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Physics 1001 - Introduction to Magnetism VO Magnets are all
Physics 1001 - Introduction to Magnetism VO Magnets are all

... but it’s not as easy to make a permanent magnet lose its polarity. Why? Well, it has to do with the type of material it is made of. Iron is considered to be a soft magnetic material because its domains can slip into and out of alignment easily. Soft iron does not make a good permanent magnet for thi ...
Electricity and magnetism quiz
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...  The “king” of all ferromagnetics is iron.  A magnet has two ends called poles, one of which is called a north pole or north-seeking pole, while the other is called a south pole or south-seeking pole.  The north pole of one magnet attracts the south pole of a second magnet, while the north pole o ...
Magnetic field - Nutley Schools
Magnetic field - Nutley Schools

... Quantitative Exercise 17.10 • An atom or molecule with a single electron removed is traveling at 1.0 x 106 m/s when it enters a mass spectrometer's 0.50-T uniform magnetic field region. Its electric charge is +1.6 x 10–19 C. It moves in a circle of radius 0.20 m until it hits the detector. 1. Deter ...
Physics, Chapter 29: The Magnetic Field
Physics, Chapter 29: The Magnetic Field

... is given by the magnitude of the force on a unit north pole, and whose direction is the direction of the force on a north pole. Algebraically, it is conventional to represent a north pole as a positive pole and a south pole as a negative pole. In cgs emu the force is stated in dynes, the pole streng ...
Physics, Chapter 29: The Magnetic Field
Physics, Chapter 29: The Magnetic Field

... is given by the magnitude of the force on a unit north pole, and whose direction is the direction of the force on a north pole. Algebraically, it is conventional to represent a north pole as a positive pole and a south pole as a negative pole. In cgs emu the force is stated in dynes, the pole streng ...
Magnets and Magnetic Fields
Magnets and Magnetic Fields

princeton university physics 104 lab
princeton university physics 104 lab

... You will get to play with several “toys” in the magnetic field. Do not put anything into the field other than the objects indicated by your tour guide. In particular, there are plenty of metal pieces lying around large enough that they would be attracted very strongly to the pole pieces — and your h ...
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... electrons are charged this corresponds to a current flowing in a wire which we know produces a magnetic field. Ferromagnetic materials are the only substances capable of being made into magnets; they are normally iron, nickel, cobalt, or alloys that are made of rare-earth metals. A magnet is created ...
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ch 27 - NMSU

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... enter Earth near the north pole. During a magnetic reversal, the lines of magnetic force run the opposite way. Scientists have determined that Earth's magnetic field has reversed itself many times in the past. These reversals occur over intervais of thousands or even millions of years. The reversals ...
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Unit 8: Electricity and Magnetism
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... produce an electric current. Claims should be supported and modeled mathematically when appropriate. Students should choose and interpret units consistently and organize and analyze data in graphs. Students might also conduct short or more sustained research projects around the concepts of electric ...
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Analyzing Magnetic Fields with Solenoids - PhysicsEd

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... Welcome to MRI Safety Jeopardy. The game is played by selecting a category, a point value,  and ‘answering’ by asking the appropriate question that would produce the provided  statement. Your responses must be in the form of a question.   When a statement is read, signal when you believe that you ha ...
Building Blocks - The SPS Observer
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HW06_01
HW06_01

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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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