What Temperature Doubles Atmospheric Pressure?

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SUMMARY

The discussion centers on calculating the temperature at which atmospheric pressure doubles, specifically using the Clausius-Clapeyron equation. The initial incorrect calculation yielded a temperature of 7000K, which was deemed unrealistic. A corrected approach, incorporating the constant of integration, led to a more reasonable temperature of 313K (40°C) when atmospheric pressure is set at 100,000 Pa. The participants emphasized the importance of accurately determining constants in thermodynamic equations.

PREREQUISITES
  • Understanding of the Clausius-Clapeyron equation
  • Familiarity with thermodynamic principles
  • Knowledge of gas laws and pressure-temperature relationships
  • Basic calculus for integration and logarithmic functions
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  • Study the derivation and applications of the Clausius-Clapeyron equation
  • Learn about the ideal gas law and its implications in thermodynamics
  • Explore the concept of integration in thermodynamic equations
  • Investigate real-world applications of pressure-temperature relationships in engineering
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Students and professionals in thermodynamics, physicists, and engineers seeking to understand pressure-temperature relationships and their implications in real-world scenarios.

unscientific
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Homework Statement



eurk9u.png


Part (b): Find the temperature in which the pressure is twice the atmospheric pressure.

Homework Equations


The Attempt at a Solution



I've done every part except part (b).

Part (b)

\Delta v \approx v_{gas} = \frac{RT}{p m'}

Therefore the clausis-clapeyron equation reads:

\frac{dp}{dT} = \frac{L}{T \Delta v'} = \frac{L m' p}{RT^2}

\int \frac{1}{p} dp = \frac{Lm'}{R} \int \frac{1}{T^2} dT

ln p = -\frac{Lm'}{RT} + const.

p = p_0 exp(-\frac{Lm'}{RT})

Taking ##p = 2p_0 = 10^5 Pa##, so ##\frac{p}{p_0} = 2##. What's the point of giving us the atmospheric pressure then? All we need is the ratio of pressures.

This gives an answer of ##T = 7000K##, which is insanely hot water. (So hot that the sun gets jealous).
 
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unscientific said:

Homework Statement



eurk9u.png


Part (b): Find the temperature in which the pressure is twice the atmospheric pressure.

Homework Equations





The Attempt at a Solution



I've done every part except part (b).

Part (b)

\Delta v \approx v_{gas} = \frac{RT}{p m'}

Therefore the clausis-clapeyron equation reads:

\frac{dp}{dT} = \frac{L}{T \Delta v'} = \frac{L m' p}{RT^2}

\int \frac{1}{p} dp = \frac{Lm'}{R} \int \frac{1}{T^2} dT

ln p = -\frac{Lm'}{RT} + const.

p = p_0 exp(-\frac{Lm'}{RT})

Taking ##p = 2p_0 = 10^5 Pa##, so ##\frac{p}{p_0} = 2##. What's the point of giving us the atmospheric pressure then? All we need is the ratio of pressures.

This gives an answer of ##T = 7000K##, which is insanely hot water. (So hot that the sun gets jealous).
You're right about not having had to be supplied with the numerical value of the atmospheric pressure, but your integration is not correct. You did not determine the constant of integration correctly. If p = p0, your equation predicts that the corresponding temperature is infinite, and not 373K.
 
Chestermiller said:
You're right about not having had to be supplied with the numerical value of the atmospheric pressure, but your integration is not correct. You did not determine the constant of integration correctly. If p = p0, your equation predicts that the corresponding temperature is infinite, and not 373K.

That's right. So at ##T = T_0## and ##P = P_0##:

ln P_0 = -\frac{Lm'}{RT_0} + const.
const. = ln (P_0) + \frac{Lm'}{RT_0}

Thus,

ln \left(\frac{P}{P_0}\right) = \frac{Lm'}{R}\left(\frac{1}{T_0} - \frac{1}{T}\right)

Where ##T_0 = 300 K## and ##P_0 = 10^5 Pa##.

This gives a temperature of ##313 K = 40 ^oC ##, which seems reasonable.
 
Last edited:

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