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- W1963624620 abstract "Abstract By the use of the CO2, CH4, H2 and CO contents of geothermal gas discharges, the CO2 partial pressure in the gas equilibration zone can be calculated. Assuming that the partial pressures of water at any temperature are fixed by the presence of liquid water, then the following function, which is nearly independent of temperature, linking CO2 partial pressure to the ratio X H 2 / X C O is obtained: log P C O 2 = 3.573 − 46 / T ( K ) − log X H 2 / X C O Assuming a hydrostatic model, geothermal gradients for five high enthalpy and two medium to low enthalpy Italian geothermal areas have been estimated. High enthalpy systems can be clearly distinguished from those of low to medium enthalpy. Finally, accurate determinations of the H2/CO ratio in fluids discharged by selected fumaroles in volcanic areas can provide a method of monitoring pressure conditions in geothermal aquifers. This fact is particularly useful when the risk of a phreatic explosion in a volcanic area is to be assessed." @default.
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- W1963624620 date "1989-09-01" @default.
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- W1963624620 title "Gas geobarometry for hydrothermal systems and its application to some Italian geothermal areas" @default.
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- W1963624620 doi "https://doi.org/10.1016/0883-2927(89)90004-8" @default.
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