Atomic Structure of Magnets: Difference between revisions

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===A Mathematical Model===
===A Mathematical Model===


The magnetic dipole in a magnet is analogous to the magnetic dipole in a current loop.  In a current loop <math>{\mu = I \pi R^2}</math>.  Since the units of <math>I</math> are <math>\frac{charge}{time}</math> The magnetic dipole is proportional to the [[The Angular Momentum Principle|angular momentum]] of the electron orbiting the nucleus.  For example <math>{\frac{d\vec{p}}{dt}}_{system} = \vec{F}_{net}</math> where '''p''' is the momentum of the system and '''F''' is the net force from the surroundings.
The magnetic dipole in a magnet is analogous to the magnetic dipole in a current loop.  In a current loop <math>{\mu = I \pi R^2}</math>.  Since the units of <math>I</math> are <math>\frac{charge}{time}</math>, the charge of an electron is <math>-e</math>, and the period for one orbit around the nuclues is <math>t = \frac{2 \pi R}{v}</math> where <math>v</math> is the speed of the the electron, the magnetic dipole for one atom in a magnet simplifies to <math>\mu = \frac{e R v}{2}</math>. The magnetic dipole is proportional to the [[The Angular Momentum Principle|angular momentum]] of the electron orbiting the nucleus.  For example <math>{\frac{d\vec{p}}{dt}}_{system} = \vec{F}_{net}</math> where '''p''' is the momentum of the system and '''F''' is the net force from the surroundings.


===A Computational Model===
===A Computational Model===

Revision as of 23:41, 4 December 2015

Austin Bryan


Short Description of Topic

The Main Idea

The magnetic field produced by a magnet is the sum of the magnetic fields generated by each individual atom. These very small magnetic fields are generated much like those of circular current loops; however instead of being generated by electrons flowing through a wire, the field in each individual atom is produced in one three different ways:

  1. An electron orbiting around the atomic nucleus.
  2. An electron rotating around its axis.
  3. The rotation of protons and neutrons within the nucleus of the atom.

All three of these situations produce a magnetic dipole proportional to the angular momentum. Together, the magnetic dipoles of all the atoms in the magnet sum to give the total magnetic dipole of the magnet. The magnetic field at an observation location can then be found from this dipole.

Although all atoms have electrons orbiting their nuclei, most materials are not magnetic. Each atom in these materials has a small magnetic dipole, however these dipoles are unaligned and disordered and therefore usually sum to zero. In magnetic materials, regions of magnetic dipoles line up. Although some of these regions cancel other regions out, enough regions align to produce a nonzero magnet field. This is allowed by interactions between atoms in certain elements (usually iron, nickel, cobalt, or alloys of these metals).


A Mathematical Model

The magnetic dipole in a magnet is analogous to the magnetic dipole in a current loop. In a current loop [math]\displaystyle{ {\mu = I \pi R^2} }[/math]. Since the units of [math]\displaystyle{ I }[/math] are [math]\displaystyle{ \frac{charge}{time} }[/math], the charge of an electron is [math]\displaystyle{ -e }[/math], and the period for one orbit around the nuclues is [math]\displaystyle{ t = \frac{2 \pi R}{v} }[/math] where [math]\displaystyle{ v }[/math] is the speed of the the electron, the magnetic dipole for one atom in a magnet simplifies to [math]\displaystyle{ \mu = \frac{e R v}{2} }[/math]. The magnetic dipole is proportional to the angular momentum of the electron orbiting the nucleus. For example [math]\displaystyle{ {\frac{d\vec{p}}{dt}}_{system} = \vec{F}_{net} }[/math] where p is the momentum of the system and F is the net force from the surroundings.

A Computational Model

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