The ratio of specific heat of air at constant pressure to the specific heat of air at constant volume is equal to -
1.41
The question asks about the ratio of the specific heat of air at constant pressure ($C_p$) to the specific heat of air at constant volume ($C_v$). This ratio is a fundamental property of gases in thermodynamics and is denoted by the Greek letter gamma ($\gamma$).
The formula for this ratio is:
\(\gamma = \frac{C_p}{C_v}\)
This ratio, $\gamma$, is also commonly known as the adiabatic index or the Poisson constant. Its value depends on the molecular structure of the gas:
Air is primarily composed of diatomic gases (about 78% Nitrogen and 21% Oxygen). Therefore, air behaves very closely to a diatomic gas in terms of its thermodynamic properties.
The theoretical value of $\gamma$ for an ideal diatomic gas is 1.4 (\(C_p = \frac{7}{2}R\) and \(C_v = \frac{5}{2}R\), where R is the ideal gas constant, so \(\gamma = \frac{7/2}{5/2} = \frac{7}{5} = 1.4\)).
In real-world conditions, the value for air is slightly different from the ideal value due to various factors, including temperature effects and the presence of small amounts of other gases. Experimental values for the specific heat ratio of dry air at room temperature are very close to 1.4.
Let's look at the given options:
Comparing the theoretical and experimental values for air with the options, the value closest to 1.4 and commonly accepted for air under standard conditions is 1.41.
The question asks for the ratio \(C_p/C_v\) for air.
Based on the composition of air and thermodynamic principles, the specific heat ratio \(\gamma\) for air is approximately 1.4. Looking at the provided options, 1.41 is the value that aligns best with the properties of air.
| Property | Symbol | Approximate Value for Air at Room Temp |
|---|---|---|
| Specific Heat at Constant Pressure | \(C_p\) | \(1.005 \text{ kJ/kg} \cdot \text{K}\) |
| Specific Heat at Constant Volume | \(C_v\) | \(0.718 \text{ kJ/kg} \cdot \text{K}\) |
| Specific Heat Ratio | \(\gamma = C_p/C_v\) | \(\frac{1.005}{0.718} \approx 1.40\) (or typically stated as 1.40 or 1.41 in various contexts) |
Therefore, the ratio of specific heat of air at constant pressure to the specific heat of air at constant volume is approximately 1.41.
| Concept | Definition | Significance |
|---|---|---|
| Specific Heat (\(C\)) | Amount of heat required to raise the temperature of a unit mass of a substance by one degree Celsius (or Kelvin). | Indicates how much energy is needed to change a substance's temperature. |
| Specific Heat at Constant Volume (\(C_v\)) | Specific heat when the volume of the substance is kept constant. | Relates heat added to internal energy change: \(\Delta U = m C_v \Delta T\). |
| Specific Heat at Constant Pressure (\(C_p\)) | Specific heat when the pressure of the substance is kept constant. | Relates heat added to enthalpy change: \(\Delta H = m C_p \Delta T\). |
| Specific Heat Ratio (\(\gamma\)) | The ratio \(C_p / C_v\). | Crucial for understanding adiabatic processes and the speed of sound in a gas. |
For an ideal gas, there is a relationship between \(C_p\), \(C_v\), and the ideal gas constant \(R\) (specifically, the specific gas constant, \(R_{specific} = R_{universal} / M\), where M is the molar mass):
Meyer's relation states: \(C_p - C_v = R_{specific}\)
Using this relation, we can also express \(C_p\) and \(C_v\) in terms of \(\gamma\) and \(R_{specific}\):
These relationships highlight how the specific heat ratio \(\gamma\) is interconnected with the specific heats themselves and the gas constant, providing further insight into the thermodynamic behavior of gases.
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