1 - 2 |
Special issue on geothermal energy - Foreword Weir G |
3 - 27 |
A simple model of a two-layered high-temperature liquid-dominated geothermal reservoir as a part of a large-scale hydrothermal convection system Hanano M |
29 - 63 |
Layered thermohaline convection in hypersaline geothermal systems Oldenburg CM, Pruess K |
65 - 80 |
A model for deep geothermal brines, I: T-p-X state-space description Palliser C, McKibbin R |
81 - 101 |
Permeability changes during the evolution of a geothermal field due to the dissolution and precipitation of quartz White SP, Mroczek EK |
103 - 127 |
Estimation of temperatures in geothermal wells during circulation and shut-in in the presence of lost circulation Garcia A, Santoyo E, Espinosa G, Hernandez I, Gutierrez H |
129 - 154 |
A model for deep geothermal brines, II: Thermodynamic properties - Density Palliser C, McKibbin R |
155 - 171 |
A model for deep geothermal brines, III: Thermodynamic properties - Enthalpy and viscosity Palliser C, McKibbin R |
173 - 204 |
Computer modeling for geothermal systems: Predicting carbonate and silica scale formation, CO2 breakout and H2S exchange Moller N, Greenberg JP, Weare JH |