gsw_Krsol_SP_pt

Contents

USAGE:

Krsol = gsw_Krsol_SP_pt(SP,pt)

DESCRIPTION:

Calculates the krypton, Kr, concentration expected at equilibrium with  
air at an Absolute Pressure of 101325 Pa (sea pressure of 0 dbar) 
including saturated water vapor.  This function uses the solubility 
coefficients derived from the data of Weiss and Kyser (1978).

INPUT:

SP  =  Practical Salinity  (PSS-78)                         [ unitless ]
pt  =  potential temperature                                   [ deg C ]
       with reference sea pressure (pr) = 0 dbar.

SP & pt need to have the same dimensions.

OUTPUT:

Krsol = solubility of krypton                                [ umol/kg ]

EXAMPLE:

SP = [34.7118; 34.8915; 35.0256; 34.8472; 34.7366; 34.7324;]
pt = [28.8099; 28.4392; 22.7862; 10.2262;  6.8272;  4.3236;]

Krsol = gsw_Krsol_SP_pt(SP,pt)

Krsol = 

   0.002018888575560
   0.002031777832566
   0.002289819733231
   0.003121753131669
   0.003434407447818
   0.003694847456584

AUTHOR:

Roberta Hamme, Paul Barker and Trevor McDougall      [ help@teos-10.org ]

VERSION NUMBER:

3.04 (6th December, 2013)

REFERENCES:

IOC, SCOR and IAPSO, 2010: The international thermodynamic equation of
 seawater - 2010: Calculation and use of thermodynamic properties.
 Intergovernmental Oceanographic Commission, Manuals and Guides No. 56,
 UNESCO (English), 196 pp.  Available from the TEOS-10 web site.

Weiss, R.F. and T.K. Kyser, 1978: Solubility of Krypton in Water and 
 Seawater. J. Chem. Thermodynamics, 23, 69-72.

The software is available from http://www.TEOS-10.org