To determine the dissolved inorganic carbon (DIC) chemistry of seawater in the treatments, total alkalinity (TA), pH on the total scale, temperature, and salinity were measured using standard procedures, and used to calculate pCO2 (uatm), HCO3 - (umolkg-1), CO3 2- (umolkg-1), and the aragonite saturation state (XArag) of seawater using CO2SYS (Pierrot et al. 2006). TA (umol kg-1) was measured through potentiometric titration (SOP 3b, Dickson et al. 2007) using an automatic titrator (DL50, Mettler Toledo) filled with certified acid titrant (0.1 M HCl, 0.6 NaCl, Dickson Laboratory, Scripps Institution of Oceanography). The pH probe (DG101-SC, Mettler Toledo) attached to the titrator was 3-point calibrated with pH 4.00, 7.00, and 10.00 buffers (Fisher, NBS). Certified reference material with a known TA (Batch 98, http://andrew.ucsd. edu/index.html) was titrated daily to determine the accuracy and precision of the analyses.
Seawater samples (50 mL) from the treatment tanks were brought to 25C, weighed and titrated in a waterjacketed beaker within 2-3 h of collection. The pH values and the titrant volumes (cm3) obtained from the titrations were sub-sampled for the range between pH 3.0 and 3.5 and inserted into a Microsoft Excel spreadsheet (Fangue et al. 2010), which calculated Gran’s function as a product of the mass of titrant added (Dickson et al. 2007). Treatment tank pH was determined spectrophotometrically using m-cresol purple dye (Sigma-Aldrich) following SOP 6b of Dickson et al. (2007) with modification (Fangue et al. 2010). Preliminary sampling of the seawater in the tanks throughout the day confirmed that the pCO2 treatments were stable over a 24-h period.
References:
Dickson AG, Sabine CL, Christian JR (eds) (2007) Guide to best practices for ocean CO2 measurements. PICES Special Publication 3, p 191
Fangue NA, O’Donnell MJ, Sewell MA, Matson PG, MacPherson AC, Hoffman GE (2010) A laboratory-based, experimental system for the study of ocean acidification effects on marine invertebrate larvae. Limnol Oceanogr Methods 8:441-452