Abstract
Abstract In this study, numerical simulations we re conducted to investigate the rise of pCO 2 in the ocean on a continental shelf by the leakage of CO 2 , which is originally stored in the aquifer under the seabed, in an extreme case. We conducted parameter studies in simple rectangular solid domains with uniform background flows to see the impacts of conditions of CO 2 leakage and those of seawater. The results show that temperature and the size of bubbles and droplets have reasonable impacts on the change of TCO 2 . Moreover, the background TCO 2 makes a larg e difference in the rise of pCO 2 .
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