钴柘榴石(Co3Al2Si3O12)的高压合成及其稳定区

稲吉 野田, 真澄 潮
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Specimens used for the identification were taken from a layer of 0.5mm thick at the central part of the specimen chamber, in order to minimize the variation of temperature and pressure of the treatment. The maximum deviation of the measured temperatures was ±40°C at 1700°C at 40kb. It decreased with decreases in temperature and pressure to ±20°C at temperatures lower than 1300°C at 20kb. The error in the pressure measurement was estimated to be ±2kb at the maximum.Cobalt garnet is stable at pressures above 23kb at 1200°C and above 24kb at 1500°C. Below these pressures at the respective temperatures, mixtures of cobalt spinel (CoO⋅Al2O3), cobalt olivine (2CoO⋅SiO2) and quartz were obtained from the glass. Garnet produced at 1400°C at 25kb broke down to spinel, olivine and quartz when it was held at 18 kb at the same temperature. Cobalt garnet melts congruently at 1670°C and 25kb. 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引用次数: 2

摘要

采用带式高压装置对3CoO⋅Al2O3⋅3SiO2玻璃进行处理,处理温度为600°~ 1900°C,压力为20 ~ 40kb。将玻璃试样置于直径3.0mm、长9.0mm的铂管加热器中。热处理温度由插入试样腔内的铂铝热电偶测量,或根据几种压力下的温度-加热功率输入关系估计。测量了试样腔内的温度分布和压力梯度。用x射线衍射法和显微观察对处理后的试样中的矿物进行了鉴定。用于鉴定的试样取自试样室中央0.5mm厚的一层,以尽量减少处理过程中温度和压力的变化。测量温度的最大偏差为±40°C, 1700°C, 40kb。当温度低于1300℃,20kb时,随温度和压力的降低而降低至±20℃。压力测量误差估计最大为±2kb。钴石榴石在1200℃的压力下稳定在23kb以上,在1500℃的压力下稳定在24kb以上。在相应的温度和压力下,从玻璃中得到钴尖晶石(CoO⋅Al2O3)、钴橄榄石(2CoO⋅SiO2)和石英的混合物。在1400°C和25kb下生产的石榴石在相同温度下保持在18kb时分解为尖晶石、橄榄石和石英。钴石榴石在1670°C和25kb时完全熔化。在1500 ~ 1670℃的温度和低于23kb的压力下,石榴石与尖晶石和液体不一致地熔化。石榴石的熔融曲线斜率为12℃/kb。在900°C时,即使在25kb时,玻璃也会分裂成尖晶石、橄榄石和石英的混合物,在800°C时,在30kb时也会得到相同的混合物。Co3Al2Si3O12钴石榴石的晶格常数a0为14.473±0.008 A,折射率nD为1.82±0.01(25°C)。石榴石的颜色是明亮的粉红色。
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コバルト柘榴石 (Co3Al2Si3O12) の高圧合成とその安定領域
Glass of 3CoO⋅Al2O3⋅3SiO2 composition was treated at temperatures ranging from 600° to 1900°C at pressures of 20 to 40kb using a girdle type high pressure apparatus. The glass specimen was placed in a platinum tube heater 3.0mm in diameter and 9.0mm long. The heat treatment temperature was measured by a platinum-alumel thermocouple inserted in the specimen chamber or was estimated from the temperature-heating power input relations at several pressures. The temperature distribution and the pressure gradient in the specimen chamber were measured. Minerals in the treated specimens were identified by the X-ray diffraction method and the microscopic observations. Specimens used for the identification were taken from a layer of 0.5mm thick at the central part of the specimen chamber, in order to minimize the variation of temperature and pressure of the treatment. The maximum deviation of the measured temperatures was ±40°C at 1700°C at 40kb. It decreased with decreases in temperature and pressure to ±20°C at temperatures lower than 1300°C at 20kb. The error in the pressure measurement was estimated to be ±2kb at the maximum.Cobalt garnet is stable at pressures above 23kb at 1200°C and above 24kb at 1500°C. Below these pressures at the respective temperatures, mixtures of cobalt spinel (CoO⋅Al2O3), cobalt olivine (2CoO⋅SiO2) and quartz were obtained from the glass. Garnet produced at 1400°C at 25kb broke down to spinel, olivine and quartz when it was held at 18 kb at the same temperature. Cobalt garnet melts congruently at 1670°C and 25kb. It seems that the garnet melts incongruently to spinel and liquid at temperatures from 1500°C to 1670°C at pressures lower than 23kb. The slope of melting curve of the garnet is 12°C/kb. At 900°C the glass devitrifies to a mixture of spinet, olivine and quartz even at 25kb, and at 800°C the same mixture was obtained at 30kb.The lattice constant a0 of the cobalt garnet (Co3Al2Si3O12) is 14.473±0.008 A and the refractive index nD is 1.82±0.01 (25°C). The color of the garnet is bright pink.
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