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Natural magnetic material
Lodestones
Permanent magnets
Induced magnets
All known magnets have 2 poles
North Pole - defined as the direction the south pole of a compass point to
South pole - defined as the direction the north pole of a compass point to
North is attracted to
South (Opposites attract)
The North geographic pole is attracted to the
North magnetic pole
North geographic pole is the
South magnetic pole (and vice versa)
Magnetism acts through
magnetic fields
They extend towards infinity
Are a vector sum so there is only 1 net magnetic field at any given point in space
Similar to electric fields
“Lines” are actually
closed loops
The direction always
Leaves from magnetic north
Enters from magnetic south
They follow the north pole of a compass
Electric fields exist because
a charge exists
Magnetic fields exist when
2 things happen
A charge exists
The charge must move
Any moving charge produces a
magnetic field
Unpaired electrons create
magnetism (like iron)
Magnetic Domains are
tiny volumes with the same magnetic field direction
The bigger the domain
the stronger net magnetic field, meaning the magnet is stronger
Since magnets are just magnetic fields,
you cannot separate N from S
Ferromagnetic
“Normal magnet” - Permanent magnets
Many lone pairs
Can form large, permanent magnetic domains
Can be made permanent
AlNiCo, NdFeB (neodymium), iron
Paramagnetic
“temporary only”
Attracted to the source of magnetic field
Have lone pairs that produce a net magnetic moment
No large, permanent magnetic domains
Can not be made permanent
Many chemicals, magnesium, lithium
Diamagnetism
All materials are diamagnetic (frogs, papers, magnets, humans, copper)
Repelled from the source magnetic field
Very weak, dominated by other magnetisms
magnets can only interact with
other magnets