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the gas in a cloud chamber at a temperature of 300k undergoes a rapid expansion. assuming the process is adiabatic, calculate the final temperature, if r=1.40 and the volume expansion ration is 1.28

Bright Obot , 4 Years ago
Grade 12
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Askiitians Tutor Team

Last Activity: 5 Months ago

To determine the final temperature of the gas in a cloud chamber after a rapid adiabatic expansion, we can use the principles of thermodynamics, specifically the adiabatic process equations. In this scenario, we know the initial temperature, the specific heat ratio (γ), and the volume expansion ratio. Let's break down the calculation step by step.

Understanding Adiabatic Processes

An adiabatic process is one in which no heat is exchanged with the surroundings. For an ideal gas undergoing adiabatic expansion, the relationship between the initial and final temperatures and volumes can be expressed using the formula:

T2 = T1 * (V1/V2)^(γ-1)

Given Values

  • Initial Temperature (T1) = 300 K
  • Specific Heat Ratio (γ) = 1.40
  • Volume Expansion Ratio (V2/V1) = 1.28

Calculating the Final Temperature

First, we need to express the volume expansion ratio in terms of V1 and V2. Since the volume expansion ratio is given as V2/V1 = 1.28, we can rearrange this to find V1/V2:

V1/V2 = 1 / 1.28

V1/V2 ≈ 0.78125

Now, we can substitute this value into the adiabatic temperature equation:

T2 = 300 K * (0.78125)^(1.40 - 1)

Calculating the exponent:

1.40 - 1 = 0.40

Now, we compute:

(0.78125)^(0.40) ≈ 0.870

Finally, substituting this back into the equation for T2:

T2 ≈ 300 K * 0.870 ≈ 261 K

Final Result

The final temperature of the gas after the adiabatic expansion is approximately 261 K. This demonstrates how the temperature of a gas decreases during an adiabatic expansion due to the work done by the gas as it expands without heat exchange.

Real-World Implications

This principle is not just theoretical; it has practical applications in various fields, such as meteorology and engineering. For example, when air rises in the atmosphere, it expands adiabatically, leading to cooling, which can result in cloud formation. Understanding these processes helps in predicting weather patterns and designing efficient thermal systems.

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