markfp Posted March 23, 2015 Share Posted March 23, 2015 Hi, I have been using GSS and SpecE8 to calculate activity coefficients and perform concentration unit conversions in brine solutions with extremely high ionic strength. I have noticed that when converting between g/kg (ppt) to mol/l, the converted values are off by 1-2 moles compared to values obtained by doing 'long-hand' calculations using density measurements. Also, I am interested in activity of H2O, and this parameter is drastically lower when calculated with SpecE8 than when measured using a calibrated relative humidity meter. I have loaded the thermo dataset thermo_hmw, which should employ Pitzer equations for calculations at high ionic strength, and have been applied previously to solutions analogous to mine. I was wondering whether I have made some error or whether I am outside the usability of the hmw dataset in the GWB Student edition. An example dataset: raw data in g/kg: Mg++ 75.44 Na+ 0.3047 K+ 1.097 SO4-- 102.9 Cl- 119.3 density: 1.227 g/cm^3 Quote Link to comment Share on other sites More sharing options...
katezat Posted March 24, 2015 Share Posted March 24, 2015 Hello Mark, Can you please explain how you are calculating your g/kg to mol/l unit conversion? What values do you think you should get and what values are calculated using GSS? Please attach your GSS and SpecE8 files so we can take a better look at your problem. In any modeling exercise, there is often some difference between values calculated from a model and those determined directly. You can find information on calculating the activity of water using the B-dot model and virial methods in Chapter 8 of the Geochemical and Biogeochemical Reaction Modeling text. Kind regards, Katelyn Quote Link to comment Share on other sites More sharing options...
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