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The helicoid, also known as helical surface, is a smooth surface embedded in three-dimensional space. It is the surface traced by an infinite line that is simultaneously being rotated and lifted along its fixed axis of rotation. It is the third to be known, after the plane and the .


Description
It was described by in 1774 and by Jean Baptiste Meusnier in 1776. Its derives from its similarity to the : for every point on the helicoid, there is a helix contained in the helicoid which passes through that point.

The helicoid is also a (and a ), meaning that it is a trace of a line. Alternatively, for any point on the surface, there is a line on the surface passing through it. Indeed, Catalan proved in 1842 that the helicoid and the plane were the only ruled . Elements of the Geometry and Topology of Minimal Surfaces in Three-dimensional Space By A. T. Fomenko, A. A. Tuzhilin Contributor A. A. Tuzhilin Published by AMS Bookstore, 1991 , , p. 33

A helicoid is also a translation surface in the sense of differential geometry.

The helicoid and the are parts of a family of helicoid-catenoid minimal surfaces.

The helicoid is shaped like , but extends infinitely in all directions. It can be described by the following parametric equations in Cartesian coordinates:

x = \rho \cos (\alpha \theta), \
y = \rho \sin (\alpha \theta), \
z = \theta, \
where and range from negative to infinity, while is a constant. If is positive, then the helicoid is right-handed as shown in the figure; if negative then left-handed.

The helicoid has principal curvatures \pm \alpha /(1+ \alpha^2 \rho ^2) \ . The sum of these quantities gives the (zero since the helicoid is a minimal surface) and the product gives the Gaussian curvature.

The helicoid is to the plane \mathbb{R}^2 . To see this, let decrease continuously from its given value down to zero. Each intermediate value of will describe a different helicoid, until is reached and the helicoid becomes a vertical plane.

Conversely, a plane can be turned into a helicoid by choosing a line, or axis, on the plane, then twisting the plane around that axis.

If a helicoid of radius revolves by an angle of around its axis while rising by a height , the area of the surface is given by

\frac{\theta}{2} \leftR,
\ c = \frac{h}{\theta}.


Helicoid and catenoid
The helicoid and the are locally isometric surfaces; see Catenoid#Helicoid transformation.


See also


Notes


External links

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