Liu Chang-Ling, Ye Yu-Guang, Meng Qing-Guo
Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao 266071, China.
Guang Pu Xue Yu Guang Pu Fen Xi. 2010 Apr;30(4):963-6.
Methane hydrates are clathrate compounds that are formed by methane molecules and water molecules under low temperature and high pressure conditions. It was found that methane hydrates exist widely in sea-shelf floor and permafrost, and are considered as a potential energy resource. In the crystal lattice of clathrate hydrate, the water molecules form both large cages (5(12)6(2)) and small cages (5(12)) under the interaction of the hydrogen-hydrogen bond. In this paper, the authors designed a set of experimental apparatus for methane hydrates formation. Based on this equipment, the authors synthesized a series of methane hydrates in various systems in laboratory, including SDS solution (3% Wt) and methane, powdered ice and methane, and powdered ice and methane and natural sand with various sizes (i. e. 250-350, 180-250, 125-180 and 63-90 microm), under different temperature and pressure. The authors also designed a small device which was proved to be convenient for Raman determination of the methane hydrates. Raman spectroscopy was used to analyze the methane hydrates and to measure the structural parameters such as hydration numbers and cage occupancies. The results show that the methane hydrate samples are all in structure I type, and hydration numbers and cage occupancies are almost independent of the sediment sizes. In the three systems, the large cages of methane hydrate samples are nearly full occupied, with the occupancy ratios larger than 97%, whereas the small cages between 80% and 86%. The hydration numbers of these methane hydrate samples are between 6.05 and 6.15.
甲烷水合物是在低温高压条件下由甲烷分子和水分子形成的笼形化合物。研究发现,甲烷水合物广泛存在于大陆架海底和永久冻土中,并被视为一种潜在的能源资源。在笼形水合物的晶格中,水分子在氢键的相互作用下形成大笼(5(12)6(2))和小笼(5(12))。本文作者设计了一套用于甲烷水合物生成的实验装置。基于该装置,作者在实验室的各种体系中合成了一系列甲烷水合物,包括3%(重量)的十二烷基硫酸钠(SDS)溶液与甲烷体系、冰粉与甲烷体系以及冰粉与甲烷和不同粒径(即250 - 350、180 - 250、125 - 180和63 - 90微米)的天然砂体系,实验处于不同的温度和压力条件下。作者还设计了一种小型装置,经证明便于对甲烷水合物进行拉曼测定。利用拉曼光谱对甲烷水合物进行分析,并测量其结构参数,如水合数和笼占有率。结果表明,甲烷水合物样品均为I型结构,水合数和笼占有率几乎与沉积物粒径无关。在这三个体系中,甲烷水合物样品的大笼几乎被完全占据,占有率大于97%,而小笼的占有率在80%至86%之间。这些甲烷水合物样品的水合数在6.05至6.15之间。