Literature DB >> 24810708

In situ study of CO₂ and H₂O partitioning between Na-montmorillonite and variably wet supercritical carbon dioxide.

John S Loring1, Eugene S Ilton, Jeffrey Chen, Christopher J Thompson, Paul F Martin, Pascale Bénézeth, Kevin M Rosso, Andrew R Felmy, Herbert T Schaef.   

Abstract

Shale formations play fundamental roles in large-scale geologic carbon sequestration (GCS) aimed primarily to mitigate climate change and in smaller-scale GCS targeted mainly for CO2-enhanced gas recovery operations. Reactive components of shales include expandable clays, such as montmorillonites and mixed-layer illite/smectite clays. In this study, in situ X-ray diffraction (XRD) and in situ infrared (IR) spectroscopy were used to investigate the swelling/shrinkage and H2O/CO2 sorption of Na(+)-exchanged montmorillonite, Na-SWy-2, as the clay is exposed to variably hydrated supercritical CO2 (scCO2) at 50 °C and 90 bar. Measured d001 values increased in stepwise fashion and sorbed H2O concentrations increased continuously with increasing percent H2O saturation in scCO2, closely following previously reported values measured in air at ambient pressure over a range of relative humidities. IR spectra show H2O and CO2 intercalation, and variations in peak shapes and positions suggest multiple sorbed types of H2O and CO2 with distinct chemical environments. Based on the absorbance of the asymmetric CO stretching band of the CO2 associated with the Na-SWy-2, the sorbed CO2 concentration increases dramatically at sorbed H2O concentrations from 0 to 4 mmol/g. Sorbed CO2 then sharply decreases as sorbed H2O increases from 4 to 10 mmol/g. With even higher sorbed H2O concentrations as saturation of H2O in scCO2 was approached, the concentration of sorbed CO2 decreased asymptotically. Two models, one involving space filling and the other a heterogeneous distribution of integral hydration states, are discussed as possible mechanisms for H2O and CO2 intercalations in montmorillonite. The swelling/shrinkage of montmorillonite could affect solid volume, porosity, and permeability of shales. Consequently, the results may aid predictions of shale caprock integrity in large-scale GCS as well as methane transmissivity in enhanced gas recovery operations.

Entities:  

Year:  2014        PMID: 24810708     DOI: 10.1021/la500682t

Source DB:  PubMed          Journal:  Langmuir        ISSN: 0743-7463            Impact factor:   3.882


  4 in total

1.  Intercalation and retention of carbon dioxide in a smectite clay promoted by interlayer cations.

Authors:  L Michels; J O Fossum; Z Rozynek; H Hemmen; K Rustenberg; P A Sobas; G N Kalantzopoulos; K D Knudsen; M Janek; T S Plivelic; G J da Silva
Journal:  Sci Rep       Date:  2015-03-05       Impact factor: 4.379

2.  Self-diffusivity, M-S and Fick diffusivity of CO2 in Na-clay: The influences of concentration and temperature.

Authors:  Haixiang Hu; Yanfei Xing; Xiaochun Li
Journal:  Sci Rep       Date:  2017-07-14       Impact factor: 4.379

3.  Image-based modeling of gas adsorption and deformation in porous media.

Authors:  Sahar Bakhshian; Zhuofan Shi; Muhammad Sahimi; Theodore T Tsotsis; Kristian Jessen
Journal:  Sci Rep       Date:  2018-05-29       Impact factor: 4.379

4.  Effects of Moisture Contents on Shale Gas Recovery and CO2 Sequestration.

Authors:  Juan Zhou; Zhehui Jin; Kai H Luo
Journal:  Langmuir       Date:  2019-06-18       Impact factor: 3.882

  4 in total

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