Adiabatic effusion and violation of energy conservation

In summary, the velocity of gas effusing out of an insulated container can be calculated using the formula \sqrt{\frac{2\gamma RT}{(\gamma-1)M}} . This results in each mole of leaking gas having an energy of \frac{\gamma RT}{(\gamma-1)} . However, this is different from the energy contained in 1 mole of gas which is \frac{RT}{(\gamma-1)} . This difference in energy is due to the process being adiabatic and not in equilibrium all the time. In the specific case of helium flowing out of a thermally insulated vessel into vacuum, the velocity can be calculated as 3.3 km/s at a temperature of 1,000
  • #1
mukul
17
2
when the gas effuse out of an insulated container, its velocity is given by
[tex]\sqrt{\frac{2\gamma RT}{(\gamma-1)M}} [/tex]
(irodov's problem 2.42)

This leads to the result that every mole of leaking gas has an energy of
[tex]\frac{\gamma RT}{(\gamma-1)} [/tex]
whereas we know the energy contained in 1 mole of gas is
[tex]\frac{RT}{(\gamma-1)} [/tex]

From where is this difference of energy coming out.

Thanks for helping!
 
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  • #2
Adiabatic. What's Tinitial? What's Tfinal?
 
  • #3
By adiabatic, I mean no heat given to the system.
Also the process here is not in equilibrium all the time. Its a free expansion.

I am posting the exact question I am referring to (from Irodov's Problems in general physics - 2.42):

Ques: Find the rave v with which helium flows out of a thermally insulated vessel into vacuum through a small hole.
The flow rate of the gas inside the vessel is assumed to be negligible under these conditions.
The temperature of helium in the vessel is T = 1,000 K.

Ans: v = [tex]\sqrt{\frac{2\gamma RT}{(\gamma-1)M}} [/tex] = 3.3 km/s
 
  • #4
What's the Joule-Thompson inversion T for He?
 
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Likes mukul
  • #5
it is 51 K at 1 atm
 
  • #6
How many hints do you want?
 
  • #7
Thanks Bystander. I got it. This happens only in case of real gas. For ideal gas rms effusion speed is same as rms speed of gas molecules.
 

Related to Adiabatic effusion and violation of energy conservation

1. What is adiabatic effusion and how does it work?

Adiabatic effusion is the process by which a gas escapes from a container through a small opening without any external heat or energy being added. This occurs because the gas particles have a range of different speeds, and those with higher speeds are able to escape through the opening, causing the average speed and therefore temperature of the gas to decrease.

2. How does adiabatic effusion relate to the violation of energy conservation?

The violation of energy conservation occurs in adiabatic effusion because the gas particles are losing kinetic energy as they escape through the opening, without any external energy being added. This goes against the principle of energy conservation, which states that energy cannot be created or destroyed, only transferred.

3. What is the formula for calculating the rate of adiabatic effusion?

The rate of adiabatic effusion can be calculated using the Graham's Law of effusion, which states that the rate of effusion is inversely proportional to the square root of the gas's molar mass. The formula is: rate of effusion ∝ 1/√molar mass.

4. How does temperature affect adiabatic effusion?

Temperature has a direct effect on adiabatic effusion because it determines the average speed of the gas particles. A higher temperature means that the gas particles have a higher average speed, increasing the rate of effusion. Conversely, a lower temperature results in slower gas particles and a slower rate of effusion.

5. What are some real-world applications of adiabatic effusion?

Adiabatic effusion has several practical applications, such as in gas chromatography, where it is used to separate different components of a gas mixture based on their molar masses. It is also used in the production of aerosol sprays, where the gas particles are forced through a small opening to create a fine mist. Additionally, adiabatic effusion is used in the design of gas pipelines to ensure a steady flow of gas from one location to another.

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