The dissolution rates of olivine have been considered by a plethora of studies in part due to
its potential to aid in carbon storage and the ease in obtaining pure samples for laboratory …

Reactions occurring at mineral–fluid interfaces are important in all geochemical processes
and essential for the cycling of elements within the Earth. Understanding the mechanism of …

Continued global use of fossil fuels places a premium on develo** technology solutions to
minimize increases in atmospheric CO2 levels. CO2 storage in reactive basalts might be …

Silicate hydration is prevalent in natural and technological processes, such as, mineral
weathering, glass alteration, zeolite syntheses and cement hydration. Tricalcium silicate …

Fluid–mineral and fluid–rock interfaces are key parameters controlling the reactivity and fate
of fluids in reservoir rocks and aquifers. The interface dynamics through space and time …

Carbon capture and storage (CCS) is likely to be a critical technology to achieve large
reductions in global carbon emissions over the next century. Research on the subsurface …

A multitude of natural processes and technical applications require our ability to provide a
reliable prediction of crystal surface reactivity. During the last decades, the detailed analysis …

Many areas of science and industry require a fundamental understanding of crystal
dissolution. Examples are diverse and include chemical weathering, pharmaceutical …

We report measurements of the calcite dissolution rate in CO 2-saturated water at pressures
ranging from (6.0 to 13.8) MPa and temperatures from (323 to 373) K. The rate of calcite …

Conspectus The reactivity of carbonate and silicate minerals is at the heart of porosity and
pore geometry changes in rocks injected with CO2, which ultimately control the evolution of …