This MCQ module is based on: Thermodynamic Processes
Thermodynamic Processes
This assessment will be based on: Thermodynamic Processes
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Thermodynamic Processes
11.9 Quasi-Static Processes
To apply the relation \(W = \int P\,dV\) we need pressure to be well defined throughout the process — a single value at every instant. That requires the process to be infinitely slow, so the gas is essentially in equilibrium at every instant. Such an idealised slow process is called a quasi-static process. Quasi-static processes can be plotted on a P–V diagram as smooth curves.
Real processes (a sudden expansion, an explosion) are not quasi-static, but for laboratory analysis we often treat them as such, knowing the predictions are good when the process is much slower than the molecular relaxation time.
11.10 The Five Standard Processes
Four classic processes plus a free expansion span almost every textbook problem.
11.10.1 Isobaric Process (P = constant)
Pressure is held constant. Examples: water boiling in an open pot at 1 atm; gas in a cylinder with a free piston pushed only by atmosphere.
\(\Delta U = \mu C_v\,\Delta T\); \(Q = \mu C_p\,\Delta T\). Verify \(Q = \Delta U + W\) ✓.
11.10.2 Isochoric / Isovolumetric Process (V = constant)
Volume is held constant; e.g. gas inside a sealed rigid container being heated. Since dV = 0:
11.10.3 Isothermal Process (T = constant)
Temperature is held constant — for example, by keeping the system in contact with a large heat reservoir. For an ideal gas \(U = U(T)\), so:
So an isothermal expansion (V₂ > V₁) absorbs exactly the same amount of heat as the work it does. The P–V curve is a hyperbola \(P = \text{const}/V\).
11.10.4 Adiabatic Process (Q = 0)
No heat exchanged with surroundings. Either the process is so fast that there is no time for heat flow, or the system is perfectly insulated. From the First Law, \(\Delta U = -W\). Combining \(dU = \mu C_v dT\) and \(\delta W = P dV = (\mu R T/V)dV\) gives:
An adiabatic curve on a P–V diagram (\(PV^\gamma = \text{const}\)) is steeper than the corresponding isotherm \(PV = \text{const}\). On adiabatic expansion, T falls; on adiabatic compression, T rises (the bicycle-pump effect, the diesel-engine principle).
11.10.5 Free Expansion
A gas expands into a vacuum through a partition that is suddenly removed. There is no work done (no piston pushed back, P_ext = 0) and no heat exchange (rigid insulated walls):
This is not a quasi-static process — pressure is undefined during the rush — so it cannot be plotted as a smooth curve on the P–V plane. Joule's free-expansion experiment was the historical proof that internal energy of an ideal gas depends only on T.
11.11 Summary of the Five Processes
| Process | Constraint | W (by gas) | Q | ΔU |
|---|---|---|---|---|
| Isobaric | P const | P ΔV = µR ΔT | µC_p ΔT | µC_v ΔT |
| Isochoric | V const | 0 | µC_v ΔT | µC_v ΔT |
| Isothermal | T const | µRT ln(V₂/V₁) | = W | 0 |
| Adiabatic | Q = 0 | (P₁V₁ − P₂V₂)/(γ−1) | 0 | −W |
| Cyclic | State returns | = area enclosed | = W | 0 |
Worked Examples
Example 11.8: Work in isothermal expansion (NCERT-style)
2.0 mol of an ideal gas at 27 °C expands isothermally and reversibly from a volume of 5 L to 25 L. Compute Q, W and ΔU. R = 8.314 J/mol·K.
\(\ln 5 = 1.609\). \(W = 2.0\times 8.314\times 300\times 1.609 = 8023\) J ≈ 8.02 kJ (work done by gas).
ΔU = 0 (isothermal, ideal gas). Q = W = 8.02 kJ.
Example 11.9: Adiabatic compression of air
Air (γ = 1.4) at 27 °C is compressed adiabatically and quasi-statically to 1/8 of its initial volume. Find the final temperature.
\(T_2 = 300 \times 8^{0.4} = 300 \times 2.297 = \boxed{689\text{ K}}\) ≈ 416 °C.
This is the principle of a diesel engine: air alone is compressed to ~1/15 its initial volume, raising T to ~700 °C — hot enough to ignite the diesel droplets injected at the top of the stroke.
Example 11.10: Cyclic process with two paths (NCERT)
An ideal gas at 30 atm and 27 °C is allowed to expand isothermally to a final pressure of 1 atm. (a) What is the work done by the gas? (b) Compare to the same process done adiabatically (γ = 1.4).
(b) Adiabatic to same P₁/P₂ = 30: \(T_2 = T_1(P_2/P_1)^{(\gamma-1)/\gamma} = 300(1/30)^{0.286}\).
\(30^{0.286} = e^{0.286\ln 30} = e^{0.973} = 2.65\). So T₂ = 300/2.65 = 113.4 K.
\(W_{ad} = \mu R(T_1 - T_2)/(\gamma -1) = 1\times 8.314 \times 186.6 / 0.4 = 3878\) J.
Adiabatic gives less work — the temperature drops, so the gas cools and pushes less.
Example 11.11: Heat in an isochoric heating
5 L of nitrogen (diatomic, C_v = 5R/2) at 1 atm and 27 °C is heated at constant volume to 327 °C. Find the heat absorbed and the final pressure.
Q = µC_v ΔT = 0.2004 × (5/2)(8.314) × 300 = 1250 J.
Final P: \(P_2/P_1 = T_2/T_1 = 600/300 = 2\), so P₂ = 2 atm.
W = 0 (constant volume); ΔU = Q.
Interactive: Process Selector & Energy Calculator L3 Apply
Pick a process; set initial state and the final volume (or pressure). The applet computes W, Q and ΔU using ideal-gas formulas (γ = 1.4 for air; C_v = 5R/2).
- Take a 2-litre PET bottle. Put about 5 mL of water inside, swirl, then strike a match and drop in a tiny amount of smoke (just a wisp).
- Cap the bottle tightly. Squeeze hard with both hands and hold for a few seconds.
- Release the squeeze suddenly while looking at the inside.
Explanation: Releasing the squeeze causes the air to expand rapidly — almost adiabatically. Adiabatic expansion drops the temperature; the cool air can no longer hold all its water vapour, which condenses on the smoke nuclei to form tiny droplets — a cloud. Real clouds form when warm moist air rises and cools adiabatically.
Competency-Based Questions
Q1. L1 Remember Define a quasi-static process.
Q2. L3 Apply Compute work in segment A→B.
Q3. L3 Apply Compute work in segment C→A (isothermal compression at 300 K).
Q4. L3 Apply Compute net work in one full cycle.
Q5. L5 Evaluate Why is an adiabatic expansion always cooler than the isothermal between the same volumes?
Assertion-Reason Questions
Assertion (A): The slope of an adiabatic curve on a P–V diagram is steeper than that of an isothermal at the same point.
Reason (R): The slope of an adiabat is −γ P/V, while the slope of an isotherm is −P/V; γ > 1.
Assertion (A): In a free expansion of an ideal gas, the temperature does not change.
Reason (R): Free expansion has Q = 0 and W = 0, so ΔU = 0; for an ideal gas, U depends only on T, hence T is constant.
Assertion (A): An isothermal expansion of an ideal gas requires heat absorbed from the surroundings.
Reason (R): ΔU = 0 in an isothermal process (ideal gas), so by First Law Q = W, and W > 0 in expansion implies Q > 0.