seacarb (version 2.4.4)

kconv: Conversion factors to change the pH scale of dissociation constants

Description

Conversion factors from the total scale to the free and seawater scales

Usage

kconv(S=35,T=25, P=0, kf="x")

Arguments

S

Salinity, default is 35

T

Temperature in degrees Celsius, default is 25oC

P

Hydrostatic pressure in bar (surface = 0), default is 0

kf

"pf" for using Kf from Perez and Fraga (1987) and "dg" for using Kf from Dickson and Riley (1979 in Dickson and Goyet, 1994); the default value is "pf", except if T is outside the ragne 9 to 33oC or of S is outside the range 10 to 40. In these cases, t

Value

• The function returns a list with 3 conversion factors :
• ktotal2SWS
  to convert from the total scale to seawater scale
• ktotal2free
  to convert from the total scale to the free scale
• kfree2SWS
  to convert from the free scale to the seawater scale

encoding

latin1

Details

It is critical to consider that each formulation is valid in specific ranges of temperature and salinity: - Perez and Fraga (1987): S ranging between 10 and 40 and T ranging between 9 and 33oC. - Dickson and Riley (1979 in Dickson and Goyet, 1994): S ranging between 0 and 45 and T ranging between 0 and 45oC.

References

Dickson A.G. and F.J. Millero, 1987 A comparison of the equilibrium constants for the dissociation of carbonic acid in seawater media. Deep-Sea Research 34:1733-1743.

See Also

pHconv.

Examples

##To convert dissociation constants from the total scale to the free scale
## (at salinity=35, temperature=25oC and atmospheric pressure):
kconv(35,25,0)
conv <- kconv()
 c(K1_total=K1(),K1_SWS=K1()*conv$ktotal2SWS,K1_free=K1()*conv$ktotal2free)