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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