Deposition of CaCO/sub 3/ from natural geothermal fluid was studied by using porous substrates made from several granular materials. These experiments aimed to explore connections between the process of steam flash from superheated CO/sub 2/-charged water and the consequent changes in the carbonate chemical equilibria. The substrates were characterized pre- and post-experiment. Flow rates and compositions of input and output fluids were determined. The resultant CaCO/sub 3/ deposits were examined from several points of view. (MHR
AbstractGeochemical trapping has been regarded as the safest process to transfer carbon dioxide (CO2...
Coupled gypsum dissolution-calcium carbonate precipitation experiments were performed in closed syst...
Objectives. The aim of the study is to develop a method of operating geothermal energy systems in th...
Abstract Fouling of heat transfer surfaces during subcooled flow boiling is a frequent engineering p...
The capacity of a geothermal liquid to carry calcium varies mainly with the concentrations of CO{sub...
Geothermal energy is produced by pumping cold water into an underground reservoir. The reservoir exi...
Injection of CO<sub>2</sub> in porous aquifers, where mineralization takes place via chemical reacti...
Injection of CO<sub>2</sub> in porous aquifers, where mineralization takes place via chemical reacti...
Mineralization of microbial biomass is a common phenomenon in geothermal habitats, but knowledge of ...
Mineralization of microbial biomass is a common phenomenon in geothermal habitats, but knowledge of ...
The concentration of carbon dioxide was measured for the four production wells at the East Mesa Geot...
Abstract Background Mineral precipitates (scaling) from deep saline thermal waters often constitute ...
Injection of CO2 in porous aquifers, where mineralization takes place via chemical reactions, is one...
l sechemical deposits of CaCO3 precipitated in geothermally-active areas usually around or along geo...
Abstract: When dissolved solids from the water precipitate and form solid deposits in geothermal pla...
AbstractGeochemical trapping has been regarded as the safest process to transfer carbon dioxide (CO2...
Coupled gypsum dissolution-calcium carbonate precipitation experiments were performed in closed syst...
Objectives. The aim of the study is to develop a method of operating geothermal energy systems in th...
Abstract Fouling of heat transfer surfaces during subcooled flow boiling is a frequent engineering p...
The capacity of a geothermal liquid to carry calcium varies mainly with the concentrations of CO{sub...
Geothermal energy is produced by pumping cold water into an underground reservoir. The reservoir exi...
Injection of CO<sub>2</sub> in porous aquifers, where mineralization takes place via chemical reacti...
Injection of CO<sub>2</sub> in porous aquifers, where mineralization takes place via chemical reacti...
Mineralization of microbial biomass is a common phenomenon in geothermal habitats, but knowledge of ...
Mineralization of microbial biomass is a common phenomenon in geothermal habitats, but knowledge of ...
The concentration of carbon dioxide was measured for the four production wells at the East Mesa Geot...
Abstract Background Mineral precipitates (scaling) from deep saline thermal waters often constitute ...
Injection of CO2 in porous aquifers, where mineralization takes place via chemical reactions, is one...
l sechemical deposits of CaCO3 precipitated in geothermally-active areas usually around or along geo...
Abstract: When dissolved solids from the water precipitate and form solid deposits in geothermal pla...
AbstractGeochemical trapping has been regarded as the safest process to transfer carbon dioxide (CO2...
Coupled gypsum dissolution-calcium carbonate precipitation experiments were performed in closed syst...
Objectives. The aim of the study is to develop a method of operating geothermal energy systems in th...