

Isothermal, Adiabatic, Isobaric & Isochoric Processes: Differences and Key Formulas
Thermodynamic processes describe how the state of a system changes when energy is transferred as heat or work. These processes form the foundation for topics like heat engines, refrigerators, and the working of steam engines. Thermodynamics, as a branch of physics, studies the movement and transformation of energy in the form of heat and work, and the rules governing these changes.
Definition of a Thermodynamic System
A thermodynamic system is a specific, defined part of the universe being studied, often described by state variables like pressure (P), volume (V), temperature (T), and internal energy (U). The system’s boundary separates it from its surroundings. There are three major types of systems:
- Open System: Mass and energy can move in or out.
- Closed System: Only energy (not mass) transfers occur.
- Isolated System: No mass or energy transfer is allowed.
What is a Thermodynamic Process?
A thermodynamic process is a pathway by which a system undergoes a change from one state to another. These processes can involve changes in temperature, pressure, volume, or internal energy. The key state variables are defined only when the system is in equilibrium with its surroundings.
Types of Thermodynamic Processes
Four primary thermodynamic processes are:
- Isothermal Process: Constant temperature (T). Heat can enter or leave the system to keep T the same. (Learn more)
- Adiabatic Process: No heat exchange (Q = 0). System is insulated thermally. (Explore adiabatic)
- Isobaric Process: Constant pressure (P). Volume may change; commonly seen when water boils in open vessels.
- Isochoric Process: Constant volume (V). Pressure or temperature may change; no work is done since ΔV = 0.
Process | Condition | Key Formula | Example |
---|---|---|---|
Isothermal | ΔT = 0 | W = nRT ln(Vf/Vi) | Melting of ice at 0°C |
Adiabatic | Q = 0 | PVγ = const | Bursting of a tyre |
Isobaric | ΔP = 0 | W = PΔV | Boiling water in open pan |
Isochoric | ΔV = 0 | W = 0 | Heating in a sealed cooker |
Key Equations and How to Apply Them
Process | Work Done (W) | Change in Internal Energy (ΔU) | Heat (Q) |
---|---|---|---|
Isothermal | nRT ln(Vf/Vi) | 0 | Q = W |
Adiabatic | [P1V1 - P2V2]/(γ - 1) | -W | 0 |
Isobaric | PΔV | Q - W | ΔU + W |
Isochoric | 0 | Q | ΔU |
How to Approach Thermodynamics Problems
- Identify the process type (isothermal, adiabatic, isobaric, isochoric).
Hint: See which state variable is constant.
- List what is given (values for P, V, T, n).
Convert volumes to m3, pressures to Pascals, etc., if needed.
- Choose the right formula from the tables above.
- Substitute values and solve stepwise.
- Interpret the answer—does it match expectations for expansion, compression, heating, or cooling?
Example Problem with Solution
Problem: An ideal gas expands isothermally at 300 K from 5 L to 10 L. If there are 2 mol of gas, calculate the work done (R = 8.314 J/mol·K).
- Isothermal process: T = 300 K, n = 2, Vi = 5 L, Vf = 10 L
- W = nRT ln(Vf/Vi)
- W = 2 × 8.314 × 300 × ln(10/5) = 2 × 8.314 × 300 × 0.6931
- W ≈ 3455 J
Work done by the gas: 3455 J
Understanding Key Thermodynamics Concepts
- Internal Energy (U): The sum of all molecular energies (kinetic + potential) in a system.
Depends only on the state, not the path.
- Enthalpy (H): H = U + PV. Used especially during constant pressure (isobaric) processes.
- Entropy (S): Represents the measure of molecular disorder, or the unusable energy in a system.
Real-World Examples of Thermodynamic Processes
Scenario | Process Type | Explanation |
---|---|---|
Melting of ice | Isothermal | Occurs at constant 0°C; heat absorbed, temp unchanged. |
Boiling water in open pan | Isobaric | Vessel open to air, pressure remains constant. |
Heating food in sealed cooker | Isochoric | Volume is fixed, only temperature and pressure rise. |
Refrigerator’s cooling cycle | Adiabatic | Rapid gas expansion cools the inside without heat entering/exiting. |
Key Laws of Thermodynamics
- Zeroth Law: Foundation for temperature measurement—if two systems are in equilibrium with a third, they are with each other.
- First Law: Conservation of energy: ΔU = Q - W (change in internal energy = heat added - work done).
- Second Law: Entropy of an isolated system always increases; heat doesn’t flow from cold to hot by itself.
- Third Law: As T → 0 K, entropy approaches a minimum (usually zero for a perfect crystal).
Continue Your Learning
- Review thermodynamics concepts and their applications.
- Try MCQs and practice sets at Physics MCQs: Units and Measurements.
- Deepen understanding of heat and temperature at heat introduction and classification and difference between heat and temperature.
- Revisit energy conservation and its role in thermodynamics.
Summary
Understanding thermodynamic processes equips students to solve physical phenomena involving heat, work, and energy conversion. Mastering the definitions, equations, and conceptual differences between isothermal, adiabatic, isobaric, and isochoric processes is essential for problem-solving in Physics, and supports success in board exams and beyond. Systematic practice and revision using tables, solved examples, and links above will build your confidence in this fundamental topic.
FAQs on Thermodynamic Processes Explained: Concepts, Types & Applications
1. What are the four primary types of thermodynamic processes as per the Class 11 Physics syllabus?
The four main types of thermodynamic processes are defined by the state variable that remains constant:
- Isothermal process: Temperature remains constant (ΔT = 0).
- Adiabatic process: No heat exchange with surroundings (Q = 0).
- Isobaric process: Pressure remains constant (ΔP = 0).
- Isochoric process: Volume remains constant (ΔV = 0).
2. What are some real-world examples of thermodynamic processes?
Thermodynamic processes occur in many everyday situations:
- Melting of ice—an isothermal process at 0°C.
- Boiling water in an open pan—isobaric process at atmospheric pressure.
- Heating food in a pressure cooker—isochoric process (fixed volume).
- Refrigerator cooling cycle—adiabatic rapid expansion of refrigerant gas.
3. Explain the key concepts of internal energy, enthalpy, and entropy in a thermodynamic system.
- Internal Energy (U): Total energy (kinetic + potential) of all molecules in a system; depends only on the current state.
- Enthalpy (H): Total heat content, defined as H = U + PV, useful for constant pressure processes.
- Entropy (S): Measure of molecular disorder or randomness; indicates unavailable energy for work.
4. Briefly explain the four laws of thermodynamics.
- Zeroth Law: If two systems are in thermal equilibrium with a third, they are in equilibrium with each other.
- First Law: Energy cannot be created or destroyed; change in internal energy equals heat added minus work done (ΔU = Q - W).
- Second Law: Entropy of an isolated system always increases; heat flows naturally from hot to cold.
- Third Law: As temperature approaches absolute zero, entropy approaches a minimum (zero for perfect crystals).
5. How is an adiabatic process fundamentally different from an isothermal process?
The main difference is in energy exchange and temperature:
- Isothermal process: Temperature is kept constant by letting heat flow in/out.
- Adiabatic process: No heat is allowed to enter or leave, so temperature changes as the system does work or has work done on it.
6. What is the difference between a state function and a path function in thermodynamics?
- State functions: Depend only on the current state, not the process followed (e.g., internal energy U, temperature T, volume V, pressure P, entropy S).
- Path functions: Depend on the actual process or path taken (e.g., work W and heat Q).
7. Why is the concept of a quasi-static process important for understanding thermodynamics?
A quasi-static process is theoretically infinitely slow, so the system remains in equilibrium at each stage. This idealization allows precise definition and measurement of properties (P, V, T) throughout the process and is essential for deriving thermodynamic equations and analyzing maximum efficiency.
8. Can a real-world process ever be truly reversible? Explain why.
No real process can be perfectly reversible. Real processes always have some friction, heat losses, or other dissipative effects that generate entropy, making them irreversible. Reversible processes are idealized models used to set theoretical efficiency limits.
9. What is the significance of the First Law of Thermodynamics in daily life and engineering?
The First Law states that energy is conserved in any process.
- In daily life, it explains energy conversions such as in our bodies and appliances.
- In engineering, it governs machines like engines and refrigerators by relating heat supplied, work done, and internal energy change.
10. What formulas are commonly used for work done in different thermodynamic processes?
- Isothermal: Work, W = nRT ln(Vf / Vi)
- Adiabatic: W = [P1V1 - P2V2]/(γ - 1)
- Isobaric: W = PΔV
- Isochoric: W = 0 (since volume is constant)
11. How do you identify which thermodynamic process is taking place in a problem?
Identify the process by the variable kept constant:
- Isothermal: Temperature (T) is constant
- Adiabatic: No heat exchange (Q = 0)
- Isobaric: Pressure (P) is constant
- Isochoric: Volume (V) is constant
12. Why are P-V diagrams important in studying thermodynamic processes?
P-V diagrams visually represent the relationship between pressure and volume during thermodynamic processes. They help students:
- Quickly identify the type of process by shape (hyperbola, vertical/horizontal line, etc.)
- Calculate work done (area under the curve)
- Compare processes for better conceptual clarity

















