We solve according to the Clapeyron-Clausius equation
ln(P2P1)=RΔHvap(T21−T11)
P1=100mmHg=0.131579 atm
R=8.314 J/(K×mol)
T2=298.15 K
T1=294.35 K
ln(P20.131579)=8.31438000(298.151−294.351)
ln(P20.131579)=−0.197905708
P20.131579=e−0.197905708
P20.131579=0.820447211
P2=0.16037473 atm or
1 the physical atmosphere is equal to 760.002211 millimeters of mercury
0.16037473 atm=121.885149 mmHg
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