Abstract

The open-cell titration of seawater was studied for alkalinity measurements by colorimetry. 1) The colorimetric pH of free hydrogen ion concentration, pH(F(ind)), was calculated from the ratio of the absorbances at 436 and 590 nm (R = (590nm)A/(436nm)A), along with the molar absorption coefficient ratios (e(1), e(2) and e(3)/e(2)) and a tentative acid dissociation constant value (pK(a(2))). 2) The perturbation of hydrogen ion was evaluated from the change in titration mass (Deltam). The total hydrogen ion concentration at m + Deltam, pH(T(at m+Deltam)), was calculated using pH(F(ind)) for a mass m and constants for sulfate (S(T)) and fluoride (F(T)). 3) The alkalinity (A(T)) was computed from the titrant mass (m + Deltam) and the corresponding pH(T(at m+Deltam)) through a non-linear least-squares approach using the pK(a(2)) value as a variable parameter. Seawater sample at 2000 m depth from the West Pacific was analyzed. The resulting A(T) (2420.92 +/- 3.35 micromol kg(-1)) was in good agreement with the A(T) measured by potentiometric electric force (2420.46 +/- 1.54 micromol kg(-1)). The resulting pK(a(2)) was 3.7037, in close proximity to that reported by King et al. (pK(a(2)) = 3.695).

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