Table 1 Estimated solution compositions of pore water that finally interacted with sediments at John Klein and Cumberland for (a) full-interaction scenario and (b) no-interaction scenario
Full-interaction scenario | No-interaction scenario | |||
---|---|---|---|---|
John Klein | Cumberland | John Klein | Cumberland | |
Na (mol/kg) | 0.085–0.24 | 0.094–0.12 | 0.038–0.42 | 0.033–0.13 |
K (mol/kg) | 0.0025–0.018 | 0.0014–0.0044 | 0.0011–0.030 | 0.00047–0.0044 |
Mg (mol/kg) | 0.0046–0.11 | 0.035–0.060 | 0.00064–0.21 | 0.0034–0.065 |
Ca (mol/kg) | 0.022–0.12 | 0.024–0.045 | <0.119 | <0.048 |
Cl (mol/kg) | 0.072–0.59 | 0.11–0.25 | 0.05–1.3 | 0.05–0.34 |
SO4 (mol/kg) | 0.025–0.14 | 0.044–0.072 | N/A | N/A |
ΣCO2 (mol/kg) | 0.0019–0.041 | 0.0023–0.016 | N/A | N/A |
Fe(II) (mol/kg) | 0.00024–0.038 | 0.00012–0.0058 | 0.00044–0.19 | 0.00011–0.013 |
pH | 6.7–7.3 | 6.9–7.3 | 6.5–8.3 | 6.8–8.1 |
\(P_{{\rm{CO}}_{2}}\) (mbar) | 6–130 | 6–40 | N/A | N/A |