Class 10 Science - Chapter 5

Heat

Original, Copyright-Free Notes aligned with Maharashtra Board syllabus

Complete coverage of thermal concepts, expansion, and heat transfer

Heat and Temperature Thermal Expansion Latent Heat Specific Heat Conduction Convection Radiation Class 10 Science Maharashtra Board

1. Introduction

Heat is a form of energy that flows from a body at higher temperature to a body at lower temperature. It is one of the most fundamental concepts in physics and plays a crucial role in our daily lives, influencing everything from weather patterns to cooking food.

Heat energy is responsible for various observable effects in matter. Understanding heat is essential not only for scientific knowledge but also for practical applications in engineering, technology, and everyday life.

Effects of Heat in Daily Life

Temperature Changes

Heating increases temperature, cooling decreases it. This affects our comfort, cooking, and industrial processes.

Expansion of Materials

Most substances expand when heated, which is considered in construction, engineering, and manufacturing.

Change of State

Heat can change solids to liquids (melting) and liquids to gases (vaporization), fundamental to many natural and industrial processes.

Heat Transfer Visualization
HOT
Higher Temperature
COLD
Lower Temperature

Heat always flows from hotter to colder objects

2. Heat and Temperature

Although often used interchangeably in everyday language, heat and temperature are distinct concepts in physics. Understanding their difference is fundamental to studying thermal physics.

Heat

Definition: Energy in transit due to temperature difference

Nature: Form of energy

Flow Direction: Always from hotter to colder body

SI Unit: Joule (J)

Depends On: Mass, specific heat, temperature change

Analogy: Like total amount of water in a container

Temperature

Definition: Degree of hotness or coldness of a body

Nature: Measure of thermal state

Flow Direction: Doesn't flow, it's a property

SI Unit: Kelvin (K)

Depends On: Average kinetic energy of particles

Analogy: Like level of water in a container

Understanding the Difference

Scenario: A cup of boiling water and a bathtub of warm water

  • The cup of boiling water has a higher temperature (100°C) but contains less heat energy (due to small mass)
  • The bathtub of warm water has a lower temperature (40°C) but contains more heat energy (due to large mass)
  • If you touch both, the cup feels hotter (higher temperature), but the bathtub has more total heat energy

Molecular Interpretation

  • Temperature: Represents the average kinetic energy of molecules in a substance
  • Heat: Represents the total internal energy (kinetic + potential) transferred between bodies
  • When temperature increases, molecular motion becomes more vigorous
  • Heat transfer increases the internal energy of a body, which may increase temperature or change state
Low Temperature
Slow molecular motion
High Temperature
Fast molecular motion

3. Measurement of Temperature

Temperature is measured using instruments called thermometers. Different temperature scales have been developed for various applications, each with its own reference points and unit divisions.

Common Types of Thermometers
Clinical Thermometer
Measures body temperature (35°C to 42°C)
Laboratory Thermometer
Measures general temperatures (-10°C to 110°C)
Digital Thermometer
Electronic temperature measurement

Common Temperature Scales

Celsius Scale (°C)

Inventor: Anders Celsius (1742)

Reference Points:

  • 0°C: Freezing point of water
  • 100°C: Boiling point of water

Usage: Most countries except USA, scientific work

Fahrenheit Scale (°F)

Inventor: Daniel Fahrenheit (1724)

Reference Points:

  • 32°F: Freezing point of water
  • 212°F: Boiling point of water

Usage: USA, some Caribbean countries

Kelvin Scale (K)

Inventor: Lord Kelvin (1848)

Reference Points:

  • 0 K: Absolute zero (-273.15°C)
  • 273.15 K: Freezing point of water
  • 373.15 K: Boiling point of water

Usage: Scientific work (SI unit)

Temperature Scale Conversions

Celsius to Kelvin:

K = °C + 273

Kelvin to Celsius:

°C = K - 273

Celsius to Fahrenheit:

°F = (9/5 × °C) + 32

Fahrenheit to Celsius:

°C = 5/9 × (°F - 32)
Example: Temperature Conversions

Problem: Convert 25°C to Kelvin and Fahrenheit.

Solution:

  1. To Kelvin: K = °C + 273 = 25 + 273 = 298 K
  2. To Fahrenheit: °F = (9/5 × °C) + 32 = (9/5 × 25) + 32 = 45 + 32 = 77°F

Result: 25°C = 298 K = 77°F

Absolute Zero

  • Definition: The lowest possible temperature where molecular motion theoretically stops
  • Value: 0 K = -273.15°C = -459.67°F
  • Significance: All thermal motion ceases; it's impossible to reach absolute zero in practice
  • In Kelvin scale: No negative values; all temperatures are positive

4. Effects of Heat

When heat is supplied to a substance, it can produce various observable effects. These effects form the basis for understanding thermal phenomena and have numerous practical applications.

1

Rise in Temperature

Description: Increase in the degree of hotness of a body

Molecular Explanation: Heat energy increases the kinetic energy of molecules, making them move faster

Quantified by: Specific heat capacity (amount of heat needed to raise temperature)

Examples: Water heating on stove, metal getting hot in sun

2

Expansion of Substances

Description: Increase in dimensions (length, area, volume) when heated

Molecular Explanation: Increased molecular motion causes molecules to occupy more space

Quantified by: Coefficients of linear, areal, and volume expansion

Examples: Railway tracks expand in summer, hot air balloons rise

3

Change of State

Description: Transformation from one state of matter to another

Molecular Explanation: Heat overcomes intermolecular forces, allowing change in arrangement

Quantified by: Latent heat (heat needed for state change without temperature change)

Examples: Ice melting, water boiling, dry ice subliming

Visualizing Heat Effects
Temperature Rise
Small
Expansion
Solid
Heat
Liquid
State Change

Other Effects of Heat (Beyond Basics)

  • Chemical Changes: Heat can cause chemical reactions (cooking, combustion)
  • Electrical Effects: Heating can change electrical resistance (used in thermistors)
  • Biological Effects: Heat affects biological processes (enzyme activity, metabolism)
  • Optical Effects: Heat can change refractive index (mirage formation)
  • Mechanical Effects: Thermal stress can cause cracks in materials

5. Expansion Due to Heat

Most substances expand when heated and contract when cooled. This property, known as thermal expansion, occurs because increased thermal energy causes particles to vibrate more vigorously and occupy more space.

Types of Thermal Expansion

Linear Expansion

Definition: Increase in length when heated

Formula: ΔL = αL₀ΔT

Where:

  • ΔL = Change in length
  • α = Coefficient of linear expansion
  • L₀ = Original length
  • ΔT = Change in temperature

Example: Railway tracks, bridges

Areal Expansion

Definition: Increase in area when heated

Formula: ΔA = βA₀ΔT

Where:

  • ΔA = Change in area
  • β = Coefficient of areal expansion (β ≈ 2α)
  • A₀ = Original area
  • ΔT = Change in temperature

Example: Metal plates, glass windows

Volume Expansion

Definition: Increase in volume when heated

Formula: ΔV = γV₀ΔT

Where:

  • ΔV = Change in volume
  • γ = Coefficient of volume expansion (γ ≈ 3α)
  • V₀ = Original volume
  • ΔT = Change in temperature

Example: Liquids, gases, solids

Example: Linear Expansion Problem

Problem: A steel rail is 10 m long at 20°C. If the coefficient of linear expansion of steel is1.2 × 10⁻⁵ /°C, how much will it expand when heated to 50°C?

Solution:

  1. Original length, L₀ = 10 m
  2. Temperature change, ΔT = 50°C - 20°C = 30°C
  3. Coefficient, α = 1.2 × 10⁻⁵ /°C
  4. Expansion, ΔL = α × L₀ × ΔT
  5. ΔL = (1.2 × 10⁻⁵) × 10 × 30
  6. ΔL = 3.6 × 10⁻³ m = 3.6 mm

The rail will expand by 3.6 mm when heated from 20°C to 50°C.

Applications of Thermal Expansion

Railway Tracks

Gaps left between rails to allow for expansion in summer, preventing buckling.

Thermometers

Liquid (mercury/alcohol) expands in a narrow tube, showing temperature change.

Bridges

Expansion joints allow for thermal expansion and contraction.

Hot Riveting

Hot rivets contract when cooled, creating tight joints in metal structures.

Fire Alarms

Bimetallic strips bend when heated, completing circuit to trigger alarm.

Opening Jar Lids

Heating metal lid expands it more than glass, making it easier to open.

Anomalous Expansion of Water

  • Most substances expand when heated, but water shows anomalous behavior
  • From 0°C to 4°C: Water contracts (density increases)
  • At 4°C: Water has maximum density (1 g/cm³)
  • Above 4°C: Water expands normally like other liquids
  • Significance: Ice floats on water, aquatic life survives in winter

6. Change of State

Matter exists in three primary states: solid, liquid, and gas. Change of state refers to the transformation from one state to another when heat is added or removed. These changes occur at specific temperatures and involve energy transfer.

Solid

Properties: Fixed shape and volume

Particle Arrangement: Regular, closely packed

Motion: Vibrational only

Liquid

Properties: Fixed volume, takes container shape

Particle Arrangement: Random, less closely packed

Motion: Vibrational + rotational + translational

Gas

Properties: No fixed shape or volume

Particle Arrangement: Very far apart, completely random

Motion: High speed in all directions

Processes of State Change

Melting

Definition: Change from solid to liquid

Temperature: Melting point (fixed for pure substances)

Energy: Absorbs heat (latent heat of fusion)

Examples: Ice to water, butter melting, wax melting

Special Cases:

  • Gallium: Melts at 30°C (in hand)
  • Tungsten: Highest melting point (3422°C)

Boiling

Definition: Change from liquid to gas throughout liquid

Temperature: Boiling point (depends on pressure)

Energy: Absorbs heat (latent heat of vaporization)

Examples: Water boiling, alcohol boiling

Special Cases:

  • Water: Boils at 100°C at sea level
  • High altitude: Lower boiling point
  • Pressure cooker: Higher boiling point

Evaporation

Definition: Slow change from liquid to gas at surface

Temperature: Occurs at any temperature

Energy: Absorbs heat from surroundings (cooling effect)

Examples: Drying clothes, sweat cooling, puddles drying

Factors Affecting:

  • Temperature (increases with temperature)
  • Surface area (more area, faster evaporation)
  • Humidity (slower in humid conditions)
  • Wind speed (faster with wind)

Other State Changes

Process Change Heat Example
Freezing Liquid → Solid Releases heat Water to ice
Condensation Gas → Liquid Releases heat Dew formation, clouds
Sublimation Solid → Gas Absorbs heat Dry ice, naphthalene balls
Deposition Gas → Solid Releases heat Frost formation
Evaporation vs Boiling
Aspect Evaporation Boiling
Temperature Occurs at any temperature Occurs at fixed boiling point
Location Only at surface Throughout the liquid
Rate Slow process Fast process
Bubbles No bubbles formed Bubbles formed throughout
Cooling Effect Causes cooling No cooling effect
Examples Drying clothes, sweat cooling Water boiling, cooking

7. Latent Heat

Latent heat is the heat energy required to change the state of a substance without changing its temperature. The term "latent" means "hidden" because this heat doesn't cause temperature rise but is absorbed or released during state changes.

Heating Curve of Water
Ice (-20°C)
Ice (0°C)
Water (0°C)
Water (100°C)
Steam (100°C)
Steam (120°C)
A: Heating ice
B: Melting (latent heat)
C: Heating water
D: Boiling (latent heat)
E: Heating steam
0°C
100°C
-20°C
120°C
Temperature

Observation: During state changes (B and D), temperature remains constant while heat is absorbed.

Latent Heat of Fusion

Definition: Heat required to change 1 kg of solid into liquid at its melting point without temperature change

Formula: Q = m × Lf

Where:

  • Q = Heat absorbed (J)
  • m = Mass (kg)
  • Lf = Latent heat of fusion (J/kg)

Examples:

  • Water: Lf = 3.34 × 10⁵ J/kg
  • Ice absorbs heat when melting
  • Water releases heat when freezing

Latent Heat of Vaporization

Definition: Heat required to change 1 kg of liquid into vapor at its boiling point without temperature change

Formula: Q = m × Lv

Where:

  • Q = Heat absorbed (J)
  • m = Mass (kg)
  • Lv = Latent heat of vaporization (J/kg)

Examples:

  • Water: Lv = 22.6 × 10⁵ J/kg
  • Water absorbs heat when boiling
  • Steam releases heat when condensing

Example: Latent Heat Calculation

Problem: How much heat is required to melt 2 kg of ice at 0°C? (Latent heat of fusion of ice = 3.34 × 10⁵ J/kg)

Solution:

Using formula: Q = m × Lf

Q = 2 kg × 3.34 × 10⁵ J/kg

Q = 6.68 × 10⁵ J = 668,000 J

Thus, 668,000 J of heat is needed to melt 2 kg of ice at 0°C.

Practical Implications of Latent Heat

  • Cooling by evaporation: Sweat evaporates using body heat, causing cooling
  • Refrigeration: Refrigerants absorb latent heat when evaporating
  • Steam burns: Steam at 100°C causes worse burns than water at 100°C because steam releases latent heat when condensing
  • Climate moderation: Large water bodies moderate climate due to high latent heat of water
  • Cooking: Food cooks faster in pressure cooker due to higher temperature of steam

8. Specific Heat Capacity

Specific heat capacity is a fundamental property of substances that determines how much heat energy is required to raise the temperature of a unit mass by one degree. Different substances have different abilities to store thermal energy.

Specific Heat Capacity Formula
Q = m × c × ΔT

Where:

  • Q = Heat energy supplied or removed (Joules)
  • m = Mass of the substance (kilograms)
  • c = Specific heat capacity (J/kg°C)
  • ΔT = Change in temperature (°C or K)

Definition of Specific Heat Capacity:

The amount of heat required to raise the temperature of 1 kg of a substance by 1°C (or 1 K).

Specific Heat Capacity of Common Substances

Substance Specific Heat Capacity (J/kg°C) Significance
Water 4186 (approximately 4200) Very high; excellent for temperature regulation
Ice 2100 About half of liquid water
Aluminium 900 High for a metal; used in cookware
Iron/Steel 450 Moderate; heats up relatively quickly
Copper 385 Low; excellent conductor of heat
Lead 130 Very low; heats up very quickly
Air (at constant pressure) 1005 Moderate; affects weather patterns
Example: Specific Heat Calculation

Problem: How much heat is required to raise the temperature of 5 kg of water from 20°C to 80°C? (Specific heat of water = 4200 J/kg°C)

Solution:

  1. Mass, m = 5 kg
  2. Specific heat, c = 4200 J/kg°C
  3. Temperature change, ΔT = 80°C - 20°C = 60°C
  4. Heat required, Q = m × c × ΔT
  5. Q = 5 × 4200 × 60
  6. Q = 1,260,000 J = 1.26 × 10⁶ J

Thus, 1.26 million joules of heat is needed.

Significance of Water's High Specific Heat

  • Climate Moderation: Oceans and large water bodies absorb and release heat slowly, moderating coastal climates
  • Biological Importance: Helps maintain stable body temperature in organisms
  • Industrial Use: Used as coolant in engines and industrial processes
  • Cooking: Water takes time to heat up and cool down, useful in cooking
  • Thermal Storage: Used in solar water heaters and thermal energy storage systems
Comparing Heating of Different Materials

Scenario: Equal masses of water and copper heated with same heat source

Aspect Water Copper
Specific Heat 4200 J/kg°C 385 J/kg°C
Heating Rate Slow (high specific heat) Fast (low specific heat)
Cooling Rate Slow to cool down Fast to cool down
Practical Implication Good for storing heat Good for transferring heat

9. Transfer of Heat

Heat can be transferred from one place to another through three distinct mechanisms: conduction, convection, and radiation. Each method operates differently and is dominant in different situations and materials.

Conduction

Mechanism: Direct transfer through collisions between adjacent particles

Medium Required: Solid materials (best in metals)

Particle Movement: Particles vibrate but don't change position

Example: Metal spoon in hot soup gets hot at handle

Convection

Mechanism: Transfer by actual movement of heated substance

Medium Required: Fluids (liquids and gases)

Particle Movement: Particles move from one place to another

Example: Hot air rises, cool air sinks (room heating)

Radiation

Mechanism: Transfer by electromagnetic waves

Medium Required: No medium needed (works in vacuum)

Particle Movement: No particle movement involved

Example: Heat from Sun reaching Earth

9.1 Conduction

Conduction is the transfer of heat through a material without any net movement of the material itself. It occurs when faster-moving particles collide with slower-moving particles, transferring kinetic energy.

How Conduction Works

  • Heat is applied to one end of the material
  • Particles at the heated end gain kinetic energy and vibrate faster
  • These particles collide with neighboring particles, transferring energy
  • The process continues throughout the material
  • No overall movement of material occurs
Hot → Warm → Cool → Cold
Heat flows from hot to cold regions
Example: Cooking Utensils

Metal cooking utensils have metal handles that conduct heat:

  • Problem: Handle gets too hot to hold
  • Solution: Use wooden or plastic handles (poor conductors)
  • Principle: Metals are good conductors, wood/plastic are insulators

9.2 Convection

Convection is the transfer of heat by the actual movement of the heated substance (fluid - liquid or gas). It involves bulk movement of molecules from one place to another.

Convection Currents

  1. Fluid near heat source gets heated
  2. Heated fluid expands, becomes less dense
  3. Less dense fluid rises
  4. Cooler, denser fluid sinks to replace it
  5. Creates a continuous circulation called convection current
Convection current cycle
Example: Sea Breeze and Land Breeze

Sea Breeze (Daytime)

  • Land heats up faster than sea during day
  • Air above land gets hot, rises
  • Cooler air from sea moves towards land
  • Breeze blows from sea to land

Land Breeze (Nighttime)

  • Land cools faster than sea at night
  • Air above sea is warmer, rises
  • Cooler air from land moves towards sea
  • Breeze blows from land to sea

9.3 Radiation

Radiation is the transfer of heat by electromagnetic waves, primarily infrared radiation. Unlike conduction and convection, radiation doesn't require any medium and can travel through vacuum.

Characteristics of Heat Radiation

  • Travels at speed of light (3 × 10⁸ m/s in vacuum)
  • Doesn't require any medium (works in space)
  • Can be reflected, absorbed, or transmitted
  • All objects above absolute zero emit thermal radiation
  • Amount of radiation depends on temperature (Stefan-Boltzmann law)
  • Dark, rough surfaces are good absorbers and emitters
  • Light, shiny surfaces are poor absorbers and emitters (good reflectors)
Example: Solar Energy

The Sun's energy reaches Earth through radiation:

  • Travels 150 million km through space (vacuum)
  • Takes about 8 minutes to reach Earth
  • Heats Earth's surface, drives weather systems
  • Solar panels convert this radiation to electricity

10. Good and Bad Conductors of Heat

Materials vary greatly in their ability to conduct heat. This property determines whether a material is suitable for applications requiring rapid heat transfer (conductors) or heat retention (insulators).

Good Conductors

Definition: Materials that allow heat to pass through easily

Properties:

  • High thermal conductivity
  • Usually metals
  • Free electrons aid heat transfer
  • Feel cold to touch (conduct heat away from hand)

Examples:

  • Silver (best conductor)
  • Copper
  • Aluminium
  • Iron
  • Gold

Uses: Cooking utensils, heat exchangers, radiators

Bad Conductors (Insulators)

Definition: Materials that don't allow heat to pass through easily

Properties:

  • Low thermal conductivity
  • Usually non-metals
  • No free electrons
  • Feel warm to touch (don't conduct heat away)

Uses: Cooking utensils, heat exchangers, radiators

Bad Conductors (Insulators)

Definition: Materials that don't allow heat to pass through easily

Properties:

  • Low thermal conductivity
  • Usually non-metals
  • No free electrons
  • Feel warm to touch (don't conduct heat away)

Examples:

  • Wood
  • Plastic
  • Glass
  • Air (when trapped)
  • Wool, cotton
  • Rubber

Uses: Handles of utensils, thermal insulation, clothing

Experiment: Comparing Conductors

Setup: Rods of different materials (copper, iron, aluminium, wood) with wax attached at ends are heated at one end.

Observation: Wax melts at different distances from heat source:

  • Copper: Wax melts farthest (best conductor)
  • Aluminium: Next best
  • Iron: Moderate conductor
  • Wood: Wax doesn't melt far (poor conductor)

Conclusion: Different materials have different thermal conductivities.

Thermal Conductivity Values

Material Thermal Conductivity (W/mK) Rank as Conductor
Silver 429 Best
Copper 401 Very Good
Aluminium 237 Good
Iron 80 Moderate
Glass 1.0 Poor
Wood 0.1 Very Poor
Air 0.024 Excellent Insulator

11. Practical Applications of Heat Transfer

Understanding heat transfer mechanisms allows us to design systems for heating, cooling, and insulation. These principles are applied in everyday objects, buildings, and industrial processes.

Cooking Utensils

Principle: Conduction

Metal bottoms for good heat conduction; wooden/plastic handles as insulators.

Woollen Clothes

Principle: Conduction + Convection

Wool traps air (poor conductor), reducing heat loss from body in winter.

Thermos Flask

Principle: All three methods minimized

Double walls with vacuum (stops conduction/convection); silvered surfaces (reduce radiation).

Building Insulation

Principle: Conduction + Convection

Insulating materials in walls/roofs reduce heat transfer, saving energy.

Car Radiators

Principle: Conduction + Convection

Metal fins conduct heat from engine; airflow carries heat away by convection.

Refrigerators

Principle: Conduction + Convection

Insulated walls minimize heat entry; coolant circulates absorbing heat.

Solar Water Heaters

Principle: Radiation + Conduction

Black pipes absorb solar radiation; water circulates transferring heat.

Sea Breeze

Principle: Convection

Natural cooling near coasts due to differential heating of land and sea.

House Design for Thermal Comfort

Hot Climates

  • Thick walls (reduce heat conduction)
  • Light-colored exterior (reflects radiation)
  • Windows with shades (block direct sunlight)
  • Cross ventilation (promotes cooling convection)
  • Insulated roofs (reduce heat entry)

Cold Climates

  • Double-glazed windows (trap air, reduce conduction)
  • Dark-colored exterior (absorbs radiation)
  • Insulation in walls/roofs (reduce heat loss)
  • South-facing windows (maximize solar gain)
  • Minimize air leaks (reduce convective heat loss)

12. Important Points for Examination

Examination Strategy & Tips

1

Differentiate Clearly Between Heat and Temperature

  • Heat: Energy in transit, measured in joules
  • Temperature: Degree of hotness, measured in °C or K
  • Heat depends on mass; temperature doesn't
  • Use examples to illustrate difference
2

Write Formulas with Correct Units

  • Heat transfer: Q = mcΔT (Joules)
  • Latent heat: Q = mL (Joules)
  • Linear expansion: ΔL = αL₀ΔT (meters)
  • Always include units in numerical answers
  • Show formula before substitution
3

Explain Processes with Examples

  • For conduction: Metal spoon in hot liquid
  • For convection: Sea breeze/land breeze
  • For radiation: Heat from Sun
  • For expansion: Railway tracks with gaps
  • For state change: Melting of ice, boiling of water
4

Draw Neat Diagrams When Required

  • Heating curve showing state changes
  • Convection currents (sea/land breeze)
  • Thermos flask construction
  • Clinical/laboratory thermometer
  • Use labels, arrows, and proper scaling
5

Understand Practical Applications

  • Why utensils have metal bottoms but wooden handles
  • Why woollen clothes keep us warm
  • How thermos flask works
  • Why gaps are left in railway tracks
  • Why water is used as coolant

Quick Revision Checklist

  1. Difference between heat and temperature
  2. Three temperature scales and conversions
  3. Three effects of heat (temperature rise, expansion, state change)
  4. Types of expansion (linear, areal, volume) with formulas
  5. Processes of state change (melting, boiling, evaporation)
  6. Latent heat (fusion and vaporization) with formulas
  7. Specific heat capacity formula and significance
  8. Three methods of heat transfer with examples
  9. Good and bad conductors with examples
  10. Practical applications of heat transfer
  11. Anomalous expansion of water
  12. Units of all physical quantities

Common Mistakes to Avoid

  • Confusing heat and temperature
  • Thinking evaporation occurs only at boiling point
  • Forgetting that temperature remains constant during state change
  • Mixing up the three methods of heat transfer
  • Not writing units in numerical answers
  • Confusing good and bad conductors
  • Forgetting anomalous expansion of water
  • Not differentiating between evaporation and boiling

Important Formulas to Remember

Heat Transfer:

Q = m × c × ΔT

Latent Heat:

Q = m × L

Linear Expansion:

ΔL = α × L₀ × ΔT

Temperature Conversion:

K = °C + 273

Heat Capacity:

c = Q / (m × ΔT)

Volume Expansion:

ΔV = γ × V₀ × ΔT