Kawakami Yoko, Yamamoto Junji, Kagi Hiroyuki
Laboratory for Earthquake Chemistry, Graduate School of Science, University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-0033, Japan.
Appl Spectrosc. 2003 Nov;57(11):1333-9. doi: 10.1366/000370203322554473.
We investigated the applicability of Raman microprobe spectroscopy for determining the density of CO2 in fluid inclusions in minerals of mantle-derived xenolith samples. A separation (delta) between two Raman bands of CO2 due to Fermi resonance can be a reliable densimeter for CO2 fluid. The relationship between the density of CO2 (g/cm3) and delta (cm-1) can be expressed as: d = -0.03238697 delta 3 + 10.08428 delta 2 - 1046.189 delta + 36163.67. This equation was obtained from the Raman data on CO2 fluid with densities from 0.1 to 1.21 g/cm3, including super critical fluids at 58-59 degrees C. The delta value was constant with increasing temperature from room temperature to 200 degrees C. This indicates that the Raman densimeter is not affected by a possible rise in temperature, an artifact induced by the high flux of the incident laser. The minimum size of measurable inclusions is 1 micron, and the precision in the determination of delta is 0.1 cm-1, corresponding to 0.02 g/cm3 for inclusions of 1 micron in size. The precision can be better for larger inclusions. The micro-Raman densimeter can determine the density of CO2 fluid inclusions over a wide range. In particular, densities of gas and mixtures of gas and liquid phases, which cannot be measured by microthermometry, can be determined.
我们研究了拉曼微探针光谱法在测定地幔源捕虏体样品矿物中流体包裹体中二氧化碳密度方面的适用性。由于费米共振导致的二氧化碳的两个拉曼谱带之间的间隔(δ)可以成为一种可靠的二氧化碳流体密度计。二氧化碳密度(g/cm³)与δ(cm⁻¹)之间的关系可以表示为:d = -0.03238697δ³ + 10.08428δ² - 1046.189δ + 36163.67。该方程是根据密度为0.1至1.21 g/cm³的二氧化碳流体的拉曼数据获得的,包括58 - 59℃下的超临界流体。从室温到200℃,δ值随温度升高保持恒定。这表明拉曼密度计不受温度可能升高的影响,而温度升高是由入射激光的高通量引起的一种假象。可测量包裹体的最小尺寸为1微米,δ测定的精度为0.1 cm⁻¹,对于尺寸为1微米的包裹体,这对应于0.02 g/cm³。对于更大的包裹体,精度可能更高。微拉曼密度计可以在很宽的范围内测定二氧化碳流体包裹体的密度。特别是,可以测定用显微测温法无法测量的气相以及气液混合相的密度。