中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Methane hydrate phase transition in marine clayey sediments: Enhanced structure change and solid migration

文献类型:期刊论文

作者Kou, Xuan1,2; Zhang, Heng1,2,3; Li, Xiao-Sen1,2; Chen, Zhao-Yang1,2; Wang, Yi1,2
刊名APPLIED ENERGY
出版日期2024-08-15
卷号368页码:17
关键词Gas hydrate Methane gas Structure change Solid migration Marine sediments Cold seeps
ISSN号0306-2619
DOI10.1016/j.apenergy.2024.123485
通讯作者Li, Xiao-Sen(lixs@ms.giec.ac.cn) ; Wang, Yi(wangyi@ms.giec.ac.cn)
英文摘要Natural gas hydrates are abundant in marine sediments and have great potential for resource development. However, there is still a lack of clarity regarding the impact of hydrate phase transition on the structure change of marine sediments. Hence, we conducted in-situ microscale experiments of hydrate phase transition in clayey sediments obtained from the active Haima cold seep area in South China Sea. By utilizing advanced X-ray Computed Tomography technology and a controlled method of hydrate phase transition, we successfully observed the dynamic behaviors of hydrate formation and decomposition, and revealed their effects on sediment structure and solid migration. Our findings suggested that methane hydrates initially occupy primary pores while generating new pores and fractures in clayey sediments. These processes lead to changes in pore morphology and anisotropy, characterized by a decrease in the degree of anisotropy and an increase in fractural and shape factor of pores. During hydrate decomposition, methane hydrates tend to be reformed in clayey sediments before initiating the decomposition process. More significantly, the combining effects of hydrates reformation and decomposition lead to occurrence of enlarged pores in sediments, resulting in unpredictable structural failure of the sediment. Furthermore, the simulation results of solid migration in sediments revealed that the solid particles migrate towards the bottom of the sediments during hydrate formation, leading to the compaction of sediment structure. Conversely, during hydrate decomposition, the solid particles move significantly towards the upper region of the sediment due to fluid seepage through newly generated and enlarged pores. The structure change and solid migration mechanisms revealed in this study highlight the potential risks during hydrate phase transition such as sediment instability and sand production, offering valuable insights into efficient and secure hydrate exploitation.
WOS关键词NATURAL-GAS HYDRATE ; NUCLEAR-MAGNETIC-RESONANCE ; FLOW
资助项目National Natural Science Foundation China[52306286] ; National Natural Science Foundation China[52122602] ; National Natural Science Foundation China[52127815] ; China Postdoctoral Science Foundation[2022M723160] ; Guangdong Special Support Program Local innovation and entrepreneurship team project[2019BT02L278] ; Special Project for Marine Economy Development of Guangdong Province[GDNRC[2022]43] ; Special Project for Marine Economy Development of Guangdong Province[GDNRC[2022]45] ; Fundamental Research & Applied Fundamental Research Major Project of Guangdong Province[2019B030302004] ; Fundamental Research & Applied Fundamental Research Major Project of Guangdong Province[2020B0301030003]
WOS研究方向Energy & Fuels ; Engineering
语种英语
WOS记录号WOS:001333519800001
出版者ELSEVIER SCI LTD
资助机构National Natural Science Foundation China ; China Postdoctoral Science Foundation ; Guangdong Special Support Program Local innovation and entrepreneurship team project ; Special Project for Marine Economy Development of Guangdong Province ; Fundamental Research & Applied Fundamental Research Major Project of Guangdong Province
源URL[http://ir.giec.ac.cn/handle/344007/43187]  
专题中国科学院广州能源研究所
通讯作者Li, Xiao-Sen; Wang, Yi
作者单位1.Chinese Acad Sci, Guangzhou Inst Energy Convers, CAS Key Lab Gas Hydrate, Guangzhou 510640, Peoples R China
2.Guangdong Prov Key Lab New & Renewable Energy Res, Guangzhou 510640, Peoples R China
3.Univ Sci & Technol China, Hefei 230026, Anhui, Peoples R China
推荐引用方式
GB/T 7714
Kou, Xuan,Zhang, Heng,Li, Xiao-Sen,et al. Methane hydrate phase transition in marine clayey sediments: Enhanced structure change and solid migration[J]. APPLIED ENERGY,2024,368:17.
APA Kou, Xuan,Zhang, Heng,Li, Xiao-Sen,Chen, Zhao-Yang,&Wang, Yi.(2024).Methane hydrate phase transition in marine clayey sediments: Enhanced structure change and solid migration.APPLIED ENERGY,368,17.
MLA Kou, Xuan,et al."Methane hydrate phase transition in marine clayey sediments: Enhanced structure change and solid migration".APPLIED ENERGY 368(2024):17.

入库方式: OAI收割

来源:广州能源研究所

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