How does a
permanent magnet
work?
Some materials
have a feature
known as ferromagnetism.
The prefix
"ferro" refers
to Iron, which
is one such
material.
Ferromagnetic
materials have
the ability to
"remember" the
magnetic fields
they have been
subjected to.
An atom consists
of a number of
negatively
charged
electrons,
orbiting around
a positively
charged nucleus.
These electrons
also possess a
quantity known
as spin,
which is roughly
analogous to a
spinning top.
The combination
of orbital and
spin motions is
called the angular momentum
of the electron.
Angular momentum
is perhaps most
easily
understood in
the case of the
Earth: The earth
spins about a
central axis,
which means it
at has an
angular momentum
around that
axis. The
planets also
have an angular
momentum as they
revolve about
the sun.
Now, the angular
momentum of an
electron is a
vector quantity,
meaning it has
direction. The
motion of the
electron
produces a
current, which
in turn
generates a tiny
magnetic field
in the direction
given by the
angular
momentum. Thus
an atom can
behave like a dipole,
meaning "two
poles". The
direction of the
orbital and spin
angular momentum
of the electron
determine the
direction of the
magnetic field
for the electron
and the entire
atom, thus
giving it
"north" and
"south" poles.
Different atoms
have different
arrangements of
electrons into
their orbits,
and thus have
different
angular momenta
and dipolar
properties.
A ferromagnetic
material is
composed of many
microscopic
magnets known as
domains.
Each domain is a
region of the
magnet,
consisting of
numerous atomic
dipoles, all
pointing in the
same direction.
A strong
magnetic field
will align the
domains of a
ferromagnet, or
in other words,
magnetize
it. Once the
magnetic field
is removed, the
domains will
remain aligned,
resulting in a
permanent
magnet. This
effect is known
as hysteresis.
Few materials
are actually
ferromagnetic;
however, all
substances have
a diamagnetic
nature.
Diamagnetism
means that the
molecules within
a substance will
align themselves
to an external
magnetic field.
The external
magnetic field
induces currents
within the
material, which
in turn result
in an internal
magnetic field
in the opposite
direction. This
effect is
usually quite
small and
disappears when
the external
magnetic field
is removed.
Some materials
are paramagnetic.
This is the case
when the orbital
and spin motions
of the electrons
in a material do
not fully cancel
each other, so
that the
individual atoms
act like
magnetic
dipoles. These
dipoles are
randomly
oriented, but
will align
themselves to an
external
magnetic field.
However, when
the field is
removed, the
material is no
longer
magnetized.
Again, this
effect is
typically small.
Neither
diamagnetic nor
paramagnetic
materials
exhibit magnetic
domains.
The atomic
behavior of
magnetic
materials is
actually
considerably
more complicated
than this, as it
relies on the
theory of quantum
mechanics.
Quantum
mechanics is the
theory of
physics used to
describe the
behavior of tiny
particles such
as electrons;
like
electromagnetic
theory, it is
complex and
involves
advanced
mathematics.