Abstract
The feasibility of carbon mineralization relies on the carbonation efficiency of CO(2)-reactive minerals, which is largely governed by the water content and state within material mesopores. Yet, the pivotal role of confined water in regulating carbonation efficiency at the nanoscale is not well understood. Here, we show that the maximum CO(2) intake occurs at an optimal relative humidity (RH(opt)) when capillary condensation initiates within the hydrophilic mesopores. At this transition state, the pore becomes filled with metastable low-density water, providing an ideal docking site for CO(2) adsorption and forming a mixed metastable state of water/CO(2). We prove that RH(opt) depends on the mesopore size through a Kelvin-like relationship, which yields a robust engineering model to predict RH(opt) for realistic mineral carbonation. Building upon classical theories of phase transition in hydrophilic mesopores, this study unveils the capacity of the metastable water in CO(2) intake and enhances the high-efficiency carbon mineralization with natural ore and industrial wastes in real-world applications.