Developing a new hydrate saturation calculation model for hydrate-bearing sediments

被引:61
作者
Dong, Huaimin [1 ,2 ]
Sun, Jianmeng [1 ]
Zhu, Jinjiang [3 ]
Liu, Lei [4 ]
Lin, Zhenzhou [5 ]
Golsanami, Naser [1 ,6 ,7 ]
Cui, Likai [1 ]
Yan, Weichao [1 ]
机构
[1] China Univ Petr East China, Sch Geosci, Qingdao 266580, Shandong, Peoples R China
[2] Heriot Watt Univ, Sch Energy Geosci Infrastruct & Soc, Inst Petr Engn, Edinburgh EH14 4AS, Midlothian, Scotland
[3] Changqing Oilfield Co, PetroChina, Oil Prod Plant 12, Xian 710200, Shaanxi, Peoples R China
[4] China Univ Petr East China, Sch Petr Engn, Qingdao 266580, Shandong, Peoples R China
[5] Chinese Acad Geol Sci, Inst Geophys & Geochem Explorat, Langfang 065000, Peoples R China
[6] Shandong Univ Sci & Technol, State Key Lab Min Disaster Prevent & Control, Qingdao 266590, Shandong, Peoples R China
[7] Shandong Univ Sci & Technol, Coll Min & Safety Engn, Qingdao 266590, Shandong, Peoples R China
基金
中国国家自然科学基金;
关键词
Hydrate-bearing sediments; Microscopic distribution; Hydrate saturation; Saturation exponent; Electrical properties; DIFFUSION-LIMITED AGGREGATION; ELECTRICAL-RESISTIVITY; METHANE HYDRATE; GAS; RESISTANCE; XENON;
D O I
10.1016/j.fuel.2019.03.038
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
This study incorporates X-ray computed tomography (CT) technology into the in-situ observation of the xenon hydrate formation process in sand sediments under excess gas conditions. While the scanning images were used to obtain microscopic distribution information of the hydrate, we implemented the finite element method (FEM) to calculate the resistivity of the hydrate-bearing samples obtained from scanning images. Consequently, it was observed that the resistivity index (RI) versus hydrate saturation (S-h) data matched better with our new calculation model rather than the simple Archie formula fitting model (i.e. experimental fitting model). Besides, we calculated the resistivity versus the hydrate saturation curves based on digital rock models with idealized hydrate distributions. These distributions included adhesive type, cemented type and scattered type. Observation of microscopic distribution and simulation results indicated that the resistivity versus hydrate saturation exhibited certain differences for the three types of hydrate distributions. We also found that saturation exponent (n) is a function of the hydrate saturation (S-h), which can be applied in the proposed new calculation model in order to calculate the resistivity versus hydrate saturation data. This suggests that the established model is a useful methodology for the purpose of saturation calculations and reservoir identification in hydrate-bearing sediments.
引用
收藏
页码:27 / 37
页数:11
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