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Force on a coil
Force on a coil

LAB: Magnetism
LAB: Magnetism

... 1. Tape the measuring tape or meter stick to the table, and tape the Magnetic Field Sensor to a convenient location. The sensor should be perpendicular to the stick, with the white spot inside the rod facing along the meter stick in the direction of increasing distance. Carefully measure the locatio ...
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... A year later the Frenchman François Arago found that a wire carrying an electric current acted as a magnet and could attract iron filings. Soon his compatriot André-Marie Ampère demonstrated that two parallel wires were attracted towards one another if each had a current flowing through it in the sa ...
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...  State and explain Lenz’s law.  Explain the relationship between moving charges and magnetic fields, as well as changing magnetic fields and electric fields, and their application to modern ...
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... Iron, cobalt, nickel, and rare earth alloys exhibit ferromagnetism. The so called exchange coupling causes electron magnetic moments of one atom to align with electrons of other atoms. This alignment produces magnetism. Whole groups of atoms align and form domains. (See Figure 32-12 on page 756) A m ...
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... Magnets got their name from a region in Greece called Magnesia The 1st magnetic rocks called lodestones which has magnetite in them, were found in this region nearly 3000 years ago These rocks are magnetic all the time and so are called permanent magnets You can turn any piece of iron into a permane ...
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Chapter 26: Magnetism - University of Colorado Boulder

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Mercury`s Weak Magnetic Field: Result of Magnetospheric Feedback?

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Physics 122 – Class #28 (4/28/15) – Announcements Torque on an

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Electricity and Magnetism - GTT-MOE-WMS

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MAPWORK CALCULATIONS 10 APRIL 2014

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Even if the forces acting on a body are balanced in

... The direction of the force is reversed if either the direction of the current or the direction of the magnetic field is reversed – so you must switch the battery connections round or turn the magnet round A coil of wire current carrying wire placed between the poles of a fixed magnet rotates because ...
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Physical Science - elyceum-beta

B. The sea floor spreads apart at divergent boundaries 1. Rift Valley
B. The sea floor spreads apart at divergent boundaries 1. Rift Valley

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Earth's magnetic field



Earth's magnetic field, also known as the geomagnetic field, is the magnetic field that extends from the Earth's interior to where it meets the solar wind, a stream of charged particles emanating from the Sun. Its magnitude at the Earth's surface ranges from 25 to 65 microteslas (0.25 to 0.65 gauss). Roughly speaking it is the field of a magnetic dipole currently tilted at an angle of about 10 degrees with respect to Earth's rotational axis, as if there were a bar magnet placed at that angle at the center of the Earth. Unlike a bar magnet, however, Earth's magnetic field changes over time because it is generated by a geodynamo (in Earth's case, the motion of molten iron alloys in its outer core).The North and South magnetic poles wander widely, but sufficiently slowly for ordinary compasses to remain useful for navigation. However, at irregular intervals averaging several hundred thousand years, the Earth's field reverses and the North and South Magnetic Poles relatively abruptly switch places. These reversals of the geomagnetic poles leave a record in rocks that are of value to paleomagnetists in calculating geomagnetic fields in the past. Such information in turn is helpful in studying the motions of continents and ocean floors in the process of plate tectonics.The magnetosphere is the region above the ionosphere and extends several tens of thousands of kilometers into space, protecting the Earth from the charged particles of the solar wind and cosmic rays that would otherwise strip away the upper atmosphere, including the ozone layer that protects the Earth from harmful ultraviolet radiation.
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