A method for determination of the gas‐water ratio in bubbling springs
Identifieur interne : 000157 ( Istex/Curation ); précédent : 000156; suivant : 000158A method for determination of the gas‐water ratio in bubbling springs
Auteurs : Y. A. Taran [Mexique]Source :
- Geophysical Research Letters [ 0094-8276 ] ; 2005-12.
Descripteurs français
- Wicri :
- topic : Géochimie.
English descriptors
- KwdEn :
- Acta, Aeolian islands, Analytical concentration, Atmospheric components, Atmospheric pressure, Baja california, Cosmochim, Equilibrium vapor, Flow rate, Geochemical evidence, Geochemistry, Geochim, Geothermal, Geothermal fields, Geothermal gases, Geothermometry, Giggenbach, Hydrothermal, Hydrothermal fluids, Hydrothermal systems, Iavcei commission, Important parameter, Meteoric water, Mole fraction, Noble gases, Panarea, Panarea fluid, Phase equilibrium, Pure water, Recharge area, Second term, Simple method, Submarine springs, Subsurface conditions, Taran, Temperature range, Thermal spring, Thermal springs, Thermal water, Thermodynamic data, Total amount, Volcanic gases, Volcanol, Water discharge, Water flow rate.
- Teeft :
- Acta, Aeolian islands, Analytical concentration, Atmospheric components, Atmospheric pressure, Baja california, Cosmochim, Equilibrium vapor, Flow rate, Geochemical evidence, Geochemistry, Geochim, Geothermal, Geothermal fields, Geothermal gases, Geothermometry, Giggenbach, Hydrothermal, Hydrothermal fluids, Hydrothermal systems, Iavcei commission, Important parameter, Meteoric water, Mole fraction, Noble gases, Panarea, Panarea fluid, Phase equilibrium, Pure water, Recharge area, Second term, Simple method, Submarine springs, Subsurface conditions, Taran, Temperature range, Thermal spring, Thermal springs, Thermal water, Thermodynamic data, Total amount, Volcanic gases, Volcanol, Water discharge, Water flow rate.
Abstract
A simple method based on the phase equilibrium between gas bubbles and water is developed for the determination of the relative gas content in bubbling springs. For the calculation of the gas‐water ratio it is necessary to know only the concentration of one of the “atmogenic” components (N2, Ar, or Ne) in a gas sample from the gas analysis. The total gas content calculated by this method can be used for the gas geothermometry and for the estimations of the gas fluxes and water flow rates from mineral and thermal springs.
Url:
DOI: 10.1029/2005GL024547
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ISTEX:F9171BB2F090D8D51C3058D0AF9F3C021F63C676Le document en format XML
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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Acta</term>
<term>Aeolian islands</term>
<term>Analytical concentration</term>
<term>Atmospheric components</term>
<term>Atmospheric pressure</term>
<term>Baja california</term>
<term>Cosmochim</term>
<term>Equilibrium vapor</term>
<term>Flow rate</term>
<term>Geochemical evidence</term>
<term>Geochemistry</term>
<term>Geochim</term>
<term>Geothermal</term>
<term>Geothermal fields</term>
<term>Geothermal gases</term>
<term>Geothermometry</term>
<term>Giggenbach</term>
<term>Hydrothermal</term>
<term>Hydrothermal fluids</term>
<term>Hydrothermal systems</term>
<term>Iavcei commission</term>
<term>Important parameter</term>
<term>Meteoric water</term>
<term>Mole fraction</term>
<term>Noble gases</term>
<term>Panarea</term>
<term>Panarea fluid</term>
<term>Phase equilibrium</term>
<term>Pure water</term>
<term>Recharge area</term>
<term>Second term</term>
<term>Simple method</term>
<term>Submarine springs</term>
<term>Subsurface conditions</term>
<term>Taran</term>
<term>Temperature range</term>
<term>Thermal spring</term>
<term>Thermal springs</term>
<term>Thermal water</term>
<term>Thermodynamic data</term>
<term>Total amount</term>
<term>Volcanic gases</term>
<term>Volcanol</term>
<term>Water discharge</term>
<term>Water flow rate</term>
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<term>Aeolian islands</term>
<term>Analytical concentration</term>
<term>Atmospheric components</term>
<term>Atmospheric pressure</term>
<term>Baja california</term>
<term>Cosmochim</term>
<term>Equilibrium vapor</term>
<term>Flow rate</term>
<term>Geochemical evidence</term>
<term>Geochemistry</term>
<term>Geochim</term>
<term>Geothermal</term>
<term>Geothermal fields</term>
<term>Geothermal gases</term>
<term>Geothermometry</term>
<term>Giggenbach</term>
<term>Hydrothermal</term>
<term>Hydrothermal fluids</term>
<term>Hydrothermal systems</term>
<term>Iavcei commission</term>
<term>Important parameter</term>
<term>Meteoric water</term>
<term>Mole fraction</term>
<term>Noble gases</term>
<term>Panarea</term>
<term>Panarea fluid</term>
<term>Phase equilibrium</term>
<term>Pure water</term>
<term>Recharge area</term>
<term>Second term</term>
<term>Simple method</term>
<term>Submarine springs</term>
<term>Subsurface conditions</term>
<term>Taran</term>
<term>Temperature range</term>
<term>Thermal spring</term>
<term>Thermal springs</term>
<term>Thermal water</term>
<term>Thermodynamic data</term>
<term>Total amount</term>
<term>Volcanic gases</term>
<term>Volcanol</term>
<term>Water discharge</term>
<term>Water flow rate</term>
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<front><div type="abstract">A simple method based on the phase equilibrium between gas bubbles and water is developed for the determination of the relative gas content in bubbling springs. For the calculation of the gas‐water ratio it is necessary to know only the concentration of one of the “atmogenic” components (N2, Ar, or Ne) in a gas sample from the gas analysis. The total gas content calculated by this method can be used for the gas geothermometry and for the estimations of the gas fluxes and water flow rates from mineral and thermal springs.</div>
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