Description Usage Arguments Details Value Author(s) References Examples
Dissociation constant of boric acid (mol/kg)
1 | Kb(S = 35, T = 25, P = 0, pHscale="T")
|
S |
Salinity, default is 35 |
T |
Temperature in degrees Celsius, default is 25oC |
P |
Hydrostatic pressure in bar (surface = 0), default is 0 |
pHscale |
choice of pH scale: "T" for using the total scale, "F" for using the free scale and "SWS" for using the seawater scale, default is total scale |
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.
Kb |
Dissociation constant of boric acid (mol/kg) |
Héloïse Lavigne, Aurélien Proye and Jean-Pierre Gattuso gattuso@obs-vlfr.fr
Dickson, A. G. 1990 Thermodynamics of the dissociation of boric acid in synthetic seawater from 273.15 to 318.15 K. Deep-Sea Research 375, 755-766.
DOE 1994 Handbook of methods for the analysis of the various parameters of the carbon dioxide system in sea water. ORNL/CDIAC-74. Oak Ridge,Tenn.: Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory.
Dickson A. G., Sabine C. L. and Christian J. R., 2007 Guide to best practices for ocean CO2 measurements. PICES Special Publication 3, 1-191.
1 | Kb(S=35,T=25,P=0,pHscale="T")
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