2000Acta Scientiarum Naturalium Universitatis SunyatseniRequires access

Gas Geothermometry in the Hveragerdi High—Temperature Geothermal Field,SW Iceland

孙占学, Halldorarmannson

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Abstract

Five gas geothermometers based on the concentrations of CO2,H2S,H2,CH2,N2 and Ar in fumaroles and wet-stem wells are applied to estimating subsurface temperatures in the Hveragerdi high-temperature geothmal field,SW Iceland,The results for fumaroles indicate that the calculated subsurface temperatures decrase from the northern part to the southern part of the field.The CO2-geothermometer gives the highers temperature values,with an average of 256℃ for the northern part,and 247℃ for the southern part.The H2S-geothermometer reveals an aquifer temperature of 211℃ for the northern part,and 203℃ for the southern part.The H2-geothermometer gives an average subsurface temperature of 229℃ for the northern part,and 184℃ for the southern part,which agerees excellently with the measured temperatures in wet-steam wells.The measured borhole temperatures in the field range from 215℃ to 230℃ for the northern part,and from 167℃ to 198℃ for the southern part.The CO2/H2-geothermometer gives the lowest subsurface temperature values,with an average of 203℃ for the northern part,and 143℃ for the southern part,The CO2/N2-geothermometer gives 249℃ for the northern part and 235℃ for the southern part.For the data from wells,the CO2-, H2S-,and H2-geothermometers,give average subsurface temperatures of 247℃ for the northern part and 246℃ for the southern part,213℃ for the northern part and 220℃ for the southern part,and 217℃ for the northern part and 216℃ for the southern part,respectively.The CO2/H2-geothermometer indicates an average subsurface tem,perature of about 200℃ for both the northern part and the southern part.The CO2/N2-geothermometer gives an average subsurface temperature of 180℃ for the northern part and 259℃ for the southern part.The discrepancy between the estimeated subsurface temperatures obtained by the various gas geothermometers has been explained in this paper.By integrating the solute geothermometric results,mixing model studies and gas geothermometric results.the maxim

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Five gas geothermometers based on the concentrations of CO2,H2S,H2,CH2,N2 and Ar in fumaroles and wet-stem wells are applied to estimating subsurface temperatures in the Hveragerdi high-temperature geothmal field,SW Iceland,The results for fumaroles indicate that the calculated subsurface temperatures decrase from the northern part to the southern part of the field.The CO2-geothermometer gives the highers temperature values,with an average of 256℃ for the northern part,and 247℃ for the southern part.The H2S-geothermometer reveals an aquifer temperature of 211℃ for the northern part,and 203℃ for the southern part.The H2-geothermometer gives an average subsurface temperature of 229℃ for the northern part,and 184℃ for the southern part,which agerees excellently with the measured temperatures in wet-steam wells.The measured borhole temperatures in the field range from 215℃ to 230℃ for the northern part,and from 167℃ to 198℃ for the southern part.The CO2/H2-geothermometer gives the lowest subsurface temperature values,with an average of 203℃ for the northern part,and 143℃ for the southern part,The CO2/N2-geothermometer gives 249℃ for the northern part and 235℃ for the southern part.For the data from wells,the CO2-, H2S-,and H2-geothermometers,give average subsurface temperatures of 247℃ for the northern part and 246℃ for the southern part,213℃ for the northern part and 220℃ for the southern part,and 217℃ for the northern part and 216℃ for the southern part,respectively.The CO2/H2-geothermometer indicates an average subsurface tem,perature of about 200℃ for both the northern part and the southern part.The CO2/N2-geothermometer gives an average subsurface temperature of 180℃ for the northern part and 259℃ for the southern part.The discrepancy between the estimeated subsurface temperatures obtained by the various gas geothermometers has been explained in this paper.By integrating the solute geothermometric results,mixing model studies and gas geothermometric results.the maxim

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Available abstract

Five gas geothermometers based on the concentrations of CO2,H2S,H2,CH2,N2 and Ar in fumaroles and wet-stem wells are applied to estimating subsurface temperatures in the Hveragerdi high-temperature geothmal field,SW Iceland,The results for fumaroles indicate that the calculated subsurface temperatures decrase from the northern part to the southern part of the field.The CO2-geothermometer gives the highers temperature values,with an average of 256℃ for the northern part,and 247℃ for the southern part.The H2S-geothermometer reveals an aquifer temperature of 211℃ for the northern part,and 203℃ for the southern part.The H2-geothermometer gives an average subsurface temperature of 229℃ for the northern part,and 184℃ for the southern part,which agerees excellently with the measured temperatures in wet-steam wells.The measured borhole temperatures in the field range from 215℃ to 230℃ for the northern part,and from 167℃ to 198℃ for the southern part.The CO2/H2-geothermometer gives the lowest subsurface temperature values,with an average of 203℃ for the northern part,and 143℃ for the southern part,The CO2/N2-geothermometer gives 249℃ for the northern part and 235℃ for the southern part.For the data from wells,the CO2-, H2S-,and H2-geothermometers,give average subsurface temperatures of 247℃ for the northern part and 246℃ for the southern part,213℃ for the northern part and 220℃ for the southern part,and 217℃ for the northern part and 216℃ for the southern part,respectively.The CO2/H2-geothermometer indicates an average subsurface tem,perature of about 200℃ for both the northern part and the southern part.The CO2/N2-geothermometer gives an average subsurface temperature of 180℃ for the northern part and 259℃ for the southern part.The discrepancy between the estimeated subsurface temperatures obtained by the various gas geothermometers has been explained in this paper.By integrating the solute geothermometric results,mixing model studies and gas geothermometric results.the maxim

Key concepts: Geology, Geothermal gradient, Fumarole, Mineralogy, Geophysics

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