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Study on the evolution mechanism of rock properties in CO2-based EGS based on rock microstructure

Authors

Xiao,  Peng
IUGG 2023, General Assemblies, 1 General, International Union of Geodesy and Geophysics (IUGG), External Organizations;

Dou,  Bin
IUGG 2023, General Assemblies, 1 General, International Union of Geodesy and Geophysics (IUGG), External Organizations;

Tian,  Hong
IUGG 2023, General Assemblies, 1 General, International Union of Geodesy and Geophysics (IUGG), External Organizations;

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Citation

Xiao, P., Dou, B., Tian, H. (2023): Study on the evolution mechanism of rock properties in CO2-based EGS based on rock microstructure, XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) (Berlin 2023).
https://doi.org/10.57757/IUGG23-4194


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021633
Abstract
The properties of rocks, especially the thermal properties, porosity and permeability properties, are of great significance to accurately predict the operational performance of Enhanced Geothermal Systems (EGS). In order to reveal the evolution mechanism of rock properties of CO2-based EGS reservoir during geothermal exploitation, experiments on the interaction between the mixed fluid of CO2 and water (the proportion of water is 0, 51.205, 100%) and granite were carried out. Based on the change of microstructure characteristics of rock samples, the changing mechanism of rock properties is analyzed. The results show that the properties of rock samples exposed to pure CO2 change most weakly, while those exposed to water change most dramatically. The porosity and permeability of rock samples exposed to water increase by 236.70% and 7497.17%, respectively, while the thermal conductivity and thermal diffusion coefficient decrease by 21.55% and 22.53%, respectively. The change of rock properties is closely related to the change of rock microstructure. The main mechanisms of microstructure change include thermal fracture caused by thermal stress, chemical reaction between fluid and rock, and the increase of micropores caused by CO2 extraction of water inside rock. The microstructure change mechanism of rock samples is different in different reaction systems. Although the mixed fluid of CO2 and water is weakly acidic and reacts with the reservoir rocks, the structure changes are the most drastic, but secondary minerals will fill the new micro-cracks and pores, delaying the influence of chemical reactions on the changes of rock properties.