Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Chemical Engineering, 1989.Vita.Includes bibliographical references (leaves 192-200).by Charles Owen Grigsby.Ph.D
The dissolution of silicate minerals in mixtures of hydrofluoric acid and strong acids such as HCl i...
The dissolution of silicate minerals by CO2–rich fluids and the subsequent precipitation of CO2 as c...
The dissolution of silicate minerals by hydrofluoric acid has been found to be catalyzed by salts su...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Chemical Engineering, 1994.Includes...
International audienceHere we report on two separate ongoing, multi-year investigations on the depen...
The chemical composition of groundwater is controlled largely by subsurface mineral/fluid interactio...
The rates of mineral dissolution control the temporal evolution of many natural processes on the sur...
The rate and magnitude of geochemical reactions can be described by two main processes; thermodynami...
The dissolution of silicate minerals by CO2-rich fluids and the subsequent precipitation of CO2 as c...
We present the results of an experimental study of the effect of anisotropy on the kinetics of K-Fel...
AbstractReal-time microscopic observations of reacting mineral surfaces have provided a significant ...
The objective is to initiate new: modeling of coupled fluid flow and chemical reactions of geologic ...
A new model has been developed which describes the acidization of sandstone cores. The results show ...
Thesis (M.S., Chemistry) -- California State University, Sacramento, 2010.Reactions between aqueous ...
The release of silicon and aluminum from purified Na-montmorillonite surfaces in aqueous systems was...
The dissolution of silicate minerals in mixtures of hydrofluoric acid and strong acids such as HCl i...
The dissolution of silicate minerals by CO2–rich fluids and the subsequent precipitation of CO2 as c...
The dissolution of silicate minerals by hydrofluoric acid has been found to be catalyzed by salts su...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Chemical Engineering, 1994.Includes...
International audienceHere we report on two separate ongoing, multi-year investigations on the depen...
The chemical composition of groundwater is controlled largely by subsurface mineral/fluid interactio...
The rates of mineral dissolution control the temporal evolution of many natural processes on the sur...
The rate and magnitude of geochemical reactions can be described by two main processes; thermodynami...
The dissolution of silicate minerals by CO2-rich fluids and the subsequent precipitation of CO2 as c...
We present the results of an experimental study of the effect of anisotropy on the kinetics of K-Fel...
AbstractReal-time microscopic observations of reacting mineral surfaces have provided a significant ...
The objective is to initiate new: modeling of coupled fluid flow and chemical reactions of geologic ...
A new model has been developed which describes the acidization of sandstone cores. The results show ...
Thesis (M.S., Chemistry) -- California State University, Sacramento, 2010.Reactions between aqueous ...
The release of silicon and aluminum from purified Na-montmorillonite surfaces in aqueous systems was...
The dissolution of silicate minerals in mixtures of hydrofluoric acid and strong acids such as HCl i...
The dissolution of silicate minerals by CO2–rich fluids and the subsequent precipitation of CO2 as c...
The dissolution of silicate minerals by hydrofluoric acid has been found to be catalyzed by salts su...