When considering the circular motion of electrons, the genesis of magnetism can be explained. Inside the atoms, electrons move in circular orbits around the nucleus, analogous to a circular coil conveying current. The orbital magnetic moment is created by the electron’s orbital motion. A spin magnetic moment is created when electrons spin about in their own axis. The vector sum of the orbital and spin magnetic moments gives the magnetic moment of an atom. Magnetic compounds are categorised into three classes based on their magnetic properties: diamagnetic, ferromagnetic, and paramagnetic.
When diamagnetic materials are exposed to an external magnetic field they become weakly magnetised in the opposite direction as the applied field. Diamagnetism describes the sort of magnetism exhibited by certain materials. Copper, gold, antimony, bismuth, silver, lead, silicon, mercury, and other diamagnetic materials are examples. An orbital magnetic moment is created by the electron’s orbital motion. Furthermore, electrons have a tendency to spin around their own axis, resulting in a spin magnetic moment. An atom’s electrons can spin either clockwise or counter clockwise. Electrons can also rotate around the nucleus in a clockwise or counter clockwise orientation.
The magnetic moments of atoms and orbital magnetic moments have been arranged in diamagnetic substances in such a way that the vector sum of an atom’s magnetic moment becomes zero.
Ferromagnetic substances are those that get strongly magnetised in an external magnetic field in the same direction as the applied field. Even after the magnetic field is removed, these substances retain their magnetic moment. Ferromagnetic materials gravitate from weaker to stronger regions of the external field. Iron, cobalt, and nickel are examples of ferromagnetic materials. Magnetic moments play a significant role in the spin of ferromagnetic materials. These compounds are made up of a huge number of tiny units called domains. When a ferromagnetic substance is exposed to an external magnetic field, torque occurs in these domains. The domains rotate and remain parallel to the direction as a result of this.
When placed in an external magnetic field in the same direction as the externally applied field, paramagnetic substances become weakly magnetised. These materials are distinct from ferromagnetic and diamagnetic materials. They have a proclivity for moving from the weaker to the stronger magnetic field. Calcium, lithium, tungsten, aluminium, platinum, and other paramagnetic materials are examples. Each atom in a paramagnetic substance has a permanent magnetic dipole moment that is orientated due to the way the atoms spin. When there is thermal motion, however, the direction of magnetic moments might have arbitrary orientations. As a result, this substance’s net magnetic moment is zero.
There are three types of magnets:
An electric current is generated by the movement of liquid iron at the Earth’s core, which causes magnetic fields. The magnetic field of the Earth is created deep within the planet’s core. Because charged metals moving through these fields produce electric currents, the cycle continues. The geodynamic is a self-sustaining loop of this type. The combined impact of magnetic fields creates a massive magnetic field that travels to the planet. The magnetic fields on Earth are caused by this.
When diamagnetic materials are exposed to an external magnetic field in the opposite direction as the applied field, they become weakly magnetised. Diamagnetism describes the sort of magnetism exhibited by certain materials. Ferromagnetic substances are those that get strongly magnetised in an external magnetic field in a direction that is the same as the direction of the externally applied field. Paramagnetic substances are those that become weakly magnetised when placed in an external magnetic field in the same direction as the externally applied field.