During the Equatorial Pacific expedition, concentrations were analyzed with a Metrohm 844 UV/VIS Compact IC equipped with a 150 × 4.0 mm Metrosep A SUPP 8 150 column. The column temperature was set to 30°C. The eluent was a 10% NaCl solution filtered through a 0.45 μm pore size filter. Approximately 0.8 ml of interstitial water was injected manually into a 250 μL sample loop. UV absorption was determined at 215 nm.
We analyzed porewater samples for dissolved Mn4+ and Fe3+ by inductively coupled plasma emission spectrometry (ICP-ES) at Boston University. We acidified the samples at sea with Fisher Optima HNO3 and stored them in a refrigerator until analysis. The samples were diluted 10-fold in 2% triple distilled HNO3, and calibrated against a seven point calibration curve of matrix matched, spiked International Association for the Physical Sciences of the Ocean standard seawater (IAPSO, S = 35, Ocean Scientific International Ltd.) that covered the full concentration range of the unknown samples. We measured Mn4+ at 257.609 and 259.373 nm using the ICP-ES monochromator and at 257.61 nm using the ICP-ES polychromator with the Jobin-Yvon Ultima C ICP-ES instrument. Using the ICP-ES monochromator, we measured Fe3+ at 238.203 and 259.939 nm, as well as at 259.94 nm using the ICP-ES polychromator. We corrected final concentrations for the 1% acid dilution due to on-board acidification. Analytical precision for both elements is ~3% of the measured value. Accuracy was confirmed by analysis of spiked IAPSO standards that were not included in the original calibration.
We quantified dissolved in porewater samples from Lake Van and Barents Sea samples using a SYKAM IC system (SYKAM, Fürstenfeldbrück, Germany) equipped with an LCA A14 column, a suppressor (SAMS™, SeQuant, Sweden) and a S3115 conductivity detector. The mobile phase was a 6.25 mmol L−1 Na2CO3 with 0.1 vol% modifier (1g 4-hydroxy-benzonitrile in 50 mL methanol). We eluted the samples at isocratic conditions at 50°C with the eluent flow set to 1 mL min−1, injection volume was 30 μL.
During the Equatorial Pacific expedition, we quantified concentrations with a Metrohm 861 Advanced Compact IC. The IC was comprised of an 853 CO2 suppressor, a thermal conductivity detector, a 150 × 4.0 mm Metrosep A SUPP 5 150 column, and a 20 μL sample loop. A Metrohm 837 IC Eluent/Sample Degasser was coupled to the system. We set the column oven to 32°C. The eluent was 3.2 mmol L−1 Na2CO3, and 1.0 mmol L−1 NaHCO3. Each sample was analyzed as a 1:50 dilution of interstitial water with 18 MOhm cm−1 deionized water. If the samples were anoxic, we added 5 μL of 10% Zn-acetate per mL of analyte to precipitate ZnS.
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