Quantitative Estimation on Methane Storage Capacity of Organic-Rich Shales from the Lower Silurian Longmaxi Formation in the Eastern Sichuan Basin, China

• Published in: Journal of earth science (Wuhan, China) China), 2023-12, Vol.34 (6), p.1851-1860
• Main Authors: Guo, Xiaowen, Luo, Tao, Dong, Tian, Yang, Rui, Han, Yuanjia, Yi, Jizheng, He, Sheng, Shu, Zhiguo, Bao, Hanyong
• Format: Article
• Language: English
• Subjects: Biogeosciences; Bulk density; Carbon dioxide; Carbonates; Clay; Clay minerals; Earth and Environmental Science; Earth Sciences; Feldspars; Gas production; Geochemistry; Geology; Geotechnical Engineering & Applied Earth Sciences; High pressure; Lithofacies; Low pressure; Methane; Minerals; Moisture content; Natural gas exploration; Oil and gas exploration; Oil and gas production; Organic matter; Petroleum Geology; Porosity; Saturation; Sedimentary rocks; Shale; Shale gas; Shales; Silica; Silurian; Sorption; Storage capacity; Storage conditions; Surface area; Total organic carbon; Water content
• ISSN: 1674-487X; 1867-111X
• DOI: 10.1007/s12583-020-1394-7

The assessment of gas storage capacity is crucial to furthering shale gas exploration and development in the eastern Sichuan Basin, China. Eleven organic-rich shale samples were selected to carry out the high pressure methane sorption, low-pressure N 2 /CO 2 gas adsorption, and bulk and skeletal density measurements to investigate the methane storage capacity (MSC). Based on the relative content of clay, carbonates, quartz + feldspar, we grouped the 11 samples into three lithofacies: silica-rich argillaceous shale (CM-1), argillaceous/siliceous mixed shale (M-2), and clay-rich siliceous shale (S-3). The total porosity of the shale samples varies from 3.4% to 5.6%, and gas saturation ranges from 47% to 89%. The measured total gas amount ranges from 1.84 mg/g to 4.22 mg/g with the ratio of free gas to total gas amount ranging from 52.7% to 70.8%. Free gas with high content in the eastern Sichuan Basin may be the key factor controlling amount of shale gas production. The TOC content critically controls the MSC of shales, because micropore, mesopore volumes and the specific surface areas associated with organic matter provide the storage sites for the free and adsorbed gas. The methane sorption capacities of samples from different lithofacies are also affected by clay minerals and moisture content. Clay minerals can provide additional surface areas for methane sorption, and water can cause a 7.1%–42.8% loss of methane sorption capacity. The total porosity, gas-bearing porosity, water saturation, free gas and adsorbed gas number of samples from different lithofacies show subtle differences if the shale samples had similar TOC contents. Our results suggest that, in the eastern Sichuan Basin, clay-rich shale lithofacies is also prospecting targets for shale gas production.