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天然气水合物粉晶X射线衍射测试参数优化及分析方法
引用本文:田苗,孟庆国,刘昌岭,李承峰,胡高伟,冯娟,赵全升.天然气水合物粉晶X射线衍射测试参数优化及分析方法[J].岩矿测试,2017,36(5):481-488.
作者姓名:田苗  孟庆国  刘昌岭  李承峰  胡高伟  冯娟  赵全升
作者单位:青岛大学环境科学与工程学院, 山东 青岛 266071;国土资源部天然气水合物重点实验室, 青岛海洋地质研究所, 山东 青岛 266071,国土资源部天然气水合物重点实验室, 青岛海洋地质研究所, 山东 青岛 266071;海洋国家实验室海洋矿产资源评价与探测技术功能实验室, 山东 青岛 266071,国土资源部天然气水合物重点实验室, 青岛海洋地质研究所, 山东 青岛 266071;海洋国家实验室海洋矿产资源评价与探测技术功能实验室, 山东 青岛 266071,国土资源部天然气水合物重点实验室, 青岛海洋地质研究所, 山东 青岛 266071;海洋国家实验室海洋矿产资源评价与探测技术功能实验室, 山东 青岛 266071,国土资源部天然气水合物重点实验室, 青岛海洋地质研究所, 山东 青岛 266071;海洋国家实验室海洋矿产资源评价与探测技术功能实验室, 山东 青岛 266071,青岛大学环境科学与工程学院, 山东 青岛 266071,青岛大学环境科学与工程学院, 山东 青岛 266071
基金项目:国家自然科学基金资助项目(41302034);中国地质调查项目"天然气水合物测试技术与模拟实验"(DD20160216)。
摘    要:天然气水合物是由烃类气体和水在低温高压下形成的一种非化学计量的笼型晶体水合物,在常温常压下极易分解,需要在低温条件下对其进行测试。本文针对天然气水合物这一特殊样品,重点研究其粉晶X射线衍射测试条件,系统地探讨了步长、扫描速度、累加次数及测试温度等因素对测试结果的影响,优化了仪器参数,建立了粉晶X射线衍射测试天然气水合物晶体结构的方法,并应用到实验合成的甲烷水合物和我国南海珠江口盆地钻获的天然气水合物样品的晶体结构测试中。结果表明,我国南海珠江口盆地的天然气水合物样品与实验合成的甲烷水合物结构相同,均属立方晶系,为典型的Ⅰ型水合物,晶胞参数分别为11.9309×10~(-10)m和11.9135×10~(-10)m。该技术可准确获得天然气水合物的结构信息,为我国天然气水合物的深入研究提供技术支撑。

关 键 词:天然气水合物  粉晶X射线衍射  甲烷水合物  晶胞参数  晶体结构
收稿时间:2017/3/16 0:00:00
修稿时间:2017/7/20 0:00:00

Parameter Optimization and Analysis Method for Determination of Natural Gas Hydrate by Powder X-ray Diffraction
TIAN Miao,MENG Qing-guo,LIU Chang-ling,LI Cheng-feng,HU Gao-wei,FENG Juan and ZHAO Quan-sheng.Parameter Optimization and Analysis Method for Determination of Natural Gas Hydrate by Powder X-ray Diffraction[J].Rock and Mineral Analysis,2017,36(5):481-488.
Authors:TIAN Miao  MENG Qing-guo  LIU Chang-ling  LI Cheng-feng  HU Gao-wei  FENG Juan and ZHAO Quan-sheng
Institution:Department of Environmental Science and Engineering, Qingdao University, Qingdao 266071, China;Key Laboratory of Gas Hydrate, Ministry of Land and Resources, Qingdao Institute of Marine Geology, Qingdao 266071, China,Key Laboratory of Gas Hydrate, Ministry of Land and Resources, Qingdao Institute of Marine Geology, Qingdao 266071, China;Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China,Key Laboratory of Gas Hydrate, Ministry of Land and Resources, Qingdao Institute of Marine Geology, Qingdao 266071, China;Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China,Key Laboratory of Gas Hydrate, Ministry of Land and Resources, Qingdao Institute of Marine Geology, Qingdao 266071, China;Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China,Key Laboratory of Gas Hydrate, Ministry of Land and Resources, Qingdao Institute of Marine Geology, Qingdao 266071, China;Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China,Department of Environmental Science and Engineering, Qingdao University, Qingdao 266071, China and Department of Environmental Science and Engineering, Qingdao University, Qingdao 266071, China
Abstract:Gas hydrate is a form of non-stoichiometric clathrate compound which is produced by hydrocarbon gas molecules and water molecules at high pressure and low temperature. Usually under atmospheric pressure and room temperature, the hydrate sample is easy to decompose and thus the analysis must be carried out at low temperature. The analysis conditions of powder X-ray Diffraction for natural gas hydrate is the focus of this study. The influencing factors (i.e., increment, scan speed, cumulative number, and the temperature) were systematically studied to optimize the analytical parameters. As a result, a powder X-ray Diffraction method to measure the crystal structure of gas hydrate is proposed. This method has been used successfully to measure the crystal structure of the hydrate samples from both the laboratory and the Pearl River Mouth basin in the South China Sea. The results show that the hydrate samples have a similar cubic crystal structure. Both the synthetic methane hydrate in the laboratory and the gas hydrate from the Pearl River Mouth basin in the South China Sea belong to the type I hydrate and have unit cell parameters of 11.9309×10-10 m and 11.9135×10-10 m, respectively. This method can be used to obtain the structural information of gas hydrate, and will provide a technical support for further research of gas hydrate in China.
Keywords:natural gas hydrate  powder X-ray Diffraction  methane hydrate  lattice parameter  crystal structure
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