Phenomenon in the force field ("magnetic field") surrounding a magnet.
Magnetism is caused by electrical charges in motion. This is not necessarily
something unique to electrical equipment, which is the case for
electromagnetism, but also for permanent magnets. It is the motion of the
electrons around the nuclei, and also the spin of the
electrons, that cause the magnetism in a natural magnet. The magnetic field of
Earth is believed to come from movements inside the planet, where oceans and
rivers of melted metals exist. (Think Jules Verne here people.)
An important concept is that of the magnetic dipole, which is basically the
physical representation of a simple magnetic rod. It has a north,
"plus", pole and a south, "minus", pole. Such a pole cannot
exist individually, so if you break up a magnetic rod in two pieces, each will
be a new magnet with two poles. This shows a fundamental difference between
magnetism and electricity, since there are free electric charges but no
free magnetic poles. One consequence of this is that magnetic field lines always
create closed circles and it is these field lines that you see when you put iron
chips around a magnet.
Magnetic fields are measured in the SI Unit weber, Wb (1 weber is
really 1 volt second), which is a measurement of the magnetic flux Φ through
a surface. The most common term is the magnetic field B, which really is the
magnetic flux density, or flux per area. This is measured in Wb/m2,
which has its own unit tesla T, after Nicolai Tesla. An older obsolete unit for this is Gs,
Gauss, which is 1/10000 of a teals.
The most important characteristics of magnetism are described by the
following laws, which shows how magnetism and electricity work together :
The B field has two components; one depending on the magnetic
field strength H and one depending on the magnetization M.
In short we can calculate the field as
B = μ0 · H + μ0 · M = μ0
· H + J
where μ0 is the permeability in vacuum. The term J
is called magnetic polarization. The magnetization M is (usually) related to
the H field as M = χm · H where χm
is the susceptibility, which is a very important characteristics of magnetic
materials.
History
The word "magnetism" comes from the area Magnesia in
ancient Asia Minor where magnetite, Fe3O4, was
mined in the 9th century B.C. It was early discovered how it would attract iron.
The first application was probably at sea, where they were used for compasses
starting from the 13th century in China as well as in Europe. During the
17th and 18th century, magnets and magnetism started to interest several
scientists and they gradually unveiled its mystery. The most important
breakthrough however would have to wait until 1820 when H.C. Ørsted
discovered the relation between magnetism and electricity. André Ampère
further developed Ørsted's experiments and came up with a mathematical
model.
The next big contribution came from Michael Faraday who introduced
the magnetic field and described its behavior. Faraday's work helped Maxwell
in his work with what later became Maxwell's equations, which are the
most central part in electromagnetic theory. The continuing work on magnetism
has gone hand in hand with the development of atomic and quantum theories and
our understanding of magnetsim is tightly couples with quantum theory.
Reference: ne.se