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作 者:付娟[1,2,5] 吴能友[3,4] 邬黛黛[2] 苏秋成[2] FU Juan;WU Neng-you;WU Dai-dai;SU Qiu-cheng(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China;Key Laboratory of Gas Hydrate, Guangzhou Institute of Energy Conversion, Chinese Academy of Sciences, Guangzhou 510650, China;Key Laboratory of Natural 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;University of Chinese Academy of Sciences, Beijing 100049, China)
机构地区:[1]中国科学院广州地球化学研究所,广东广州510640 [2]中国科学院天然气水合物重点实验室,中国科学院广州能源研究所,广东广州510650 [3]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 [4]青岛海洋科学与技术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 [5]中国科学院大学,北京100049
出 处:《波谱学杂志》2017年第2期148-155,共8页Chinese Journal of Magnetic Resonance
基 金:国家自然科学基金资助项目(41273022);中国石油-中科院科技合作项目(2015A-4813);中国科学院广州能源研究所所长创新基金培育专项(y307p51001)
摘 要:甲烷水合物(CH_4·n H_2O)是主要由甲烷和水分子构成的冰状笼型化合物,在自然界储量巨大.固体核磁共振(NMR)波谱和激光拉曼光谱是在分子水平分析甲烷水合物的重要手段.该文利用低温固体核磁共振碳谱(^(13)C NMR)对合成的甲烷水合物结构进行了研究,分别使用^(13)C交叉极化(^(13)C CP)和高功率质子去偶(1H HPDEC)2种脉冲程序采集甲烷水合物的^(13)C NMR谱图,结合实验结果分析及理论推导可知,使用1H HPDEC方法得到的^(13)C NMR谱图信号更强,更利于定量分析;甲烷气体与冰粉合成的甲烷水合物为I型,其大笼和小笼占有率分别为0.988和0.824,水合数为6.07;甲烷气体与SH2站位沉积物和冰粉合成的甲烷水合物也为I型,其大笼和小笼占有率分别为0.987和0.887,水合数为5.98;SH2站位沉积物使合成的甲烷水合物的小笼占有率提高、水合数降低、水合物饱和度提高.激光拉曼光谱结果证实了上述结果的准确性.该文为甲烷水合物测试提供了重要的方法参考.Methane hydrates(CH4·nH2O)mainly composed of methane and water are ice-like crystalline clathrate compounds.They form a large natural gas reservoir due to their abundance.Solid-state NMR and laser Raman spectroscopy are two techniques which can be used for microscopic analysis for methane hydrates.In this paper,a low temperature solid-state13C NMR technology was used to study the structures of synthesized methane hydrates.It was shown that1H high power decoupling(1H HPDEC)had a better performance than13C cross polarization(13C CP)for quantitative analysis for methane hydrates.The NMR results indicated that the methane hydrates synthesized by mixing methane gas with ice powder had a type-I structure,with large and small cage occupancies of0.988and0.824,respectively,and a hydrate number of6.07.Methane hydrates synthesized by mixing the methane gas with the continental slope of the South China Sea site SH2sediments and ice powder also had a type-I structure,with large and small cage occupancies of0.987and0.887,respectively,and a hydrate number of5.98.The result showed that addition of site SH2sediments could reduce hydrate number of methane hydrates,and make small cage occupancy and hydrate saturation higher,which were verified by laser Raman spectroscopy.
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