The water gas shift (WGS) reaction was conducted in the presence of two natural and two synthetic CaO-based sorbents. It was shown that such sorbents can affect the WGS in two ways: (i) by catalysis of the reaction and (ii) by altering the equilibrium position by abstraction of CO 2 from the gas phase. It was shown that CaO can significantly enhance the production of H 2 during the WGS reaction; however, a trade-off between the production of H 2 and contamination of the product gas with CO 2 (the “CO 2 slip”) has to be made. It was found that CaO catalyzes the WGS reaction. The carbonation reaction was very close to thermodynamic equilibrium, even at small contact times at 650 °C. However, the concentration of H 2 was significantly below that predicted from equilibrium considerations. In our experiments, once the sorbent had been fully carbonated, it was regenerated by heating to release the CO 2 so that it could be reused. In such a cyclic experiment, calcium magnesium acetate, a synthetic sorbent, was the best sorbent tested, albeit only over five cycles of reaction, with respect to the amount of H 2 produced. The other sorbents, especially limestone, revealed a decrease in the production of hydrogen with the number of cycles.
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Müller et al. (2009) studied this question.
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