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^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.

^Velocity selector

Velocity selector

A beam of charged particles is passed in a region of electric & magnetic fields acting at right angles (called cross fields) with such a velocity that the electric & magnetic force balances each other & the beam of charge particles pass undeflected through the region of cross fields. i.e.

Felectric = Fmagnetic   ⇒ qE = Bqv  ⇒

 

^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.

^Ampere’s Circuital Law

Ampere’s Circuital Law

Ampere’s law is useful to find magnetic field in symmetrical situations. It states that the line integral of magnetic field for a closed plane curve is equal to ‘m 0’ times the current crossing the area bounded by the closed curve provided the electric field inside the loop remains the constant. i.e.

^Arbitrary current carrying conductor

Arbitrary current carrying conductor

Magnetic field at point P around a conductor of arbitrary shape

Here  is called current element.

^Sign of thermoelectric power

Sign of thermoelectric power

Sign of S is sign of cold side i.e., potential of cold side.  By convention, the sign of S represents the potential of the cold side with respect to the hot side. If electrons diffuse from hot to cold end, then the cold side is negative with respect to the hot side and the Seebeck coefficient is negative. In a p – type semiconductor, on the other hand, holes would diffuse from the hot to the cold end. The cold side would be positive with respect to the hot side which would make S a positive quantity.

The total voltage difference between two points where temp. are T0 ­ and T, from equation (1), is given by _ _ _ _ (2)

In practice one rarely measures the absolute thermopower of the material of interest. This is due to the fact that electrodes attached to a voltmeter must be placed onto the material in order to measure the thermoelectric voltage.

The temperature gradient then also typically induces a thermoelectric voltage across one leg of the measurement electrodes.

Therefore the measured thermopower includes a contribution from the thermopower of the material of interest and the material of the measurement electrodes. Suppose that we try to measure the voltage difference DV across the aluminium rod (heated at one end and cooled at the other end) by using aluminium connecting wires to a voltmeter as shown.

The same temperature difference, however, now also exists across the aluminium connecting wires and therefore an identical voltage also develops across the connecting wires, opposing that across the aluminium rod.

Consequently no net voltage will be registered by the voltmeter.

It is, however possible to read a net voltage difference, if the connecting wires are of different material, i.e. have a different coefficient than that of aluminium , so that across this material the thermoelectric voltage is different than that across the aluminium rod.

The voltage across each metal element depends upon on its Seebeck coefficient so that the potential difference between the two wires will depend on SA – SB. The emf between the two wires,  VAB = DVA – DVB, by virtue of eqn. (2), is then given by

Here SAB is defined as the thermoelectric power for the thermocouple pair A – B.

The Seebeck coefficients are non-linear as a function of temperature, and depend on the conductors’ absolute temperature, material, impurities, imperfections, and structural changes. If the Seebeck coefficients are effectively constant for the measured temperature range, the above formula can be approximated as:

VAB = (SA – SB)·(T – T0)

The thermopower is an important material parameter that determines the efficiency of a thermoelectric material. A larger induced thermoelectric voltage for a given temperature gradient will lead to a larger efficiency. Ideally one would want very large thermopower values since only a small amount of heat is then necessary to create a large voltage. This voltage can then be used to provide electric power.

Typically metals have small thermopowers because most have half-filled bands. Electrons (negative charges) and holes (positive charges) both contribute to the induced thermoelectric voltage thus canceling each other’s contribution to that voltage and making it small. In contrast, semiconductors can be doped (adding impurities) with an excess amount of electrons or holes and thus can have large positive or negative values of the thermopower depending on the charge of the excess carriers.

*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]
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