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CBSE Class 12th Physics Notes: Magnetism and Matter (Part ‒ II)

Dec 13, 2016 16:30 IST

    Chapter wise notes of Class 12 Physics, Magnetism & Matter are available here. This article is a continuation of the revision notes on Magnetism and Matter (Part ‒ I). In previous parts, we have studied important topics like origin of magnetism, basic properties of a magnet, properties of magnetic field lines, magnetic dipole, dipole Moment etc. In this part we will study some more topics which are given below

    The Earth’s Magnetism

    Causes of the Earth’s Magnetism

    Basic features of the Earth’s Magnetism

    Magnetic Element of the Earth’s Magnetic Field

    Magnetic Declination

    Horizontal Components of the Earth’s Magnetic Field

    Angle of dip or Magnetic inclination

    Neutral Points

    Mathematical Relation between Magnetic Elements of the Earth’s Magnetic Field

    Tangent Law: Superposition of magnetic fields

    The notes are as follows:

    The Earth’s Magnetism

    The earth behave likes a huge bar magnet. Strength of the earth’s magnetic field varies from place to place on the earth’s surface. The magnitude of the earth’s magnetic field is of the order of 10–5 T.

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    Causes of the Earth’s Magnetism

    Exact causes the earth’s magnetism is not clear yet. There are some Earth Magnetism Theory which are as follows:

    • The magnetic field of the earth is thought to arise due to electrical currents produced by convective motion of metallic fluids (consisting mostly of molten iron & nickel) in the outer core of the earth. This effect is also known as the dynamo effect.

    • In outer layers of earth’s atmosphere, various gases are in ionized state. Due to rotation of the earth about its axis, strong electric current are set up due to movement of charged ions.

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    Basic features of the Earth’s Magnetism

    Magnetic field lines of the earth resemble with a (hypothetical) giant magnetic dipole located at the centre of the earth.

    The axis of the dipole does not coincide with the axis of rotation of the earth.

    Basic features of the Earth’s Magnetism

    Image Source: NCERT Textbooks

    • The axis of the dipole is titled by approximately 11.3º with respect to the later.

    • The magnetic poles are located where the magnetic field lines due to the dipole enter or leave the earth.

    • North magnetic pole is located at a latitude of 79.74º N and a longitude of 71.8º W (in north Canada)

    • The magnetic south pole is located at 79.74º S, 108.22º E (in Antarctica)

    • The pole near the geographic north pole of the earth is called the north magnetic pole.

    • The pole near the geographic south pole of the earth is called the south magnetic pole.

    • Nomenclature of the poles is confusing and one should not get confuse. If we look at the magnetic field lines of the earth (as shown in figure given above), we observe that unlike in the case of a bar magnet, the field lines go into the earth at the north magnetic pole (Nm) and come out from the south magnetic pole (Sm).

    • The convention arose because the magnetic north was the direction to which the north pole of a magnetic needle pointed; the north pole of a magnet was so named as it was the north seeking pole.

    • The north magnetic pole behaves like the south pole of a bar magnet inside the earth and vice versa.

    Magnetic Element of the Earth’s Magnetic Field

    These are the quantities which completely describe magnitude and direction of the earth’s magnetic field at a place.

    There are three magnetic elements of the earth:

    • Magnetic Declination

    • Horizontal component of the earth’s magnetic field

    • Angle of dip or Magnetic inclination

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    Magnetic Declination:

    It is the angle between magnetic meridian and geographic meridian at a place.

    Magnetic Needle Freely Suspended in Earth's Magnetic Field

    Image Source: NCERT Textbooks

    In the figure shown above, the angle between the true geographic north and the north shown by a compass needle is called the magnetic declination or simply declination.

    The declination is greater at higher latitudes and smaller near the equator.

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    Horizontal Components of the Earth’s Magnetic Field:

    The earth’ magnetic field is nowhere horizontal except at equator. So, at any place, the earth’s magnetic field (BE) in the magnetic meridian may be resolved into a horizontal component (HE) and vertical component (ZE).

    Components of the Earth's Magnetic Field

    Image Source: NCERT Textbooks

    The horizontal component of the earth’s magnetic field is the component of the earth’s magnetic field in horizontal direction.

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    Angle of dip or Magnetic inclination

    Angle of declination at a place is the angle between the direction of the earth’s magnetic field and the horizontal in the magnetic meridian at that place.

    Neutral Points

    At certain points the field due to a bar magnet may be completely neutralized by the horizontal component of the earth’s magnetic field. These points are known as neutral points.

    Mathematical Relation between Magnetic Elements of the Earth’s Magnetic Field:

    With reference to the figures given above,

    ZE = BE sin I, HE = BE cos I which gives tan I = ZE/HE

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    Tangent Law: Superposition of magnetic fields

    If a magnetic needle is under the influence of two uniform magnetic fields B1 and B2 in mutually perpendicular directions, then, the magnetic needle will align itself along the resultant field.

    Tangent Law: Superposition of magnetic fields

    In the figure shown above, if the resultant of B1 and B2 makes an angle θ with B1, then, tan θ = |B2|/|B1|.

    CBSE Class 12th Physics Notes: Magnetism and Matter (Part ‒ I)

    DISCLAIMER: JPL and its affiliates shall have no liability for any views, thoughts and comments expressed on this article.

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