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The dissolution of silicate minerals by CO2-rich fluids and the subsequent precipitation of CO2 as carbonate minerals represent a means of permanently storing anthropogenic CO2 waste products in a solid and secure form. Modelling the progression of these reactions is hindered by our poor understanding of the rates of mineral dissolution–precipitation reactions and mineral surface properties in natural...
Groundwater chemical fluxes from the Pingtung Plain in SW Taiwan to the ocean were determined by analysing waters from 43 wells at varying depths through a 237m deep window across the Pingtung Plain, for major dissolved cations, anions, dissolved SiO 2 , and stable isotopic composition of O and H, and computing their subsurface water fluxes from measurements of hydraulic heads and formation...
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