Dynamo Effect Of Earth
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Dynamo effect of earth. Historically this was believed to be caused by some kind of permanent magnetization of material in the earth and dynamo theory was orginally put forward to explain the sun s magnetic eld. A dynamo is thought to be the source of the earth s magnetic field and the magnetic fields of. Heat from radioactive decay in the core is thought to induce. The results of our study support the idea that galaxy magnetic fields are generated by a rotating dynamo effect similar to the process that produces the sun s magnetic field sui ann mao minerva research group leader for the max planck institute for radio astronomy in bonn germany said.
In this dynamo mechanism fluid motion in the earth s outer core moves conducting material liquid iron across an already existing weak magnetic field and generates an electric current. The dynamo effect is a geophysical theory that explains the origin of the earth s main magnetic field in terms of a self exciting or self sustaining dynamo. As scientists refine their understanding of how this field works in their ongoing probe of planetary history one idea they use to explain this process is dynamo theory the idea that a large dynamo or magnetic field generator exists within earth s outer core where liquid iron constantly moves as the planet cools. 2 earth s field the earth s magnetic eld is basically a dipole which is aligned o the rotation axis by about 11 degrees.
In physics the dynamo theory proposes a mechanism by which a celestial body such as earth or a star generates a magnetic field the dynamo theory describes the process through which a rotating convecting and electrically conducting fluid can maintain a magnetic field over astronomical time scales. Dynamo theory geophysical theory that explains the origin of earth s main magnetic field in terms of a self exciting or self sustaining dynamo. Dynamo effect 94 the process by which a rotating convecting body of conducting matter such as. The dynamo effect is a geophysical theory that explains the origin of the earth s main magnetic field in terms of a self exciting or self sustaining dynamo.