The equilibrium fractionation factor between two phases is of importance for the understanding of many planetary and environmental processes. Although thermodynamic equilibrium can be achieved between minerals at high temperature, many natural processes involve reactions between liquids or aqueous solutions and solids. For crystals, the fractionation factor a can be theoretically determined using a statistical thermodynamic approach based on the vibrational properties of the phases. These calculations are mostly performed in the harmonic approximation, using empirical or ab-initio force fields. In the case of aperiodic and dynamic systems such as liquids or solutions, similar calculations can be done using finite-size molecular clusters or ...
Hydrogen fractionation laws between selected hydrous minerals (brucite, kaolinite, lizardite, and gi...
The theoretical determination of the isotopic fractionation between an aqueous solution and a minera...
isotopic fractionation between minerals and water, as predicted by first-principles calculations
The equilibrium fractionation factor between two phases is of importance for the understanding of ma...
By combining path-integrals molecular dynamics simulations with the accurate MB-pol potential energy...
The shift in chemical equilibria due to isotope substitution is frequently exploited to obtain insig...
The shift in chemical equilibria due to isotope substitution is frequently exploited to obtain insig...
At room temperature, the quantum contribution to the kinetic energy of a water molecule exceeds the ...
Experimental data for hydrogen isotope and, in general, stable isotope fractionation between mineral...
A dual QM and MM approach for computing equilibrium isotope effects has been described. In the first...
The stable isotopes of water are extensively used as tracers in many fields of research. For this us...
International audienceHydrogen fractionation laws between selected hydrous minerals (brucite, kaolin...
Isotopic fractionation factors for oxygen, hydrogen and silicon have been calculated using first-pri...
By combining path-integrals molecular dynamics simulations with the accurate MB-pol potential energy...
Hydrogen fractionation laws between selected hydrous minerals (brucite, kaolinite, lizardite, and gi...
Hydrogen fractionation laws between selected hydrous minerals (brucite, kaolinite, lizardite, and gi...
The theoretical determination of the isotopic fractionation between an aqueous solution and a minera...
isotopic fractionation between minerals and water, as predicted by first-principles calculations
The equilibrium fractionation factor between two phases is of importance for the understanding of ma...
By combining path-integrals molecular dynamics simulations with the accurate MB-pol potential energy...
The shift in chemical equilibria due to isotope substitution is frequently exploited to obtain insig...
The shift in chemical equilibria due to isotope substitution is frequently exploited to obtain insig...
At room temperature, the quantum contribution to the kinetic energy of a water molecule exceeds the ...
Experimental data for hydrogen isotope and, in general, stable isotope fractionation between mineral...
A dual QM and MM approach for computing equilibrium isotope effects has been described. In the first...
The stable isotopes of water are extensively used as tracers in many fields of research. For this us...
International audienceHydrogen fractionation laws between selected hydrous minerals (brucite, kaolin...
Isotopic fractionation factors for oxygen, hydrogen and silicon have been calculated using first-pri...
By combining path-integrals molecular dynamics simulations with the accurate MB-pol potential energy...
Hydrogen fractionation laws between selected hydrous minerals (brucite, kaolinite, lizardite, and gi...
Hydrogen fractionation laws between selected hydrous minerals (brucite, kaolinite, lizardite, and gi...
The theoretical determination of the isotopic fractionation between an aqueous solution and a minera...
isotopic fractionation between minerals and water, as predicted by first-principles calculations