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CBSE · Class 11 · Physics

Chapter 10: Thermal Properties of Matter

8 concepts · Free to read

Temperature, heat and temperature scales

From daily life

A cup of tea feels hotter than a glass of water at room temperature, and heat flows from the tea to the cup. Link to earlier classes : heat and temperature of class 7 and 9 are now defined more carefully.

Simple definition

Temperature is a measure of how hot or cold a body is. Heat is the energy that flows between two bodies because of a temperature difference; it flows from higher to lower temperature. Unit of heat : joule (J).

Rule 1: Temperature scales — F = (9 ÷ 5) C + 32 and K = C + 273.15 (C = degree Celsius, F = degree Fahrenheit, K = kelvin, the SI unit). The triple point of water is 273.16 K.

  • Easy : 37 °C = (9 ÷ 5) × 37 + 32 = 98.6 °F.
  • Medium : 50 °C = 122 °F = 323 K.
  • Exam : At −40 the Celsius and Fahrenheit readings are equal : C = (9 ÷ 5) C + 32 ⇒ C = −40.
Remember

Heat is energy in transit; temperature is a state; K = C + 273.

Common mistake

Calling temperature "the amount of heat in a body".

Shortcut

Memory clue : "Heat Hops, Temperature Tells."

Spot the difference

QuantityMeaningUnit
Heatenergy that flowsjoule
Temperaturedegree of hotnesskelvin

The ideal-gas equation

From daily life

A football pumped in the cold morning feels softer than in the afternoon sun. Link to earlier classes : Boyle's and Charles' laws of class 9 are now joined into one equation.

Simple definition

An ideal gas obeys one relation between pressure, volume and absolute temperature at all conditions : it is a good model for real gases at low pressure and high temperature.

Rule 1: Ideal-gas equation — P V = n R T (P = pressure, V = volume, n = number of moles, R = 8.314 J mol⁻¹ K⁻¹, T = temperature in kelvin). For a fixed amount of gas, P₁V₁ ÷ T₁ = P₂V₂ ÷ T₂.

  • Easy : 1 mol at 273.15 K and 1 atm occupies V = nRT ÷ P = 8.314 × 273.15 ÷ 101 325 = 0.0224 m³ = 22.4 litre.
  • Medium : 2 mol at 300 K in a 10 litre vessel gives P = 2 × 8.314 × 300 ÷ 0.010 = 4.99 × 10⁵ Pa.
  • Exam : A gas at 27 °C and 1 atm is compressed to half its volume while the temperature rises to 127 °C. P₂ = P₁ × (V₁ ÷ V₂) × (T₂ ÷ T₁) = 1 × 2 × 400 ÷ 300 = 2.67 atm.
Remember

Always use kelvin in the gas laws.

Common mistake

Putting Celsius temperature into P V = n R T.

Shortcut

Memory clue : "Please Visit New Restaurant Today : P V = n R T."

Spot the difference

LawConstantRelation
BoyleTP ∝ 1 ÷ V
CharlesPV ∝ T
Gay-LussacVP ∝ T

Thermal expansion

From daily life

Gaps are left between railway tracks, and a tight metal lid opens when held under hot water. Link to earlier classes : expansion on heating of class 7 is now measured.

Simple definition

Most solids, liquids and gases expand when heated. The coefficient of linear expansion α is the fractional change in length per kelvin.

Rule 1: Linear, area and volume expansion — ΔL = α L ΔT. The area coefficient is about 2α and the volume coefficient is γ = 3α.

  • Easy : A steel rod (α = 1.2 × 10⁻⁵ K⁻¹) of length 10 m heated by 30 K expands by 1.2 × 10⁻⁵ × 10 × 30 = 3.6 × 10⁻³ m = 3.6 mm.
  • Medium : Copper has α = 1.7 × 10⁻⁵ K⁻¹, so γ = 5.1 × 10⁻⁵ K⁻¹.
  • Exam : A steel rod fixed between two rigid walls is heated by 50 K. The thermal stress = Y α ΔT = 2 × 10¹¹ × 1.2 × 10⁻⁵ × 50 = 1.2 × 10⁸ Pa.

Rule 2: Anomalous expansion of water — Water contracts as it is heated from 0 °C to 4 °C, so its density is the highest at 4 °C. That is why a lake freezes from the top and fish survive underneath.

  • Easy : At 4 °C water has the smallest volume.
  • Medium : Ice floats because its density is lower than that of water.
  • Exam : A bimetallic strip bends on heating because the two metals have different α.
Remember

ΔL = αLΔT; γ = 3α; water is densest at 4 °C.

Common mistake

Using α for the volume instead of γ = 3α.

Shortcut

Memory clue : "Line α, Area 2α, Volume 3α : 1-2-3."

Spot the difference

CoefficientSymbolValue
Linearαα
Areaβ2α
Volumeγ3α

Specific heat capacity and calorimetry

From daily life

The sand of a beach becomes very hot while the sea water stays cool. Link to earlier classes : specific heat of class 9 is now used in mixing problems.

Simple definition

The specific heat capacity c of a substance is the heat needed to raise the temperature of 1 kg of it by 1 K. Calorimetry is measuring heat by mixing substances in an insulated container.

Rule 1: Heat and temperature change — Q = m c ΔT (Q = heat, m = mass, c = specific heat, ΔT = temperature change). For water c = 4186 J kg⁻¹ K⁻¹.

  • Easy : 2 kg of water heated from 20 °C to 70 °C needs Q = 2 × 4186 × 50 = 4.19 × 10⁵ J.
  • Medium : 0.5 kg of copper (c = 385) cooled from 100 °C to 20 °C gives out Q = 0.5 × 385 × 80 = 1.54 × 10⁴ J.
  • Exam : A 0.2 kg aluminium block (c = 900) at 100 °C is dropped into 0.5 kg of water at 20 °C. Heat lost = heat gained : 0.2 × 900 × (100 − T) = 0.5 × 4186 × (T − 20) ⇒ T = 26.3 °C.
Remember

Q = mcΔT; in an insulated mixture heat lost equals heat gained; water has a high specific heat.

Common mistake

Forgetting the mass or using the initial temperature instead of the change.

Shortcut

Memory clue : "Q = m c ΔT : Quantity of heat is Mass, Constant, Temperature-change."

Spot the difference

QuantityMeaningUnit
Heat capacityheat per kelvin for the whole bodyJ K⁻¹
Specific heatheat per kelvin per kgJ kg⁻¹ K⁻¹

Change of state and latent heat

From daily life

Ice at 0 °C cools a drink better than water at 0 °C because it takes in extra heat while melting. Link to earlier classes : melting and boiling of class 7 and 9 are now counted in joules.

Simple definition

Latent heat L is the heat needed to change the state of 1 kg of a substance at a constant temperature.

Rule 1: Latent heat — Q = m L. For ice, L_f = 3.34 × 10⁵ J kg⁻¹ (fusion); for water, L_v = 2.26 × 10⁶ J kg⁻¹ (vaporisation) at 100 °C. The temperature stays constant during the change.

  • Easy : Melting 0.5 kg of ice at 0 °C needs 0.5 × 3.34 × 10⁵ = 1.67 × 10⁵ J.
  • Medium : Condensing 0.1 kg of steam at 100 °C gives out 0.1 × 2.26 × 10⁶ = 2.26 × 10⁵ J.
  • Exam : To turn 1 kg of ice at −10 °C into steam at 100 °C : 1 × 2100 × 10 = 21 000 J (warm ice) + 3.34 × 10⁵ J (melt) + 1 × 4186 × 100 = 4.19 × 10⁵ J (warm water) + 2.26 × 10⁶ J (boil) = 3.03 × 10⁶ J.
Remember

Q = mL; no temperature change while the state changes; steam burns more than boiling water.

Common mistake

Using mcΔT during a change of state.

Shortcut

Memory clue : "Latent = Hidden : the heat goes into the bonds, not into the thermometer."

Spot the difference

ProcessHeat formulaTemperature
Warmingm c ΔTchanges
Melting / boilingm Lconstant

Heat transfer : conduction and convection

From daily life

A metal spoon in hot tea becomes hot, but a wooden spoon does not; a room heater warms the air near the ceiling first. Link to earlier classes : the three ways of heat transfer from class 7.

Simple definition

Conduction is the flow of heat through a material without any movement of the material itself. Convection is heat carried by the movement of a fluid.

Rule 1: Conduction — H = K A (T₁ − T₂) ÷ L (H = rate of heat flow, K = thermal conductivity, A = area, L = length or thickness, T₁ − T₂ = temperature difference).

  • Easy : A copper rod (K = 385 W m⁻¹ K⁻¹), A = 1 × 10⁻⁴ m², L = 0.5 m, ΔT = 100 K : H = 385 × 10⁻⁴ × 100 ÷ 0.5 = 7.7 W.
  • Medium : Doubling the length halves the heat flow (H ∝ 1 ÷ L).
  • Exam : A window pane (K = 1.0 W m⁻¹ K⁻¹), 2 m² and 5 mm thick, with a 10 K difference between faces, conducts H = 1.0 × 2 × 10 ÷ 0.005 = 4000 W.

Rule 2: Convection — A heated fluid expands, becomes lighter and rises, while the cooler denser fluid sinks. This sets up a convection current (sea breeze, land breeze, boiling water).

  • Easy : A heater is placed near the floor to warm the whole room.
  • Medium : Sea breeze blows in the day, as air over the land rises.
  • Exam : Convection cannot occur in a solid or in a vacuum.
Remember

H = KA ΔT ÷ L; metals have a large K; convection needs a fluid.

Common mistake

Mixing up K (conductivity) and k (spring constant or Boltzmann constant).

Shortcut

Memory clue : "Conduction : touch the hot end. Convection : the fluid carries it."

Spot the difference

ProcessMediumParticles move along?
Conductionsolids mostlyno
Convectionfluidsyes

Radiation, Stefan's law and Wien's law

From daily life

We feel the warmth of the Sun, though nothing material connects us to it. Link to earlier classes : radiation as the third way of heat transfer.

Simple definition

Thermal radiation is energy sent out as electromagnetic waves by every body above absolute zero; it needs no medium. A black body absorbs all radiation falling on it.

Rule 1: Stefan–Boltzmann law — P = σ A T⁴ for a black body (σ = 5.67 × 10⁻⁸ W m⁻² K⁻⁴). For a surface at T in surroundings at T₀ : P = σ A (T⁴ − T₀⁴).

  • Easy : A black body of A = 1 m² at 300 K radiates P = 5.67 × 10⁻⁸ × 300⁴ = 459 W.
  • Medium : Doubling the temperature increases the radiated power 16 times.
  • Exam : A 1 m² black body at 400 K in surroundings at 300 K loses a net P = 5.67 × 10⁻⁸ × (400⁴ − 300⁴) = 992 W.

Rule 2: Wien's displacement law — λ_m T = 2.9 × 10⁻³ m K (λ_m = wavelength of maximum emission). A hotter body radiates at a shorter wavelength.

  • Easy : For the Sun (T = 5800 K), λ_m = 2.9 × 10⁻³ ÷ 5800 = 5.0 × 10⁻⁷ m = 500 nm, in the visible range.
  • Medium : A body at 290 K peaks near 10 μm, in the infrared.
  • Exam : A star twice as hot peaks at half the wavelength.
Remember

P ∝ T⁴; λ_m ∝ 1 ÷ T; use kelvin.

Common mistake

Using °C in P = σAT⁴.

Shortcut

Memory clue : "Stefan = Fourth power; Wien = Why shorter when hotter."

Spot the difference

LawStatesDepends on
Stefanpower radiatedT⁴
Wienwavelength of the peak1 ÷ T

Newton's law of cooling

From daily life

A cup of tea cools quickly at first and slowly later. Link to earlier classes : cooling of a hot body in a cooler room.

Simple definition

Newton's law of cooling : the rate of loss of heat of a body is proportional to the difference between the temperature of the body and that of its surroundings (for a small difference).

Rule 1: Law of cooling — dT ÷ dt = −k (T − T₀), so T − T₀ = (T_i − T₀) e^(−kt).

  • Easy : A body cools from 80 °C to 50 °C in 5 min in a room at 20 °C ⇒ ln(60 ÷ 30) = k × 5 ⇒ k = 0.139 min⁻¹.
  • Medium : With the same k, cooling from 60 °C to 30 °C needs t = ln(40 ÷ 10) ÷ k = 1.386 ÷ 0.139 = 10 min.
  • Exam : A hotter body loses heat faster : the rate at 80 °C (60 K above the room) is twice the rate at 50 °C (30 K above).
Remember

Cooling rate ∝ (T − T₀); the graph of T against t is an exponential curve.

Common mistake

Taking the cooling rate to be constant.

Shortcut

Memory clue : "Hot cools fast, warm cools slow — rate follows the gap."

Spot the difference

TimeTemperature gapCooling rate
earlylargefast
latersmallslow