Condensable Atmosphere

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==Condensable Atmosphere==
 
 
 
The coefficients for the saturation temperature relation for the condensing gas are now input parameters.  
 
The coefficients for the saturation temperature relation for the condensing gas are now input parameters.  
 
KRC uses the Clausius-Clapeyron relation:
 
KRC uses the Clausius-Clapeyron relation:

Revision as of 09:59, 15 January 2019

The coefficients for the saturation temperature relation for the condensing gas are now input parameters. KRC uses the Clausius-Clapeyron relation:


ln P = a - b/T


where P is pressure in Pascal and T is temperature in Kelvin.

This should be useful for Mars, Titan, Pluto etc.


SatPrA correspond to the Clausius-Clapeyron coefficient 'a'.


SatPrB corresponds to the Clausius-Clapeyron coeffcient 'b'.

Values for CO2 are a = 27.9546 and b = 3182.48 (Provided by HHK, most likely from the Mars book). Values for N2 are a = 9.2338 and b = -724.9720 (Derived by SP using this table: File:Clausius Clapeyron.xlsx

The proper molecular weight should be input AMW. The Mass-fraction of mean atmosphere that is non-condensing should also be specified with FANON.

Mars

SatPrB = 3182.48
SatPrA = 27.9546
AMW    = 43.54             #SP's own calculation
FANON  = 0.040             #Paul R. Mahaffy, Science 2013 (SAM)
KPREF  = 1


Pluto

 SatPrB = 9.2338
 SatPrA = -724.9720
 AMW    = 27.
 FANON  = 0.1
 KPREF  = 0


Titan

SatPrB = 9.2338
SatPrA = -724.9720
AMW    = 28.8
FANON  = 0.016
KPREF  = 0


KRC function: KRC_Cond_Gas()

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