Abstract--Analytical data from aqueous dissolution studies of minerals, mineral systems, and naturally equilibrated so-Jutions such as surface waters and groundwaters provide the basic ingredients necessary tocalculate comparative solubility (or activity) products (CKs) and comparative free energies of formation (CAGf ~ of possible minerals or hypothetical min-erals. Using a thermodynamic approach, quasi-thermodynamic values are obtained which can help in understanding the relative stabilities of different but similar materials and changes in reacting systems. Illite equilibrated solutions demon-strated that: 1) there is a 5 kcal spread in comparative free energies of formation of the five illites used, 2) the comparative stabilities remain...
Thermodynamic models of Essentuki and Nagutsky fields of Caucasian Mineral Waters deposits (KMW) are...
The evolution of the water chemistry and secondary mineral development in the vicinity of the near-f...
Evolving pressure-temperature conditions during metamorphism drive changes in the stable mineral ass...
ABSTRACT: A method for estimating Gibbs free energies and stabilities of clay minerals i proposed fo...
Gibbs free energies of formation ({Delta}G{degree}{sub f}) for several structurally related U(VI) mi...
Mineral stability relations in the system A120a-$iO•-H,20 were investigated via the aqueous ilica-de...
Abstract-A thermodynamic analysis of F-Cl-OH partitioning between minerals and hydrothermal fluids h...
The mineral scale that deposits in digesters and bleach plants is formed by a chemical precipitation...
lower activities ofAI 3+ when obtained by a speciation procedure (fractionation with an ionic column...
The formation of a solid mineral deposit can cause major problems in the conduct of industrial proce...
Abstract The activities of thermodynamic components of clay minerals corresponding i composition to ...
Analysis of phase diagrams and cation distributions within crystalline solutions as means of obtaini...
Solubility equilibria are related to thertnodynainic properties in general and chemical po-tentials ...
The rates of mineral dissolution control the temporal evolution of many natural processes on the sur...
The Gibbs energies of formation for clay minerals have been approximated by a model which assumes th...
Thermodynamic models of Essentuki and Nagutsky fields of Caucasian Mineral Waters deposits (KMW) are...
The evolution of the water chemistry and secondary mineral development in the vicinity of the near-f...
Evolving pressure-temperature conditions during metamorphism drive changes in the stable mineral ass...
ABSTRACT: A method for estimating Gibbs free energies and stabilities of clay minerals i proposed fo...
Gibbs free energies of formation ({Delta}G{degree}{sub f}) for several structurally related U(VI) mi...
Mineral stability relations in the system A120a-$iO•-H,20 were investigated via the aqueous ilica-de...
Abstract-A thermodynamic analysis of F-Cl-OH partitioning between minerals and hydrothermal fluids h...
The mineral scale that deposits in digesters and bleach plants is formed by a chemical precipitation...
lower activities ofAI 3+ when obtained by a speciation procedure (fractionation with an ionic column...
The formation of a solid mineral deposit can cause major problems in the conduct of industrial proce...
Abstract The activities of thermodynamic components of clay minerals corresponding i composition to ...
Analysis of phase diagrams and cation distributions within crystalline solutions as means of obtaini...
Solubility equilibria are related to thertnodynainic properties in general and chemical po-tentials ...
The rates of mineral dissolution control the temporal evolution of many natural processes on the sur...
The Gibbs energies of formation for clay minerals have been approximated by a model which assumes th...
Thermodynamic models of Essentuki and Nagutsky fields of Caucasian Mineral Waters deposits (KMW) are...
The evolution of the water chemistry and secondary mineral development in the vicinity of the near-f...
Evolving pressure-temperature conditions during metamorphism drive changes in the stable mineral ass...