형성하지는 않는 것을 알 수 있었다. 상업용 페라이트의 경우 115$0^{\circ}C$ 소결 온도에서 접합이 가능한 조성은 다량의 액상이 존재하며 접합계면의 폭이 상대적으로 넓으므로 서미스터 특성에도 좋지 않은 영향을 줄 수 있을 것으로 생각된다. 반면에 MFN1과 MFN2 조성은 접합계면에서 새로운 2차상이 형성되지 않고 원소의 상호확산도 작아 NTC 서미스터의 동시소결용 보호재로서의 가능성이 높은 것으로 확인되었다.

• Journal of the Mineralogical Society of Korea
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• v.18 no.4 s.46
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• pp.237-248
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• 2005

Results from in-situ high temperature X-ray diffraction measurements show that $Mg_{2}SiO_{4}{-}$spinel converts back to olivine phase only when heated in vacuum, and that at some high temperature, the olivine phase grows with time at the expense of the spinel phase strongly suggesting a 'nucleation and growth' type transition. In order to obtain the activation energy of spinel-olivine back transformation, kinetics measurements were performed on $Mg_{2}SiO_{4}{-}$spinel in vacuum at high temperatures between 1023 and 1116 K. Activation energy was determined using 'time to a given fraction method'. By employing the Avrami equation, it was found that n values generally increase with increasing temperature in a wide range implying that the nucleation and growth mechanism is probably temperature-dependent. It is likely that in spinel, at a relatively lower transformation temperature, after nucleation sites saturated, the growth of the new phase starts on the surface and gradually moves inwards. At high temperatures, however, after nucleation sites saturated, the growth starts both on the surface as well as at the interior.

• Proceedings of the Petrological Society of Korea Conference
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• 2004.05a
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• pp.39-41
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• 2004

• Journal of the Korean Chemical Society
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• v.42 no.1
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• pp.122-134
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• 1998

In this review, we describe the electrochemical properties of spinel-type lithium manganese oxides $(Li_xMn_2O_4)$ and their failure modes encountered in 4 V lithium rechargable cells. The long-term cyclability (reversibility) of spinel electrodes is determined partly by the purity, size and distribution of spinel particles, and also by the microstructure of electrode plates. A proper selection of electrolytes is another important task in cyclability enhancements. In the spinel preparation, impurity formation and cation mixing should be minimized. The carbon content in composite cathodes should also be minimized to the extent where the cell polarization does not bring about adverse effects on cell performances. The binder content should be optimized on the basis of dispersion of component materials and mechanical strength of the plates. Cathodic capacity losses arising from solvent oxidation and spinel dissolution can be mitigated by using electrolytes composed of carbonates and/or fluorine-containing lithium salts. The carbon additives may be selected after a trade-off between the cell polarization in composite cathodes and the solvent oxidation on carbon surface.

• Journal of the Korean earth science society
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• v.26 no.3
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• pp.305-312
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• 2005

Degrees of serpentinization from the original rocks of Choongnam serpentinites such as dunite and harzburgite are well matched with O'Hanley's textural stages of serpentinites (1996). Colors of chromian spinels in serpentinites are brown and/or red in dunites, and red in harzburgite. Also, colors of chromian spinels changed darker from brown and/or red according to the degree of serpentinization and more darker by steatitization because of increasing Fe ions.

• Proceedings of the Materials Research Society of Korea Conference
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• 2007.11a
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• pp.4-4
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• 2007

• Proceedings of the Mineralogical Society of Korea Conference
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• 2004.05a
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• pp.39-41
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• 2004

• Proceedings of the KSEEG Conference
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• 2002.04a
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• pp.203-206
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• 2002