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. 2018 Mar 1;18(3):259–293. doi: 10.1089/ast.2017.1680

Table 4.

Results of the PHREECQ-Modeled Runs for Mineral Precipitation in Hadean Seawater

PCO2 T (C) Final pH [Ca]T (m/L) [Fe(II)]T (m/L) SI (calcite) SI (siderite) Model
1.0 50 7.99 5.02E-04 1.10E-07 1.01 −1.29 1
3.2 50 7.70 6.55E-04 3.29E-07 1.1 −1.04 1
10.0 50 7.44 9.48E-04 9.55E-07 1.19 −0.83 1
100.0 50 7.04 2.14E-03 6.10E-06 1.42 −0.43 1
1.0 100 7.08 5.18E-05 5.93E-07 −0.41 −0.59 1
3.2 100 6.81 5.35E-05 1.68E-06 −0.41 −0.37 1
10.0 100 6.56 5.44E-05 4.60E-06 −0.47 −0.17 1
100.0 100 6.14 5.37E-05 2.99E-05 −0.68 0.18 1
1.0 50 7.28 2.85E-06 1.87E-06 −1.37 −0.7 2
3.2 50 7.12 3.86E-06 3.98E-06 −1.3 −0.54 2
10.0 50 7.00 5.88E-06 7.73E-06 −1.14 −0.35 2
100.0 50 6.87 9.25E-06 1.78E-05 −0.84 0.05 2
1.0 100 6.74 5.38E-05 2.24E-06 −0.43 −0.31 2
3.2 100 6.54 5.44E-06 4.98E-06 −0.48 −0.16 2
10 100 6.36 5.45E-05 1.11E-05 −0.55 −0.01 2
100.0 100 6.04 5.39E-05 5.10E-05 −0.75 0.29 2

T = total concentration.

Model 1 = Initial equilibration with atmospheric CO2 followed by equilibration with minerals.

Model 2 = Equilibration with CO2 and minerals simultaneously.