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 =
590nmA/
436nmA), along with the molar absorption coefficient ratios (
e1,
e2 and
e3/
e2) and a tentative acid dissociation constant value (p
Ka2). 2) The perturbation of hydrogen ion was evaluated from the change in titration mass (Δ
m). The total hydrogen ion concentration at
m + Δ
m, pH
T(at m+Δm), was calculated using pH
F(ind) for a mass
m and constants for sulfate (
ST) and fluoride (
FT). 3) The alkalinity (
AT) was computed from the titrant mass (
m + Δ
m) and the corresponding pH
T(at m+Δm) through a non-linear least-squares approach using the p
Ka2 value as a variable parameter. Seawater sample at 2000 m depth from the West Pacific was analyzed. The resulting
AT (2420.92 ± 3.35 μmol kg
−1) was in good agreement with the
AT measured by potentiometric electric force (2420.46 ± 1.54 μmol kg
−1). The resulting p
Ka2 was 3.7037, in close proximity to that reported by King
et al. (p
Ka2 = 3.695).
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