Wednesday, February 27, 2013

Generalized Helices: Curves of Constant Slope

A regular curve in space is said to have constant slope when its tangents make a constant angle with a given fixed line. Such a curve is also called a generalized helix, or even just a helix amongst the cognoscenti. The line is called the axis of the helix.


An analytic way of stating the condition is as follows: Let A be a unit vector parallel to the axis . Denote the parametrized curve by X and its arclength parameter by s. We use standard notation for the Frenet-Serret apparatus. Then the definition means that
(1)T,A=cosα.
Here α is the angle mentioned because T and A are both unit vectors.

Our goal is to describe the consequences of equation (1) for the shape of the curve.



The geometry of a curve is encoded by the curvature and torsion functions? Is there a way to characterize helices by using these functions?

Lancret's Theorem: A regular curve has constant slope if and only if the ratio κ/τ of curvature to torsion is constant.

Proof: We begin by differentiating equation (1) with respect to s. This gives us
κN,A+T,A=0.
Since A is a constant, we deduce
(2)N,A=0.
Thus A must be parallel to the rectifying planes of X. (All of them!) Though we often picture our vectors as "free" vectors, they really are all bound with their tails at the origin, so we know that A lies in Span{T,B}. Since {T,B} is an orthonormal basis for the rectifying plane, we can express the unit vector A as a linear combination this way:
(3)A=cos(α)T+sin(α)B.
We differentiate this to find
0=cos(α)κN+sin(α)(τ)N=(cos(α)κsin(α)τ)N.
Now, N is a unit vector, so we deduce that the coefficient must vanish, from which we can deduce that
(4)κτ=tan(α).
a constant.

Now, suppose that X is a regular curve with κ/τ=C. We choose α to be the unique real number so that α(π/2,π/2) and tan(α)=C. Then a little algebraic manipulation gives us that cos(α)κsin(α)τ=0. Now define a vector A by
A=cos(α)T+sin(α)B.
One can check that A is a unit vector, and then
A=dds(cos(α)T+sin(α)B)=cos(α)κNsin(α)τN=0.
Hence A is a constant vector, and the tangents make angle cos(α) with A. Thus X is a helix.

Suppose we choose coordinates so that the axis is in the direction of our third coordinate, and hence the helix is expressed in the form
(x(s),y(s),cos(α)s).
This means that our upward drift is well understood, and what remains to be investigated is the plane curve (x(s),y(s)).


Theorem: Let Y be the projection of the helix X with angle α onto a plane perpendicular to the axis . The principal normal to Y is parallel to the principal normal to the helix, and the curvature of Y is κY=κXcsc2(α).

Proof: By definition of orthogonal projection, we know that Y=XX,AA. We differentiate this with respect to s to find
(5)Y=TT,AA=Tcos(α)A.
It is important to remember that s=sX is the arclength parameter for X, and not necessarily for Y. So when we want to compute things for Y we will need to use the chain rule.

(dsYds)2=Y,Y=Tcos(α)A,Tcos(α)A
(dsYds)2=T,T2cos(α)A,T+cos2(α)A,A=1cos2(α)
Or, more simply,
dsYds=sin(α).
So we get the very useful measurement of the speed of the projection:
(6)dsYds=sin(α).

Now it is straightforward to compute derivatives for the planar projection Y in terms of its arclength s1. The tangent to Y is

TY=dYdsY=dsdsYdYds=1sin(α)(Tcos(α)A)=csc(α)Tcot(α)A.
And so we differentiate to find NY and κY:
ddsYTY=1sin(α)(csc(α)κXNX)=csc2(α)κXNX.
Now, NX is a unit vector, so it must also be the principal normal to Y, and we get the desired description of the curvature of Y.


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