中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Nonempirical fractal permeability model and experimental verification of hydrate-bearing sediments based on heterogeneous distribution of particles

文献类型:期刊论文

作者Peng, Hao3,5,6; Li, Xiao-Sen2,4,5,6; Chen, Zhao-Yang2,4,5,6; Ji, Hong-Fei1,5,6; Zhang, Yu2,4,5,6; You, Chang-Yu3,5,6
刊名GEOENERGY SCIENCE AND ENGINEERING
出版日期2024-06-01
卷号237页码:18
关键词Natural gas hydrates Normalized permeability Fractal Porous media Pore morphology Heterogeneous
ISSN号2949-8929
DOI10.1016/j.geoen.2024.212773
通讯作者Chen, Zhao-Yang(chenzy@ms.giec.ac.cn)
英文摘要The one of the factors limiting production of gas-water is affected by sediments ' permeability. Evaluating the normalized permeability ( K n ) of sediments containing hydrates is necessary for analyzing the saturation (decomposition level) and flow capacity. The mistakes in K n prediction are frequently brought about by the assumption such as homogenous particles distribution and ignoring microscopic pore structure. To address the issue, a fractal-based nonempirical prediction model of K n was developed by modeling, parameter acquisition using SEM and Analyzer, experiment validation, error comparison with published data, and sensitivity analysis for evolution, respectively. Assuming that sediment skeleton particles were misaligned spherical particles of equal diameter. The heterogeneity of sediments was described by the vertical and horizontal distance ratio ( m ) and offset angle ( theta ) of the particles. This led to a novel approach for determining average tortuosity ( tau av,0 ) and tortuosity fractal dimension ( D tau,0 ). The viability of the model was confirmed by permeability measurement experiments. Additionally, using the measuring function of SEM, the maximum pore diameter of sediments was obtained. Furthermore, a comparison with earlier data demonstrated the effect. Considering heterogeneity, the average accuracy of Geometric Mean Variance in K n has increased to 9.66%. Finally, each parameter ' s impact on prediction was examined. At m = 1.357, D tau,0 grows symmetrically. K n,GC varies 15 times more with an increase in D tau,0 than K n,PF . All findings indicate that the new model is more likely to be forecasted K n for a variety of systems, including clayey-silt, sand, and silty-sand system, and especially in reflecting the heterogeneity.
WOS关键词METHANE HYDRATE ; POROUS-MEDIA ; GAS-PRODUCTION ; FLOW ; CONDUCTIVITY ; PERCOLATION ; TORTUOSITY
资助项目National Key R & D Program of China[2021YFC2800902] ; National Natural Science Foundation of China[51736009] ; Special Project for Marine Economy Development of Guangdong Province ; Guangdong Major Project of Basic and Applied Basic Research[202204910339] ; China Scholarship Council[GDNRC [2022] 43] ; [2020B0301030003]
WOS研究方向Energy & Fuels ; Engineering
语种英语
WOS记录号WOS:001223349600001
出版者ELSEVIER
资助机构National Key R & D Program of China ; National Natural Science Foundation of China ; Special Project for Marine Economy Development of Guangdong Province ; Guangdong Major Project of Basic and Applied Basic Research ; China Scholarship Council
源URL[http://ir.giec.ac.cn/handle/344007/41697]  
专题中国科学院广州能源研究所
通讯作者Chen, Zhao-Yang
作者单位1.Univ Sci & Technol China, Sch Energy Sci & Engn, Hefei, Peoples R China
2.CNOOC Res Inst, State Key Lab Nat Gas Hydrates, Beijing 100028, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Guangdong Prov Key Lab New & Renewable Energy Res, Guangzhou 510640, Guangdong, Peoples R China
5.CAS Key Lab Gas Hydrate, Guangzhou 510640, Guangdong, Peoples R China
6.Chinese Acad Sci, Guangzhou Inst Energy Convers, Guangzhou 510640, Guangdong, Peoples R China
推荐引用方式
GB/T 7714
Peng, Hao,Li, Xiao-Sen,Chen, Zhao-Yang,et al. Nonempirical fractal permeability model and experimental verification of hydrate-bearing sediments based on heterogeneous distribution of particles[J]. GEOENERGY SCIENCE AND ENGINEERING,2024,237:18.
APA Peng, Hao,Li, Xiao-Sen,Chen, Zhao-Yang,Ji, Hong-Fei,Zhang, Yu,&You, Chang-Yu.(2024).Nonempirical fractal permeability model and experimental verification of hydrate-bearing sediments based on heterogeneous distribution of particles.GEOENERGY SCIENCE AND ENGINEERING,237,18.
MLA Peng, Hao,et al."Nonempirical fractal permeability model and experimental verification of hydrate-bearing sediments based on heterogeneous distribution of particles".GEOENERGY SCIENCE AND ENGINEERING 237(2024):18.

入库方式: OAI收割

来源:广州能源研究所

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