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The Boiling Point of Water at High Altitude

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The Boiling Point of Water at High Altitude
The relationship between the equilibrium vapor pressure of a liquid or solid and temperature is given by
the Clausius-Clapeyron equation.
In this assignment you will measure the vapor pressure of water at a given temperature and use this
data and the Clausius-Clapeyron equation to calculate the boiling point of water on the top of Mt. Denali
in Alaska.
Assignment
The balloon is filled with 0.40 moles of water vapor at a pressure of 1500 Torr and a temperature of 400
K. Click the down arrows in the Live Data Temperature control area until the temperature stops
decreasing. This temperature represents the equilibrium temperature where water as a gas exists in
equilibrium with water as a liquid. The pressure at this temperature is the vapor pressure. Record the
vapor pressure (in Torr) and the temperature (in K) below
π‘ƒπ‘Ÿπ‘’π‘ π‘ π‘’π‘Ÿπ‘’ = 1500 π‘‘π‘œπ‘Ÿπ‘Ÿ
π‘‡π‘’π‘šπ‘π‘’π‘Ÿπ‘Žπ‘‘π‘’π‘Ÿπ‘’ = 393.38 𝐾
The Clausius-Clapeyron equation may be written in several forms. For this assignment, the most useful
form can be written as
βˆ†π»π‘£π‘Žπ‘ 1
𝑃2
1
𝑙𝑛 ( ) = −
( − )
𝑃1
𝑅
𝑇2 𝑇1
If P1 and T1 are the experimental vapor pressure and temperature that you measured and the pressure
at the top of Mt. Denali, P2, is 340 Torr, the boiling point of water, T2, at the top of the mountain can be
calculated by solving the Clausius-Clapeyron equation for T2.
The value of R is 8.314 J·K-1·mol-1 and ΔHvap for water is 40.67 kJ/mol
Calculate the boiling point of water at the top of Mt. Denali.
βˆ†π»π‘£π‘Žπ‘ 1
𝑃2
1
𝑙𝑛 ( ) = −
( − )
𝑃1
𝑅
𝑇2 𝑇1
π‘…π‘’π‘Žπ‘Ÿπ‘Žπ‘›π‘”π‘–π‘›π‘” π‘’π‘žπ‘’π‘Žπ‘‘π‘–π‘œπ‘› π‘‘π‘œ π‘šπ‘Žπ‘˜π‘’ 𝑇2 π‘‘β„Žπ‘’ 𝑠𝑒𝑏𝑗𝑒𝑐𝑑
−
𝑅
𝑃2
1
1
𝑙𝑛 ( ) = ( − )
βˆ†π»π‘£π‘Žπ‘
𝑃1
𝑇2 𝑇1
[−
𝑅
𝑃2
1
1
𝑙𝑛 ( )] +
=
βˆ†π»π‘£π‘Žπ‘
𝑃1
𝑇1
𝑇2
π‘‡β„Žπ‘’π‘Ÿπ‘’π‘“π‘œπ‘Ÿπ‘’
1
𝑅
𝑃2
1
= [−
𝑙𝑛 ( )] +
𝑇2
βˆ†π»π‘£π‘Žπ‘
𝑃1
𝑇1
𝑃1 = 1500 π‘‡π‘œπ‘Ÿπ‘Ÿ, 𝑃2 = 340 π‘‡π‘œπ‘Ÿπ‘Ÿ, 𝑇1 = 393.38 𝐾 π‘Žπ‘›π‘‘ 𝑇2 =?
𝑅 = 8.314 𝐽 βˆ™ 𝐾 −1 βˆ™ π‘šπ‘œπ‘™ −1
βˆ†π»π‘£π‘Žπ‘ = 40.67𝐾𝐽/π‘šπ‘œπ‘™ = 40.67 × 103 𝐽 βˆ™ π‘šπ‘œπ‘™ −1
1
8.314 𝐽 βˆ™ 𝐾 −1 βˆ™ π‘šπ‘œπ‘™ −1
340 π‘‡π‘œπ‘Ÿπ‘Ÿ
1
= [−
× π‘™π‘› (
)] +
3
−1
𝑇2
40.67 × 10 𝐽 βˆ™ π‘šπ‘œπ‘™
1500 π‘‡π‘œπ‘Ÿπ‘Ÿ
393.38 𝐾
1
1
= [3.034 × 10−4 ]𝐾 −1 +
𝑇2
393.38 𝐾
1
= (2.8455 × 10−3 )𝐾 −1
𝑇2
𝑇2 =
1
(2.8455 × 10−3 )𝐾 −1
𝑇2 = 351.4 𝐾
Therefore, the boiling point of water on top of Mt. Denali = 351.4 K
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