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An in-depth exploration of magnetostatics, the branch of physics that deals with magnetic fields and their interactions with currents. the historical background, the definition of magnetic fields, the Lorentz force, and the Biot-Savart law. It also discusses the field equations for steady currents and the concept of the vector potential. essential for students studying electromagnetism, as it forms the foundation for understanding the behavior of magnetic fields and their relationship with electric currents.
Typology: Study notes
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Overview. Like electricity, magnetism has ancient roots. Aristotle cites Thales, about 300 years before him, as the first to describe magnetic phenomena scientifically. The first phenomena involved stones found in various places, especially the province of Magnesia, that had the power to attract bits of iron. It was also found that a small bit of iron could be “magnetized” by contact with these stones. Around 1000 CE the ability to determine the direction of north by a magnetized needle was discovered. In 1600 Gilbert explained this by asserting that the earth behaved like a giant magnet itself. It was not until 1820 that the connection between magnetism and electric currents was discovered, by Oersted. Within a decade the laws governing the creation of magnetic fields by currents, and the action of those fields on currents, had been laid out by Ampere and others. All the laws governing magnetic phenomena of currents that do not change with time had been found. Those laws are the subject of these notes. The magnetic field. At the time of Ampere the microscopic picture of electric currents was still vague, because nobody knew how the flow of charge was constituted. By 1900 it was known that a current in a wire is a flow of electrons, and the effect of a magnetic field on a current was understood as a collective effect of the interaction of the field with the moving electrons. This changed the way a magnetic field was defined. We now define a magnetic field, called B , by the force it exerts on a single charged particle. But the charge must be moving for such a force to exist. The definition of B comes from the law for that force (often called the Lorentz force), which is F = q v × B. Here q is the charge and v its velocity. There are some interesting features of this force:
If the surface is closed, the current outward through it must equal the decrease in charge within the surface, by conservation of charge, so we have
d dt
But by the divergence theorem
so we find ∇ ⋅ j = − ∂ ρ ∂ t
This field equation is usually called Ampere’s law. Because the field has zero divergence it can be written as the curl of another vector field: B = ∇ × A. This field, A , is called the vector potential. Like the electrostatic scalar potential. it is not unique. To it can be added the gradient of any scalar, since the curl of a gradient is identically zero. The choice of such a gradient is called choosing a gauge , and a change of that choice is a gauge transformation. One popular choice is to make ∇ ⋅ A = 0. This choice is called the “Coulomb gauge”, because A satisfies an equation resembling Poisson’s equation: ∇^2 A = − μ 0 j. The solution of this is analogous to the formula for the scalar potential in electrostatics: A ( r ) = μ 0 4 π d^3 r ′ j ( r ′)
Example: a uniform B-field. The field A ( r ) = 1 2 B × r gives both ∇ × A = B and ∇ ⋅ A = 0. Exercise: Prove these claims. The integral form of the curl equation, like the integral form of Gauss’s law for electricity, can be used to make formal arguments about the field, and, in a few cases of high symmetry, to calculate the field to a good approximation. This equation reads:
Here Ilinked is the net current (the flux of j ) passing through the area bounded by the closed curve over which the line integral is taken. The direction of a positive current is determined by a right hand rule: curl your right hand fingers around the way the closed curve is integrated; your thumb indicates positive current. There are several examples of this use of Ampere’s law worked out in G. Summary of static fields. The field equations, up to now, are these:
Note that none of the equations involves both E and B. To these must be added the law specifying the force the fields exert on a single point charge: F = q ( E + v × B ). As noted, at this point we require ∇ ⋅ j = 0 , so only steady currents and time independent charge densities are described by these equations. When those restrictions are relaxed, we find additional terms are needed in the field equations, linking E and B.