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The effect of temperature and pressure on the adsorption of CO2 and CH4 gases on calcite (104) has been studied by means of classical molecular dynamics. The results show that carbon dioxide greatly improves methane desorption in the 323–373 K range, even at low CO2 concentrations. However, this effect is less pronounced for very high temperatures (423 K), where most of the methane is desorbed and...
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