Ks: Stability constant of hydrogen sulfate (mol/kg)
Description
Stability constant of hydrogen sulfate (mol/kg)
Usage
Ks(S = 35, T = 25, P = 0, ks="d")
Arguments
S
Salinity, default is 35
T
Temperature in degrees Celsius, default is 25oC
P
Hydrostatic pressure in bar (surface = 0), default is 0
ks
"d" for using Ks from Dickson (1990), "k" for using Ks from Khoo et al. (1977), default is "d"
Value
KsStability constant of hydrogen sulfate (mol/kg), pHscale = free scale
encoding
latin1
Details
The Dickson (1990) constant is recommended by Guide to Best Practices for Ocean CO2 Measurements (2007). It is, however, critical to consider that each formulation is only valid for specific ranges of temperature and salinity:
Dickson (1990): S ranging between 5 and 45 and T ranging between 0 and 45oC.
Khoo et al. (1977): S ranging between 20 and 45 and T ranging between 5 and 40oC.
Note that the arguments can be given as a unique number or as vectors. If the lengths of the vectors are different, the longer vector is retained and only the first value of the other vectors is used. It can therefore be critical to use vectors of the same length.
The pressure correction was applied on the free scale.
References
Dickson A. G., 1990 Standard potential of the reaction: AgCI(s) + 1/2H2(g) = Ag(s) + HCI(aq), and the standard acidity constant of the ion HSO4 in synthetic sea water from 273.15 to 318.15 K. Journal of Chemical Thermodynamics22, 113-127.
Dickson A. G., Sabine C. L. and Christian J. R., 2007 Guide to best practices for ocean CO2 measurements. PICES Special Publication3, 1-191.
Khoo H. K., Ramette R. W., Culberson C. H. and Bates R. G., 1977 Determination of Hydrogen Ion Concentration in Seawater from 5 to 40oC: Standard Potentials at Salinities from 20 to 45. Analytical Chemistry22, vol49 29-34.