Shuaijun Li, Jidong Zhang, Yang Ge, Weixin Pang, Junjie Ren, Yuhang Gu, Keguang Zhou and Zhenyuan Yin*,
{"title":"井底压力对下伏含游离气藏三相含水合物沉积物降压能量回收的影响","authors":"Shuaijun Li, Jidong Zhang, Yang Ge, Weixin Pang, Junjie Ren, Yuhang Gu, Keguang Zhou and Zhenyuan Yin*, ","doi":"10.1021/acs.energyfuels.5c0021310.1021/acs.energyfuels.5c00213","DOIUrl":null,"url":null,"abstract":"<p >Methane hydrates are considered as the future clean energy resource. Geological exploration results indicate that the symbiosis of underlying gas is a typical characterization of natural gas hydrate (NGH) reservoirs. Co-production from NGH reservoir and underlying gas reservoir shows significant potential for future commercial production. However, the fluid production, thermal response, and sediment displacement evolution during co-production are still unclear and warrant investigation. In this study, we synthesized three-phase methane hydrate-bearing sediments with hydrate saturations of 12.0 and 26.0% at 15.0 °C and prepared the underlying gas reservoir with gas saturation of 87.7% at 17.5 °C. Fluid production and evolution of temperature and sediment displacement were examined during depressurization from the underlying gas reservoir under four bottom-hole pressures, <i>i.e.,</i> 8.0, 6.0, 4.0, and 2.0 MPa. A novel quantification method was developed for estimation of gas and water production from each reservoir. By lowering bottom-hole pressure from 8.0 to 2.0 MPa, gas recovery ratio increased by nearly 30% in both cases. Water production was significantly delayed compared with gas production and only started when water saturation of underlying gas reservoir reached above 40% in all cases. Increasing <i>S</i><sub>H</sub> from 12.0 to 26.0% result in a decrease in the minimum temperature of three-phase methane hydrate-bearing sediments from 7.5 °C to 2.5 °C. Displacement sensor monitors the downward displacement of the three-phase methane hydrate-bearing sediments during depressurization. The volume strain increases from 0.12 to 0.38% when decreasing BHP, while that for low <i>S</i><sub>H</sub> only increases 0.06%. Our findings expand the understanding of fluid production behaviour from three-phase methane hydrate-bearing sediments with underlying gas. It provides guidance in the optimization of producion strategy for future field-scale co-production tests.</p>","PeriodicalId":35,"journal":{"name":"Energy & Fuels","volume":"39 11","pages":"5391–5405 5391–5405"},"PeriodicalIF":5.3000,"publicationDate":"2025-03-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Effects of Bottom-Hole Pressure on Energy Recovery from Three-Phase Hydrate-Bearing Sediments with Underlying Free-Gas Reservoir via Depressurization\",\"authors\":\"Shuaijun Li, Jidong Zhang, Yang Ge, Weixin Pang, Junjie Ren, Yuhang Gu, Keguang Zhou and Zhenyuan Yin*, \",\"doi\":\"10.1021/acs.energyfuels.5c0021310.1021/acs.energyfuels.5c00213\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p >Methane hydrates are considered as the future clean energy resource. Geological exploration results indicate that the symbiosis of underlying gas is a typical characterization of natural gas hydrate (NGH) reservoirs. Co-production from NGH reservoir and underlying gas reservoir shows significant potential for future commercial production. However, the fluid production, thermal response, and sediment displacement evolution during co-production are still unclear and warrant investigation. In this study, we synthesized three-phase methane hydrate-bearing sediments with hydrate saturations of 12.0 and 26.0% at 15.0 °C and prepared the underlying gas reservoir with gas saturation of 87.7% at 17.5 °C. Fluid production and evolution of temperature and sediment displacement were examined during depressurization from the underlying gas reservoir under four bottom-hole pressures, <i>i.e.,</i> 8.0, 6.0, 4.0, and 2.0 MPa. A novel quantification method was developed for estimation of gas and water production from each reservoir. By lowering bottom-hole pressure from 8.0 to 2.0 MPa, gas recovery ratio increased by nearly 30% in both cases. Water production was significantly delayed compared with gas production and only started when water saturation of underlying gas reservoir reached above 40% in all cases. Increasing <i>S</i><sub>H</sub> from 12.0 to 26.0% result in a decrease in the minimum temperature of three-phase methane hydrate-bearing sediments from 7.5 °C to 2.5 °C. Displacement sensor monitors the downward displacement of the three-phase methane hydrate-bearing sediments during depressurization. The volume strain increases from 0.12 to 0.38% when decreasing BHP, while that for low <i>S</i><sub>H</sub> only increases 0.06%. Our findings expand the understanding of fluid production behaviour from three-phase methane hydrate-bearing sediments with underlying gas. 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Effects of Bottom-Hole Pressure on Energy Recovery from Three-Phase Hydrate-Bearing Sediments with Underlying Free-Gas Reservoir via Depressurization
Methane hydrates are considered as the future clean energy resource. Geological exploration results indicate that the symbiosis of underlying gas is a typical characterization of natural gas hydrate (NGH) reservoirs. Co-production from NGH reservoir and underlying gas reservoir shows significant potential for future commercial production. However, the fluid production, thermal response, and sediment displacement evolution during co-production are still unclear and warrant investigation. In this study, we synthesized three-phase methane hydrate-bearing sediments with hydrate saturations of 12.0 and 26.0% at 15.0 °C and prepared the underlying gas reservoir with gas saturation of 87.7% at 17.5 °C. Fluid production and evolution of temperature and sediment displacement were examined during depressurization from the underlying gas reservoir under four bottom-hole pressures, i.e., 8.0, 6.0, 4.0, and 2.0 MPa. A novel quantification method was developed for estimation of gas and water production from each reservoir. By lowering bottom-hole pressure from 8.0 to 2.0 MPa, gas recovery ratio increased by nearly 30% in both cases. Water production was significantly delayed compared with gas production and only started when water saturation of underlying gas reservoir reached above 40% in all cases. Increasing SH from 12.0 to 26.0% result in a decrease in the minimum temperature of three-phase methane hydrate-bearing sediments from 7.5 °C to 2.5 °C. Displacement sensor monitors the downward displacement of the three-phase methane hydrate-bearing sediments during depressurization. The volume strain increases from 0.12 to 0.38% when decreasing BHP, while that for low SH only increases 0.06%. Our findings expand the understanding of fluid production behaviour from three-phase methane hydrate-bearing sediments with underlying gas. It provides guidance in the optimization of producion strategy for future field-scale co-production tests.
期刊介绍:
Energy & Fuels publishes reports of research in the technical area defined by the intersection of the disciplines of chemistry and chemical engineering and the application domain of non-nuclear energy and fuels. This includes research directed at the formation of, exploration for, and production of fossil fuels and biomass; the properties and structure or molecular composition of both raw fuels and refined products; the chemistry involved in the processing and utilization of fuels; fuel cells and their applications; and the analytical and instrumental techniques used in investigations of the foregoing areas.