Tuesday, 24 February 2026

Ch 13: Magnets 🧲

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Chapter 13: Magnets 🧲

A Comprehensive Guide for PSTET Paper-2 (Science)


Chapter Overview

Section | Topic | PSTET Weightage | Page No. |
|:---:|:---|::---:|:---:|
| 13.1 | Discovery of Magnets and Magnetic Materials | Medium | 2 |
| 13.2 | Types of Magnets (Natural and Artificial) | High | 6 |
| 13.3 | Poles of a Magnet and Magnetic Attraction/Repulsion | High | 10 |
| 13.4 | Finding Directions with a Magnet | Medium | 15 |
| 13.5 | Making a Magnet | Medium | 18 |
| 13.6 | Earth as a Giant Magnet | High | 23 |
Practice Zone | MCQs & Pedagogical Questions | - | 28 |


Learning Objectives 🎯

After studying this chapter, you will be able to:

  • ✅ Trace the historical discovery of magnets and identify magnetic materials

  • ✅ Differentiate between natural and artificial magnets with examples

  • ✅ Explain the concept of magnetic poles and the law of magnetic attraction/repulsion

  • ✅ Demonstrate how a magnet can be used to find directions

  • ✅ Describe various methods of making magnets (single-touch, double-touch, induction, electrical)

  • ✅ Explain the concept of Earth as a giant magnet and its importance in navigation

  • ✅ Apply pedagogical strategies to teach magnetism effectively to upper primary students


Pedagogical Link 🔗

For Teachers: This chapter directly aligns with:

  • Class 6 Science NCERT Chapter 13: "Fun with Magnets"

Teaching Tips:

  • Begin with a "Mystery Box" activity—students guess what's inside by how it attracts paper clips

  • Create a "Magnetic Materials Discovery Station" with various objects for testing

  • Use iron filings to visualize magnetic field patterns (sprinkle on paper over magnet)

  • Conduct compass-making activities using magnetized needles and water

  • Connect to history and geography when discussing navigation and Earth's magnetism


Section 13.1: Discovery of Magnets and Magnetic Materials 🏔️

Introduction

The story of magnets begins thousands of years ago with a curious rock that had the magical power to attract iron. This rock, called lodestone or magnetite, was humanity's first introduction to the mysterious world of magnetism .


13.1.1 The Legend of Magnes

According to ancient Greek legend, a shepherd named Magnes was tending his sheep in a region of northern Greece called Magnesia. As he walked, the iron tip of his staff and the iron nails in his sandals were pulled toward a large black rock. This rock, which attracted iron, was later named magnetite after either the shepherd or the region .

Historical Fact: Whether the story is true or not, the region of Magnesia in Greece does contain large deposits of magnetite, and the word "magnet" likely comes from this region .


13.1.2 Early Discoveries in China

The Chinese were among the first to observe and document magnetic phenomena :

PeriodDevelopment
2600-2300 BCENatural magnetic iron ore (Fe₃O₄) was first discovered
4th Century BCEA book called "Book of the Devil Valley Master" noted: "The lodestone attracts iron"
2nd Century BCEThe first magnetic compasses were made using lodestone

📝 PSTET Note: The earliest mention of a needle attracted to a lodestone appears in a Chinese text published around 80 CE .


13.1.3 Ancient Names for Magnets

Chinese Tradition: The Chinese originally called magnets "Ci Shi" (慈石)—meaning "loving stone" or "motherly stone." They believed the magnet loved iron like a mother loves her child, pulling it close .

Other Ancient Names:

  • Hercules Stone (by Greeks)

  • Iron Stone (by various cultures)


13.1.4 Understanding Magnetic Materials

A. What are Magnetic Materials?

Definition: Magnetic materials are substances that are attracted to magnets and can themselves be magnetized .

The Magnetic Elements: Only three elements are naturally magnetic at room temperature :

ElementSymbolMagnetic Property
IronFeStrongly magnetic (ferromagnetic)
NickelNiStrongly magnetic (ferromagnetic)
CobaltCoStrongly magnetic (ferromagnetic)

Other Magnetic Materials:

  • Steel (alloy of iron and carbon)

  • Alnico (alloy of aluminum, nickel, cobalt, and iron)

  • Neodymium (rare earth element used in powerful magnets)

B. Non-Magnetic Materials

Definition: Non-magnetic materials are substances that are not attracted to magnets and cannot be magnetized .

Examples of Non-Magnetic Materials:

  • Wood, plastic, rubber, glass, paper, cloth

  • Copper, aluminum, gold, silver, brass

  • Water, air, stone

🧪 Classroom Activity: Magnetic Material Hunt

StepProcedure
1Give students a magnet and a collection of various objects
2Ask them to predict which objects will be attracted
3Test each object by bringing the magnet close
4Record results in a table

Sample Recording Table:

ObjectMaterialAttracted? (Yes/No)Magnetic/Non-Magnetic
Paper clipSteelYesMagnetic
Aluminum foilAluminumNoNon-magnetic
Copper coinCopperNoNon-magnetic
Iron nailIronYesMagnetic
Plastic rulerPlasticNoNon-magnetic

13.1.5 The Mystery of Magnetism Explained

For centuries, people had no explanation for why magnets worked. Ancient Greek philosopher Thales of Miletus (6th century BCE) believed magnets possessed souls .

Modern Explanation: Magnetism is caused by the movement of electrons within atoms. In magnetic materials, tiny regions called magnetic domains align their electrons in the same direction, creating a net magnetic field .


13.1.6 Pedagogical Implications

Teaching StrategyDescriptionPSTET Focus
StorytellingTell the legend of Magnes to capture interestEngaging introduction
Historical TimelineCreate a timeline of magnet discoveriesCross-curricular (history)
Material Testing StationTest various objects to classify as magnetic/non-magneticHands-on investigation
"Magnetic or Not?" GameQuick classification activityFormative assessment

Section 13.2: Types of Magnets (Natural and Artificial) 🔧

Introduction

Magnets can be broadly classified into two main categories based on their origin: natural magnets found in the earth and artificial magnets made by humans .


13.2.1 Natural Magnets

Definition: Natural magnets are magnets that are found naturally in the earth's crust .

The Only Natural Magnet: The only naturally occurring magnetic material is magnetite (Fe₃O₄), also called lodestone .

Characteristics of Natural Magnets:

  • Irregular shape (not manufactured)

  • Relatively weak magnetic strength

  • Found in various parts of the world

  • May have been naturally magnetized by lightning strikes

📝 PSTET Note: A lodestone is a rock rich in magnetite that has become magnetized naturally .


13.2.2 Artificial Magnets

Definition: Artificial magnets are magnets made by humans from magnetic materials .

Why Artificial Magnets?

  • Can be made in any desired shape and size

  • Can be made much stronger than natural magnets

  • Can be manufactured consistently and reliably

Shapes of Artificial Magnets:

ShapeDescriptionCommon Uses
Bar Magnet 🧲Rectangular bar with poles at endsSchool laboratories, compass needles
Horse-shoe (U-shaped) MagnetBent like a horseshoeLifting heavy objects, older radios
Ring MagnetCircular ringSpeakers, motors
Cylindrical MagnetRod-shapedVarious applications
Button/Disc MagnetFlat, circularRefrigerator magnets, crafts
Magnetic NeedleThin, pointedCompasses

13.2.3 Permanent vs. Temporary Magnets

Artificial magnets can be further classified based on how long they retain their magnetism :

A. Permanent Magnets

Definition: Permanent magnets retain their magnetic properties over a long period of time .

Characteristics:

  • Made from hard magnetic materials (like steel)

  • Difficult to magnetize but retain magnetism well

  • Do not lose magnetism easily

Examples:

  • Bar magnets

  • Horse-shoe magnets

  • Alnico magnets

  • Ceramic (ferrite) magnets

  • Rare-earth magnets (neodymium, samarium-cobalt)

B. Temporary Magnets

Definition: Temporary magnets lose their magnetic properties after the magnetizing influence is removed .

Characteristics:

  • Made from soft magnetic materials (like soft iron)

  • Easy to magnetize but lose magnetism quickly

  • Act as magnets only while near a permanent magnet or in a magnetic field

Examples:

  • Iron nails attracted to a magnet become temporary magnets

  • Electromagnets (when current flows)

  • Paper clips while stuck to a magnet

Table 13.1: Permanent vs. Temporary Magnets

FeaturePermanent MagnetTemporary Magnet
MaterialHard magnetic materials (steel)Soft magnetic materials (iron)
RetentionRetains magnetism for long timeLoses magnetism quickly
MagnetizationDifficult to magnetizeEasy to magnetize
DemagnetizationResists demagnetizationEasily demagnetized
ExamplesBar magnet, horse-shoe magnetIron nail, paper clip on magnet

13.2.4 Modern Artificial Magnets by Composition

Since the 20th century, scientists have developed various types of artificial magnets with different properties :

TypeCompositionCharacteristicsDeveloped
Alnico MagnetsAluminum, Nickel, Cobalt, IronStrong, temperature stable, expensive1930s
Ferrite (Ceramic) MagnetsIron oxide, Strontium/BariumLow cost, corrosion-resistant, brittle1950s
Samarium-Cobalt MagnetsSamarium, CobaltVery strong, high temperature stability, very expensive1960s-70s
Neodymium MagnetsNeodymium, Iron, BoronExtremely strong (strongest type), can corrode1980s

🌍 Did You Know? Neodymium magnets are so strong that two magnets can shatter if they snap together from a distance!


13.2.5 Pedagogical Implications

Teaching StrategyDescriptionPSTET Focus
Magnet CollectionShow different shapes of magnets to studentsVisual recognition
Compare and ContrastCompare permanent vs. temporary magnetsAnalytical thinking
Temporary Magnet DemoShow how an iron nail can pick up paper clips only when touching a magnetHands-on demonstration
Sorting ActivitySort given magnets into categoriesClassification skills

Section 13.3: Poles of a Magnet and Magnetic Attraction/Repulsion 🔄

Introduction

Every magnet, regardless of its shape or size, has two special points where its magnetic force is strongest. These points are called poles. Understanding poles and how they interact is fundamental to understanding magnetism .


13.3.1 What are Magnetic Poles?

Definition: Magnetic poles are the regions in a magnet where the magnetic force is strongest .

Characteristics of Poles:

  • They occur in pairs—every magnet has two poles

  • The poles are of equal strength

  • They are usually located near the ends of a magnet

Visual Demonstration: If you dip a bar magnet in iron filings, you'll see the filings cluster most thickly at the ends—showing where the poles are located .


13.3.2 Naming the Poles: North and South

The poles are named based on how the magnet behaves when freely suspended :

PoleFull NameBehavior When Suspended
North Pole (N)North-seeking polePoints toward geographic north
South Pole (S)South-seeking polePoints toward geographic south

Important Convention:

  • The end that points north is called the North Pole of the magnet

  • The end that points south is called the South Pole of the magnet

📝 PSTET Note: This naming convention comes from navigational use—the pole that seeks north is called the north pole .


13.3.3 The Law of Magnetic Poles

Fundamental Law: Like poles repel each other; unlike poles attract each other .

Table 13.2: Magnetic Pole Interactions

InteractionResultWhy?
N + NRepelLike poles
S + SRepelLike poles
N + SAttractUnlike poles

Simple Demonstration:

StepActionObservation
1Take two bar magnets marked N and S-
2Bring two N poles close togetherThey push apart (repel)
3Bring two S poles close togetherThey push apart (repel)
4Bring N pole near S poleThey pull together (attract)

13.3.4 The Most Important Fact: Poles Always Come in Pairs

Key Principle: If you break a magnet into pieces, each piece becomes a complete magnet with both a north and a south pole .

Demonstration:

text
Original Bar Magnet:
    [ N ========= S ]
         ↓ (break)
    [ N = S ]  [ N = S ]

Why This Happens:

  • Magnets are made of tiny molecular magnets (domains) aligned in the same direction

  • Each tiny magnet has both N and S poles

  • Breaking the magnet doesn't destroy these tiny magnets—they just rearrange slightly

📝 PSTET Note: This is a key difference between magnetic poles and electric charges. Electric charges (positive and negative) can exist separately, but magnetic poles always come in pairs .


13.3.5 Magnetic Field and Field Lines

Definition: The magnetic field is the region around a magnet where its magnetic force can be detected .

Properties of Magnetic Field Lines:

PropertyDescription
DirectionOutside the magnet, field lines go from N pole to S pole
Inside the magnetField lines continue from S pole to N pole (forming closed loops)
Strength indicationCloser lines = stronger field; spread lines = weaker field
Never crossField lines never intersect each other

Visualizing Magnetic Field:

MethodProcedure
Iron Filings MethodPlace paper over magnet, sprinkle iron filings, tap gently—filings align along field lines
Compass MethodPlace small compasses around magnet—needles point along field lines

Field Patterns for Different Situations:

SituationField Pattern
Single bar magnetCurved lines from N to S, concentrated at poles
Two like poles facing (N-N)Field lines push apart, showing repulsion
Two unlike poles facing (N-S)Field lines connect, showing attraction

13.3.6 Testing if an Object is a Magnet

The Sure Test: Repulsion is the only sure test of magnetism .

Why Repulsion is the Only Sure Test:

TestResult with MagnetResult with Magnetic Material
Bring N pole nearIf N of unknown, repels; if S of unknown, attractsAlways attracts (no repulsion)
Bring S pole nearIf S of unknown, repels; if N of unknown, attractsAlways attracts (no repulsion)

Conclusion:

  • If an object repels a known pole, it must be a magnet

  • Attraction alone is not proof (magnets attract magnetic materials)


13.3.7 Pedagogical Implications

Teaching StrategyDescriptionPSTET Focus
Pole IdentificationStudents find N and S poles using suspended magnetHands-on learning
Magnetic Field VisualizationSprinkle iron filings on paper over magnetVisual learning
"Magnet or Not?" ChallengeTest objects using repulsion testCritical thinking
Breaking a Magnet DemoShow (or describe) what happens when magnet breaksConceptual understanding

Section 13.4: Finding Directions with a Magnet 🧭

Introduction

One of the most important uses of magnets throughout history has been for navigation. A freely suspended magnet always aligns itself in a north-south direction, making it a simple but effective compass .


13.4.1 How a Magnet Finds Direction

Principle: When a magnet is free to rotate (suspended by a thread or floated on water), it comes to rest with its north pole pointing toward the geographic north of the Earth .

Why This Happens:

  • The Earth itself behaves like a giant magnet

  • It has its own magnetic poles

  • The north pole of a magnet is attracted to the Earth's magnetic south pole (located near geographic north)

📝 PSTET Note: This is a common point of confusion—the Earth's magnetic pole near geographic north is actually a south-seeking pole because it attracts the north pole of a compass needle .


13.4.2 The Magnetic Compass

Definition: A magnetic compass is an instrument that uses a magnetized steel bar to indicate direction relative to the Earth's magnetic poles .

Parts of a Simple Compass:

PartFunction
Magnetic NeedleFreely rotating magnet (usually marked N at one end)
PivotAllows needle to rotate with minimal friction
Compass CardMarked with directions (N, S, E, W)
HousingProtective case, often transparent

13.4.3 Making a Simple Compass

Activity 13.1: Making a Floating Compass

StepProcedure
1Magnetize a sewing needle by stroking it with a magnet (50 times in one direction)
2Push the magnetized needle through a small piece of cork or foam
3Fill a shallow dish with water
4Float the cork with needle on the water surface
5Observe which direction the needle points

Observation: The needle will rotate and come to rest pointing approximately north-south.

Why It Works:

  • The floating setup allows free rotation with minimal friction

  • The Earth's magnetic field exerts torque on the magnetized needle

  • The needle aligns with the field lines


13.4.4 Finding All Directions

Once you know north, you can find all other directions :

If you face...Behind you is...Left is...Right is...
NorthSouthWestEast
SouthNorthEastWest
EastWestNorthSouth
WestEastSouthNorth

Simple Rule: North → South opposite; East → West opposite.


13.4.5 History of Magnetic Compass

PeriodDevelopment 
2300+ years agoChinese made first compass—lodestone spoon on bronze plate (south-pointing spoon)
~1000 CEChinese used magnetized iron needles for navigation
1100sCompass technology spread to Europe and Arabia
1405-1433Zheng He used compass for ocean voyages
1488-1521Columbus, da Gama, Magellan used compass for exploration

🌍 Did You Know? The magnetic compass is considered one of China's Four Great Inventions.


13.4.6 Limitations of Magnetic Compass

LimitationExplanation
Magnetic declinationMagnetic north and true north are not the same; varies by location
Local interferenceNearby iron/steel objects can affect readings
Can't use near magnetic polesCompass becomes unreliable near magnetic poles
Not accurate on shipsShip's metal affects compass (corrected with special adjustments)

13.4.7 Pedagogical Implications

Teaching StrategyDescriptionPSTET Focus
Make Your Own CompassStudents make floating compassesHands-on learning
Compass Treasure HuntHide treasure; give directions using compassEngaging application
Historical ConnectionDiscuss role of compass in explorationCross-curricular
Compare DirectionsUse compass to find directions in schoolReal-world application

Section 13.5: Making a Magnet 🔨

Introduction

Magnets can be made from magnetic materials using various methods. These methods work by aligning the tiny magnetic domains within the material in the same direction .


13.5.1 The Molecular Theory of Magnetism

Weber's Theory (Molecular Magnet Theory):

  • Every magnetic material is composed of tiny molecular magnets 

  • In unmagnetized material, these molecular magnets point in random directions—their magnetic effects cancel out

  • In magnetized material, the molecular magnets align with their north poles pointing in the same direction

  • This alignment creates a net magnetic field 

Visual Representation:

text
Unmagnetized:   ↑ ↓ → ← ↙ ↗ ↘ ↖  (random)
Magnetized:      ↑ ↑ ↑ ↑ ↑ ↑ ↑ ↑  (aligned)

13.5.2 Methods of Making Magnets

There are three main methods to make magnets :

A. Single-Touch Method

Procedure:

StepAction
1Place the iron/steel bar to be magnetized on a table
2Take a strong bar magnet
3Place one pole (say N) at one end of the bar
4Stroke firmly along the bar to the other end
5Lift the magnet well away from the bar
6Repeat 30-50 times, always stroking in the same direction

Important Rules:

  • Always stroke in the same direction (never back and forth)

  • Lift the magnet away after each stroke before starting again

  • The end where the stroke ends gets opposite polarity to the stroking pole

Result: The bar becomes magnetized.

B. Double-Touch Method

Procedure:

StepAction
1Place the bar to be magnetized on a table
2Take two bar magnets
3Place opposite poles of the two magnets together at the center of the bar
4Draw them apart toward opposite ends simultaneously
5Lift both magnets well away
6Repeat several times

Advantage: This method produces stronger magnetization than single-touch method.

C. Induction Method

Procedure:

StepAction
1Place the iron/steel bar in contact with a strong permanent magnet
2Leave it in contact for some time
3Remove it and test

Explanation: When a magnetic material touches a magnet, some of the magnetic domains align, making the material a temporary magnet .

Example: An iron nail stuck to a magnet can pick up other paper clips—it has become magnetized by induction.

D. Electrical Method (Using Electricity)

Procedure:

StepAction 
1Take a long insulated copper wire
2Wind it around the object to be magnetized (e.g., iron rod) forming a coil (solenoid)
3Connect the ends of the wire to a battery (DC source)
4Pass current for some time
5Switch off and test

Result: The object becomes magnetized.

Advantages of Electrical Method:

  • Can produce very strong magnets

  • Magnetic polarity can be reversed by reversing current

  • Magnetism can be controlled by current


13.5.3 Which Materials Make Good Magnets?

For Permanent Magnets:

  • Use hard magnetic materials like steel

  • Hard to magnetize but retain magnetism

  • Example: Steel knife blade

For Temporary Magnets:

  • Use soft magnetic materials like soft iron

  • Easy to magnetize but lose magnetism quickly

  • Example: Electromagnet cores


13.5.4 Demagnetization

Magnets can lose their magnetism through :

CauseExplanation
HeatingHeating above Curie temperature randomizes domains
Hammering/DroppingPhysical shock disrupts domain alignment
Strong opposing fieldExternal field can reverse/randomize domains
TimeVery old magnets may weaken (especially steel magnets)

Storage of Magnets:

  • Store with keepers (soft iron pieces across poles)

  • Keep unlike poles together when storing multiple magnets

  • Avoid dropping or heating magnets


13.5.5 The Curie Temperature

Definition: The Curie temperature (or Curie point) is the temperature above which a magnetic material loses its magnetism .

MaterialCurie Temperature (approximate)
Iron770°C (1390°F)
Nickel358°C
Cobalt1130°C

What Happens: Above the Curie temperature, thermal energy overcomes the forces keeping domains aligned—domains become random and material becomes non-magnetic .


13.5.6 Pedagogical Implications

Teaching StrategyDescriptionPSTET Focus
Make a Magnet ActivityStudents make magnets using stroking methodHands-on learning
Induction DemonstrationShow paper clips hanging from magnetized nailVisual learning
Compare MethodsCompare strength of magnets made by different methodsScientific investigation
Domain ModelUse students as "magnetic domains" to demonstrate alignmentKinesthetic learning

Section 13.6: Earth as a Giant Magnet 🌍

Introduction

The Earth itself behaves like a giant magnet, with a magnetic field extending far into space. This is why compasses work—the Earth's magnetic field exerts a force on magnetized needles, causing them to align in a north-south direction .


13.6.1 Evidence that Earth is a Magnet

EvidenceExplanation
Compass behaviorFreely suspended magnets align north-south everywhere on Earth
AurorasCharged particles from Sun follow Earth's magnetic field to poles, creating auroras
Magnetic rocksAncient rocks preserve record of Earth's magnetic field
Magnetic surveysInstruments detect variations in Earth's magnetic field

13.6.2 Earth's Magnetic Poles

Important Fact: Earth's magnetic poles are NOT the same as its geographic poles .

TypeLocationDescription
Geographic North PoleNorthern axis pointTrue north; axis of rotation
Geographic South PoleSouthern axis pointTrue south
Magnetic North PoleNorthern Canada (currently)Where field lines point vertically down; moves slowly
Magnetic South PoleOff coast of AntarcticaWhere field lines point vertically up; moves slowly

Current Locations:

  • Magnetic North Pole: ~86°N, 175°W (in Arctic Canada; moving toward Russia)

  • Magnetic South Pole: ~64°S, 136°E (off coast of Antarctica)


13.6.3 The Magnetic Pole Confusion

The Key Point: The north pole of a compass needle points toward the Earth's magnetic pole located in the Arctic. But this means that the magnetic pole near the geographic north pole must be a south-seeking pole magnetically !

Table 13.3: Earth's Magnetic Poles Explained

LocationGeographic NameMagnetic PolarityAttracts
Near Geographic NorthNorth PoleSouth magnetic poleNorth pole of compass
Near Geographic SouthSouth PoleNorth magnetic poleSouth pole of compass

Simple Memory Aid:

  • Opposites attract: N pole of magnet points to Earth's magnetic S pole

  • Earth's magnetic S pole is near geographic N pole


13.6.4 Magnetic Declination

Definition: Magnetic declination is the angle between geographic north (true north) and magnetic north at a given location .

Why Declination Matters:

  • Compasses point to magnetic north, not true north

  • Navigators must adjust for declination to find true north

  • Declination varies by location and changes over time

Declination in India:

  • Varies from about 0° to 3° east depending on location

  • Relatively small compared to high-latitude regions


13.6.5 Earth's Magnetic Field

Characteristics of Earth's Magnetic Field :

FeatureDescription
ShapeSimilar to field of a giant bar magnet inside Earth
StrengthAbout 0.25 to 0.65 Gauss (25-65 μT)
SourceMotion of molten iron in Earth's outer core (dynamo effect)
ProtectionDeflects solar wind, protects atmosphere
VariationChanges over time; reverses polarity every few hundred thousand years

The Magnetosphere: The region of space dominated by Earth's magnetic field. It extends tens of thousands of kilometers into space and protects us from harmful solar radiation .


13.6.6 Magnetic Reversals

Fact: Earth's magnetic field has reversed polarity hundreds of times throughout history .

What Happens During a Reversal:

  • Magnetic north becomes magnetic south, and vice versa

  • The field weakens during reversal but doesn't disappear completely

  • Reversals take thousands of years

  • Last reversal was about 780,000 years ago

Evidence: Magnetic minerals in volcanic rocks record the direction of Earth's field at the time they cooled.


13.6.7 Why Is Earth Magnetic?

The Dynamo Theory:

  • Earth's core consists of molten iron and nickel

  • This liquid metal circulates due to heat from the inner core

  • The motion of electrically conductive fluid in presence of Earth's rotation creates electric currents

  • These electric currents generate magnetic field

  • This self-sustaining process is called the geodynamo 


13.6.8 Planets and Their Magnetic Fields

PlanetMagnetic FieldReason
EarthStrongLiquid iron core, rapid rotation
JupiterVery strongMetallic hydrogen, rapid rotation
MarsWeak, localizedSmall, mostly solid core
VenusVery weakSlow rotation, possibly solid core
MercuryWeak but presentPartially liquid core

13.6.9 Pedagogical Implications

Teaching StrategyDescriptionPSTET Focus
Globe DemonstrationShow geographic vs. magnetic poles on globeVisual learning
Compass Around WorldDiscuss how compass behaves in different locationsCritical thinking
Magnetic Declination ActivityFind declination for your location using online resourcesReal-world application
Aurora VideosShow videos of auroras; explain connection to Earth's magnetic fieldEngaging visual

Chapter Summary: Key Points for Revision 📝

Quick Revision Table

TopicKey PointsCommon PSTET Questions
DiscoveryMagnetite (Fe₃O₄) found in Magnesia, Greece; Chinese called it "loving stone"Who discovered magnets?
Magnetic MaterialsIron, nickel, cobalt, steel; non-magnetic: wood, plastic, copper, aluminumGive examples of magnetic/non-magnetic materials
Natural MagnetsFound in nature (lodestone/magnetite); irregular shape, weakWhat is a natural magnet?
Artificial MagnetsMade by humans; various shapes (bar, horseshoe, ring)Name different magnet shapes
Permanent MagnetsRetain magnetism; made of steel/hard materialsExamples of permanent magnets
Temporary MagnetsLose magnetism quickly; made of soft ironWhat is a temporary magnet?
Magnetic PolesN and S poles; like poles repel, unlike attractState law of magnetic poles
Breaking MagnetsEach piece becomes complete magnet with both polesWhat happens when you break a magnet?
Finding DirectionsFreely suspended magnet points N-S; used in compassHow does a compass work?
Making MagnetsSingle-touch, double-touch, induction, electrical methodsDescribe single-touch method
Earth as MagnetEarth has magnetic field; magnetic poles near geographic polesWhy does a compass point north?
Magnetic DeclinationAngle between true north and magnetic northWhat is magnetic declination?

Practice Zone: PSTET-Style Questions 🎯

Content-Based MCQs

Q1. The only naturally occurring magnetic material is:
a) Iron
b) Nickel
c) Magnetite
d) Cobalt

Q2. Which of the following is a non-magnetic material?
a) Iron nail
b) Steel spoon
c) Copper coin
d) Nickel coin

Q3. When a magnet is freely suspended, it comes to rest pointing in which direction?
a) East-West
b) North-South
c) Random direction
d) Depends on magnet size

Q4. Like poles of two magnets:
a) Attract each other
b) Repel each other
c) Have no effect
d) Sometimes attract, sometimes repel

Q5. If you break a bar magnet into two pieces, you will get:
a) One piece with N pole only, other with S pole only
b) Two pieces with no magnetism
c) Two complete magnets, each with N and S poles
d) One piece with stronger magnetism

Q6. The sure test of magnetism is:
a) Attraction
b) Repulsion
c) Color
d) Weight

Q7. Earth's magnetic field is generated by:
a) Solar wind
b) Molten iron in outer core
c) Ocean currents
d) Atmospheric pressure

Q8. The north pole of a compass needle points toward:
a) Geographic North Pole
b) Magnetic North Pole (which is magnetically south)
c) Geographic South Pole
d) Magnetic South Pole

Q9. Which method of making magnets uses electricity?
a) Single-touch method
b) Double-touch method
c) Induction method
d) Electrical method (solenoid)

Q10. Heating a magnet above its Curie temperature causes it to:
a) Become stronger
b) Become permanently magnetized
c) Lose its magnetism
d) Reverse its poles


Pedagogical MCQs

Q11. A teacher wants to demonstrate that like poles repel. The best activity would be:
a) Show a diagram in textbook
b) Bring two bar magnets and let students bring like poles together to feel repulsion
c) Lecture about it
d) Show a video only

Q12. To introduce the topic of magnets to Class 6 students, the most engaging approach would be:
a) Start with definition and properties
b) Give students magnets and various objects to explore freely first
c) Write notes on board
d) Show pictures of magnets

Q13. A student asks, "Why does a compass always point north?" The teacher should explain using:
a) "That's how it's made"
b) Earth behaves like a giant magnet, and compass aligns with Earth's magnetic field
c) "I don't know"
d) "It's magic"

Q14. While teaching magnetic materials, the most effective approach is:
a) List all magnetic materials for students to memorize
b) Provide various objects and let students test which are attracted to magnets
c) Only use textbook examples
d) Show pictures of magnetic materials

Q15. A teacher demonstrates breaking a chocolate bar into pieces and explains that magnets behave similarly. This is an example of:
a) Rote learning
b) Analogy method
c) Lecture method
d) Textbook method


Answer Key with Explanations

Q.No.AnswerExplanation
1c) MagnetiteMagnetite (Fe₃O₄) is the only naturally occurring magnetic material (lodestone) 
2c) Copper coinCopper is non-magnetic; iron, steel, nickel are magnetic
3b) North-SouthFreely suspended magnet aligns with Earth's magnetic field 
4b) Repel each otherLike poles repel; unlike poles attract 
5c) Two complete magnetsMagnetic poles always occur in pairs; each piece becomes complete magnet 
6b) RepulsionAttraction can happen with magnetic materials too; only repulsion proves it's a magnet 
7b) Molten iron in outer coreEarth's magnetic field is generated by dynamo effect in outer core 
8b) Magnetic North Pole (magnetically south)Opposites attract—N pole attracted to Earth's magnetic S pole near geographic N 
9d) Electrical methodElectrical method uses current in coil to magnetize 
10c) Lose its magnetismCurie temperature is where thermal energy randomizes domains 
11b) Hands-on activityDirect experience is most effective for this concept
12b) Free explorationDiscovery learning engages curiosity
13b) Scientific explanationCorrect explanation builds understanding
14b) Hands-on testingStudents learn by doing and discovering
15b) Analogy methodUsing analogy makes abstract concept concrete

Pedagogical Reflection for Teachers 🤔

Think-Pair-Share Activity:

  1. Think: How would you explain to students why the north pole of a compass points north, even though opposite poles attract?

  2. Pair: Discuss with a colleague how you would set up a "Magnetism Discovery Center" with activities for each section of this chapter.

  3. Share: Design a 15-minute activity to teach the difference between magnetic and non-magnetic materials using everyday objects.


NCERT Textbook Linkages 📚

ClassChapterTopic
Class 6Chapter 13Fun with Magnets
Class 10Chapter 13Magnetic Effects of Electric Current
Class 12Chapter 5Magnetism and Matter

Chapter End Notes

Key Terminology Glossary

TermDefinition
MagnetObject that attracts iron and materials containing iron, nickel, or cobalt
Magnetic materialsMaterials attracted to magnets (iron, nickel, cobalt, steel)
Non-magnetic materialsMaterials not attracted to magnets (wood, plastic, copper, aluminum)
Natural magnetMagnet found in nature (lodestone/magnetite)
Artificial magnetMagnet made by humans
Permanent magnetMagnet that retains magnetism for long time
Temporary magnetMagnet that loses magnetism quickly
Magnetic poleRegion where magnetic force is strongest
North pole (N)End of magnet that points north when freely suspended
South pole (S)End of magnet that points south when freely suspended
Magnetic fieldRegion around magnet where magnetic force acts
Magnetic compassInstrument using magnetized needle to find direction
Magnetic declinationAngle between true north and magnetic north
Curie temperatureTemperature above which material loses magnetism

Quick Tips for PSTET Aspirants ⚡

✅ Memorize with Mnemonics:

  • Magnetic Elements: "Iron Never Comes" = Iron, Nickel, Cobalt

  • Pole Rule: "Like Leave, Unlike Unite" = Like repel, Unlike attract

  • Earth's Magnetic Poles: "North Seeks South" = Compass N points to Earth's magnetic S pole (near geographic N)

  • Magnet Making Methods: "Stroke Double Induce Electric" = Single-touch, Double-touch, Induction, Electrical

✅ Common Exam Traps:

  • Magnetite is the ONLY natural magnet—iron, nickel, cobalt are magnetic but not naturally occurring as magnets

  • Repulsion is the ONLY sure test—attraction can happen with magnetic materials

  • Broken magnets become COMPLETE magnets—never isolated poles

  • Earth's magnetic N pole is actually a SOUTH pole magnetically—this confuses many students

  • Geographic poles ≠ Magnetic poles—they are at different locations

✅ Important Facts:

  • Lodestone = magnetite (Fe₃O₄)

  • Curie temperature of iron: 770°C

  • Magnetic field strength: Earth ~0.5 Gauss; small bar magnet ~100 Gauss; neodymium magnet ~12,000 Gauss

  • Compass invented: China, ~1000 CE

  • Magnetic poles always in pairs

  • Last magnetic reversal: ~780,000 years ago


Answers to "Check Your Understanding"

[To be filled by student]


📝 Note for Self-Study: After completing this chapter, ensure you can:

  • Tell the story of how magnets were discovered

  • List 5 magnetic and 5 non-magnetic materials

  • Differentiate between natural and artificial magnets with examples

  • Explain the law of magnetic poles and demonstrate with examples

  • Describe what happens when you break a magnet

  • Explain how a compass works and how Earth's magnetism causes it

  • Describe three methods of making magnets

  • Explain the difference between permanent and temporary magnets

  • Describe Earth's magnetic field and its characteristics