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Boundary Conditions in Magnetostatics

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We will consider separately component of B parallel to surface but perpendicular ... Above it is paramagnetic. phase transition. The Earth as a magnet! ... – PowerPoint PPT presentation

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Title: Boundary Conditions in Magnetostatics


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  • Boundary Conditions in Magnetostatics

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General Case
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Now our surface is 2 dimensional so we need 2
directions to describe it, just as above we had a
sheet in the x,y plane The i and j vectors are
tangential to the surface. We will consider
separately component of B parallel to surface but
perpendicular to current and component of B
parallel to surface and parallel to current
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Magnetic materials
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  • Rather than integrating over all the dipoles
  • We can deal with these bound currents.

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Ampères Law in Magnetized Materials
  • We have found that the effect of magnetization is
    to establish bound currents within the volume and
    surface currents on the surface. Suppose we have
    in addition free currents flowing in the
    material,Jf

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Microscopic Magnetism
  • Semi-classical picture
  • Electrons move in orbits around nucleus
  • Spins on its axis
  • Electrons fill up the shells of an atom
    systematically, pairs of electrons tend to have
    opposite spins

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  • The effect of spin is to give electron a
    permanent dipole moment me
  • The effect of a magnetic field is to induce a
    torque
  • Nme?B
  • The indivdual dipoles will try to line up with
    the field--paramagnetism

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  • However for atoms with an even number of
    electrons the electrons come in pairs with
    opposite dipole moments which tend to cancel
    giving a zero torque

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  • Thus if we have a material that has all its
    orbitals full, then the permanent dipole moments
    tend to cancel out in pairs but
  • the effect of the electron motion adds up,
  • so for such a material there is a tendency to
  • oppose an applied magnetic field
  • this is the origin of diamagnetism

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Transition Elements
The 3d level, 10 orbitals fills us before the 4p,
one electron goes into each orbital before the
second in each
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FeAr4s23d6
  • Lots of half filled d orbitals,
  • In the absence of a magnetic field all these
    dipoles are randomly oriented but if you apply a
    field they will line up with the field
  • Take the field away the dipoles tend to stay
    aligned---
  • Materials like iron are said to be ferromagnetic!

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  • If you take a piece of of raw unmagnetized iron
    and examine it microscopically you find there
    are small areas of the material
  • known as domains. Each domain contains a vast
    number of atoms whose dipoles are aligned.Each
    domain has an overall dipole moment. If you place
    the iron in a strong magnetic field,

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  • Eventually all the domains will be aligned
  • The iron is thensaturated
  • Take the field away and you have a permanent
    magnet

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Magnetic domains in Co
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Hysterisis
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Hysterisis
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Hysterisis Loop
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  • Random thermal motions compete with the ordering
    of the domains. In fact at a material specific
    temperature materials change their character.
  • This temperature is known as the Curie
    temperature.
  • For iron it is 7700C

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  • Below this temperature
  • The material is ferromagnetic
  • Above it is paramagnetic
  • phase transition.

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The Earth as a magnet!
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Where does the field come from
  • Could it be a giant ferromagnet?

No the earths coreisvery hot There is iron there
but temperature far exceeds the Curie temperature
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  • earths-inner-structure

volcanoes
earths-magnetic-field-video.htm
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