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Natural Structural Transition of Gas Hydrates From sI to sII in the Deep Seafloor
Ma, Liang1,2,3,4; Luan, Zhendong1,2,3,4; Du, Zengfeng1,2; Wang, Minxiao1,2; Li, Lianfu4; Xi, Shichuan4; Zhang, Yitong1,2,3; Zhang, Xiong1,2,3; Zhang, Xin1,2,3,4
2024-06-28
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
卷号51期号:12页码:10
通讯作者Zhang, Xin(xzhang@qdio.ac.cn)
摘要The evolution of gas hydrates influenced by the seawater environment is unknown. We present a model of structural transformation from sI hydrate to sII hydrate due to the influence of seawater environment and vent fluid in nature through in situ experiments of gas hydrate formation in the Haima cold seep area. The in situ experimental results indicate that gas hydrates preferentially form as sI hydrates even in cold seep environments where C2+ hydrocarbons are present. During subsequent evolution, the sI hydrates could restructured at the effect of seawater environment and vent fluid, causing transformation to sII hydrates under the influence of hydrate stability. The supply of gas and direct contact with seawater environment are critical factors for structural transformation. Such structural transformation is the result of gas hydrates seeking thermodynamic stability and may be common in active cold seep areas. Plain Language Summary At high pressures and low temperatures, methane molecules are able to be captured by water in a solid hydrate state, known as natural gas hydrate. The significance of the abundant reserves of natural gas hydrates in the oceans, both in terms of global climate issues and energy resources, has been widely recognised. Since most natural gas reservoirs are dominated by methane (>90%), it is generally accepted that gas hydrates in the oceans tend to be structure I. However, through a field experiment in an active cold seep area, we found that newly generated gas hydrates under the influence of the same cold seep area were of structure I, whereas naturally exposed gas hydrates that had existed for a long period of time on the seafloor were instead of structure II. Based on this, we propose a model of structural transformation (structure I to structure II) of gas hydrates under the influence of seawater environment and vent fluid. This structural transformation may be a natural phenomenon that is common in active cold seep areas.
关键词gas hydrates in situ detection structural transition Raman spectroscopy
DOI10.1029/2023GL106839
收录类别SCI
语种英语
资助项目National Natural Science Foundation of China ; Laoshan laboratory Science and Technology Innovation Project[LSKJ202203101] ; Strategic Priority Research Program, CAS[XDB42040305] ; Young Taishan Scholars Program[tsqn201909158] ; Key Project of Ocean Research Center, Chinese Academy of Sciences[COMS2020J03] ; Qingdao science and technology benefit the people demonstration project ; [42221005] ; [52001303] ; [42049582]
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:001247584000001
出版者AMER GEOPHYSICAL UNION
WOS关键词CLATHRATE HYDRATE ; RAMAN ; SLOPE ; DECOMPOSITION ; GEOCHEMISTRY
引用统计
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/186564
专题海洋地质与环境重点实验室
通讯作者Zhang, Xin
作者单位1.Chinese Acad Sci, Key Lab Ocean Observat & Forecasting, Key Lab Marine Geol & Environm, Qingdao, Peoples R China
2.Chinese Acad Sci, Inst Oceanol, Ctr Deep Sea Res, Ctr Ocean Mega Sci, Qingdao, Peoples R China
3.LaoShan Lab, Qingdao, Peoples R China
4.Univ Chinese Acad Sci, Beijing, Peoples R China
第一作者单位深海极端环境与生命过程研究中心
通讯作者单位深海极端环境与生命过程研究中心
推荐引用方式
GB/T 7714
Ma, Liang,Luan, Zhendong,Du, Zengfeng,et al. Natural Structural Transition of Gas Hydrates From sI to sII in the Deep Seafloor[J]. GEOPHYSICAL RESEARCH LETTERS,2024,51(12):10.
APA Ma, Liang.,Luan, Zhendong.,Du, Zengfeng.,Wang, Minxiao.,Li, Lianfu.,...&Zhang, Xin.(2024).Natural Structural Transition of Gas Hydrates From sI to sII in the Deep Seafloor.GEOPHYSICAL RESEARCH LETTERS,51(12),10.
MLA Ma, Liang,et al."Natural Structural Transition of Gas Hydrates From sI to sII in the Deep Seafloor".GEOPHYSICAL RESEARCH LETTERS 51.12(2024):10.
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