A new formula for saturated water steam pressure within the temperature range −25 to 220°C
Instead of approximation formula ln( E ( t )/ E (0)) = [( a − bt ) t /( c + T )] commonly used at present for representing dependence of pressure of saturated streams of liquid water E upon temperature we suggested new approximation formula of greater accuracy in the form ln( E ( t )/ E (0)) = [( A...
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Veröffentlicht in: | Izvestiya. Atmospheric and oceanic physics 2009-12, Vol.45 (6), p.799-804 |
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Sprache: | eng |
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Zusammenfassung: | Instead of approximation formula ln(
E
(
t
)/
E
(0)) = [(
a
−
bt
)
t
/(
c
+
T
)] commonly used at present for representing dependence of pressure of saturated streams of liquid water
E
upon temperature we suggested new approximation formula of greater accuracy in the form ln(
E
(
t
)/
E
(0)) = [(
A
−
Bt
+
Ct
2
)
t
/
T
], where
t
and
T
are temperature in °C and K respectively. For this formula with parameters
A
= 19.846,
B
= 8.97 × 10
−3
,
C
= 1.248 × 10
−5
and
E
(0) = 6.1121 GPa with ITS-90 temperature scale and for temperature range from 0°C to 110°C relative difference of approximation applying six parameter formula by W. Wagner and A. Pruß 2002, developed for positive temperatures, is less than 0.005%, that is approximately 15 times less than accuracy obtained with the firs formula. Increase of temperature range results in relative difference increasing, but for even temperature range from 0°C to 220°C it does not higher than 0.1%. For negative temperatures relative difference between our formula and a formula of D. M. Murphy and T. Koop, 2005, is less than 0.1% for temperatures higher than −25°C. This paper also presents values of coefficients for approximation of Goff and Grach formula recommended by IMO. The procedure of finding dew point
T
d
for known water steam pressure
e
n
based on our formula adds up to solving an algebraic equation of a third degree, which coefficients are presented in this paper. For simplifying this procedure this paper also includes approximation ratio applying a coefficient
A
noted above, in the form
T
d
(
e
n
) =
+ 0.0866ɛ
2
+ 0.0116ɛ
10/3
, where ɛ = ln(
e
n
/
E
(
T
0
)). Error of dew point recovery in this ratio is less than 0.005 K within the range from 0 to 50°C. |
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ISSN: | 0001-4338 1555-628X |
DOI: | 10.1134/S0001433809060139 |