If you run this file you will see that the amount of Fe+3 produced is equal to the amount of Cr+3. I have removed nitrate and reduced the amount of iron to simplify the problem. If you include nitrate, then it will consume some electrons and you may not get the reduction of Cr that you expect. As you add more iron, other electron acceptors get into the act and also the pH increases. The model says that Fe(OH)4- exists even in the presence of sulfide. I'm not sure I believe that, but that is another issue. The number of electrons is conserved. It may not be calculating the reactions that you expect, but I am convinced that it is calculating the correct thermodynamic reactions for the aqueous model. TITLE MW-15 Precision Groundwater reaction with 1X Fe+2 SOLUTION 1 temp 23.41 pH 7.0 pe O2(g) -0.68 units mg/L density 1 Al 0 Alkalinity 292.9 as HCO3- Ca 310 Cl 730 K 3.3 Mg 160 Si 36 as SiO2 # N(5) 12 as NO3- Na 600 C(4) 0 as CO3-2 S(6) 1500 as SO4-2 Cr(6) 86.00 # Andco Cr determination SAVE solution 1 END USE Solution 1 # Note no reaction is specified separately REACTION 1 Fe 1 #4.96e-3 # This is 1X amount 4.96e-4 END This may be a better model because it precipitates solids and keeps the pH a bit lower. TITLE MW-15 Precision Groundwater reaction with 1X Fe+2 SOLUTION 1 temp 23.41 pH 7.0 pe O2(g) -0.68 units mg/L density 1 Al 0 Alkalinity 292.9 as HCO3- Ca 310 Cl 730 K 3.3 Mg 160 Si 36 as SiO2 # N(5) 12 as NO3- Na 600 C(4) 0 as CO3-2 S(6) 1500 as SO4-2 Cr(6) 86.00 # Andco Cr determination SAVE solution 1 END USE Solution 1 # Note no reaction is specified separately REACTION 1 Fe 1 4.96e-3 # This is 1X amount EQUILIBRIUM_PHASES Fe(OH)3(a) 0 0 Cr_hydroxide 0 0 END David Parkhurst (dlpark@xxxxxxxx) U.S. Geological Survey Box 25046, MS 413 Denver Federal Center Denver, CO 80225 Project web page: https://wwwbrr.cr.usgs.gov/projects/GWC_coupled
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