Investigation 17A Key Question: How do magnets and compasses work? Magnetism.

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Investigation 17A Key Question: How do magnets and compasses work? Magnetism

Transcript of Investigation 17A Key Question: How do magnets and compasses work? Magnetism.

Page 1: Investigation 17A  Key Question: How do magnets and compasses work? Magnetism.

Investigation 17A

Key Question:How do magnets and compasses work?

Magnetism

Page 2: Investigation 17A  Key Question: How do magnets and compasses work? Magnetism.

17.1 Properties of Magnets If a material is magnetic, it has the

ability to exert forces on magnets or other magnetic materials nearby.

A permanent magnet is a material that keeps its magnetic properties.

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17.1 Properties of Magnets All magnets have

two opposite magnetic poles, called the north pole and south pole.

If a magnet is cut in half, each half will have its own north and south poles.

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17.1 Properties of Magnets

Whether the two magnets attract or repel depends on which poles face each other.

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17.1 Magnetic fields

The force from a magnet gets weaker as it gets farther away.

Separating a pair of magnets by twice the distance reduces the force by 8 times or more.

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17.1 Magnetic fields

A special kind of diagram is used to map the magnetic field.

The force points away from the north pole and towards the south pole.

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17.1 Magnetic field lines

A compass needle is a magnet that is free to spin.

Because the needle aligns with the local magnetic field, a compass is a great way to “see” magnetic field lines.

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17.1 Geographic and magnetic poles

The planet Earth has a magnetic field that comes from the core of the planet itself.

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17.1 Declination and “true north”Because Earth’s geographic north

pole (true north) and magnetic south pole are not located at the exact same place, a compass will not point directly to the geographic north pole.

The difference between the direction a compass points and the direction of true north is called magnetic declination.

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17.1 Declination and “true north” Magnetic declination is

measured in degrees and is indicated on topographical maps.

Most good compasses contain an adjustable ring with a degree scale used compensate for declination.

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17.1 Earth’s magnetism

Studies of earthquake waves reveal that the Earth’s core is made of hot, dense molten metals.

Huge electric currents flowing in the molten iron produce the Earth’s magnetic field.

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17.1 Earth’s magnetism

Today, Earth’s magnetic field is losing approximately 7 percent of its strength every 100 years.

If this trend continues, the magnetic poles will reverse sometime in the next 2,000 years.