For an ideal gas, the slopes of the adiabatic and isothermal curves are related to the specific heat capacities and the ratio of specific heats \( \gamma \).
The general relationship between the slopes of the adiabatic and isothermal curves is given by: \[ \frac{c_p}{c_v} = \gamma \] The slope of the adiabatic curve \( m_a \) and the slope of the isothermal curve \( m_i \) are related through the ratio of specific heats \( \gamma \).
From the ideal gas laws and thermodynamic relationships, we know that: \[ m_a = \gamma m_i \]
Thus, the correct relationship between the slopes is \( m_a = \gamma m_i \).
Kepler's second law (law of areas) of planetary motion leads to law of conservation of
An ideal diatomic gas is made up of molecules that do not vibrate. Its volume compressed by a factor of 32,without any exchange of heat. If the initial and final pressures are P1 and P2,respectively,the ratio P1:P2,is:
Kepler's second law (law of areas) of planetary motion leads to law of conservation of