A systematic deviation from Na-K-Ca geothermometer below 75°C and above 10 -4 atm P co 2

Details A systematic deviation from Na-K-Ca geothermometer below 75°C and above 10 -4 atm P co 2 A systematic deviation from Na-K-Ca geothermometer below 75°C and above 10 -4 atm P co 2

Apr 1975

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1975gecoa..39..541p&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 39, Issue 4, pp.541-544

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Scientific paper

If the temperature of ground water is below 75°C and the partial pressure of CO 2 in the aquifer is above 10 -4 atm, a chemical steady-state between water and felsic rocks (rather than chemical equilibrium) may be maintained. The temperature of water in the aquifer may be estimated using a modified form of the Na-K-Ca geothermometer from, I = -1.36 -0.253 log P co 2 . where the departure of the steady-state from equilibrium, I , is a function of P co 2 : I = -1.36 -0.253 log P co 2 .

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