Effect of pH on H-2H exchange,H2 production and H2 uptake,catalysed by the membrane-bound hydrogenase of Paracoccus denitrificans

(1) The kinetics of isotope exchange catalysed by the membrane-bound hydrogenase of Paracoccus denitrificans have been studied by measuring H²H, H₂ or ²H₂ produced when the enzyme catalyses the exchange between ²H₂ and H₂O or H₂ and ²H₂O. (2) In the ²H₂-H₂O system the measured rate of H₂ production was always higher than that of H²H. The $\text{H}{}_2\text{H}{}^2\text{H}$ ratio remained constant (about 1.70) in the protein concentration range 0.08–1.32 mg. The very rapid formation of H₂ with respect to H²H is consistent with the hypothesis of a heterolytic cleavage of ²H₂ into a deuteron and an enzyme hydride that can exchange with the solvent. (3) In the H₂-²H₂O system, the exchange rate was much lower than in the ²H₂-H₂O system, indicating a marked isotopic effect of ²H₂O. (4) The H-²H exchange activity, determined from the initial velocity of H²H formation, is optimal at pH 4.5. A second maximum of activity is observed at pH 8.3. The pH value of 4.5 is also the pH optimum for H₂ production while at pH 8.3–8.5 there is a maximum of H₂ oxidation activity. (5) In ordinary H₂O the K_m for hydrogen uptake estimated either from H₂ consumption or from benzyl viologen reduction was 0.06–0.07 μM for both H₂ and ²H₂ indicating a strong affinity of the enzyme for hydrogen at pH 8.3–8.5. Shifting from H₂O to ²H₂O does not affect the K_m of the enzyme for H₂ but lowers the V_max value about 10-fold. The K_m for benzyl viologen and methyl viologen was 0.08 and 2 mM, respectively.