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RADIO SPECTROSCOPY METHODS Electron spin resonance (ESR
RADIO SPECTROSCOPY METHODS Electron spin resonance (ESR

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Magnetostatics – Magnetic Flux Density

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... South Pole. And it also has the magnetic North Pole and the magnetic South Pole. The Earth emits a large magnetic field just like a magnet. The Earth has magnetic field lines which run in a circle from north to south and back. The Earth also has magnetic poles which are about 1500 km way from the ge ...
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...  In most materials, these magnetic fields cancel one another and neutralize the overall magnetic effect.  In other materials, such as iron, cobalt, and nickel, the atoms behave as tiny magnets because of certain orientations of the electrons inside the atom.  These atoms are grouped in a tiny reg ...
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... CONCLUSION From the simulation results, we found that the yoke steel providing a high permeability magnetic circuit makes the GMFG easy to generate high gradient magnetic field and as well as to reduce power consumption. Although the image of the phantom has been reconstructed, our present MPI syste ...
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... verify than the corresponding electric law. It is not even possible to define the most fundamental property of a permanent magnet: i.e. that the total magnetic charge of each magnet is zero. Instead, there only remains the rather pale claim that a magnet has (at least) two poles. For a normal bar ma ...
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... iron, nickel, cobalt, or mixtures of those metals. • Another kind of magnet is the electromagnet. This is a magnet made by an electric current. • Temporary magnets are made from materials that are easy to magnetize. But they tend to lose their magnetization easily. • Permanent magnets are difficult ...
B v Q l - Rowan County Schools
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... • A wire 36 m long carries a current of 22 A from east to west. If the magnetic force on the wire due to Earth’s magnetic field is downward (towards Earth) and has a magnitude of 0.04 N, find the magnitude and direction of the magnetic field at this location. ...
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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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