dD and d18O in waters, d13C in CO2 and CH4, 3He/4He and 40Ar/36Ar ratios in natural gases were used to define the origin of water, CO2 and CH4. A good correspondence were obtained between measured chemical compositions of thermal springs emerging at Berici Hills and in the exploited area, and those computed by means of a numerical simulation
Chemical and isotopic features and flow path modelling of thermal fluids of the Abano system, Italy
Gherardi F;Magro G;Pennisi M
1998
Abstract
dD and d18O in waters, d13C in CO2 and CH4, 3He/4He and 40Ar/36Ar ratios in natural gases were used to define the origin of water, CO2 and CH4. A good correspondence were obtained between measured chemical compositions of thermal springs emerging at Berici Hills and in the exploited area, and those computed by means of a numerical simulationFile in questo prodotto:
Non ci sono file associati a questo prodotto.
I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
