“…The evident desorption peak in the temperature range of 800–1000 °C is attributed to strong basic sites such as bidentate carbonate species, which react with surface carbon species generated, for example, in the methane decomposition reaction (CH 4 → C + H 2 ), resulting in lower carbon deposition. ,,,, It is noteworthy that Sr promotion resulted in peaks in the range of ≈800 to 900 °C (Figure B,D), which were obviously related to the strong basic site, leading to an increase in the total peak area. ,,,,, The increased peak area signifies a higher amount of CO 2 adsorption, combination, and dissociation, resulting from the enhanced basicity of the catalysts. In addition, strongly basic sites are widely known to have beneficial effects on the activation of CO 2 , ,,− ,, that is, oxygen species generated from CO 2 dissociation and/or bidentate carbonate species on the basic sites are accepted by the surrounding oxygen vacancies . Hence, a large amount of CO 2 adsorption can contribute to the production of a significant amount of oxygen species.…”