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Thermal Properties of Matter

NCERT Class 11 · Physics Based on NCERT Class 11 Physics textbook · Free CBSE study kit

Chapter Notes

TEMPERATURE AND HEAT

**Temperature** is a measure of the degree of hotness or coldness of a body. It is a relative measure and indicates the thermal state of matter. We perceive temperature through touch, but this sense is unreliable and limited in range for scientific purposes.

**Heat** is the form of energy transferred between two or more systems (or a system and its surroundings) by virtue of temperature difference. When a temperature difference exists, heat spontaneously flows from the higher temperature region to the lower temperature region until thermal equilibrium is established.

**Key Distinctions:**

  • Temperature is a property of a body (state function)
  • Heat is energy in transit between bodies (path function)
  • A hot cup of tea has high temperature; the tea loses heat to surroundings
  • An ice-cold glass of water has low temperature; it gains heat from surroundings
  • **SI Units:**

  • Heat energy: Joule (J)
  • Temperature: Kelvin (K) or degree Celsius (°C)
  • 1 calorie = 4.186 J (1 cal = heat required to raise 1 g water by 1°C)
  • **Real-Life Example:** A blacksmith heating an iron ring—the ring gains heat from the furnace, its temperature rises, allowing it to expand and fit on a wheel rim. Once removed, it loses heat to the environment and contracts.

    ---

    MEASUREMENT OF TEMPERATURE

    Temperature is measured using a **thermometer**, an instrument based on variation of physical properties with temperature.

    **Physical Property Used:** Volume change of liquids with temperature. Liquids like mercury and alcohol expand linearly with temperature over wide ranges, making them ideal thermometer liquids.

    **Thermometer Calibration:**

    Two fixed reference points standardize temperature scales:

  • **Ice point (freezing point of water):** 0°C = 32°F
  • **Steam point (boiling point of water):** 100°C = 212°F
  • These are measured under standard atmospheric pressure (1 atm = 101,325 Pa).

    **Temperature Scales:**

    **Celsius Scale:**

  • Ice point: 0°C
  • Steam point: 100°C
  • 100 equal intervals between fixed points
  • Also called centigrade scale
  • **Fahrenheit Scale:**

  • Ice point: 32°F
  • Steam point: 212°F
  • 180 equal intervals between fixed points
  • Primarily used in USA
  • **Conversion Formula:**

    The relationship between Celsius and Fahrenheit temperatures is linear (straight line):

    $$\frac{t_F - 32}{180} = \frac{t_C}{100}$$

    Or: **t_F = (9/5)t_C + 32**

    Or: **t_C = (5/9)(t_F - 32)**

    **Example:** Convert 25°C to Fahrenheit:

    t_F = (9/5) × 25 + 32 = 45 + 32 = 77°F

    **Worked Problem:** If water boils at 212°F, what is this in Celsius?

    t_C = (5/9)(212 - 32) = (5/9) × 180 = 100°C ✓

    ---

    IDEAL-GAS EQUATION AND ABSOLUTE TEMPERATURE

    **Boyle's Law (constant temperature):**

    For a fixed mass of gas at constant temperature:

    $$PV = \text{constant}$$

    Or: **P₁V₁ = P₂V₂** (at constant T)

    Pressure and volume are inversely proportional.

    **Charles' Law (constant pressure):**

    For a fixed mass of gas at constant pressure:

    $$\frac{V}{T} = \text{constant}$$

    Or: **V₁/T₁ = V₂/T₂** (at constant P)

    Volume and absolute temperature are directly proportional.

    **Combined Gas Law:**

    For a fixed mass of gas:

    $$\frac{PV}{T} = \text{constant}$$

    **Ideal Gas Equation (General Form):**

    For any quantity of any gas at low density:

    $$PV = \mu RT$$

    Where:

  • **P** = pressure (Pa)
  • **V** = volume (m³)
  • **μ** = number of moles (mol)
  • **R** = universal gas constant = **8.31 J mol⁻¹ K⁻¹**
  • **T** = absolute temperature (K)
  • **Absolute Zero and Kelvin Scale:**

    Extrapolating pressure-temperature graphs for low-density gases shows that pressure approaches zero at **T = -273.15°C**. This is **absolute zero**, the theoretical lowest possible temperature where all molecular motion ceases (in classical sense). No substance can be cooled below absolute zero.

    **Kelvin (Absolute) Temperature Scale:**

  • Zero point: 0 K = -273.15°C
  • Founded on absolute zero as reference
  • Same interval size as Celsius scale
  • Used in all scientific calculations
  • **Temperature Conversion:**

    $$T(K) = t(°C) + 273.15$$

    For most calculations, use: **T(K) = t(°C) + 273**

    **SI unit of temperature is Kelvin (K).**

    **Relationship between scales:**

  • 0°C = 273.15 K (approximately 273 K)
  • 100°C = 373.15 K
  • Absolute zero = 0 K = -273.15°C
  • **Example:** Room temperature at 25°C in Kelvin:

    T = 25 + 273 = 298 K

    **Gas Thermometer Principle:**

    A constant-volume gas thermometer uses P ∝ T relationship. By measuring pressure change at constant volume, temperature can be determined. All gases give identical readings regardless of type (at low densities)—this property validates the ideal gas law.

    ---

    THERMAL EXPANSION

    **Definition:** Thermal expansion is the increase in dimensions (length, area, or volume) of a substance due to increase in its temperature. Most substances expand on heating and contract on cooling.

    **Cause:** Increased thermal energy causes atoms/molecules to vibrate more vigorously, requiring more space.

    **Types of Thermal Expansion:**

    Linear Expansion (Change in Length)

    For a rod of length **l** experiencing temperature change **ΔT**:

    $$\frac{\Delta l}{l} = \alpha_l \Delta T$$

    Or: **ΔL = L₀ α_l ΔT** (absolute change)

    **Final length:** **L = L₀(1 + α_l ΔT)**

    Where:

  • **α_l** = coefficient of linear expansion (K⁻¹ or °C⁻¹)
  • **ΔL** = change in length
  • **L₀** = original length
  • **ΔT** = change in temperature
  • **α_l depends on material type but is independent of length.**

    **Typical Values (Table 10.1):**

    | Material | α_l (10⁻⁵ K⁻¹) |

    |----------|----------------|

    | Aluminium | 2.5 |

    | Brass | 1.8 |

    | Copper | 1.7 |

    | Iron | 1.2 |

    | Silver | 1.9 |

    | Glass (pyrex) | 0.32 |

    | Lead | 0.29 |

    **Key Observation:** Metals have larger linear expansion coefficients than glass. Copper expands ~5 times more than pyrex glass for same temperature change.

    **Worked Example (Blacksmith Problem):**

    Iron ring diameter at 27°C = 5.231 m

    Rim diameter at 27°C = 5.243 m

    Coefficient of linear expansion for iron: α_l = 1.2 × 10⁻⁵ K⁻¹

    Using **L_T2 = L_T1[1 + α_l(T₂ - T₁)]**:

    5.243 = 5.231[1 + 1.2 × 10⁻⁵(T₂ - 27)]

    Solving: T₂ = 218°C

    The ring must be heated to ~218°C to expand and fit the rim.

    Area Expansion

    For a rectangular sheet of area **A**:

    $$\frac{\Delta A}{A} = \alpha_A \Delta T = 2\alpha_l \Delta T$$

    **Proof (Example 10.1):**

    Consider rectangle with length a, breadth b. When temperature increases by ΔT:

  • Δa = α_l a ΔT
  • Δb = α_l b ΔT
  • ΔA = ΔA₁ + ΔA₂ + ΔA₃ = a(Δb) + b(Δa) + (Δa)(Δb)
  • ΔA = aα_l b ΔT + bα_l a ΔT + (α_l)² ab(ΔT)²
  • Since α_l ≈ 10⁻⁵ K⁻¹, the term (α_l)² ab(ΔT)² ≈ 0 (negligible)

    Therefore: **ΔA/A = 2α_l ΔT**

    Or: **α_A = 2α_l**

    **Final area:** **A = A₀(1 + 2α_l ΔT)**

    Volume Expansion

    For a solid or liquid experiencing temperature change **ΔT**:

    $$\frac{\Delta V}{V} = \alpha_v \Delta T$$

    Or: **ΔV = V₀ α_v ΔT**

    **Final volume:** **V = V₀(1 + α_v ΔT)**

    Where **α_v** = coefficient of volume expansion (K⁻¹)

    **Relationship between α_v and α_l:**

    Consider a cube of side length **l** expanding equally in all directions:

  • Δl = α_l l ΔT
  • New volume: V' = (l + Δl)³
  • ΔV = (l + Δl)³ - l³ = 3l²(Δl) + 3l(Δl)² + (Δl)³
  • Neglecting higher order terms (Δl << l):

  • ΔV ≈ 3l²(Δl) = 3l² × α_l l ΔT = 3l³ α_l ΔT = 3V α_l ΔT
  • Therefore: **α_v = 3α_l**

    **Typical Values (Table 10.2):**

    | Material | α_v (K⁻¹) |

    |----------|-----------|

    | Aluminium | 7 × 10⁻⁵ |

    | Brass | 6 × 10⁻⁵ |

    | Iron | 3.55 × 10⁻⁵ |

    | Mercury | 18.2 × 10⁻⁵ |

    | Water | 20.7 × 10⁻⁵ |

    | Alcohol | 110 × 10⁻⁵ |

    | Glass (pyrex) | 1 × 10⁻⁵ |

    | Invar | 2 × 10⁻⁶ |

    Thermal Expansion in Gases

    Gases expand far more than solids and liquids at ordinary temperatures.

    **For an ideal gas at constant pressure:**

    From PV = μRT:

    $$\Delta V = \frac{\mu R \Delta T}{P}$$

    $$\frac{\Delta V}{V} = \frac{\Delta T}{T}$$

    **Therefore:** **α_v = 1/T** (temperature dependent)

    At 0°C (273 K): α_v = 1/273 ≈ 3.7 × 10⁻³ K⁻¹

    At room temperature (~300 K): α_v ≈ 3.3 × 10⁻³ K⁻¹

    This is **1000 times larger** than typical liquid or solid expansion coefficients.

    ---

    ANOMALOUS EXPANSION OF WATER

    **Water exhibits unique behavior:** It **contracts on heating** from 0°C to 4°C (opposite to normal thermal expansion).

    **Characteristics:**

  • Volume decreases as water cools from room temperature to 4°C
  • Volume increases as water cools further below 4°C
  • **Maximum density occurs at 4°C** (~1000 kg/m³)
  • Below 4°C, density decreases as temperature decreases
  • **Environmental Significance:**

    Lakes and ponds freeze from the **top down**, not bottom up:

    1. As water cools toward 4°C, surface water becomes denser and sinks

    2. Warmer water rises from bottom (convection)

    3. Once surface reaches below 4°C, it becomes less dense and remains at top

    4. Ice forms on surface, insulating deeper water

    5. Aquatic life survives in liquid water below the ice layer

    **Without this anomaly:** Water would freeze from bottom up, killing fish and plant life. This unique property is crucial for freshwater ecosystem survival.

    ---

    THERMAL STRESS

    When thermal expansion is **prevented** by rigid constraints, the substance develops internal stress called **thermal stress**.

    **Physical Situation:**

    A rod fixed at both ends experiences temperature increase but cannot expand. External forces must provide compressive strain to prevent expansion.

    **Calculation of Thermal Stress:**

    If a rod of length l, cross-sectional area A, coefficient of linear expansion α_l is prevented from expanding when temperature increases by ΔT:

    **Compressive strain:** ε = (Δl/l) = α_l ΔT

    **Thermal stress:** σ = Y × ε = **Y α_l ΔT**

    Where **Y** = Young's modulus (Pa)

    **Force developed:** **F = A × σ = AY α_l ΔT**

    **Worked Example:**

    Steel rail: length L₀ = 5 m, area A = 40 cm² = 40 × 10⁻⁴ m²

    Temperature increase: ΔT = 10°C

    α_l (steel) = 1.2 × 10⁻⁵ K⁻¹

    Y (steel) = 2 × 10¹¹ N/m²

    Strain: ε = 1.2 × 10⁻⁵ × 10 = 1.2 × 10⁻⁴

    Stress: σ = 2 × 10¹¹ × 1.2 × 10⁻⁴ = 2.4 × 10⁷ N/m²

    Force: F = 2.4 × 10⁷ × 40 × 10⁻⁴ = 9.6 × 10⁵ N ≈ 10⁵ N

    This enormous force can **bend or fracture rails** if not accommodated by expansion joints.

    **Practical Applications:**

  • Railroad tracks have expansion joints every 10-20 m
  • Bridge supports include bearings allowing expansion
  • Building joints prevent cracks from thermal stress
  • Power transmission lines sag in summer to prevent breakage
  • ---

    SPECIFIC HEAT CAPACITY

    **Definition:** Specific heat capacity of a substance is the amount of heat required to raise the temperature of unit mass of the substance by one unit temperature without any change in its state.

    **Mathematical Definition:**

    $$s = \frac{1}{m} \frac{\Delta Q}{\Delta T}$$

    Or: **ΔQ = m × s × ΔT**

    Where:

  • **ΔQ** = heat energy (J)
  • **m** = mass of substance (kg)
  • **s** = specific heat capacity (J kg⁻¹ K⁻¹)
  • **ΔT** = temperature change (K or °C)
  • **SI Unit:** J kg⁻¹ K⁻¹ or J kg⁻¹ °C⁻¹

    **Key Points:**

  • Specific heat capacity is a **material property**—depends on nature of substance
  • Also depends weakly on temperature (usually neglected for small ΔT)
  • Water has one of the **highest specific heat capacities** (~4186 J kg⁻¹ K⁻¹)
  • Metals typically have lower specific heat capacities than water
  • **Physical Meaning:**

  • High s means more heat needed to raise temperature by 1°C
  • Water requires more heat energy than oil for same temperature rise (hence longer heating time in experiment)
  • Explains why coastal regions have moderate climates—water's high s capacity buffers temperature changes
  • **Worked Example:**

    How much heat is needed to raise the temperature of 2 kg of water from 20°C to 80°C?

    s(water) = 4186 J kg⁻¹ K⁻¹

    ΔQ = m × s × ΔT = 2 × 4186 × (80 - 20) = 2 × 4186 × 60 = 502,320 J ≈ 5.02 × 10⁵ J

    ---

    MOLAR SPECIFIC HEAT CAPACITY

    When heat capacity is expressed per mole instead of per unit mass:

    $$C = \frac{1}{\mu} \frac{\Delta Q}{\Delta T}$$

    Or: **ΔQ = μ × C × ΔT**

    Where:

  • **C** = molar specific heat capacity (J mol⁻¹ K⁻¹)
  • **μ** = number of moles (mol)
  • ΔQ = heat energy
  • ΔT = temperature change
  • **Relation between s and C:**

    $$C = M \times s$$

    Where **M** = molar mass (kg/mol)

    Or: **s = C/M**

    **For Gases—Two Important Cases:**

    Molar Specific Heat Capacity at Constant Pressure (C_p)

    When gas is allowed to expand freely at constant pressure during heating:

  • Gas does work on surroundings as it expands
  • More heat needed to achieve same temperature rise compared to constant volume
  • **C_p > C_v**
  • Molar Specific Heat Capacity at Constant Volume (C_v)

    When volume is held constant during heating (rigid container):

  • No expansion work done
  • All heat goes into increasing internal energy and temperature
  • **C_v < C_p**
  • **Mayer's Relation:** C_p - C_v = R (8.31 J mol⁻¹ K⁻¹)

    Detailed treatment covered in Chapter 11 (Thermodynamics).

    ---

    HEAT CAPACITY

    **Definition:** Heat capacity of a body is the amount of heat required to raise its temperature by one unit without change of state.

    $$S = \frac{\Delta Q}{\Delta T}$$

    **SI Unit:** J K⁻¹ or J °C⁻¹

    **Relationship to Specific Heat Capacity:**

    $$S = m \times s$$

    Heat capacity is **extensive** (depends on mass), while specific heat capacity is **intensive** (independent of mass).

    **Thermal Inertia:**

    Heat capacity measures the **thermal inertia** of a body—resistance to temperature change. Large heat capacity means large heat input needed for temperature change.

    **Experimental Observations (from heating experiments):**

    1. **Varying ΔT, constant mass, same substance:**

  • Heat required ∝ ΔT
  • ΔQ ∝ ΔT
  • 2. **Varying mass, constant ΔT, same substance:**

  • Heat required ∝ m
  • ΔQ ∝ m
  • 3. **Different substances, same m and ΔT:**

  • Heat required varies with substance nature
  • Different substances have different specific heat capacities
  • Oil requires less heat than water for same mass and temperature rise
  • These observations validate: **ΔQ = m s ΔT**

    ---

    CALORIMETRY

    **Definition:** Calorimetry is the branch of physics dealing with measurement of heat energy and thermal properties using a calorimeter.

    **Principle:** Based on **conservation of thermal energy** (Law of Thermal Exchanges):

    When two bodies at different temperatures are brought into thermal contact and isolated from surroundings:

  • Heat lost by hot body = Heat gained by cold body (algebraically: ΣQ = 0)
  • System reaches thermal equilibrium at common final temperature
  • No heat exchange with surroundings (ideal calorimeter)
  • **Calorimeter Setup:**

  • Insulated container (typically copper or aluminum)
  • Liquid (usually water) for heat exchange
  • Thermometer for temperature measurement
  • Stirrer for uniform mixing
  • Inner and outer walls for insulation
  • **Basic Calorimetry Equation:**

    When hot and cold substances mix:

    $$m_1 s_1 (T_1 - T_f) = m_2 s_2 (T_f - T_2)$$

    Where:

  • m₁, s₁, T₁ = mass, specific heat, initial temperature of hot substance
  • m₂, s₂, T₂ = mass, specific heat, initial temperature of cold substance
  • T_f = final equilibrium temperature
  • **Or in general form:** **Σ(ΔQ) = 0** for isolated system

    **Worked Example:**

    100 g of aluminum at 80°C is mixed with 200 g of water at 20°C.

    s(Al) = 900 J kg⁻¹ K⁻¹, s(water) = 4186 J kg⁻¹ K⁻¹

    Heat lost by aluminum: Q₁ = 0.1 × 900 × (80 - T_f)

    Heat gained by water: Q₂ = 0.2 × 4186 × (T_f - 20)

    At equilibrium: Q₁ = Q₂

    0.1 × 900 × (80 - T_f) = 0.2 × 4186 × (T_f - 20)

    90(80 - T_f) = 837.2(T_f - 20)

    7200 - 90T_f = 837.2T_f - 16,744

    23,944 = 927.2T_f

    T_f ≈ 25.8°C

    **Applications:**

  • Determining specific heat capacity of substances
  • Finding latent heat of fusion/vaporization
  • Measuring heat of chemical reactions
  • Quality control in food/pharmaceutical industries
  • **Limitations:**

  • Heat losses to surroundings (imperfect insulation)
  • Heat absorbed by calorimeter vessel itself
  • Incomplete mixing
  • Temperature variation during measurement
  • **Corrections:**

  • Use calorimeter vessel heat capacity: Q_vessel = m_vessel × s_vessel × ΔT
  • Account for heat losses using Newton's law of cooling
  • Allow sufficient equilibration time
  • ---

    CHANGE OF STATE (LATENT HEAT)

    **Definition:** Change of state refers to transformation between different phases of matter (solid ↔ liquid ↔ gas) at constant temperature during heat absorption/release.

    **Key Feature:** During phase change, temperature remains constant despite continuous heat flow.

    Fusion (Solid → Liquid)

    **Melting:** Process of converting solid to liquid by heating at constant temperature (melting point).

    **Example:** Ice melting at 0°C under standard pressure

  • Temperature stays at 0°C throughout melting
  • Heat energy breaks intermolecular bonds, creating space between molecules
  • Latent heat of fusion (L_f): energy per unit mass required to melt solid at melting point
  • **Latent Heat of Fusion (L_f):**

    $$Q_f = m L_f$$

    Where:

  • **Q_f** = heat required for fusion (J)
  • **m** = mass (kg)
  • **L_f** = latent heat of fusion (J/kg)
  • **SI Unit:** J kg⁻¹

    **Typical Values:**

  • Ice (at 0°C): L_f = 3.34 × 10⁵ J/kg (334 J/g)
  • Lead (at 327°C): L_f = 2.3 × 10⁴ J/kg
  • Aluminum: L_f = 3.8 × 10⁵ J/kg
  • **Freezing:** Reverse of melting (liquid → solid)

  • Occurs at same temperature as melting (freezing point)
  • Heat released = m × L_f (latent heat of fusion)
  • Freezing and melting points are identical for pure substances at 1 atm
  • **Worked Example:**

    How much heat is needed to melt 250 g of ice at 0°C?

    L_f(ice) = 3.34 × 10⁵ J/kg

    Q = m × L_f = 0.25 × 3.34 × 10⁵ = 8.35 × 10⁴ J

    Vaporization (Liquid → Gas)

    **Boiling:** Conversion of liquid to gas by heating at constant temperature (boiling point).

    **Example:** Water boiling at 100°C at standard pressure

  • Temperature constant throughout boiling
  • Heat energy breaks liquid structure completely
  • Molecules escape as gas
  • Latent heat of vaporization (L_v): energy per unit mass required to vaporize liquid at boiling point
  • **Latent Heat of Vaporization (L_v):**

    $$Q_v = m L_v$$

    Where:

  • **Q_v** = heat required for vaporization (J)
  • **m** = mass (kg)
  • **L_v** = latent heat of vaporization (J/kg)
  • **SI Unit:** J kg⁻¹

    **Typical Values:**

  • Water (at 100°C): L_v = 2.26 × 10⁶ J/kg (2260 J/g)
  • Mercury (at 357°C): L_v = 2.7 × 10⁵ J/kg
  • Alcohol (at 78°C): L_v = 8.55 × 10⁵ J/kg
  • **Note:** L_v >> L_f for same substance (water: 2.26 × 10⁶ vs 3.34 × 10⁵)

    Much more heat needed to vaporize than to melt.

    **Condensation:** Reverse of vaporization (gas → liquid)

  • Occurs at same temperature as boiling (condensation point)
  • Heat released = m × L_v
  • Condensation and boiling points are identical at given pressure
  • **Worked Example:**

    How much heat is released when 1 kg of steam at 100°C condenses to water at 100°C?

    L_v(water) = 2.26 × 10⁶ J/kg

    Q = m × L_v = 1 × 2.26 × 10⁶ = 2.26 × 10⁶ J

    Sublimation (Solid → Gas)

    **Definition:** Direct conversion of solid to gas without passing through liquid phase at specific temperature and pressure (sublimation point).

    **Example:** Dry ice (solid CO₂) converts to CO₂ gas below -78°C at 1 atm

    Naphthalene (mothballs) sublimes at room temperature

    Frost on grass converts directly to water vapor

    **Latent Heat of Sublimation (L_s):**

    $$Q_s = m L_s$$

    **Relationship:** L_s = L_f + L_v (approximately)

    Sublimation energy equals fusion energy plus vaporization energy.

    **Deposition:** Reverse of sublimation (gas → solid)

  • Occurs at sublimation temperature
  • Frost formation from water vapor
  • ---

    CALORIMETRY WITH CHANGE OF STATE

    When substances undergo phase changes during heat exchange:

    **Total Heat Calculation:**

    $$\Delta Q_{total} = \Delta Q_{sensible} + \Delta Q_{latent}$$

    Sensible heat: raises/lowers temperature (Q = mcΔT)

    Latent heat: changes state at constant temperature (Q = mL)

    **Worked Example:**

    Convert 100 g ice at -10°C to steam at 110°C

    s_ice = 2100 J kg⁻¹ K⁻¹, s_water = 4186 J kg⁻¹ K⁻¹, s_steam = 2000 J kg⁻¹ K⁻¹

    L_f = 3.34 × 10⁵ J/kg, L_v = 2.26 × 10⁶ J/kg

    **Step 1:** Heat ice from -10°C to 0°C

    Q₁ = 0.1 × 2100 × 10 = 2,100 J

    **Step 2:** Melt ice at 0°C

    Q₂ = 0.1 × 3.34 × 10⁵ = 3.34 × 10⁴ J

    **Step 3:** Heat water from 0°C to 100°C

    Q₃ = 0.1 × 4186 × 100 = 4.186 × 10⁴ J

    **Step 4:** Vaporize water at 100°C

    Q₄ = 0.1 × 2.26 × 10⁶ = 2.26 × 10⁵ J

    **Step 5:** Heat steam from 100°C to 110°C

    Q₅ = 0.1 × 2000 × 10 = 2,000 J

    **Total Heat:** Q_total = 2.1 × 10³ + 3.34 × 10⁴ + 4.186 × 10⁴ + 2.26 × 10⁵ + 2 × 10³

    = 300,500 J ≈ 3 × 10⁵ J

    Vaporization dominates heat requirement.

    ---

    HEAT TRANSFER

    **Definition:** Heat transfer is the spontaneous flow of thermal energy from regions of higher temperature to regions of lower temperature.

    **Driving Force:** Temperature difference (ΔT) between regions

    **Three Mechanisms:**

    1. CONDUCTION

    **Definition:** Heat transfer through a material without bulk motion of the material. Heat flows from molecule to molecule by direct contact.

    **Mechanism:**

  • Hot molecules vibrate vigorously
  • Transfer kinetic energy to neighboring cooler molecules through collisions
  • Energy propagates as temperature wave through material
  • No mass transport
  • **Examples:**

  • Touching a hot iron rod—heat conducts through metal to hand
  • Metal spoon heating up when immersed in hot tea
  • Frost spreading into ground from surface
  • **Thermal Conductivity:**

    Heat conducted through material depends on:

    1. Temperature difference (ΔT)

    2. Material's thermal conductivity (λ or k)

    3. Cross-sectional area (A)

    4. Length/thickness (d)

    **Fourier's Law of Heat Conduction:**

    Heat flow rate (power):

    $$H = -\lambda A \frac{dT}{dx}$$

    For steady-state with uniform temperature gradient:

    $$H = \lambda A \frac{\Delta T}{d}$$

    Or: **Q = λ A ΔT t / d**

    Where:

  • **Q** = heat energy conducted (J)
  • **H** = heat flow rate/power (W or J/s)
  • **λ** = thermal conductivity (W m⁻¹ K⁻¹)
  • **A** = cross-sectional area (m²)
  • **ΔT** = temperature difference (K)
  • **d** = thickness/distance (m)
  • **t** = time (s)
  • **SI Unit of λ:** W m⁻¹ K⁻¹ (or J s⁻¹ m⁻¹ K⁻¹)

    **Thermal Conductivity Values (approx):**

    | Material | λ (W m⁻¹ K⁻¹) |

    |----------|-----------------|

    | Silver | 429 |

    | Copper | 385 |

    | Aluminum | 205 |

    | Steel | 50 |

    | Brick | 0.9 |

    | Concrete | 1.4 |

    | Glass | 0.8 |

    | Water | 0.6 |

    | Air | 0.026 |

    | Wood | 0.1-0.2 |

    **Key Observations:**

  • Metals (good conductors): high λ (silver: 429)
  • Insulators: low λ (air: 0.026)
  • λ increases with temperature for metals
  • λ depends on material composition and structure
  • **Thermal Resistance (R-value):**

    $$R = \frac{d}{\lambda}$$

    Analogous to electrical resistance. Higher R means poorer conductor.

    **Worked Example:**

    A copper rod 10 cm long, 2 cm² cross-section, with ends at 100°C and 0°C. How much heat flows in 1 minute?

    λ

    MCQs — 10 Questions with Answers

    Q1. What is the SI unit of heat?

    • A. Joule (J) ✓
    • B. Calorie (cal)
    • C. Watt (W)
    • D. Kelvin (K)

    Answer: A — Joule is the SI unit of energy, including heat energy; other units are either non-SI or measure different quantities (W measures power, K measures temperature).

    Q2. The ice point and steam point of water on the Celsius scale are:

    • A. −40°C and 60°C
    • B. 0°C and 100°C ✓
    • C. 32°C and 212°C
    • D. 273 K and 373 K

    Answer: B — By definition, pure water freezes at 0°C and boils at 100°C under standard atmospheric pressure on the Celsius scale.

    Q3. Using the relation (tF − 32)/180 = tC/100, what is 32°F in Celsius?

    • A. 0°C ✓
    • B. 180°C
    • C. 32°C
    • D. 100°C

    Answer: A — Substituting tF = 32: (32 − 32)/180 = tC/100 gives 0/180 = tC/100, so tC = 0°C (ice point).

    Q4. If a gas at constant volume has pressure P₁ at temperature T₁, what is its pressure at temperature 2T₁?

    • A. P₁/2
    • B. P₁
    • C. 2P₁ ✓
    • D. 4P₁

    Answer: C — From ideal gas law at constant volume: P/T = constant, so P₁/T₁ = P₂/2T₁, giving P₂ = 2P₁.

    Q5. The value of the universal gas constant R in SI units is:

    • A. 0.082 L atm mol⁻¹ K⁻¹
    • B. 8.31 J mol⁻¹ K⁻¹ ✓
    • C. 1.987 cal mol⁻¹ K⁻¹
    • D. 0.0821 bar L mol⁻¹ K⁻¹

    Answer: B — R = 8.31 J mol⁻¹ K⁻¹ is the SI value used in the ideal gas equation PV = µRT; other options use non-SI units.

    Q6. A gas thermometer reads the same for all low-density gases because:

    • A. All gases have the same boiling point
    • B. All gases obey Boyle's and Charles' laws identically ✓
    • C. All gases have the same density
    • D. All gases conduct heat at the same rate

    Answer: B — All low-density gases exhibit identical expansion behaviour following PV/T = constant, making gas thermometers universal; other factors are not related to thermometric consistency.

    Q7. Which statement about absolute zero is NOT correct?

    • A. Absolute zero is −273.15°C on the Celsius scale
    • B. Absolute zero is 0 K on the Kelvin scale
    • C. Absolute zero is the temperature where molecular motion stops completely and can be achieved experimentally ✓
    • D. Absolute zero is the lower limit of the Kelvin temperature scale

    Answer: C — Absolute zero cannot be practically achieved due to thermodynamic laws; it is a theoretical limit, not an experimentally reachable temperature.

    Q8. If pressure P of a fixed mass of gas at constant volume is plotted against Celsius temperature, the line extrapolates to meet the temperature axis at −273.15°C because:

    • A. This is the freezing point of water
    • B. The P vs T relationship is linear, and P = 0 at this absolute temperature ✓
    • C. All gases liquefy at this temperature
    • D. This is the boiling point of all substances

    Answer: B — From PV = µRT (constant V), P ∝ T absolutely; the line must pass through origin in P vs T(K) graph, which corresponds to −273.15°C on Celsius scale where P = 0.

    Q9. Which pair correctly matches a temperature scale property with its value?

    • A. Fahrenheit: 180 equal intervals between ice and steam points
    • B. Celsius: 273.15 equal intervals between ice and steam points
    • C. Kelvin: Ice point at 273.15 K and steam point at 373.15 K, 100 equal intervals ✓
    • D. All scales: Same absolute zero temperature

    Answer: C — Kelvin scale has ice point = 273.15 K and steam point = 373.15 K with 100 equal intervals, matching Celsius; Fahrenheit has 180 intervals; only Kelvin has true absolute zero at 0 K.

    Q10. A constant-pressure gas thermometer measures temperature by reading the volume change of gas. If volume V₁ at temperature T₁ (in Kelvin) increases to V₂ at temperature T₂, derive the relation between V₁, V₂, T₁, and T₂ using Charles' law, and calculate T₂ if V₁ = 100 cm³ at T₁ = 273 K and V₂ = 150 cm³.

    • A. V₁/V₂ = T₁/T₂; T₂ = 409.5 K
    • B. V₁/T₁ = V₂/T₂; T₂ = 409.5 K ✓
    • C. V₁T₁ = V₂T₂; T₂ = 182 K
    • D. V₁/T₂ = V₂/T₁; T₂ = 150 K

    Answer: B — Charles' law at constant pressure: V/T = constant, so V₁/T₁ = V₂/T₂; substituting values: T₂ = T₁(V₂/V₁) = 273 × (150/100) = 273 × 1.5 = 409.5 K.

    Flashcards

    What is the SI unit of heat energy?

    Joule (J) is the SI unit of heat energy.

    Define temperature in physics.

    Temperature is a relative measure of the hotness or coldness of a body, indicating the average kinetic energy of its particles.

    State Boyle's law for gases.

    At constant temperature, the product of pressure and volume of a fixed mass of gas is constant: PV = constant.

    What is the relationship between Celsius and Kelvin scales?

    T(K) = tC + 273.15, where both scales have the same unit size but different zero points.

    Define heat in thermodynamics.

    Heat is the form of energy transferred between two systems or a system and surroundings due to temperature difference.

    What are the two fixed reference points for temperature scales?

    Ice point (freezing point of water at 0°C) and steam point (boiling point of water at 100°C) under standard atmospheric pressure.

    State Charles' law for gases.

    At constant pressure, the volume of a fixed mass of gas is directly proportional to absolute temperature: V/T = constant.

    What is the ideal gas equation?

    PV = µRT, where P is pressure, V is volume, µ is number of moles, R is universal gas constant (8.31 J mol⁻¹ K⁻¹), and T is absolute temperature.

    Convert 98.6°F to Celsius.

    Using (tF - 32)/180 = tC/100: tC = (98.6 - 32) × 100/180 = 37°C.

    What is absolute zero and why is it important?

    Absolute zero (-273.15°C or 0 K) is the lowest possible temperature where all molecular motion theoretically stops, defining the Kelvin scale's zero point.

    Important Board Questions

    Define heat and temperature. Explain why heat flows from a body at higher temperature to one at lower temperature. [2 marks]

    State that temperature measures hotness (average kinetic energy of particles) and heat is energy transferred due to temperature difference; explain that systems spontaneously move toward thermal equilibrium.

    Derive the ideal gas equation starting from Boyle's law and Charles' law. Show all steps and explain what each law represents physically. [5 marks]

    Begin with PV = const (Boyle's law at constant T) and V/T = const (Charles' law at constant P); combine these relations to show PV/T = constant for a given mass; introduce moles and universal gas constant R to obtain PV = µRT; explain that Boyle's law represents inverse pressure-volume relationship and Charles' law represents direct volume-temperature proportionality.

    A blacksmith heats an iron ring before fitting it onto the wooden rim of a cart wheel. Explain this technique using the concept of thermal expansion and derive the linear expansion formula. Why cannot the ring be forced on at room temperature? [6 marks]

    Explain that heating increases atomic spacing, causing the ring's diameter to expand; derive ΔL = αL₀ΔT by considering that fractional expansion is proportional to temperature change and initial length; show that at room temperature the ring's diameter is smaller than the wheel rim, making fitting impossible without expansion; at elevated temperature, the expanded ring diameter matches the rim, allowing easy fitting and subsequent tight grip upon cooling.

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