Polytropic process


Polytropic Process

A polytropic process is a thermodynamic process that obeys the relation:

[ PV^n = \text{constant} ]

where ( P ) is the pressure, ( V ) is the volume, ( n ) is the polytropic index, and the constant depends on the specific properties of the gas involved in the process.

Understanding the Polytropic Index

The polytropic index ( n ) determines the nature of the process:

  • ( n = 0 ): Isochoric process (constant volume)
  • ( n = 1 ): Isobaric process (constant pressure)
  • ( n = \gamma ) (ratio of specific heats, ( C_p/C_v )): Adiabatic process (no heat transfer)
  • ( n = \infty ): Isothermal process (constant temperature)

Polytropic Process Equation

The general equation for a polytropic process can be written as:

[ PV^n = C ]

where ( C ) is a constant for a particular process.

Work Done in a Polytropic Process

The work done ( W ) during a polytropic process is given by:

[ W = \frac{P_1V_1 - P_2V_2}{1 - n} ]

where ( P_1 ) and ( V_1 ) are the initial pressure and volume, and ( P_2 ) and ( V_2 ) are the final pressure and volume, respectively.

Heat Transfer in a Polytropic Process

The heat transfer ( Q ) can be calculated using the first law of thermodynamics:

[ Q = \Delta U + W ]

where ( \Delta U ) is the change in internal energy.

Differences and Important Points

Property Isochoric Isobaric Adiabatic Isothermal Polytropic
Volume Constant Variable Variable Variable Variable
Pressure Variable Constant Variable Variable Variable
Temperature Variable Variable Variable Constant Variable
Heat Transfer Variable Variable Zero Variable Variable
Work Done Zero Variable Variable Variable Variable
Polytropic Index ( n = 0 ) ( n = 1 ) ( n = \gamma ) ( n = \infty ) Any value

Examples

Example 1: Adiabatic Process

For an adiabatic process where ( n = \gamma ), the work done is:

[ W = \frac{P_1V_1 - P_2V_2}{1 - \gamma} ]

Since there is no heat transfer, ( Q = 0 ), and ( \Delta U = -W ).

Example 2: Isothermal Process

For an isothermal process where ( n = \infty ), the work done is:

[ W = P_1V_1 \ln\left(\frac{V_2}{V_1}\right) ]

Here, ( \Delta U = 0 ) since the temperature is constant, and ( Q = W ).

Example 3: Polytropic Process with a Specific Index

Consider a polytropic process with ( n = 1.2 ), ( P_1 = 100 ) kPa, ( V_1 = 1 ) m³, ( P_2 = 50 ) kPa, and ( V_2 = 2 ) m³. The work done is:

[ W = \frac{100 \times 1 - 50 \times 2}{1 - 1.2} = \frac{0}{-0.2} = 0 ]

This is a special case where the work done is zero, which can occur depending on the values of ( P ), ( V ), and ( n ).

Conclusion

The polytropic process is a versatile concept in thermodynamics that can describe a wide range of processes by varying the polytropic index ( n ). Understanding this process is crucial for solving problems in heat and thermodynamics, especially in engineering applications.