Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Section 4.2: Inorganic and Isotope Geochemistry, Telegrafenberg, 14473 Potsdam, Germany.
Spectrochim Acta A Mol Biomol Spectrosc. 2013 Nov;115:528-36. doi: 10.1016/j.saa.2013.06.065. Epub 2013 Jun 29.
Hydrate formation processes and kinetics are still not sufficiently understood on a molecular level based on experimental data. In particular, the cavity formation and occupancy during the initial formation and growth processes of mixed gas hydrates are rarely investigated. In this study, we present the results of our time-depending Raman spectroscopic measurements during the formation of hydrates from ice and gases or gas mixtures such as CH4, CH4-CO2, CH4-H2S, CH4-C3H8, CH4-iso-C4H10, and CH4-neo-C5H12 at constant pressure and temperature conditions and constant composition of the feed gas phase. All investigated systems in this study show the incorporation of CH4 into the 5(12) cavities as first step in the initial stages of hydrate formation. Furthermore, the results imply that the initial hydrate phases differ from the resulting hydrate phase having reached a steady state regarding the occupancy and ratio of the small and large cavities of the hydrate.
基于实验数据,水合物的形成过程和动力学在分子水平上仍未得到充分理解。特别是,在混合气体水合物的初始形成和生长过程中,对空腔的形成和占据很少进行研究。在这项研究中,我们介绍了在恒定压力和温度条件以及进料气相组成恒定的情况下,从冰和气体或气体混合物(例如 CH4、CH4-CO2、CH4-H2S、CH4-C3H8、CH4-iso-C4H10 和 CH4-neo-C5H12)中形成水合物时,随时间变化的拉曼光谱测量结果。在本研究中,所有被调查的系统都表明 CH4 被掺入到 5(12)空腔中,这是水合物形成初始阶段的第一步。此外,这些结果表明,初始水合物相在占据和水合物的小空腔和大空腔的比例方面与达到稳定状态的最终水合物相不同。