Evaluating the potential of a sedimentary basin reservoir to securely store CO 2 benefits
from a comprehensive understanding of the geochemical reactions that take place once CO …

This is the second paper on principles of demineralization. The initial paper is dedicated to
the common definitions and the history of demineralization. In present work we review the …

Dissolution rates of calcite, dolomite and magnesite were measured at 25, 60, 100 and 150°
C at far from equilibrium conditions in 0.1 M NaCl solutions of pH from 3 to 6 as a function of …

Magnesite growth rates and step velocities have been measured systematically as a
function of temperature from 80 to 105° C and saturation state in 0.1 M NaCl solutions using …

Magnesite precipitation rates were measured at temperatures from 100 to 200° C as a
function of saturation state and reactive fluid composition in mixed flow reactors. Measured …

Assessment of the microbial impact on mineral dissolution is crucial for a predictive
understanding of basic (Ca, Mg bearing) silicate weathering and the associated CO2 …

The rate of dissolution of polycrystalline siderite planes has been measured at 25, 60, 80
and 100° C in 0.1 M (NaCl+ HCl) solutions and pH from 1 to 4.6 at far from equilibrium …

Ocean acidification from fossil fuel burning is lowering the mean global ocean saturation
state (Ω= C a 2+ CO 3 2− K sp′), thus increasing the thermodynamic driving force for …

Carbonic acid ionization and sodium bicarbonate and carbonate ion pair formation
constants have been experimentally determined in dilute hydrothermal solutions to 200° C …

We present here a methodology, using holographic interferometry, enabling to measure the
pure surface reaction rate constant of the dissolution of a mineral in water, unambiguously …