Intermolecular forces and states of matter
Link to Std 9–10 : In Std 9–10 you learnt solid, liquid and gas from particle spacing; here we see the kind and strength of attraction between particles.
Umbrellas packed together are hard to separate; the stronger the attraction between particles the firmer the substance (higher boiling point).
Intermolecular force: attraction between molecules. Types: London (dispersion) force (everywhere), dipole–dipole (polar molecules), hydrogen bond (H on F, O or N) and ion–dipole (ion + polar molecule).
In the figure : The three main forces and their strength.
Rule 1: London force — The electron cloud shifts for an instant ⇒ temporary dipole ⇒ induced dipole in the neighbour. More electrons / bigger size ⇒ stronger force.
- Easy : Boiling points: He 4 K, Ne 27 K, Ar 87 K, Kr 120 K — rising with size.
- Medium : n-pentane (309 K) boils higher than neopentane (283 K); the long chain has more contact area.
- Exam-type : CH₄ is a gas (112 K) while C₈H₁₈ is a liquid; more electrons.
Rule 2: Dipole–dipole force — The δ+ end of one polar molecule attracts the δ− end of the next. Stronger than in a non-polar molecule of similar size.
- Easy : HCl (188 K) boils higher than Ar (87 K) of similar size.
- Medium : CH₃Cl is polar so it boils higher than CH₄.
- Exam-type : Propanone (329 K) boils higher than butane (273 K).
Rule 3: Hydrogen bond — H on F, O or N is pulled towards the lone pair of a neighbouring F/O/N. The strongest dipole-type force (inter- or intramolecular).
- Easy : H₂O (373 K) vs H₂S (213 K): H-bonding keeps water liquid.
- Medium : Ice floats; the open hexagonal H-bonded lattice has lower density.
- Exam-type : Ethanol (351 K) boils higher than dimethyl ether (249 K).
Method to rank forces (step-by-step)
- Step 1: Are ions present? If so ion–ion / ion–dipole is strongest.
- Step 2: Is H bonded to F/O/N? If so, hydrogen bond.
- Step 3: Is the molecule polar? If so dipole–dipole.
- Step 4: Otherwise London force; among similar types the larger molecule boils higher.
CET level (MCQ)
- CET 1) Which liquid shows H-bonding? 1) CH₃Cl 2) C₂H₅OH 3) CH₄ 4) CCl₄ — Answer: 2). (Time saver: look for O–H, N–H or F–H.)
- CET 2) Highest boiling point? 1) He 2) Ne 3) Ar 4) Kr — Answer: 4). (Bigger size = stronger London force.)
Real-life use: Water droplets on a cold bottle hold together through H-bonds; a gecko climbs walls using London forces.
Strength: ion–ion > ion–dipole > H-bond > dipole–dipole > London; H-bond needs H on F/O/N only.
Confusing intermolecular forces with covalent bonds; covalent bonds hold atoms inside a molecule.
HCl has no H-bond; an H on carbon (CH₄, CHCl₃) does not form H-bonds.
Memory clue: "H on FON = hydrogen bond".
Spot the difference
| Force | Where | Strength |
|---|---|---|
| London | All molecules | Weakest |
| Dipole–dipole | Polar | Medium |
| H-bond | H–F/O/N | Strong |
| Ion–dipole | NaCl in water | Strongest (between species) |
Practice questions
- 1In which molecules is the London force present?
- 2Which boils higher, He or Ar?
- 3State the condition for H-bonding.
- 4Why does n-pentane boil higher than neopentane?
- 5Write the forces in order of strength.
- 6Why is HF's boiling point higher than HCl's?
- 7Order of boiling points of Ar, Kr and Xe with reason.
- 8Why does ice float on water?
Show answers (try them yourself first)
- 1All molecules (non-polar and polar).
- 2Ar (larger size).
- 3H must be attached to F, O or N.
- 4The longer chain has more contact area ⇒ stronger London force.
- 5ion–ion > ion–dipole > H-bond > dipole–dipole > London.
- 6HF has H-bonds, HCl does not.
- 7Ar < Kr < Xe; electrons and size increase.
- 8The open H-bonded lattice makes ice less dense.
Gas laws: Boyle, Charles, Gay-Lussac
Pressing a cycle pump compresses the air and raises pressure; a balloon swells when warmed in the sun.
A gas has four variables: pressure P, volume V, temperature T (kelvin) and moles n. Boyle: constant T ⇒ P ∝ 1/V. Charles: constant P ⇒ V ∝ T. Gay-Lussac: constant V ⇒ P ∝ T.
In the figure : Boyle's hyperbola and Charles's straight line (V = 0 at 0 K).
Gas laws: Boyle, Charles, Gay-Lussac
In the app you can move this figure with your finger.
Open in the appRule 1: Boyle's law — P₁V₁ = P₂V₂ (n, T constant).
- Easy : 2 L gas at 1 atm; at 0.5 atm V = 1 × 2 ÷ 0.5 = 4 L.
- Medium : 5 L cylinder at 100 atm released to 1 atm: V = 100 × 5 ÷ 1 = 500 L.
- Exam-type : 3 L at 2 atm ⇒ at 6 atm V = 2 × 3 ÷ 6 = 1 L.
Rule 2: Charles's law — V₁ ÷ T₁ = V₂ ÷ T₂ (T in kelvin; T(K) = t°C + 273).
- Easy : 6 L at 300 K ⇒ at 450 K V = 6 × 450 ÷ 300 = 9 L.
- Medium : 250 mL at 27°C ⇒ at 327°C: 250 × 600 ÷ 300 = 500 mL (double).
- Exam-type : To double V, double T (in kelvin).
Rule 3: Gay-Lussac's law — P₁ ÷ T₁ = P₂ ÷ T₂ (V, n constant).
- Easy : 2 atm at 300 K ⇒ at 400 K P = 2 × 400 ÷ 300 = 2.67 atm.
- Medium : 1 atm at 250 K ⇒ 2 atm at 500 K.
- Exam-type : A closed tyre heated in the sun gains pressure.
Derivation: combined gas equation
- Step 1: (P₁, V₁, T₁) ⇒ change pressure to P₂ at T₁ (Boyle): V′ = P₁V₁ ÷ P₂.
- Step 2: At P₂ change T₁ → T₂ (Charles): V₂ = V′ × T₂ ÷ T₁.
- Step 3: Rearranging: P₁V₁ ÷ T₁ = P₂V₂ ÷ T₂.
Formulas, units and dimensional formulae
| Quantity | Unit | Conversion |
|---|---|---|
| P | atm, Pa, bar, mmHg | 1 atm = 101325 Pa = 760 mmHg = 1.013 bar |
| V | L, m³, mL | 1 m³ = 1000 L; 1 L = 1000 mL |
| T | K | T(K) = t°C + 273 |
CET level (MCQ)
- CET 1) 500 mL of gas at 27°C is heated to 127°C at constant pressure. New V? 1) 400 2) 500 3) 667 4) 750 mL — Answer: 3). (500 × 400 ÷ 300 = 666.7; use kelvin!)
- CET 2) 2 L at 1 atm, 300 K ⇒ 4 atm, 600 K. New V? 1) 1 L 2) 2 L 3) 4 L 4) 0.5 L — Answer: 1). (Pressure ×4 but T ×2 ⇒ V ÷2.)
Real-life use: Tyres are under-inflated slightly in summer; divers surface slowly because the gas in their lungs expands.
Always use kelvin for T; Boyle = hyperbola, Charles = straight line.
Putting T in Celsius; this makes the answer wrong.
CET combines changes in P and T — use the combined equation; do not mix mmHg and atm.
Memory clue: "Boyle = Burden (P↑ V↓), Charles = Cook (T↑ V↑)".
Spot the difference
| Law | Constant | Relation |
|---|---|---|
| Boyle | n, T | P ∝ 1/V |
| Charles | n, P | V ∝ T |
| Gay-Lussac | n, V | P ∝ T |
Practice questions
- 1A gas of 3 L at 2 atm: volume at 6 atm?
- 24 L at 200 K ⇒ V at 300 K?
- 31 atm at 250 K ⇒ P at 500 K?
- 410 L, 2 atm, 300 K ⇒ V at 4 atm and 600 K?
- 5How many mmHg is 1.5 atm?
- 6Volume of 3 L at 27°C, 760 mmHg at STP?
- 7To double V at constant P, to what °C must a gas at 27°C be heated?
- 8A 5 L cylinder at 100 atm: what volume at 1 atm?
Show answers (try them yourself first)
- 1V = 2 × 3 ÷ 6 = 1 L.
- 2V = 4 × 300 ÷ 200 = 6 L.
- 3P = 1 × 500 ÷ 250 = 2 atm.
- 4V = 2 × 10 × 600 ÷ (300 × 4) = 10 L.
- 51.5 × 760 = 1140 mmHg.
- 6V = 3 × 273 ÷ 300 = 2.73 L.
- 7T = 600 K = 327°C.
- 8V = 100 × 5 ÷ 1 = 500 L.
The ideal gas equation PV = nRT
While filling a balloon, the amount (n), size (V), heat (T) and pressure (P) all depend on one another.
An ideal gas obeys Boyle, Charles and Avogadro exactly. PV = nRT (R = universal gas constant).
In the figure : Three laws combine into PV = nRT.
The ideal gas equation PV = nRT
In the app you can move this figure with your finger.
Open in the appRule 1: Using PV = nRT — P in atm, V in L, T in K ⇒ R = 0.0821; in SI (P in Pa, V in m³) R = 8.314 J K⁻¹ mol⁻¹.
- Easy : 2 mol, 300 K, 5 L: P = 2 × 0.0821 × 300 ÷ 5 = 9.85 atm.
- Medium : 8 g O₂ (0.25 mol), 4 L, 27°C: P = 0.25 × 0.0821 × 300 ÷ 4 = 1.54 atm.
- Exam-type : 4 g H₂ (2 mol), 2 atm, 300 K: V = 2 × 0.0821 × 300 ÷ 2 = 24.6 L.
Rule 2: Molar mass and density — M = dRT ÷ P (d = density in g/L).
- Easy : d = 1.25 g/L, 1 atm, 273 K: M = 1.25 × 0.0821 × 273 ÷ 1 = 28 g/mol (N₂).
- Medium : d = 2.5 g/L, 2 atm, 300 K: M = 2.5 × 0.0821 × 300 ÷ 2 = 30.8.
- Exam-type : CO₂ density at STP = 44 ÷ 22.4 = 1.96 g/L.
Rule 3: Molar volume at STP — 1 mol of gas at STP (1 atm, 273 K) is 22.4 L; hence R = 22.4 ÷ 273.
- Easy : 11.2 L of gas at STP = 0.5 mol.
- Medium : 5.6 L O₂ at STP = 0.25 mol = 8 g.
- Exam-type : 1 L at 2 atm, 300 K becomes 2 × 1 × 273 ÷ 300 = 1.82 L at STP.
Derivation: value of R and M = dRT/P
- Step 1: At STP n = 1, P = 1 atm, V = 22.4 L, T = 273 K ⇒ R = PV ÷ nT = 22.4 ÷ 273 = 0.0821 L atm K⁻¹ mol⁻¹.
- Step 2: n = w ÷ M ⇒ PV = (w ÷ M) RT.
- Step 3: d = w ÷ V so P = dRT ÷ M ⇒ M = dRT ÷ P.
Formulas, units and dimensional formulae
| Quantity | Unit (atm system) | SI unit |
|---|---|---|
| P | atm | Pa |
| V | L | m³ |
| n | mol | mol |
| R | 0.0821 L atm K⁻¹ mol⁻¹ | 8.314 J K⁻¹ mol⁻¹ |
| T | K | K |
CET level (MCQ)
- CET 1) 0.5 mol gas at 300 K in 10 L. Pressure? 1) 1.23 2) 2.46 3) 0.62 4) 4.93 atm — Answer: 1). (0.5 × 0.0821 × 300 ÷ 10 = 1.23.)
- CET 2) A gas has density 1.25 g/L at 1 atm, 273 K; M? 1) 14 2) 28 3) 32 4) 44 — Answer: 2). (At STP M = d × 22.4 = 28.)
Real-life use: Finding the moles in an LPG cylinder or how long an oxygen cylinder will last — all use PV = nRT.
R = 0.0821 (atm, L) or 8.314 (SI); T in kelvin; 22.4 L at STP.
Mixing the units of R (L atm and Pa m³).
Do not use 22.4 blindly on seeing 'STP' unless P and T really are 1 atm and 273 K; otherwise use PV = nRT.
Memory clue: "Pivot = n-R-T" — say 'PV equals nRT' like a rhythm.
Spot the difference
| Item | Ideal gas | Real gas |
|---|---|---|
| PV = nRT | Always | At low P, high T |
| Particle volume | Zero | Not zero |
| Attraction | None | Present |
Practice questions
- 1Write one value of R.
- 2How many moles in 11.2 L of gas at STP?
- 3What mass is 5.6 L of O₂ at STP?
- 4Pressure of 0.5 mol at 300 K in 10 L?
- 5Density of CO₂ at STP?
- 6M for d = 2.5 g/L at 2 atm and 300 K?
- 7Volume of 4 g H₂ at 27°C and 2 atm?
- 8How many moles in a 20 L cylinder at 300 K and 10 atm?
Show answers (try them yourself first)
- 10.0821 L atm K⁻¹ mol⁻¹ or 8.314 J K⁻¹ mol⁻¹.
- 211.2 ÷ 22.4 = 0.5 mol.
- 30.25 mol × 32 = 8 g.
- 40.5 × 0.0821 × 300 ÷ 10 = 1.23 atm.
- 544 ÷ 22.4 = 1.96 g/L.
- 6M = 2.5 × 0.0821 × 300 ÷ 2 = 30.8.
- 7n = 2 mol; V = 2 × 0.0821 × 300 ÷ 2 = 24.6 L.
- 8n = 10 × 20 ÷ (0.0821 × 300) = 8.12 mol.
Dalton's law of partial pressures
In a noisy class the total noise is the sum of each speaker's; the pressure of a gas mixture is the sum of each gas's pressure.
The partial pressure is the pressure one gas would exert alone in the same V and T. P_total = p₁ + p₂ + … (non-reacting gases).
In the figure : 2 atm + 3 atm = 5 atm; each gas behaves independently.
Rule 1: Sum of partial pressures — P_total = p_A + p_B + …
- Easy : p_A = 2 atm, p_B = 3 atm ⇒ P = 5 atm.
- Medium : 0.5 mol H₂ + 1.5 mol He, 10 L, 300 K: P = 2 × 0.0821 × 300 ÷ 10 = 4.93 atm.
- Exam-type : In air N₂ is 0.78 atm and O₂ 0.21 atm (at 1 atm).
Rule 2: Mole fraction and partial pressure — p_A = x_A × P_total; x_A = n_A ÷ n_total.
- Easy : 2 mol N₂ + 3 mol O₂, P = 5 atm: p_N₂ = 2/5 × 5 = 2 atm.
- Medium : 4 g H₂ (2 mol) + 32 g O₂ (1 mol), P = 5 atm: p_H₂ = 2/3 × 5 = 3.33 atm.
- Exam-type : x_A + x_B = 1 always.
Rule 3: Gas collected over water — P_dry gas = P_atm − water vapour pressure (aqueous tension).
- Easy : 760 mmHg at 25°C (aqueous tension 23.8) ⇒ P_dry = 736.2 mmHg.
- Medium : 750 mmHg, aqueous tension 24 ⇒ 726 mmHg.
- Exam-type : 100 mL moist O₂ (25°C, 760) ⇒ dry at STP: 100 × 736.2 × 273 ÷ (760 × 298) = 88.7 mL.
Derivation: p_A = x_A P
- Step 1: p_A V = n_A RT and P V = n RT.
- Step 2: Divide: p_A ÷ P = n_A ÷ n = x_A.
- Step 3: Hence p_A = x_A P.
CET level (MCQ)
- CET 1) 2 mol N₂ and 3 mol O₂ at P = 5 atm. p_O₂? 1) 2 2) 3 3) 2.5 4) 1.5 atm — Answer: 2). (3/5 × 5 = 3; use the mole fraction directly.)
- CET 2) Atmospheric pressure 760 mmHg, aqueous tension 24 mmHg. Pressure of dry gas? 1) 784 2) 736 3) 760 4) 24 — Answer: 2).
Real-life use: Scuba mixes of O₂ and He are set by partial pressures; the same correction is used when collecting gases over water in the lab.
p_A = x_A × P; mole fractions add to 1; subtract aqueous tension when a gas is collected over water.
Using mass fraction instead of mole fraction; always convert to moles.
Dalton's law is only for non-reacting gases; NH₃ + HCl is different.
Memory clue: "Partial pressure = mole share × total pressure" (a slice of the pie).
Spot the difference
| Quantity | Formula |
|---|---|
| Partial pressure | p_A = x_A P |
| Mole fraction | x_A = n_A ÷ n |
| Dry gas | P − जलताण / P − aq. tension |
Practice questions
- 1p_A = 2 atm, p_B = 3 atm; P_total?
- 2x_N₂ in 2 mol N₂ + 3 mol O₂?
- 3What correction applies when a gas is collected over water?
- 40.5 mol H₂ + 1.5 mol He in 10 L at 300 K: p_H₂?
- 5750 mmHg, aqueous tension 24 ⇒ dry pressure?
- 64 g H₂ + 32 g O₂ at P = 5 atm: p_H₂ and p_O₂.
- 7100 mL moist O₂ at 25°C, 760 mmHg ⇒ dry volume at STP.
- 8If x(N₂) in air is 0.78, find p_N₂ at 1 atm.
Show answers (try them yourself first)
- 15 atm.
- 22/5 = 0.4.
- 3Subtract aqueous tension.
- 4P = 4.93 atm; p_H₂ = 0.5/2 × 4.93 = 1.23 atm.
- 5750 − 24 = 726 mmHg.
- 6n = 2 : 1; p_H₂ = 3.33 atm, p_O₂ = 1.67 atm.
- 788.7 mL.
- 80.78 atm.
Kinetic theory of gases and real gases
A fragrance slowly spreads across a room — particles move constantly and randomly.
Kinetic theory: gas particles are tiny, in constant random motion, with no mutual attraction and elastic collisions; mean kinetic energy ∝ T. A real gas deviates from ideal at low T / high P.
In the figure : Maxwell distribution: the most probable speed rises with T.
In the figure : Z = PV ÷ nRT: Z = 1 for an ideal gas.
Rule 1: Types of speed — u_rms = √(3RT ÷ M); u_av = √(8RT ÷ πM); u_mp = √(2RT ÷ M). Ratio u_mp : u_av : u_rms = 1 : 1.128 : 1.224. (M in kg/mol)
- Easy : N₂ at 300 K: u_rms = √(3 × 8.314 × 300 ÷ 0.028) ≈ 517 m/s.
- Medium : Same gas: u_av ≈ 476, u_mp ≈ 422 m/s.
- Exam-type : If T becomes four times, u_rms doubles.
Rule 2: Graham's law of diffusion — r₁ ÷ r₂ = √(M₂ ÷ M₁) = t₂ ÷ t₁ (same conditions). Lighter gas is faster.
- Easy : H₂ vs O₂: √(32 ÷ 2) = 4 times faster.
- Medium : A gas takes 40 s and O₂ takes 20 s ⇒ M = 32 × (40÷20)² = 128.
- Exam-type : NH₃ (17) is faster than HCl (36.5).
Rule 3: Real gases: van der Waals — (P + an²/V²)(V − nb) = nRT; a = attraction, b = particle volume. Z < 1 attraction dominates; Z > 1 repulsion dominates.
- Easy : CO₂ (a = 3.59, b = 0.0427), 1 mol, 5 L, 300 K: P = 4.82 atm (ideal 4.93).
- Medium : H₂: small a ⇒ Z > 1 even at modest T.
- Exam-type : Very high T, low P ⇒ real gas approaches ideal.
Derivation: van der Waals corrections
- Step 1: Particles have their own volume ⇒ free volume = V − nb.
- Step 2: Attraction lowers the wall pressure ⇒ P_ideal = P + an²/V².
- Step 3: Put into the ideal equation: (P + an²/V²)(V − nb) = nRT.
CET level (MCQ)
- CET 1) Which gas diffuses fastest? 1) O₂ 2) N₂ 3) H₂ 4) CO₂ — Answer: 3). (Smallest M.)
- CET 2) To double u_rms, T must be? 1) doubled 2) quadrupled 3) halved 4) ×8 — Answer: 2). (u ∝ √T.)
Real-life use: Smells spreading; helium balloons deflating quickly (He diffuses fast); separating uranium isotopes by diffusion.
KE_mean ∝ T; u ∝ √(T/M); Z < 1 attraction; Z > 1 repulsion; larger a ⇒ easier to liquefy.
Putting M in grams in u_rms; use kg/mol.
All gases have the same mean KE at the same T, but different speeds (depends on M).
Memory clue: "1 : 1.128 : 1.224 — mp < av < rms in increasing order".
Spot the difference
| Item | Ideal | Real |
|---|---|---|
| Z | 1 | ≠ 1 |
| Attraction | None | Present |
| Equation | PV = nRT | van der Waals |
Practice questions
- 1State two postulates of the kinetic theory.
- 2Write the formula for u_rms.
- 3What is Z?
- 4Find u_rms of N₂ at 300 K.
- 5Ratio of diffusion rates of H₂ and O₂?
- 6When is the deviation from ideality greater?
- 7A gas takes 40 s, O₂ takes 20 s; find M.
- 8Find the pressure of CO₂ by van der Waals (1 mol, 5 L, 300 K).
Show answers (try them yourself first)
- 1Particles move randomly; no mutual attraction.
- 2u_rms = √(3RT ÷ M).
- 3Z = PV ÷ nRT.
- 4≈ 517 m/s.
- 5√(32÷2) = 4 : 1.
- 6At low temperature and high pressure.
- 7M = 32 × 4 = 128.
- 8P = 0.0821 × 300 ÷ (5 − 0.0427) − 3.59 ÷ 25 ≈ 4.82 atm.
Liquefaction of gases and critical constants
Droplets form on a cold glass — vapour cools into liquid.
Critical temperature T_c: above it a gas cannot be liquefied by pressure alone. Critical pressure P_c: the minimum pressure to liquefy at T_c. Critical volume V_c: volume of 1 mol at T_c and P_c.
In the figure : Andrews isotherms: flat part (liquid + gas) for T < T_c.
Rule 1: Andrews' experiments (CO₂) — CO₂ has T_c ≈ 304 K (31°C) and P_c ≈ 73 atm. Below T_c pressure liquefies it; above, it does not.
- Easy : CO₂ at 298 K can be liquefied by pressure.
- Medium : At 320 K no pressure liquefies it.
- Exam-type : At C the difference between liquid and gas vanishes.
Rule 2: Critical constants and a, b — T_c = 8a ÷ 27Rb; P_c = a ÷ 27b²; V_c = 3b.
- Easy : CO₂: a = 3.59, b = 0.0427 ⇒ T_c = 303 K, P_c = 72.9 atm, V_c = 0.128 L.
- Medium : NH₃: a = 4.17, b = 0.0371 ⇒ T_c ≈ 406 K, P_c ≈ 112 atm.
- Exam-type : Larger a ⇒ higher T_c ⇒ easier liquefaction.
Rule 3: Methods of liquefaction — Cool and compress; Joule–Thomson effect: a gas cools on expansion (Linde process).
- Easy : O₂ has T_c = 154.3 K; at room temperature (300 K) pressure alone cannot liquefy it.
- Medium : Water's T_c is 647 K, so it liquefies easily.
- Exam-type : LPG has a high T_c ⇒ liquid in a cylinder.
Derivation: V_c = 3b, T_c, P_c
- Step 1: For 1 mol, P = RT ÷ (V − b) − a ÷ V².
- Step 2: At the critical point the curve has an inflection: dP/dV = 0 ⇒ RT = 2a(V − b)² ÷ V³; d²P/dV² = 0 ⇒ RT = 3a(V − b)³ ÷ V⁴.
- Step 3: Equate: 2V = 3(V − b) ⇒ V_c = 3b.
- Step 4: Substituting back gives T_c = 8a ÷ 27Rb and P_c = a ÷ 27b².
Formulas, units and dimensional formulae
| Quantity | Formula | Unit |
|---|---|---|
| T_c | 8a ÷ 27Rb | K |
| P_c | a ÷ 27b² | atm |
| V_c | 3b | L mol⁻¹ |
| a | आकर्षण / attraction | L² atm mol⁻² |
| b | आकारमान / volume | L mol⁻¹ |
CET level (MCQ)
- CET 1) V_c = ? 1) b 2) 2b 3) 3b 4) 8b — Answer: 3).
- CET 2) Which gas has the highest T_c? (a: He 0.034, H₂ 0.244, CO₂ 3.59, NH₃ 4.17) — Answer: NH₃. (larger a ⇒ higher T_c.)
Real-life use: Storage of LPG, liquid CO₂ (fire extinguishers) and liquid O₂/N₂ depends on knowing T_c and pressure.
T_c = 8a/27Rb; P_c = a/27b²; V_c = 3b; above T_c no pressure liquefies.
Believing liquefaction happens by pressure alone above T_c.
CET asks the units of a and b; remember b = 4 × the volume of the molecules.
Memory clue: "V three b (3b), T eight a over 27 R b".
Spot the difference
| Item | T < T_c | T > T_c |
|---|---|---|
| Liquefaction | Possible | Impossible |
| Isotherm | Flat part | Smooth |
Practice questions
- 1Define T_c.
- 2What is T_c of CO₂?
- 3V_c = ?
- 4Find T_c from a = 3.59 and b = 0.0427.
- 5Find P_c from the same a, b.
- 6Why can O₂ not be liquefied at room temperature by pressure?
- 7T_c of NH₃ from a = 4.17 and b = 0.0371.
- 8Briefly derive V_c = 3b.
Show answers (try them yourself first)
- 1Above it a gas cannot be liquefied by pressure.
- 2≈ 304 K.
- 33b.
- 48 × 3.59 ÷ (27 × 0.0821 × 0.0427) ≈ 303 K.
- 53.59 ÷ (27 × 0.0427²) ≈ 72.9 atm.
- 6T_c = 154.3 K < 300 K.
- 7≈ 406 K.
- 8Equate dP/dV = 0 and d²P/dV² = 0 to get 2V = 3(V − b).
Liquid state: vapour pressure, surface tension and viscosity
After rain leaves hold round droplets; honey flows slowly and water quickly.
Vapour pressure: pressure of the vapour in equilibrium with its liquid. Boiling point: vapour pressure = external pressure. Surface tension γ: energy needed to increase surface area by one unit (N/m). Viscosity η: internal friction between layers (Pa s).
In the figure : Capillary rise and the vapour pressure–temperature curve.
Rule 1: Vapour pressure and boiling — Vapour pressure rises with T; a lower external pressure lowers the boiling point (mountains), a higher one raises it (pressure cooker).
- Easy : Water boils at 100°C at 1 atm.
- Medium : On a high mountain water boils below 100°C.
- Exam-type : Evaporation is at the surface; boiling occurs throughout.
Rule 2: Surface tension and capillarity — h = 2γ cosθ ÷ (ρ g r). Water rises (θ < 90°), mercury falls (θ > 90°). γ falls as T rises.
- Easy : Water γ = 0.072 N/m, r = 0.5 mm, θ = 0: h = 2 × 0.072 ÷ (1000 × 9.8 × 0.0005) = 2.94 cm.
- Medium : Half the radius (0.25 mm) ⇒ double h = 5.88 cm.
- Exam-type : Drops are spherical because the surface area is minimum.
Rule 3: Viscosity — In liquids viscosity falls as T rises (in gases it rises). Unit Pa s; 1 poise = 0.1 Pa s.
- Easy : Water at 20°C ≈ 1 mPa s (0.01 poise).
- Medium : Honey is far more viscous than water (H-bonds).
- Exam-type : Engine oil thins when hot.
Derivation: capillary rise h
- Step 1: Upward force from surface tension = γ cosθ × (2πr).
- Step 2: Weight of the column = π r² h ρ g.
- Step 3: Equate: h = 2γ cosθ ÷ (ρ g r).
Formulas, units and dimensional formulae
| Quantity | SI unit | Dimension |
|---|---|---|
| γ | N m⁻¹ | [M T⁻²] |
| η | Pa s | [M L⁻¹ T⁻¹] |
| P_v | Pa | [M L⁻¹ T⁻²] |
CET level (MCQ)
- CET 1) When T rises, the surface tension of a liquid? 1) increases 2) decreases 3) stays 4) doubles — Answer: 2).
- CET 2) If the capillary radius is halved the rise? 1) halves 2) doubles 3) ×4 4) same — Answer: 2). (h ∝ 1/r.)
Real-life use: Pressure cookers, ink soaking into blotting paper, water rising in plants, and soap lowering surface tension to clean.
Vapour pressure = external pressure ⇒ boiling; T↑ ⇒ P_v↑, γ↓, η(liquid)↓; h ∝ 1/r.
Writing that a liquid's viscosity rises with temperature.
Evaporation and boiling are different; mercury falls in a capillary because θ > 90°.
Memory clue: "Hot ⇒ slippery: γ and η fall".
Spot the difference
| Property | On heating |
|---|---|
| Vapour pressure | Rises |
| Surface tension | Falls |
| Viscosity (liquid) | Falls |
Practice questions
- 1What is boiling point?
- 2Unit of surface tension?
- 3SI unit of viscosity?
- 4Find the capillary rise of water for r = 0.5 mm.
- 5What is the rise for r = 0.25 mm?
- 6Why does mercury fall in a capillary?
- 7Why does food cook faster in a pressure cooker?
- 8How does soap change surface tension and why is it useful?
Show answers (try them yourself first)
- 1The temperature at which vapour pressure equals external pressure.
- 2N m⁻¹.
- 3Pa s.
- 4h = 2 × 0.072 ÷ (1000 × 9.8 × 0.0005) ≈ 2.94 cm.
- 5Double ≈ 5.88 cm.
- 6θ > 90°; mercury does not wet glass.
- 7Higher pressure ⇒ higher boiling point ⇒ higher temperature.
- 8Lowers γ; helps oil and dirt mix with water.
Quick revision of the whole lesson
| Concept | Key formula / fact |
|---|---|
| IMF order | ion–ion > ion–dipole > H-bond > dipole > London |
| Boyle / Charles | P₁V₁ = P₂V₂ ; V₁/T₁ = V₂/T₂ |
| Ideal gas | PV = nRT ; R = 0.0821 / 8.314 ; M = dRT/P |
| Dalton | P = Σp ; p_A = x_A P |
| Kinetic | u_rms = √(3RT/M); 1 : 1.128 : 1.224 |
| Graham | r₁/r₂ = √(M₂/M₁) |
| van der Waals | (P + an²/V²)(V − nb) = nRT |
| Critical | T_c = 8a/27Rb ; P_c = a/27b² ; V_c = 3b |
| Capillary | h = 2γcosθ/(ρgr) |
🚀 Quick revision of the whole lesson
In the app you can move this figure with your finger.
Open in the app🎯 Most important points for the exam
- Types of forces and their strength order.
- Three gas laws and the combined equation; T in kelvin.
- PV = nRT and M = dRT/P.
- Partial pressures and the aqueous-tension correction.
- u_rms, Graham's law, Z and van der Waals.
- Critical constants and their link with a and b.
- Vapour pressure, surface tension, viscosity and the effect of T.
understand the idea → remember the formula → solve the example → solve problems yourself.