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Gauss's Law is always true: Φ = ∫surface E • dA = qenclosed/ε0, but it isn't always useful for finding the electric field, which is what we are usually interested in. This should not be too surprising, because to find E, using an equation like ∫surface E • dA = qenclosed/ε0, E has to be able to come out of the integral, and for that to happen, E needs to be constant on a surface. This is where symmetry comes in. Gauss's law is only useful for calculating electric fields when the symmetry is such that you can construct a Gaussian surface so that the electric field is constant over the surface, and the angle between the electric field and the normal to the Gaussian surface does not vary over the surface (position is given in meters and electric field strength is given in newtons/coulonb). In practice, this means that you pick a Gaussian surface with the same symmetry as the charge distribution. Restart.
Consider a sphere around a point charge. The blue test charge shows the direction of the electric field. There is also a vector pointing in the direction of the surface normal to the sphere.
Now, put a box around the same point charge. The test charge now shows the direction of the electric field, and the smallest angle between the vector and a vertical axis is shown (in degrees). The red vector points in the direction of the surface normal to the box (two sides show).
Let's try another charge configuration. Put a sphere around a charged plate (assume the gray circles you see are long rods of charge that extend into and out of the screen to create a charged plate that you see in cross section).
Now, put a box around a charged plate (assume the points you see are long rods of charge that extend into and out of the screen to create a charged plate that you see in cross section).
For the plate, using a box as a Gaussian surface means that E • dA = E dA cosθ is a constant for each section (top, bottom, and sides) and the electric field is a constant on the surface. This means you can write:
∫surface E • dA = E ∫surface dA = EA (for the surfaces where the flux is nonzero).
Exploration authored by Anne J. Cox.
Script authored by Wolfgang Christian and modified by Anne J. Cox.
© 2004 by Prentice-Hall, Inc. A Pearson Company