Cuspidal cubic
In mathematics, a cuspidal cubic or semicubical parabola is an algebraic plane curve defined parametrically as
Its implicit equation is
which can be solved in y to yield the equation
This cubic curve has a singular point at the origin, which is a cusp.
If one sets u = at, X = a2x, and Y = a3y, one gets
This implies that, for any value of a, the curve is homothetic to the curve for which a = 1, or, equivalently, that the curves corresponding to different values of a differ only by the choice of the unit length.
A special case of the semicubical parabola is the evolute of the parabola. It has the equation
Expanding the Tschirnhausen cubic catacaustic shows that it is also a semicubical parabola:
An additional defining property of the semicubical parabola is that it is an isochrone curve, meaning that a particle following its path while being pulled down by gravity travels equal vertical intervals in equal time periods. In this way it is related to the , for which particles at different starting points always take equal time to reach the bottom, and the , the curve that minimizes the time it takes for a falling particle to travel from its start to its end.
The semicubical parabola was discovered in 1657 by William Neile who computed its arc length. Although the lengths of some other non-algebraic curves including the logarithmic spiral and cycloid had already been computed (that is, those curves had been rectified), the semicubical parabola was the first algebraic curve (excluding the line and circle) to be rectified.
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