Abstract
The major sedimentary basins in China contain abundant shale gas resources to be explored, and the exploration of shale gas has received more attention in recent years. Shale gas exists mainly in two states, i.e., free and adsorbed. The latter mainly exists on the surface of media, including organic matter and clay minerals, etc., but its adsorption state remains unknown. In this paper, we take the Longmaxi Formation marine shale in the southern Sichuan Basin of southern China as the research object. The state of methane molecule adsorption on different media in marine shales is analyzed by conducting mineral composition analysis, TOC content analysis, isothermal adsorption experiments, FIB-SEM, and FIB-HIM experiments on the core samples referring to previous research. The conclusions are as follows: the adsorbed gas mainly exists in the organic-matter pores, which feature excellent roundness and connectivity with a large number of small pores inside like a hive. The surface of the organic matter contains many adsorption sites, featuring strong adsorption capacity and making methane molecules continuously distributed on the internal surface of the organic-matter pores. The organic matter has a large specific surface area and is lipophilic, which offers an ideal condition for the adsorption of methane molecules. Part of the adsorbed gas exists in the pores of clay minerals, which are lamellar and triangular. The surface of clay minerals contains fewer adsorption sites, featuring poorer adsorption capacity and making methane molecules discontinuously distributed on the surface of the clay minerals. The clay minerals have a smaller specific surface area than the organic matter, thus featuring a smaller space for adsorption. The clay minerals are hydrophilic. In addition to methane molecules, mixed-layer illite/smectite (I/S) and chlorite also adsorb water molecules. The illite surface adsorbs mainly water molecules and, to a lesser extent, methane molecules. Finally, the adsorption state patterns of methane molecules on organic matter and clay minerals were summarized.
Highlights
In recent years, with the improvement in geological ideas as well as the advancement of good horizontal drilling and hydraulic fracturing technologies, the target of oil and gas exploration has changed from conventional clastic and carbonate reservoirs to unconventional shale ones, and great success in shale gas exploration has been achieved in North America (Curtis, 2002)
Li et al (2017) concluded from a study on the shales of the Lower Cambrian Niutitang Formation in the Fenggang Block, northern Guizhou, southern China, that the methane adsorption quantity of shales is related to organic carbon content, clay minerals, organic matter pore morphology, pressure, temperature and water saturation (Li et al, 2017)
Gao et al (2018) concluded that adsorbed gas is an important state of shale gas, mainly existing on the surface or inside the pores of clay minerals and organic matter particles and that the adsorption characteristics of shale play a crucial role in gas content
Summary
With the improvement in geological ideas as well as the advancement of good horizontal drilling and hydraulic fracturing technologies, the target of oil and gas exploration has changed from conventional clastic and carbonate reservoirs to unconventional shale ones, and great success in shale gas exploration has been achieved in North America (Curtis, 2002). Li et al (2017) concluded from a study on the shales of the Lower Cambrian Niutitang Formation in the Fenggang Block, northern Guizhou, southern China, that the methane adsorption quantity of shales is related to organic carbon content, clay minerals, organic matter pore morphology, pressure, temperature and water saturation (Li et al, 2017).
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.