Earth's Magnetic Field: Cause, Theory & Components

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The Earth's magnetic field is the magnetic field that extends from the inside of the Earth into space, where it interacts with the solar wind, a stream of charged particles emitted by the Sun.

  • It is also known as the Geomagnetic field.
  • The magnetic field is created by electric currents induced by the movements of convection currents of molten iron and nickel in Earth's outer core.
  • These convection currents are caused by heat escaping from the core, which is a natural phenomenon known as a geodynamo.
  • At the surface, the magnitude of the Earth's magnetic field ranges from 25 to 65 T (0.25 to 0.65 G).
  • It is approximated by a magnetic dipole field that is now inclined at an angle of around 11° with regard to the Earth's rotating axis.
  • The North magnetic pole of the Earth actually represents the South pole of Earth's magnetic field, while the South geomagnetic pole is the North pole of Earth's magnetic field.

Key Terms: Earth's Magnetism, Dynamo Effect, Magnetic-field Strength, Magnet, Bar Magnet, Electric Current, Magnetic Pole


What Is Earth’s Magnetic Field?

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The Earth's magnetic field, also known as the geomagnetic field, is formed in our planet's interior and reaches into space, forming the magnetosphere.

  • Life on Earth would be impossible without the magnetic field, which protects us from the constant attack of charged particles generated by the sun known as the solar wind.
  • The Earth has two poles: the geographic pole and the magnetic pole.
  • Imagine a huge bar magnet within our planet as roughly aligned with the Earth's axis, to represent the magnetic field.
  • Each end of the magnet is quite near the geographic North and South poles (approximately 11 degrees).
  • At each magnetic pole, the Earth's invisible magnetic field lines move in a closed, continuous loop and are almost vertical.
  • The Earth's magnetic field stretches millions of kilometers into space and resembles a bar magnet. The earth's magnetic pole is positioned between the Northern Pole and the North Pole's Antarctic magnets.
  • That is why a compass magnet's north pole points north (north and south poles attract). 

Read More: Magnetism and Matter Important Questions


Dynamo Effect

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It is not a clear theory of the Earth’s magnetism as to what causes the Earth to have its own magnetic field.

  • Initially, the magnetic field was visualized as a gigantic bar magnet located approximately along the axis of rotation of the earth and within its center.
  • Obviously, that was way too simple to explain away. 
  • Now, the Dynamo Effect states that the Earth’s magnetic field has emerged because of the presence of metallic fluids like molten iron and nickel in the outer core of the planet.
  • The convective motion of these fluids produces an electric current, causing the magnetic field to arise. 

Related Topics to Magnetism:


What Causes the Earth's Magnetism?

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The Earth's magnetism is generated by molten iron and nickel convection currents in the Earth's core. Charged particles in these currents generate magnetic fields.

  • The sun also releases ionizing charged particles towards the earth known as solar winds.
  • The earth’s magnetic field deflects these particles and prevents them from entering the atmosphere. 
  • Had this magnetic shield not been present, solar winds would have eroded our atmosphere rendering life inhabitable on Earth.
  • An example of this is Mars, where the absence of a magnetic field has created an atmosphere unable to sustain life. 
  • The magnetic poles and the geographical north and south poles of the Earth are not aligned with each other.
  • This means that the southern magnetic pole is in Canada, while the northern magnetic pole is in Antarctica.
  • The magnet poles have around an 11o inclination to the rotational axis.

Earth's magnetic field

Earth’s magnetic field

Read More: SI unit of Magnetic Field


Components of the Earth's Magnetic Field

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Three components determine the magnitude and direction of the Earth's magnetic fields: 

  1. Magnetic Declination
  2. Magnetic inclination (angle of dip)
  3. The horizontal component of the Earth’s magnetic field

Components of Earth’s Magnetic Field

Components of Earth’s Magnetic Field

Magnetic Declination 

The angle between the true north and the magnetic north is known as the magnetic declination. The true north is never constant; its position keeps changing based on the earth’s surface and time.

Magnetic Inclination

Also known as the angle of dip, the magnetic inclination is the angle formed by the horizontal plane on the earth’s surface. The angle of dip at the magnetic equator is 0° and 90o at the magnetic poles. 

Horizontal Component of Earth's Magnetic Field 

Two factors account for the intensity of the Earth's magnetic field: 

  • Horizontal component (H) 
  • Vertical Component (v)

vertical component

Various Components and its Definition

Component Definition Description
B The total magnetic-field strength The total magnetic-field strength
X Magnetic field component in the direction of Geographic North Magnetic field component in the direction of Geographic North
Y Component of the magnetic field in the direction of Geographic East Component of the magnetic field in the direction of Geographic East
H Component of the magnetic field that is parallel to the earth's surface (Points towards the magnetic south pole) Component of the magnetic field that is parallel to the earth's surface (Points towards the magnetic south pole)
α Magnetic declination: Angle formed between the true north and magnetic north. Magnetic declination: Angle formed between the true north and magnetic north.
θ Magnetic Inclination is a calculation of the angle between the horizontal and the magnetic field vector. At magnetic poles, the angle is 90o. Magnetic Inclination is a calculation of the angle between the horizontal and the magnetic field vector. At magnetic poles, the angle is 90o.

Solved Examples

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Ques. Calculate the vertical component of the earth’s magnetic field at the equator if the horizontal component of the earth’s magnetic field is at B and the angle of dip is 60°.

Ans. The horizontal component of the earth’s magnetic field, H = Be cos 60° = B

Be x ½ = B

Be = 2B

The vertical component of the earth’s magnetic field, V = Be sin 60°

V = 2B x √3/2

V = √3B

Ques. Calculate the angle of dip for a place whose horizontal and vertical components of the earth’s magnetic field are equal.

Ans. The angle of dip is, δ = tan-1(BV/BH)

BV is the vertical component of the Earth’s magnetic field

BH is the horizontal component of the Earth’s magnetic field

BV = BH

δ = tan-1(1) = 45° = angle of dip

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Previous Year Questions 

  1. An electron in motion is associated with… [ KCET 1996]
  2. Two parallel wires carry electric current in same direction. The wires... [ KCET 1996]
  3. Resistance of an ideal ammeter is...[ KCET 1996]
  4. If a current of 0.1 A is passed through the coil, what is the couple acting?...[CBSE Class 12 ]
  5. The acceleration of the falling magnet is..[NEET]
  6. A bar magnet is equivalent to ............[KCET 2004]
  7. A metal ring is held horizontally and bar magnet is dropped through….[NEET]
  8. The total charge, induced in a conducting loop when it is moved in magnetic field depend on...[NEET 1992]
  9. If a charge particle enters perpendicular in the uniform magnetic field, then...[JIPMER 2016]
  10. Who invented the cyclotron?
  11. When a charged particle moving with velocity is….
  12. The angle of dip at a place is….
  13. The associated magnetic moment is given by….
  14. A uniform electric field and a uniform magnetic field are produced…
  15. Ampere’s circuital law can be derived from…..
  16. If a magnetic dipole of moment M situated in the direction of …
  17. If the susceptibility of dia, para and ferro magnetic materials are ….
  18. Materials suitable for permanent magnet, must have which of the following properties ?
  19. At what temperature, the ferromagnetic substances become paramagnetic ?
  20. a magnetic induction of strength at its centre is...

Things to Remember

  • The earth’s magnetic field is also known as the Geomagnetic field.
  • The magnitude of the Earth's magnetic field ranges from 25 to 65 T (0.25 to 0.65 G).
  • The Earth has two poles: the geographic pole and the magnetic pole.
  • The North magnetic pole of the Earth represents the South pole of Earth's magnetic field, while the South geomagnetic pole is the North pole of Earth's magnetic field.
  • Dynamo Effect states that the Earth’s magnetic field has arisen because of the presence of metallic fluids like molten iron and nickel in the outer core of the planet.
  • The angle between the true north and the magnetic north is known as the magnetic declination.
  • The magnetic inclination is the angle formed by the horizontal plane on the earth’s surface.

Sample Questions

Ques. The horizontal component of the earth’s magnetic field at a place is B and the angle of dip is 60°. What is the value of the vertical component of the Earth’s magnetic field at the equator? (3 Marks)

Ans. The horizontal and vertical components of the Earth’s magnetic field are perpendicular to each other. 

The horizontal component of Earth’s magnetic field,

The horizontal component of Earth’s magnetic field,

The Vertical component of Earth’s magnetic field,

Ques. What is the angle of dip at a place where the horizontal and vertical components of the earth’s magnetic field are equal? (3 Marks)

Ans. 

What is the angle of dip at a place where the horizontal and vertical components of the earth’s magnetic field are equal

Ques. A magnetic needle free to rotate in a vertical plane parallel to the magnetic meridian has its North tip down at 60° with the horizontal. The horizontal component of the earth’s magnetic field at the place is known to be 0.4 G. Determine the magnitude of the earth’s magnetic field at the place. (3 Marks)

Ans. 

A magnetic needle free to rotate in a vertical plane parallel to the magnetic meridian has its North tip down at 60° with the horizontal. The horizontal component of the earth’s magnetic field at the place is known to be 0.4 G. Determine the magnitude of the earth’s magnetic field at the place.

Ques. A wheel with 8 metallic spokes each 50 cm long is rotated with a speed of 120 rev/min in a plane normal to the horizontal component of the each’s magnetic field. The earth’s magnetic field at the place is 0.4 G and the angle of dip is 60°. Calcu] ate the emf induced between the 3txle and the rim of wheel. How will the value of emf be affected if the number of spokes were increased? (3 Marks)

Ans. 

A wheel with 8 metallic spokes each 50 cm long is rotated with a speed of 120 rev/min in a plane normal to the horizontal component of the each’s magnetic field. The earth’s magnetic field at the place is 0.4 G and the angle of dip is 60°.

Ques. Is the world's magnetic field different in different places? (2 Marks)

Ans. Yes, the magnetic field varies depending on where you are. The magnetic field varies with both place and time. The propagation of the magnetic field is measured by satellites, around 200 active magnetic monitoring centers around the world, and many other temporary locations.

Ques. Has the earth's magnetic field shifted in recent years? (3 Marks)

Ans. The Earth's magnetic field fluctuates slowly and seems to have evolved. When tectonic plates form along oceanic ridges, the current magnetic field is impressed on the rock as it cools to around 700 degrees Celsius. The slowly shifting plates act like a tape recorder, allowing you to see the intensity and direction of previous magnetic fields. By collecting these rocks and using radiometric dating techniques, the background of the Earth's magnetic field for the past 160 million years has been reconstructed.

Ques. What do you mean by geomagnetic reversal? (3 Marks) 

Ans. A transition in a planet's magnetic field that swaps the north and south magnetic poles is known as a geomagnetic reversal (not to be confused with geographic north and geographic south). The Earth's field alternated between periods of natural polarity, in which the prevailing direction of the field was the same as the current direction, and periods of opposite polarity, in which the predominant direction of the field was the opposite of the current direction. Chronological periods are referred to as chrons.

Ques. What is the horizontal component of the Earth's magnetic field and dip-angle in a vertical plane with a magnet needle free to move? (1 Mark) 

Ans. The horizontal part of the earth's magnetic field is zero since the magnetic needle is free to spin in a vertical plane. In the dip angle, this would be 900. 

Ques. How does the Earth's magnetism work? (1 Mark)

Ans. The earth's magnetism is caused by circulating ions, which result in the creation of the current loops in the earth's center. These current loops are responsible for the creation of the magnetic field.

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CBSE CLASS XII Related Questions

  • 1.
    In his experiment on photoelectric effect, Robert A. Millikan found the slope of the cut-off voltage versus frequency of incident light plot to be \( 4.12 \times 10^{-15} \, \text{Vs} \). Calculate the value of Planck’s constant from it.


      • 2.
        An electric dipole consists of charges \(\pm 4 \mu C\) separated by a distance of \(6\,cm\). Calculate the electric field at a point on the axial line at a distance \(20\,cm\) from its center.


          • 3.
            State any three characteristics of electromagnetic waves.


              • 4.
                Two wires of the same material and the same radius have their lengths in the ratio 2:3. They are connected in parallel to a battery which supplies a current of 15 A. Find the current through the wires.


                  • 5.
                    Write vector form of Biot–Savart law.


                      • 6.
                        A 1 cm straight segment of a conductor carrying 1 A current in \( x \)-direction lies symmetrically at the origin of Cartesian coordinate system. The magnetic field due to this segment at point (1m, 1m, 0) is:

                          • \( 1.0 \times 10^{-9} \, \text{T} \)
                          • \( -1.0 \times 10^{-9} \, \text{T} \)
                          • \( \frac{5.0}{\sqrt{2}} \times 10^{-10} \, \text{T} \)
                          • \( -\frac{5.0}{\sqrt{2}} \times 10^{-10} \, \text{T} \)
                        CBSE CLASS XII Previous Year Papers

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