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Ch24: Magnetism
1
Magnetism
 The term magnetism comes from the name
Magnesia, a coastal district of ancient Thessaly,
Greece.
 Unusual stones were found by the Greeks more
than 2000 years ago.
 These stones, called lodestones, had the
intriguing property of attracting pieces of iron.
 Magnets were first fashioned into compasses
and used for navigation by the Chinese in the
12th century.
Magnetic Force
Magnetic force between a pair of magnets
 Force of attraction or repulsion between a
pair of magnets depends on which end of
the magnet is held near the other.
 Behavior similar to electrical forces.
 Strength of interaction depends on the
distance between the two magnets.
Ch24: Magnetism
2
Magnetic Poles
 Two types interacting with each other
– north pole (north-seeking pole)
– south pole (south-seeking pole)
Rule for magnetic forces between magnetic poles:
 Like poles repel; opposite poles attract.
Ch24: Magnetism
3
Magnetic Poles
 In all magnets—can’t have one pole without the other
 No single pole known to exist
Example:
– simple bar magnet: poles at the two ends
– horseshoe magnet: bent U shape - poles at ends
Ch24: Magnetism
4
Magnetic Field
 Region of magnetic influence surrounding magnet
 Magnetic field lines are closed loops
 By convention, direction is from the north pole to
the south pole, produced by motions of electric
charge in atoms
Ch24: Magnetism
5
Magnetic Field
 Strength indicated by closeness of the lines
– lines close together  strong magnetic field
– lines farther apart  weak magnetic field
Ch24: Magnetism
6
Magnetic Field
 Produced by two kinds of electron motion
 electron spin
– main contributor to magnetism
– pair of electrons spinning in same direction
creates a stronger magnet
– pair of electrons spinning in opposite
direction cancels magnetic field of the other
 electron revolution
Ch24: Magnetism
7
Magnetic Domains
 Magnetized clusters of aligned
magnetic atoms
 Permanent magnets made by
– placing pieces of iron or similar
magnetic materials in a strong
magnetic field.
– stroking material with a magnet to
align the domains.
Ch24: Magnetism
8
Magnetic Domains
 Difference between permanent magnet and
temporary magnet
• Permanent magnet
– alignment of domains remains once
external magnetic field is removed
• Temporary magnet
– alignment of domains returns to random
arrangement once external magnetic field is
removed
Ch24: Magnetism
9
Magnetic Domains
Ch24: Magnetism
10
Electric Current and Magnetic Field
 Connection between electricity and magnetism
 Electric current creates magnetic field
 Magnetic field forms a pattern
of concentric circles around
a current-carrying wire.
 When current reverses direction,
the direction of the field lines
reverse.
Ch24: Magnetism
11
Electric Current and Magnetic Field
 If the wire is bent into a loop, the magnetic
field lines become bunched up inside the loop
Ch24: Magnetism
12
Electric Current and Magnetic Field
Magnetic field intensity
 increases as the number of loops increase in a
current-carrying coil temporary magnet.
Ch24: Magnetism
13
Magnetic Force on Moving Charge
Moving charges in a magnetic field experience
a deflecting force.
• Greatest force
– particle movement in direction perpendicular to the
magnetic field lines
• Least force
– particle movement other than perpendicular to the
magnetic field lines
• No force
– particle movement parallel to the magnetic field lines
Ch24: Magnetism
14
Magnetic Force on Moving Charges
 Moving charges in a magnetic
field experience a deflecting force
Ch24: Magnetism
15
Magnetic Force on Current-
Carrying Wires
 Current of charged particles moving through a
magnetic field experiences a deflecting force.
– Direction is perpendicular to both magnetic field
lines and current (perpendicular to wire).
– Strongest when current is perpendicular to the
magnetic field lines.
Ch24: Magnetism
16
Earth’s Magnetic Field
 Earth is itself a huge magnet.
 The magnetic poles of Earth are
widely separated from the geographic
poles.
 The magnetic field of Earth is not due
to a giant magnet in its interior—it is
due to electric currents.
 Most Earth scientists think that
moving charges looping around
within the molten part of Earth create
the magnetic field.
 Earth’s magnetic field reverses
direction: 20 reversals in last 5 million
years.
Ch24: Magnetism
17
Earth’s Magnetic Field
 Universe is a shooting gallery of
charged particles called cosmic
rays.
 Cosmic radiation is hazardous to
astronauts.
 Cosmic rays are deflected away
from Earth by Earth’s magnetic
field.
 Some of them are trapped in the
outer reaches of Earth’s magnetic
field and make up the Van Allen
radiation belts
Ch24: Magnetism
18
Earth’s Magnetic Field
 Storms on the Sun hurl charged
particles out in great fountains,
many of which pass near Earth and
are trapped by its magnetic field.
The trapped particles follow
corkscrew paths around the
magnetic field lines of Earth and
bounce between Earth’s magnetic
poles high above the atmosphere.
 Disturbances in Earth’s field often
allow the ions to dip into the
atmosphere, causing it to glow like
a fluorescent lamp.
Hence the aurora borealis or
aurora australis. Ch24: Magnetism
19

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3. Magnetic force of moed particles.pptx

  • 1. Ch24: Magnetism 1 Magnetism  The term magnetism comes from the name Magnesia, a coastal district of ancient Thessaly, Greece.  Unusual stones were found by the Greeks more than 2000 years ago.  These stones, called lodestones, had the intriguing property of attracting pieces of iron.  Magnets were first fashioned into compasses and used for navigation by the Chinese in the 12th century.
  • 2. Magnetic Force Magnetic force between a pair of magnets  Force of attraction or repulsion between a pair of magnets depends on which end of the magnet is held near the other.  Behavior similar to electrical forces.  Strength of interaction depends on the distance between the two magnets. Ch24: Magnetism 2
  • 3. Magnetic Poles  Two types interacting with each other – north pole (north-seeking pole) – south pole (south-seeking pole) Rule for magnetic forces between magnetic poles:  Like poles repel; opposite poles attract. Ch24: Magnetism 3
  • 4. Magnetic Poles  In all magnets—can’t have one pole without the other  No single pole known to exist Example: – simple bar magnet: poles at the two ends – horseshoe magnet: bent U shape - poles at ends Ch24: Magnetism 4
  • 5. Magnetic Field  Region of magnetic influence surrounding magnet  Magnetic field lines are closed loops  By convention, direction is from the north pole to the south pole, produced by motions of electric charge in atoms Ch24: Magnetism 5
  • 6. Magnetic Field  Strength indicated by closeness of the lines – lines close together  strong magnetic field – lines farther apart  weak magnetic field Ch24: Magnetism 6
  • 7. Magnetic Field  Produced by two kinds of electron motion  electron spin – main contributor to magnetism – pair of electrons spinning in same direction creates a stronger magnet – pair of electrons spinning in opposite direction cancels magnetic field of the other  electron revolution Ch24: Magnetism 7
  • 8. Magnetic Domains  Magnetized clusters of aligned magnetic atoms  Permanent magnets made by – placing pieces of iron or similar magnetic materials in a strong magnetic field. – stroking material with a magnet to align the domains. Ch24: Magnetism 8
  • 9. Magnetic Domains  Difference between permanent magnet and temporary magnet • Permanent magnet – alignment of domains remains once external magnetic field is removed • Temporary magnet – alignment of domains returns to random arrangement once external magnetic field is removed Ch24: Magnetism 9
  • 11. Electric Current and Magnetic Field  Connection between electricity and magnetism  Electric current creates magnetic field  Magnetic field forms a pattern of concentric circles around a current-carrying wire.  When current reverses direction, the direction of the field lines reverse. Ch24: Magnetism 11
  • 12. Electric Current and Magnetic Field  If the wire is bent into a loop, the magnetic field lines become bunched up inside the loop Ch24: Magnetism 12
  • 13. Electric Current and Magnetic Field Magnetic field intensity  increases as the number of loops increase in a current-carrying coil temporary magnet. Ch24: Magnetism 13
  • 14. Magnetic Force on Moving Charge Moving charges in a magnetic field experience a deflecting force. • Greatest force – particle movement in direction perpendicular to the magnetic field lines • Least force – particle movement other than perpendicular to the magnetic field lines • No force – particle movement parallel to the magnetic field lines Ch24: Magnetism 14
  • 15. Magnetic Force on Moving Charges  Moving charges in a magnetic field experience a deflecting force Ch24: Magnetism 15
  • 16. Magnetic Force on Current- Carrying Wires  Current of charged particles moving through a magnetic field experiences a deflecting force. – Direction is perpendicular to both magnetic field lines and current (perpendicular to wire). – Strongest when current is perpendicular to the magnetic field lines. Ch24: Magnetism 16
  • 17. Earth’s Magnetic Field  Earth is itself a huge magnet.  The magnetic poles of Earth are widely separated from the geographic poles.  The magnetic field of Earth is not due to a giant magnet in its interior—it is due to electric currents.  Most Earth scientists think that moving charges looping around within the molten part of Earth create the magnetic field.  Earth’s magnetic field reverses direction: 20 reversals in last 5 million years. Ch24: Magnetism 17
  • 18. Earth’s Magnetic Field  Universe is a shooting gallery of charged particles called cosmic rays.  Cosmic radiation is hazardous to astronauts.  Cosmic rays are deflected away from Earth by Earth’s magnetic field.  Some of them are trapped in the outer reaches of Earth’s magnetic field and make up the Van Allen radiation belts Ch24: Magnetism 18
  • 19. Earth’s Magnetic Field  Storms on the Sun hurl charged particles out in great fountains, many of which pass near Earth and are trapped by its magnetic field. The trapped particles follow corkscrew paths around the magnetic field lines of Earth and bounce between Earth’s magnetic poles high above the atmosphere.  Disturbances in Earth’s field often allow the ions to dip into the atmosphere, causing it to glow like a fluorescent lamp. Hence the aurora borealis or aurora australis. Ch24: Magnetism 19