Magnetism.

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Presentation transcript:

Magnetism

History of Magnets (~800 BC) Ancient Chinese and Greeks discovered that certain stones would attract and magnetize iron. Small slivers of the stone were found to align themselves with the North Pole. Chinese were the first to use magnets for navigation. The orienting properties were used to align streets in cities in the North-South / East-West direction.

Applications Computer disc drives (hard and floppy) VCR and cassette tape Credit cards Speakers Motors (Both AC and DC) Speed sensors Solenoids for relays, valves, etc. Magnetos (piston engine aircraft)

Poles of a Magnet Magnets have a North and South Pole. Like poles repel. Unlike poles attract. What happens if you break a magnet in half? Will you get two monopoles? No. N S N S +

Magnetic Field Lines Characteristically similar to electric field lines. Magnetic field lines point away from the north pole and towards the south pole. Magnetic field lines are continuous (They do not terminate on the surface!). Magnetic field lines never cross. The magnetic field is strongest where the field lines are most concentrated (North and South Pole).

Oddly shaped magnets still have a north and a south Magnets either attract or repel each other South poles are attracted to north poles

Magnetic Field Lines vs. Electric Field Lines Electric Dipole Magnetic Dipole

Magnets either attract or repel each other Like poles repel South poles are attracted to north poles Unlike poles attract

The Earth’s Magnetic Field The earth has a magnetic field that scientist believe is a result of the dynamo effect due to electrical currents created in the molten iron and nickel outer core. PHET Magnet and Compass The Earth's Magnetic Field Bar Magnet - 3D

Sometimes the field completely flips Sometimes the field completely flips. The north and the south poles swap places. Such reversals, recorded in the magnetism of ancient rocks, are unpredictable.  They come at irregular intervals averaging about 300,000 years; the last one was 780,000 years ago. Are we overdue for another? No one knows.

The magnetic North Pole is responsible for more than just the direction a compass points. It's also the source of the aurora borealis, the dramatic lights that appear when solar radiation bounces off the Earth's magnetic field.  This happens at the South Pole as well. In the southern hemisphere, the lights are called the aurora australas.

Source of Magnetic Fields Electrical Charge in motion. Currents occur at the atomic level in atoms due to the orbits of electrons around the nucleus. The intrinsic spin (+1/2, -1/2) is critical in the case of magnetism.

Magnetic Domains A: Iron absent of a magnetic field. B: Iron in the presence of a magnetic field. C: A non-magnetic material.

Magnetic Domains = groups of atoms with aligned poles Magnets can be temporary (like the needle used in the compass). This nail has its atoms aligned, but the effect is only temporary.  You can get this affect by rubbing the nail on a magnet. Neat fact:  Hitting the nail can demagnetize it, you are basically scrambling the atoms.

Types of Magnetism Ferromagnetism: Ferromagnetic materials (Iron, Cobalt, Nickel) exhibit a long-range ordering phenomenon at the atomic level which causes the unpaired electron spins to line up parallel with each other in a region called a domain. (Bind ~ Bapp x 105) Paramagnetism: Paramagnetic materials (Aluminum, Tungsten, Oxygen) form weak magnetic dipoles at the atomic level when exposed to a magnetic field (Bind ~ Bapp x 10-5). Thermal motion results in randomization of the dipoles and a weak net magnetic field. Diamagnetism: Diamagnetic materials (Gold, Copper, Water) respond to magnetic fields by developing a weakly opposing magnetic field (Bind ~ -Bapp x 10-5). Bind = Induced Magnetic Field, Bapp = Applied Magnetic Field

Ferromagnetism Per 6 4/6 Soft Ferromagnets: (Silicon-steels and Iron-Nickel alloys) When the domains align themselves when exposed to an external magnetic field and re-randomize in its absence. Hard Ferromagnets: (ALNICO, ferrite and neodymium iron boron) Magnetic field persists even in the absence of an external field. Domains may realign themselves when exposed to an external magnetic field. Shocking them may re-randomize the domains, such as by dropping. Heat at or above the Curie point will re-randomize the domains. Ferromagnets lose their ferromagnetism when heated above a specific temperature , because the thermal energy melts the magnetic alignment.

Metals that are ferromagnetic: nickel, iron, cobalt   Things that are not magnetic:  aluminum, plastic, glass

Magnetism of Soft Ferromagnetic Materials How does a magnet attract screws, bolts nails, paperclips, etc. when they are not magnetic to start with? Soft ferromagnetic material align their domains in the presence of an external magnetic field creating a magnetic dipole. When the magnetic field is removed, the domains re-randomize resulting in no magnetic attraction. They are temporary Soft ferromagnetic material is attracted to both the North pole and South pole. N S S

Example 1: Application of Magnetism What type of ferromagnetic material would you use for video cassette tapes, audio cassette tapes, credit card strips, hard drives or floppy discs? Soft Ferromagnetic Hard Ferromagnetic Diamagnetic Paramagnetic Diamagnetism and paramagnetism are too weak, and soft ferromagnetic material is temporary while the external field exists.

Types of Magnets Temporary: When charged particles move through space, they induce a magnetic field (Electromagnets). Permanent: Electrons have an intrinsic magnetic field that may add together in certain matter to create a magnetic field (Speakers). Temporary Permanent

Key Ideas All magnets have North and South Poles Magnetic field lines originate in the North and end at the south pole. Magnetic field lines do not cross. Magnetism exists at the atomic level. Magnetism is the result of moving charges. Some magnets are temporary while others are permanent. Types of Magnetism. Ferromagnetism. Paramagnetism. Diamagnetism.