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(Calculated once Scilit publication data is synced: current year − year of first publication + 1)
<mml:math display="inline"><mml:msub><mml:mi>p</mml:mi><mml:mrow><mml:mi>C</mml:mi><mml:msub><mml:mi>O</mml:mi><mml:mn>2</mml:mn></mml:msub></mml:mrow></mml:msub></mml:math>pCO2 gradient. Minor transport of oxide ions and hydroxide ions in the molten carbonate is observed under a <mml:math display="inline"><mml:msub><mml:mi>p</mml:mi><mml:msub><mml:mi>O</mml:mi><mml:mn>2</mml:mn></mml:msub></mml:msub></mml:math>pO2 gradient and <mml:math display="inline"><mml:msub><mml:mi>p</mml:mi><mml:mrow><mml:msub><mml:mi>H</mml:mi><mml:mn>2</mml:mn></mml:msub><mml:mi>O</mml:mi></mml:mrow></mml:msub></mml:math>pH2O gradient, respectively. This offers an alternative understanding and operation of molten carbonate dual-phase membranes.No biography provided yet