CAS Key Laboratory of Marine Geology and Environment & Center of Deep Sea Research, Institute of Oceanology, Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China; Laboratory for Marine Geology, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266061, China; University of Chinese Academy of Sciences, Beijing 100049, China.
CAS Key Laboratory of Marine Geology and Environment & Center of Deep Sea Research, Institute of Oceanology, Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Spectrochim Acta A Mol Biomol Spectrosc. 2023 Aug 5;296:122651. doi: 10.1016/j.saa.2023.122651. Epub 2023 Mar 23.
The carbon isotopic composition of CO is traced to its different origins and widely used in the fields of geology, biology, and chemistry. Raman spectroscopy can be performed in situ, is nondestructive, and requires no sample preparation; these characteristics enable Raman spectroscopy to be considered a new alternative method to measure the carbon isotopic composition of CO. In this work, Raman spectra of high-purity CO, CO, and six CO-CO binary mixtures with known mixing ratios were collected using a High Pressure Optical Cell (HPOC) at 50-450 °C and 50-400 bar. The results showed that the characteristic peak positions of both CO and CO shift to lower wavenumbers with increasing temperature and decreasing pressure, but the peak positions of CO show a larger shift. The peak position difference of the corresponding characteristic peaks between CO and CO is greater than 15 cm under the above temperatures and pressures, and the peaks can be distinguished. However, ν overlays ν near 1265 cm, ν overlaps ν near 1288 cm. The existence of CO can cause a change in the Fermi diad splitting of CO and affect the establishment of CO Raman densimeters. The positive correlation obtained between the peak intensity ratio and the content ratio is affected by temperature, pressure, and CO content. I/I and I/I were selected as the quantitative indices to establish Raman quantitative analysis models for the determination of the carbon isotopic composition of CO, which can be applied to in-situ measurements of high-temperature and high-pressure systems.
CO 的碳同位素组成可追溯到其不同的来源,广泛应用于地质学、生物学和化学领域。拉曼光谱可以在原位进行,无损且无需样品制备;这些特性使得拉曼光谱成为测量 CO 碳同位素组成的一种新的替代方法。在这项工作中,使用高压光学池 (HPOC) 在 50-450°C 和 50-400bar 下收集了高纯 CO、CO 和六种已知混合比的 CO-CO 二元混合物的拉曼光谱。结果表明,随着温度的升高和压力的降低,CO 和 CO 的特征峰位置都向低波数移动,但 CO 的峰位置移动更大。在上述温度和压力下,CO 和 CO 的对应特征峰的峰位差大于 15cm,可以区分开。然而,ν在 1265cm 附近重叠 ν,ν在 1288cm 附近重叠 ν。CO 的存在会引起 CO 的费米二联体分裂的变化,并影响 CO 拉曼密度计的建立。峰强度比与含量比之间的正相关性受温度、压力和 CO 含量的影响。选择 I/I 和 I/I 作为定量指标,建立了用于测定 CO 碳同位素组成的拉曼定量分析模型,可应用于高温高压体系的原位测量。