| The main anthropogenic greenhouse gas i.e.carbon dioxide(CO2)emitted from the traditional fossil energy including coal,oil and natural gas,has caused global climate change and a series of environmental issues.Hereby,it is urgent to mitigate CO2emissions.There have been many options to reduce CO2 emissions in recent years.Among these,the CO2 sequestration in deep coal seams with enhanced coalbed methane(CH4)recovery(CO2-ECBM)is a viable option to mitigate CO2 emissions.The optimum depth for CO2 sequestration in coal seams is recommended as 800-1000m,where CO2 exits in form of supercritical fluid(scCO2).Given the characteristics of scCO2 and coal matrix,multiple fluid-solid interactions do exist between them.The aforementioned interactions affect the pore structure and surface chemistry property of coals,thereby affecting validity regarding CO2 storage.In addition,the scCO2 can change the surrounded rocks of coal reservoir including roof and floor,thereby influencing the stability and safety regarding CO2 storge in target coal seams.Therefore,the interactions of scCO2-H2O and coal,roof(standstone)and floor(mudstone)were conducted in a self-designed high-pressure vessel for 8 months.The opereting temperature and pressure are 318.15 K and 12 MPa,respectively.Multiple characracting methods including CO2 adsorption,N2 adsorption and desorption,mercury instrusion,X-Ray diffractometer(XRD)and X-ray photoelectron spectroscopy(XPS)were adopted to determine the change of pore structure,mineral compositions and main functional groups of coal matrix,roof and floor before and after long-term scCO2-H2O exposure.Moreover,the volumetric method was used to measure the CO2 adsorption and desorption capability of coal samples before and after long-term scCO2-H2O exposure.The main conclusions derived from this study are as follows:(1)The long-term scCO2-H2O exposure changes the physicochemical property o f varios rank coals.On the one hand,the exposu re changes coal pore structure.Particularly,it decreases the micropore surface area of ZT coal,while i t increases that of DT and BLG coals.However,the long-term scCO2-H2O exposure shows minor effect on micropores of FY coal.Furthermore,the meso-macropore volume of all coals decreases after the long-term scCO2-H2O exposure.The exposre dependence of coal pore structure mainly arises from coal matrix swelling and mineral dissolution.Particularly,the exposure increases quartz content of ZT coal,while decreases the content of kaolinite and calcite of DT coal.When it comes to the other two coals,the exposre decreases the content of boehmite,kaolinite and calcite of BLG coal and the content of quartz and kaolinite of FY coal.On the other hand,the exposure alters surface chemistry prope y of coals.Results indicate that the content of oxygenic functional groups(C-O,C=O and COOH)and nitric functional groups(pyridine and oxid-N)reduces.These changes are mainly associated with CO2 chemisorption and small organic compouds extraction due to scCO2.(2)The long-term scCO2-H2O exposure shows different effects on CO2 adsorption equilibrium and kinetics on various rank coals.With repect to adsorption equilibrium,the Ono-Kondo(OK)lattice model can well describe CO2 adsorption equilibrium on coals before and after long-term scCO2 exposure.The model fitting results show that the maximum CO2 adsorption capacity of ZT and DT coals increases after exposure,while that of BLG and FY coals decreases.In addition,the long-term scCO2-H2O exposure decreases the isosteric heat of adsorption of CO 2 by 1.52-7.77%for all the coals.With respect to CO2 adsorption kinetics on coals,the process can be devided into two stages before and after long-term scCO2-H2O exposure,i.e.the initial fast stage and subsequent low stage.Compared with the pseudo-first-order model and pseudo-second-order model,the bidisperse model is of higher predictive accuracy for CO2 adsorption kinetics on coals before and after the long-term scCO2-H2O exposure.The model fitting results indicate that the exposure reduces the value of Dmacro/R2macroof coals,implying that scCO2 weakens the CO2 adsorption and diffusion rate within coal macropores.(3)The long-term scCO2-H2O exposure changes CO2 adsorption and desorption hysteresis loop on all coals.In comparison with raw coals,the hysteresis loop area of all the coals after exposure increase by 0.18-377.35%.Such change indicates that the long-term scCO2-H2O exposure is beneficial to CO2 storage in coal seams.(4)The long-term scCO2-H2O exposure changes the mineral composition and pore structure characteristics of sandstone and mudstone.Particularly,it reduces the content of dolomite and kaolinite in sandstone and the content of kaolinite and quartz in mudstone.The long-term scCO2-H2O exposure increases micropore surface area of sandstone and mudstone,the increasing amplitude of which is approximatedly 23.77%and 15.01%,respectively.Moreover,the long-term scCO2-H2O exposure increases the meso-and macropore volume of sandstone and mudstone by 5.74%and 4.60%,respectively.Next,the exposure increases the amount of open macropore of mudstone.Finally,the muil-fractal analysis show that the long-term scCO2-H2O exposure reduces the pore heterogeneity,while enhances the macroporous connectivity of sandstone and mudstone.Such results imply that the diffusion rate of CO2 in sandstone and mudstone are expected increased,which do not favor the stable storage of CO2 within coal seams.To sum up,the long-term scCO2-H2O exposure is capable of changing pore structure and function groups,therby affecting CO2 adsorption and desorption capability of coals.Moreover,the long-term scCO2-H2O exposure also alters mineral composition and pore structure of sandstone and mudstone,thereby affecting safety and stability of CO2 storage.The main results and conclusions devived from this study not only gain further insight into CO 2-ECBM,but also provide important basis to evaluate the validity,stability and safety regarding CO2 storage in target coal seams. |