Methane concentrations (mmol per litre of porewater) were calculated using the following equation:
[CH4] = (ρ(CH4)Vheadspace)/(RTφVsed1000)
where p(CH4) is the partial pressure of methane (in ppmv), Vheadspace is the volume of the serum vial headspace (ml) after the sediment and KOH are added, R is the universal gas constant, T is the temperature at time of measurement in Kelvin and Vsed is the volume (ml) of whole sediment added to the serum vial.
Porosity, φ, was calculated using the formula:
φ = (mw/ ρw)/(mw/ρw+((md-S*mw/1000)/ρds))
where mw is the mass of the water lost on drying, md is the mass of the dried sediment, ρw is the density of pure water, ρds is the density of dry sediment (assumed to be 2.5 g cm−3), and S is salinity in grams per kilogram (assumed to be 19 grams per kilogram for all samples).
Standards at sulfate concentrations 0, 0.1, 0.5, 1, 5, 10 mM measure prior to samples from each core and sample peak areas were converted to sulfate concentrations using the standard curves after accounting for the dilution ((peak area * slope + intercept) * 0.7 / 0.6) by the 10% HCl.
No samples have been flagged as below the detection limit.
BCO-DMO Processing:
- added conventional header with dataset name, PI name, version date
- renamed parameters to BCO-DMO and BODC standards
- replaced NaN with nd
- removed CH4_mod data