Gas-Bearing Property in Deep Marine Shale and Its Micro Controlling Factors: Evidence from the Lower Silurian Longmaxi Formation in Southern Sichuan, China

Author:

Wang Xin123,Zeng Jianhui12ORCID,Chen Jinhui45ORCID,Jiang Zhenxue13,Xue Zixin13,Kong Xiangye123ORCID,Wang Qianyou13,Jia Kunkun12

Affiliation:

1. 1 State Key Laboratory of Petroleum Resources and Prospecting China University of Petroleum Beijing 102249 China cup.edu.cn

2. 2 College of Geosciences China University of Petroleum Beijing 102249 China cup.edu.cn

3. 3 Unconventional Natural Gas Institute China University of Petroleum Beijing 102249 China cup.edu.cn

4. 4 School of Public Policy and Management Tsinghua University Beijing 100084 China tsinghua.edu.cn

5. 5 High-Tech Research and Development Center Ministry of Science and Technology Beijing 100044 China most.go.th

Abstract

Abstract The gas content in shale reservoirs is often determined by the micro storage and sealing capacities of the reservoir. Deep shale reservoirs are in the high- or over-thermale maturity stage and have complex pore structure and connectivity, which are highly heterogeneous in vertical distribution. Research on the gas-bearing property of deep shale reservoirs is limited by these complex microscopic conditions. To analyze the gas-bearing characteristics of deep shale reservoirs, this work collected and summarized data on total organic carbon content, mineral composition, porosity, water saturation, and gas content measured on-site for the Longmaxi Formation in the Sichuan Basin in southern Sichuan, China. Then, experimental methods, such as X-ray photoelectron spectroscopy, transmission electron microscope, low-pressure N2 adsorption, spontaneous imbibition, and high-pressure methane adsorption, were used to analyze the micro storage and sealing capacities of the deep shale reservoirs. The results show that, different from shallow shale reservoirs (<3500 m), deep shale reservoirs have a higher graphitization degree and water saturation. An abundance of graphite structures often leads to weak resistance of organic matter to compression, deformation, or even collapse of pores in organic matter and severe damage to the gas storage space. However, a higher degree of graphitization can enhance the ability of the shale reservoirs to adsorb gas and self-sealing. The high water saturation in the reservoirs can interact with clay minerals and negatively affect the gas accumulation, storage, and transmission capacities of the shale reservoirs. However, the upper shale reservoirs with higher water saturation can seal the lower shale reservoirs, helping it preserve shale gas. Based on the vertical distribution of graphite structure, clay minerals contents, lithofacies, and water content in deep shale reservoirs, the essential microscopic conditions for deep shale reservoirs to have high gas content were proposed. This paper provides a detailed explanation and evaluation of deep shale’s storage and sealing capacities at the microscopic scale and can serve as a reference for further identifying the patterns for high-yield and rich shale gas reservoirs and improving deep shale gas exploration technologies.

Funder

National Natural Science Foundation of China

Publisher

GeoScienceWorld

Subject

Geology

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