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Thermodynamics

01
CONCEPT

Gas Laws & Ideal Gas Equation

In one line
A gas is described by four quantities: P, V, T and amount n. The gas laws link them, and together they give PV = nRT.
SYSTEM

13.1.1 Thermodynamic system

  1. System: the part (usually a gas) we study; everything outside is the surroundings.
  2. Open: exchanges energy and matter. Closed: energy only. Isolated: neither.
  3. State variables: P, V, T, U, n. They fix the state of the system.
Openenergy + matterClosedenergy onlyIsolatednothing
Open, closed and isolated systems
ZEROTH LAW

13.1.2 Zeroth law of thermodynamics

  1. If A and B are each in thermal equilibrium with C, then A and B are in thermal equilibrium with each other.
  2. This law defines temperature: bodies in equilibrium have the same T.
ABCA ⇌ CB ⇌ Cso A ⇌ B
BOYLE’S LAW

13.1.3 Boyle’s law (T constant)

PV = constant  ·  P₁V₁ = P₂V₂
  1. Also Pρ = constant, since ρ ∝ 1V.
  2. P–V graph: rectangular hyperbola. PV–P graph: horizontal line.
  3. Volume falls by x% ⇒ pressure rises by 100x100 − x% (not x%).
CHARLES’S LAW

13.1.4 Charles’s law (P constant)

V ∝ T  ·  V₁T₁ = V₂T₂
  1. In °C: Vt = V₀(1 + t273.15).
  2. V–t line meets the t-axis at −273.15°C. Always use kelvin in the formula.
GAY-LUSSAC’S LAW

13.1.5 Gay-Lussac’s law (V constant)

P ∝ T  ·  P₁T₁ = P₂T₂
VPBoyle: PV = constt (°C)V−273Charles: V ∝ TTPGay-Lussac: P ∝ T
Boyle, Charles and Gay-Lussac graphs
AVOGADRO AND DALTON

13.1.6 Avogadro’s and Dalton’s laws

  1. Avogadro: equal volumes of all gases at the same P and T have equal numbers of molecules.
  2. 1 mole of any gas at STP occupies 22.4 L and has NA = 6.023 × 10²³ molecules.
  3. Dalton: total pressure of non-reacting gases = sum of partial pressures.
P = P₁ + P₂ + P₃ + …
IDEAL GAS EQUATION

13.1.7 Ideal gas equation

PV = nRT
Amount of gasEquationConstant
n molesPV = nRTR = 8.31 J mol⁻¹ K⁻¹
N moleculesPV = NkBTkB = RNA = 1.38 × 10⁻²³ J K⁻¹
mass mPV = mMRTM = molar mass
  1. R ≈ 8.31 J mol⁻¹ K⁻¹ ≈ 2 cal mol⁻¹ K⁻¹.
  2. PV has the unit of energy (N m = J).
DENSITY AND NUMBER

13.1.8 Density and number of molecules

ρ = PMRT  ·  ρP ∝ 1T
N ∝ PVT  ·  nv = NV = PkBT
  1. Same P, V, T ⇒ same number of molecules, whatever the gas.
  2. Gas leaking from a fixed vessel: mass left ∝ PT.
  3. Two vessels joined, total internal energy kept: P(V₁ + V₂) = P₁V₁ + P₂V₂ (same T) and n is conserved.
Practise PYQs on this topicGas Laws & Ideal Gas Equation · 86 questions with solutions
02
CONCEPT

Degrees of Freedom & Internal Energy

In one line
Degrees of freedom count the independent ways a molecule can move. Each one stores energy, so they decide the internal energy of a gas.
DEGREES OF FREEDOM

13.2.1 Degrees of freedom

Degrees of freedom
  1. A = number of atoms, B = number of fixed bonds (constraints).
  2. Translational f is always 3 (motion along x, y, z).
  3. Rotation about the axis of a linear molecule is not counted (negligible moment of inertia).
monoatomicf = 3diatomicf = 3 + 2 = 5non-linear triatomicf = 3 + 3 = 6
Monoatomic, diatomic and non-linear triatomic molecules
GasExamplef (room temperature)
monoatomicHe, Ne, Ar3 (trans)
diatomicH₂, O₂, N₂5 (3 trans + 2 rot)
triatomic linearCO₂5 (rigid)
triatomic non-linearH₂O, CH₄6 (3 trans + 3 rot)
diatomic, vibratinghigh T7 (+2 vibrational)
  1. One vibrational mode adds 2 degrees of freedom (kinetic + potential energy).
INTERNAL ENERGY

13.2.2 Internal energy

  1. U = kinetic energy + potential energy of the molecules.
  2. Ideal gas: no intermolecular force ⇒ U is wholly kinetic and depends on T only.
  3. Each degree of freedom carries 12kBT per molecule (law of equipartition, proved in Kinetic Theory of Gases).
U = f2nRT  ·  ΔU = f2nRΔT = nCvΔT
U = f2PV
  1. U is a state function: ΔU depends only on the initial and final states, not on the path.
  2. For a cyclic process ΔU = 0.
MIXTURES

13.2.3 Internal energy of a mixture

U = f₁2n₁RT + f₂2n₂RT
fmix = n₁f₁ + n₂f₂n₁ + n₂  ·  Tmix = n₁f₁T₁ + n₂f₂T₂n₁f₁ + n₂f₂
MOVING CONTAINER STOPPED

13.2.4 Moving container stopped suddenly

12Mv² = f2RΔT  ⇒  ΔT = Mv²fR = (γ − 1)Mv²2R
  1. M = molar mass. Insulated container: no heat is lost.
  2. Monoatomic: ΔT = Mv² ÷ 3R. Diatomic: ΔT = Mv² ÷ 5R.
Practise PYQs on this topicDegrees of Freedom & Internal Energy · 45 questions with solutions
03
CONCEPT

Specific Heats of Gases

In one line
A gas has two main specific heats: at constant volume (Cv) and at constant pressure (Cp). Cp is larger because some heat goes into work.
MOLAR SPECIFIC HEATS

13.3.1 Molar specific heats

Cv = 1n(ΔQΔT)V  ·  Cp = 1n(ΔQΔT)P
  1. Specific heat per unit mass: c = C ÷ M.
  2. Constant volume: all heat raises U. Constant pressure: heat raises U and does work PΔV.
MAYER’S RELATION

13.3.2 Mayer’s relation

Cp − Cv = R
  1. Per unit mass: cp − cv = RM.
  2. So Cp > Cv always.
  3. Using cal: R ≈ 2 cal mol⁻¹ K⁻¹; then J = R (in J)R (in cal).
IN TERMS OF f

13.3.3 Specific heats in terms of f

Cv = f2R  ·  Cp = (f2 + 1)R
γ = CpCv = 1 + 2f
Cv = Rγ − 1  ·  Cp = γRγ − 1  ·  f = 2γ − 1
GasfCvCpγ
monoatomic332R52R53 = 1.67
diatomic (rigid)552R72R75 = 1.4
diatomic (vibrating)772R92R97 = 1.29
polyatomic (non-linear)63R4R43 = 1.33
  1. More degrees of freedom ⇒ Cv and Cp rise, γ falls towards 1.
  2. γ is always greater than 1.
  3. RCv = γ − 1 (asked often).
MIXTURE OF GASES

13.3.4 Specific heat of a mixture

Cv,mix = n₁Cv1 + n₂Cv2n₁ + n₂  ·  Cp,mix = Cv,mix + R
γmix = Cp,mixCv,mix  ·  n₁ + n₂γmix − 1 = n₁γ₁ − 1 + n₂γ₂ − 1
  1. Never average γ directly; average Cv first.
HEAT CAPACITY OF A PROCESS

13.3.5 Heat capacity of a process

ProcessMolar heat capacity
isochoricCv
isobaricCp
isothermal (ΔT = 0)∞
adiabatic (ΔQ = 0)0
polytropic PVx = constCv + R1 − x
Practise PYQs on this topicSpecific Heats of Gases - Cp, Cv, γ & Mayer's Relation · 65 questions with solutions
04
CONCEPT

Heat, Work & First Law

In one line
Heat given to a gas is shared between raising its internal energy and doing work: ΔQ = ΔU + ΔW.
HEAT AND WORK

13.4.1 Heat and work

  1. Heat flows because of a temperature difference.
  2. Work done by a gas against a piston:
dW = P dV  ·  W = ∫V₁V₂ P dV
VPV₁V₂W = area
Work = area under the P–V curve
  1. Heat and work are path functions; U is a state function.
FIRST LAW

13.4.2 First law of thermodynamics

ΔQ = ΔU + ΔW
Quantity+−
ΔQheat given to the systemheat taken out
ΔWwork done by the gas (expansion)work done on the gas (compression)
ΔUtemperature risestemperature falls
  1. All three in the same unit (J; 1 cal = 4.2 J).
  2. If W is the work done on the gas: ΔQ = ΔU − W.
  3. As rates: dQdt = dUdt + dWdt (power in, power out).
  4. Limitation: it does not tell the direction of heat flow (that is the second law).
CHANGE OF STATE

13.4.3 Change of state

ΔU = mL − PΔV
  1. Boiling: volume rises a lot ⇒ part of mL goes into work.
  2. Melting of ice: volume falls ⇒ work is done on the system by the atmosphere.
Practise PYQs on this topicHeat, Work & First Law of Thermodynamics · 24 questions with solutions
05
CONCEPT

Isobaric & Isochoric Processes

In one line
A thermodynamic process changes the state (P, V, T) of a gas. In an isobaric process P stays fixed; in an isochoric process V stays fixed.
TYPES OF PROCESSES

13.5.1 Types of processes

ProcessConstantKey result
isobaricPV ∝ T
isochoricVW = 0
isothermalTΔU = 0
adiabaticQ (no heat flow)ΔU = −W
cyclicreturns to startΔU = 0, Q = W
VPisobaricP constant: W = PΔVVPisochoricV constant: W = 0
Isobaric and isochoric lines on a P–V graph
ISOBARIC

13.5.2 Isobaric process

W = PΔV = nRΔT  ·  ΔU = nCvΔT  ·  Q = nCpΔT
ΔQ : ΔU : ΔW = Cp : Cv : R = γ : 1 : (γ − 1)
  1. Charles’s law holds: V ∝ T.
  2. Fraction of heat used as work = RCp = 1 − 1γ.
  3. Monoatomic: 40% work, 60% to U. Diatomic: 27 work, 57 to U.
  4. ΔU = PΔVγ − 1.
GasΔQ : ΔU : ΔW
monoatomic5 : 3 : 2
diatomic7 : 5 : 2
ISOCHORIC

13.5.3 Isochoric process

W = 0  ·  Q = ΔU = nCvΔT
  1. Gay-Lussac’s law holds: P ∝ T.
  2. All heat supplied raises the internal energy.
  3. On a P–V graph: a vertical line.
SAME HEAT, TWO CYLINDERS

13.5.4 Same heat, two cylinders

ΔTP = ΔTVγ
  1. Free piston (constant P) heats up less, because part of the heat does work.
Practise PYQs on this topicThermodynamic Processes · 255 questions with solutions
06
CONCEPT

Isothermal & Adiabatic Processes

In one line
Isothermal: temperature constant, heat flows freely. Adiabatic: no heat flow, so the temperature changes.
ISOTHERMAL

13.6.1 Isothermal process

PV = constant  ·  ΔU = 0  ·  Q = W
W = nRT lnV₂V₁ = 2.303 nRT logV₂V₁ = nRT lnP₁P₂
VPT₁T₂T₃T₃ > T₂ > T₁
Isotherms: higher T lies farther from the axes
  1. Walls perfectly conducting; process very slow.
  2. Examples: melting of ice, boiling of water.
  3. Molar heat capacity is infinite; vrms does not change.
  4. Slope of P–V curve = −PV. Isothermal bulk modulus = P.
ADIABATIC

13.6.2 Adiabatic process

PVγ = const  ·  TVγ − 1 = const
TγPγ − 1 = const
W = nR(T₁ − T₂)γ − 1 = P₁V₁ − P₂V₂γ − 1  ·  ΔU = −W
  1. Sudden compression or expansion; bursting of a tyre; sound waves in air.
  2. Expansion cools the gas; compression heats it.
  3. P ∝ Tγ/(γ − 1): monoatomic 2.5, diatomic 3.5.
  4. Molar heat capacity is zero. Adiabatic bulk modulus = γP.
GasP ∝T ∝
monoatomic (γ = 53)V−53V−23
diatomic (γ = 75)V−75V−25
polyatomic (γ = 43)V−43V−13
COMPARISON

13.6.3 Isothermal vs adiabatic

VPisothermaladiabatic (steeper)
Through the same point the adiabatic curve is steeper
(slope)adiabatic = γ × (slope)isothermal
  1. Equal expansion: Wiso > Wadi, final Piso > Padi.
  2. Equal compression: Wadi > Wiso, final Padi > Piso.
  3. Expanded to 2V: PisoPadi = 2γ − 1.
Practise PYQs on this topicThermodynamic Processes · 255 questions with solutions
07
CONCEPT

Polytropic & Other Processes

In one line
Every process of the form PVx = constant is polytropic. Isobaric, isothermal, adiabatic and isochoric are its special cases.
POLYTROPIC PROCESS

13.7.1 Polytropic process

W = P₁V₁ − P₂V₂x − 1 = nR(T₁ − T₂)x − 1
C = Cv + R1 − x = Rγ − 1 − Rx − 1
xProcessC
0isobaricCp
1isothermal∞
γadiabatic0
∞isochoricCv
  1. C = 0 ⇒ x = γ (adiabatic).
  2. Monoatomic gas with PV³ = constant: C = 32R − R2 = R.
READING T FROM THE LAW

13.7.2 Reading T from the process law

  1. PV² = constant ⇒ T ∝ 1V: the gas cools on expansion.
  2. VP² = constant ⇒ P ∝ V−12 ⇒ T ∝ √V.
  3. P ∝ V (straight line through origin) ⇒ T ∝ V².
ADIABATIC EXPONENTS

13.7.3 Adiabatic exponents

RelationExponent
P ∝ Txγγ − 1
TVx = constγ − 1
P ∝ V−xγ
Practise PYQs on this topicThermodynamic Processes · 255 questions with solutions
08
CONCEPT

P-V Diagrams & Cyclic Processes

In one line
On a P–V diagram, the area under the curve is the work. Work depends on the path; internal energy does not.
WORK FROM A P-V GRAPH

13.8.1 Work from a P-V graph

  1. Expansion (V increases): W positive. Compression: W negative.
  2. Straight-line path: W = area of the trapezium.
trapezium: W = 12(P₁ + P₂)(V₂ − V₁)
VPABpath 2: more Wpath 1: less W
Same end points, different work
TWO PATHS, SAME END POINTS

13.8.2 Two paths, same end points

ΔU = Q₁ − W₁ = Q₂ − W₂
  1. Find ΔU from the path whose Q and W are known.
  2. Then Q or W on the other path follows.
  3. Change in U from the end points: ΔU = f2(P₂V₂ − P₁V₁).
CYCLIC PROCESS

13.8.3 Cyclic process

ΔU = 0  ·  Qnet = Wnet = area enclosed
VPclockwise: W > 0VPanticlockwise: W < 0
Clockwise cycle: positive work; anticlockwise: negative
  1. Clockwise on P–V: W positive (engine). Anticlockwise: W negative (refrigerator).
  2. Rectangle: W = ΔP × ΔV; circle: W = πrPrV.
  3. Same cycle on a V–P graph (axes swapped): the sign is reversed.
FREE EXPANSION

13.8.4 Free expansion

  1. Sudden and uncontrolled; intermediate states are not equilibrium states, so it cannot be drawn on a P–V diagram.
  2. Ideal gas: T does not change.
GRAPHS OF THE FOUR PROCESSES

13.8.5 Graphs of the four processes

VPP–VTPP–TTVV–Tisobaricisothermaladiabaticisochoric
Same four processes on three kinds of graph
ProcessP–VP–TV–T
isobarichorizontalhorizontalline through origin
isochoricverticalline through originhorizontal
isothermalhyperbolaverticalvertical
adiabaticsteeper hyperbolaP ∝ Tγ/(γ−1)V ∝ T−1γ−1
Practise PYQs on this topicP-V Diagrams & Cyclic Processes · 92 questions with solutions
09
CONCEPT

Heat Engines, Second Law & Refrigerators

In one line
A heat engine runs in a cycle: it takes heat Q₁ from a hot source, turns part of it into work and rejects Q₂ to a cold sink. No engine can turn all heat into work.
HEAT ENGINE

13.9.1 Heat engine

Source T₁Sink T₂Engine(cycle)Q₁Q₂W = Q₁ − Q₂
Heat engine
W = Q₁ − Q₂  ·  η = WQ₁ = 1 − Q₂Q₁
  1. Working substance: steam, petrol vapour, an ideal gas.
  2. Real engines: steam ~ 8–15%, petrol ~ 40%, diesel ~ 50–55%.
SECOND LAW

13.9.2 Second law of thermodynamics

  1. Kelvin–Planck: no engine working in a cycle can convert all the heat taken from a source into work. So η < 1.
  2. Clausius: heat cannot flow from a colder body to a hotter body by itself, without external work.
CARNOT ENGINE

13.9.3 Carnot engine

VPABCDT₁T₂
Carnot cycle: two isotherms, two adiabats
  1. A → B isothermal expansion at T₁ (heat Q₁ in).
  2. B → C adiabatic expansion (T falls to T₂).
  3. C → D isothermal compression at T₂ (heat Q₂ out).
  4. D → A adiabatic compression (back to T₁).
Q₂Q₁ = T₂T₁  ·  η = 1 − T₂T₁
  1. Use kelvin. η depends only on T₁ and T₂, not on the working substance.
  2. η = 1 only if T₂ = 0 K (impossible).
  3. Carnot theorem: no engine between the same two temperatures beats a Carnot engine.
  4. Sink lowered by ΔT at fixed T₁: Δη = ΔTT₁.
REFRIGERATOR

13.9.4 Refrigerator (heat pump)

Source T₁Sink T₂Fridge(cycle)Q₁ = Q₂ + WQ₂W in
Refrigerator
β = Q₂W = Q₂Q₁ − Q₂ = T₂T₁ − T₂
β = 1 − ηη  ·  η = 11 + β
  1. T₂ = inside (cold), T₁ = room (hot).
  2. β can be greater than 1. β = 0 when T₂ = 0 K.
  3. Heat released to the room Q₁ = Q₂ + W; Q₂ = βQ₁1 + β.
  4. Power needed = Q₂ per second ÷ β.
Practise PYQs on this topicHeat Engines, Refrigerators & Second Law · 95 questions with solutions
EXAM-DAY CARD

Just see this before the exam

Thermodynamics
PV = nRT
gas law
U = (f2)nRT
internal energy
Cp − Cv = R
Mayer
ΔQ = ΔU + ΔW
first law
PVγ = const
adiabatic
η = 1 − T₂T₁
Carnot
FORMULA SHEET

Whole chapter on one page

Gas laws

PV = nRT, PV = NkBT

ρ = PMRT

P₁V₁T₁ = P₂V₂T₂

P = P₁ + P₂ + …

Internal energy

f = 3A − B

U = (f2)nRT

ΔU = nCvΔT

stopped: ΔT = Mv²fR

Specific heats

Cp − Cv = R

Cv = Rγ − 1

γ = 1 + 2f

C = Cv + R1 − x

First law

ΔQ = ΔU + ΔW

W = ∫P dV = area

isobaric: W = nRΔT

isochoric: W = 0

Iso / adiabatic

Wiso = nRT ln(V₂V₁)

PVγ, TVγ−1 = const

Wadi = nR(T₁ − T₂)γ − 1

slope ratio = γ

Engines

η = 1 − Q₂Q₁ = 1 − T₂T₁

β = T₂T₁ − T₂

β = (1 − η)/η

cycle: Q = W, ΔU = 0

TOP MISTAKES

Avoid these = easy marks

MISTAKE ✗

Using °C in PV = nRT or η = 1 − T₂T₁

Averaging γ of a mixture directly

Isothermal: thinking Q = 0

Cycle sign: ignoring the direction

CORRECT ✓

Always convert to kelvin

Average Cv by moles, then γ

Isothermal: ΔU = 0, Q = W

Clockwise on P–V: W > 0