Thermodynamics of the dissociation of ammonium ion in seawater from 5 to 40°C

The dissociation constant of NH4+ and the associated thermodynamic functions ΔH° and ΔS° in synthetic seawaters of salinity 20.31, 35.00, and 44.55‰ have been determined by emf measurements of cells without liquid junction over the temperature range 5 to 40°C. Cells with hydrogen electrodes and silver-silver chloride electrodes, whose standard potentials in seawater media were determined in an earlier investigation, were used. At a given temperaturet (in °C), pKa varies linearly with the formal ionic strengthIf (uncorrected for ion pairing) according to pKa=pKaw+(0.1552−0.0003142t)If where pKaw is the pK in pure water. The medium effect of seawater on ΔH° amounts to less than 200 cal-mole−1 for a change inIf from 0 to 0.72 mole-kg−1, and ΔS° is less than 1 cal-°K−1-mole−1 in all of the media studied, as it is in water. The observed salt effect on pKa is in close agreement with values predicted from theories of ion-ion interactions.

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