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Magnetism

Magnetism. Chapter 36. Magnetic Poles. Magnetic Poles – one of the regions on a magnet that produces magnetic forces The end of a magnet that points northward is called the north-seeking (north) pole , and the end that points southward is the south-seeking (south) pole

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Magnetism

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  1. Magnetism Chapter 36

  2. Magnetic Poles • Magnetic Poles – one of the regions on a magnet that produces magnetic forces • The end of a magnet that points northward is called the north-seeking (north) pole, and the end that points southward is the south-seeking (south) pole • All magnets have a north and south pole, in a common bar magnet they are on either end Like poles repel; opposite poles attract • If you break a bar magnet in half, each half will still behave as a complete magnet

  3. Magnetic Poles

  4. Magnetic Fields • Magnetic Field - a force field that fills the space around every magnet or current-carrying wire; another magnet or current-carrying wire introduced into this region will experience a magnetic force • The shape of the field is revealed by magnetic field lines; the lines spread out from one pole, curve around the magnet, and return to the other pole • The direction of the field outside the magnet is from the north to the south pole; where the lines are closer together, the field strength is greater

  5. Magnetic Fields

  6. The Nature of a Magnetic Field • Just as an electric charge is surrounded by an electric field, the same charge is also surrounded by a magnetic field if it is moving • A magnetic field is produced by the motion of an electric charge • In magnetic substances, such as iron, the magnetic fields created by spinning electrons do not cancel each other out; large clusters of magnetic atoms align to form magnetic domains • In nonmagnetic substances, electron pairs within the atoms spin in opposite directions; there is no net magnetic field

  7. The Nature of a Magnetic Field

  8. Magnetic Domains • Magnetic Domains – a microscopic cluster of atoms with their magnetic fields aligned • The difference between a piece of ordinary iron and an iron magnet is the alignment of domains • In a common iron nail, the domains are randomly oriented • In an iron magnet, the domains have been aligned with each other

  9. Magnetic Domains

  10. Electric Currents and Magnetic Fields • A moving charge produces a magnetic field • Many charges in motion—an electric current—also produce a magnetic field • The magnetic field around a current-carrying wire are in concentric circles about the wire • If the wire is bent into a loop, the field lines will become bunched up within the loop • Electromagnet – magnet with a field produced by electric current; usually in the form of a wire coiled around a piece of iron

  11. Electric Currents and Magnetic Fields

  12. Electric Currents and Magnetic Fields

  13. Magnetic Forces on Moving Charged Particles • A charged particle at rest will not interact with a static magnetic field • But if the charged particle moves in a magnetic field, the magnetic character of its motion will be evident • The charged particle experiences a deflecting force • The force is greatest when the particle moves in a direction perpendicular to the magnetic field lines • The direction of force is always perpendicular to both the magnetic field lines and the velocity of the charged particle • So, a moving charge is deflected when it crosses magnetic field lines but not when it travels parallel to the field lines

  14. Magnetic Forces on Moving Charged Particles

  15. Magnetic Forces on Current-Carrying Wires • If the particles are trapped inside a wire when they respond to the deflecting force, the wire will also move • If the direction of current in the wire is reversed, the deflecting force acts in the opposite direction • The force is maximum when the current is perpendicular to the magnetic field lines • The force is perpendicular to both field lines and current, and it is a sideways force

  16. Magnetic Forces on Current-Carrying Wires

  17. Meters to Motors A simple DC motor A simple galvanometer

  18. Earth’s Magnetic Field • A compass points northward because Earth itself is a huge magnet; the compass aligns with the magnetic field of Earth • The magnetic poles do not correspond with the geographic poles, but vary greatly (and move!) • Magnetic Declination – discrepancy between the orientation of a compass and true north • The field is thought to be caused by Earth’s liquid iron outer core, rotating around its solid iron inner core • The magnetic field of Earth is not stable, but reverses itself (20 times in the last 5 million years)

  19. Earth’s Magnetic Field

  20. Homework Assignment • Read Chapter 36 (pg. 562-574) • Do Chapter Assessment #21-32 (pg. 576)

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