Modelling Aqueous - Geochemistry I - Exam, Exams of Geochemistry

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Practical 1: Modelling Aqueous Solutions with PHREEQC
1. Calculate the solubility of anhydrite as a function of temperature. Set up the
phreeqe file with vi or some other text editor..
TITLE Solubility of anhydrite
SOLUTION 1
units mol/kgw
pH 4.00
temp 300.0
EQUILIBRIUM_PHASES
Anhydrite
END
Note that temperature in PHREEQC is input in ºC. Edit the input file to cover a
range of temperatures from 25 to 300 ºC. USE THE llnl.dat DATABASE FILE
SINCE THAT HAS THE Cp INFO etc.
In the output, you'll find
--------------Distribution of species--------------------
Log Log Log
Species Molality Activity Molality Activity Gamma
H+ 2.790e-05 2.685e-05 -4.554 -4.571 -0.017
OH- 2.010e-07 1.932e-07 -6.697 -6.714 -0.017
H2O 5.553e+01 1.000e+00 1.744 -0.000 0.000
Ca 9.391e-05
Ca+2 7.637e-05 6.531e-05 -4.117 -4.185 -0.068
CaSO4 1.753e-05 1.753e-05 -4.756 -4.756 0.000
CaOH+ 3.575e-13 3.436e-13 -12.447 -12.464 -0.017
The "solubility of anhydrite" can be taken as the concentration of Ca. The line
Ca 9.391e-05
means that the total Ca concentration is 9.39x10-5 molal. Anhydrite has a
"retrograde solubility". What might that mean?
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Practical 1: Modelling Aqueous Solutions with PHREEQC

  1. Calculate the solubility of anhydrite as a function of temperature. Set up the phreeqe file with vi or some other text editor.. TITLE Solubility of anhydrite SOLUTION 1 units mol/kgw pH 4. temp 300. EQUILIBRIUM_PHASES Anhydrite END Note that temperature in PHREEQC is input in ºC. Edit the input file to cover a range of temperatures from 25 to 300 ºC. USE THE llnl.dat DATABASE FILE SINCE THAT HAS THE Cp INFO etc. In the output, you'll find --------------Distribution of species-------------------- Log Log Log Species Molality Activity Molality Activity Gamma H+ 2.790e- 05 2.685e- 05 - 4.554 - 4.571 - 0. OH- 2.010e- 07 1.932e- 07 - 6.697 - 6.714 - 0. H2O 5.553e+01 1.000e+00 1.744 - 0.000 0. Ca 9.391e- 05 Ca+2 7.637e- 05 6.531e- 05 - 4.117 - 4. 185 - 0. CaSO4 1.753e- 05 1.753e- 05 - 4.756 - 4.756 0. CaOH+ 3.575e- 13 3.436e- 13 - 12.447 - 12.464 - 0. The "solubility of anhydrite" can be taken as the concentration of Ca. The line Ca 9.391e- 05 means that the total Ca concentration is 9.39x10-^5 molal. Anhydrite has a "retrograde solubility". What might that mean?
  1. Calculate the solubility (i.e., total Ag in solution) of AgCl (chlorargyrite) as a function of [Cl] (0.0 to 0.2 m) and temperature (25- 300 ºC) using PHREEQC. To do this, set up the input file: TITLE Solubility of AgCl SOLUTION 1 units mol/kgw pH 4. temp 25. Na 0.20 charge Cl 0. EQUILIBRIUM_PHASES Chlorargyrite 0.0 1. END In this input, the block SOLUTION 1 sets up the initial solution (saltwater). The second block, EQUILIBRIUM_PHASES, requires that there be a target saturation index for Chlorargyrite to be 0.0 (i.e., at saturation) but says we have a total of 1.0 moles of AgCl per kg of water (which ought to be enough to prevent it from all dissolving...). Edit the file to change the temperature and [Na] and [Cl] as you wish.. In the output file (if all goes well..) you'll find, near the end, the speciation of Ag under the block -----------------Distribution of species------------------- Log Log Log Species Molality Activity Molality Activity Gamma H+ 9.915e- 05 8.935e- 05 - 4.004 - 4.049 - 0. OH- 6.500e- 08 5.805e- 08 - 7.187 - 7.236 - 0. H2O 5.553e+01 9.999e- 01 1.744 - 0.000 0. Ag(1) 6.843e- 03 AgCl 4.538e- 03 4.538e- 03 - 2.343 - 2.343 0. Ag+ 1.774e- 03 1.581e- 03 - 2.751 - 2.801 - 0. AgCl2- 5.305e- 04 4.742e- 04 - 3.275 - 3.324 - 0. AgCl3- 2 9.005e- 08 5.749e- 08 - 7.046 - 7.240 - 0. AgCl4- 3 3.899e- 11 1.420e- 11 - 10.409 - 10.848 - 0. The line