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^Neutral points

^Neutral points

Neutral points are the positions where the magnetic field of a magnet is completely neutralised by the horizontal component of earth’s magnetic field. The position & number of neutral points depends upon the position of magnet.

If a magnet is placed vertically as shown then we get only one neutral point situated at point L at left side of magnet if magnet’s north is down. On reversing the magnet neutral point will be at right side of magnet at point R.

Consider a magnet of dipole moment M, length 2L placed horizontally. Following drawings show the top view of the situation

 Horizontal component of earth’s field is towards . When the magnet’s north (n) is towards earth’s south (S), then magnetic field of the magnet will be towards opposite to that of BH & both get cancelled at a point somewhere on the axial line of magnet & thus two neutral points (shown by cross marks) are obtained on the axial line (i.e. towards geographic north south line). If neutral points are situated at distance r from the centre of the magnet then at these points we can write

On reversing the magnet i.e. when magnet’s north (n) is towards earth’s north (N), two neutral points are obtained on the equatorial line (i.e. towards east – west line). At these points we can write

 

^Cause of earth’s magnetism

^Cause of earth’s magnetism

1. Gilbert suggested that the earth itself behaves like a giant magnet. The earth’s core is known to contain iron. Yet geologists do not regard this as a source of earth’s magnetism. As the molten iron is not ferromagnetic.

2. Due to Ionization of gases of atmosphere layer of charge particles called ionosphere is formed, which rotates with the rotation of the earth & hence produces magnetism.

Dynamo theory: Rotation of conducting ions of ferromagnetic materials like Fe & Ni in molten state produce current loops & hence magnetism is produced. Although the details of the dynamo effect are not known in detail, at present the dynamo theory seems to be most probable, because our moon which has no molten core, has no magnetism.

^Retentivity (ob) :

The value of I even when the H is reduced to zero.

^Hysteresis

Hysteresis

Hysteresis is the lag of intensity of magnitisation (I) behind the magnetising field (H) is called hystersis.

^Ferromagnetism

Ferromagnetism

The existence of domains leads to strongest magnetism in ferromagnetics. Due to the presence of cohesive forces in ferromagnetics the unpaired electron spins to line up parallel with each other in a region called a domain. A ferromagnetic domain is a region of crystalline matter whose volume may be between 10–12 m3 to 10–8 m3. Each domain contains about 1017 – 1021 atoms. The various atomic magnets are aligned in the same direction in a domain even in the absence of external magnetising field but different domains have magnetic moments in different directions such that within the domain, the magnetic field is intense, but in a bulk sample the material will usually be unmagnetized because the many domains will themselves be randomly oriented with respect to one another. When a ferromagnetic material is kept in external magnetising field, its domain experience force and torque which tends to align them along a definite direction, till magnetic saturation. This is called Magnetostriction effect.  The extent of alignment is found to depends directly upon the intensity of the magnetising field & inversaly upon the temperature of the material.

^Hall effect

Hall effect

Is the phenomena of production of transverse emf in a current carrying strip of metal or a semiconductor when it is placed in a region of uniform magnetic field acting at right angles to current. It can be used to, calculate drift velocity of charge carriers, number density of charge carriers & nature of charge carriers.

^Arbitrary current carrying conductor

Arbitrary current carrying conductor

Magnetic field at point P around a conductor of arbitrary shape

Here  is called current element.

*Quantities having same dimensions

*Quantities having same dimensions

Momentum, impulse. [MLT – 1]
Surface tension, spring constant. [MT – 2]
Latent heat, gravitational potential. [L2  T – 2]
Gravity, gravitational field intensity. [LT – 2]
Angular momentum, Planck’s constant. [ML2  T – 1]
Solar constant, pointing vector & wave intensity. [MT – 3]
Frequency, angular frequency, velocity gradient, decay constant. [T – 1]
Thermal capacity, gas constant, Boltzmann constant and entropy. [ML2 T – 2 K – 1]
Length, breadth, height, distance, displacement, radius of gyration & wavelength. [L]
Work, torque (or moment of force), Energy of any kind e.g. internal, potential, kinetic, heat etc. [ML2 T – 2]
Pressure, stress, elasticity of any kind e.g., Young’s, bulk’s, modulus of rigidity, energy density. [MLT – 2]
Strain, refractive index, relative density, angle, solid angle, dielectric constant, relative permeability. [M0 L0  T0]
Energy gradient, force of any kind e.g. gravitational (weight), EM (upthrust, friction) nuclear etc. [MLT – 2]
Momentum, impulse. [MLT – 1]
Surface tension, spring constant. [MT – 2]

^At balanced state

At balanced state

1. current in the galvanometer arm Ig is zero and

2. current flowing in the mesh ABCD is

3. Potential drop across AB is V = IRp

4. Potential gradient K = V/L

5. As ξA is balanced against the potential drop of  length AN, thus

6. ξA ∝ b is called the principle of potentiometer.

7. To get the null point within the length of the  potentiometer ξD > ξA

Greater the length of the potentiometer wire (L), smaller is the potential gradient (k) & more is the balancing length (b), hence more is the accuracy. ‘k’ is independent of the emf of auxillary cell (ξA) but depends upon emf of driver cell (ξD), its internal resistance (rD), resistance of potentiometer wire (AB) & any resistance (R) in the main circuit. 

^Description of motion 

^Description of motion 

Three parameters used to describe the motion of a body are; position, velocity & acceleration. Usually a reference point plus a clock is used to describe motion of an object.

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