For two-dimensional potential flow, streamlines are perpendicular to equipotential lines.
2.
As such, a grid obtained by drawing a series of equipotential lines is called a flownet.
3.
Lines of constant \ psi are known as streamlines and lines of constant \ phi are known as equipotential lines ( see equipotential surface ).
4.
External rays together with equipotential lines of Douady-Hubbard potential ( level sets ) form a new polar coordinate system for complement ) of K \,.
5.
If we colour the Fatou domain according to the iteration number ( and " not " the real iteration number ), the bands of iteration show the course of the equipotential lines.
6.
Figure 1 : Equipotential lines of electric convection field within the equatorial plane of the magnetosphere ( left ), and superposition of the convection field with the co-rotation field ( right ) during magnetically quiet conditions
7.
There are 16 green equipotential lines ( 15 equal drops in hydraulic head ) between the 5 m upstream head to the 1m downstream head ( 4 m / 15 head drops = 0.267 m head drop between each green line ).
8.
The idea behind this formula is simple : When the equipotential lines for the potential function \ phi ( z ) lie close, the number | \ phi'( z ) | is large, and conversely, therefore the equipotential lines for the function \ phi ( z ) / | \ phi'( z ) | should lie approximately regularly.
9.
The idea behind this formula is simple : When the equipotential lines for the potential function \ phi ( z ) lie close, the number | \ phi'( z ) | is large, and conversely, therefore the equipotential lines for the function \ phi ( z ) / | \ phi'( z ) | should lie approximately regularly.
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