Table 2.
Seawater parameter | Ambient CO2 | Mid-CO2 | High CO2 |
Temperature, °C | −1.67 | −1.68 | −1.69 |
Salinity | 30.89 ± 1.41 | 29.97 ± 0.59 | 29.38 ± 0.48 |
DIC, μmol⋅kg−1 | 2,067.5 ± 2.3 | 2,183.1 ± 9.7 | 2,156.2 ± 12.8 |
TA, μmol⋅kg−1 | 2,156.4 ± 9.3 | 2,201.9 ± 3.8 | 2,122.5 ± 29.9 |
pH, total | 8.04 ± 0.03 | 7.80 ± 0.05 | 7.60 ± 0.09 |
pCO2, μatm | 371 ± 26.7 | 698 ± 76.8 | 1,092 ± 202.8 |
Ω Calcite | 1.82 ± 0.10 | 1.08 ± 0.12 | 0.67 ± 0.14 |
Ω Aragonite | 1.13 ± 0.06 | 0.67 ± 0.08 | 0.41 ± 0.09 |
In situ seawater temperature (°C) was measured in the ice hole, and salinity, DIC, and TA were measured in the header tanks. Measured parameters were used to calculate, using CO2sys, the additional parameters: pH (total) in situ temperature (°C), pCO2, and saturation states for calcite (Ω Calcite) and aragonite (Ω Aragonite).