Clifford parallel

In elliptic geometry, two lines are Clifford parallel or paratactic lines if the perpendicular distance between them is constant from point to point. The concept was first studied by William Kingdon Clifford in elliptic space and appears only in spaces of at least three dimensions. Since parallel lines have the property of equidistance, the term "parallel" was appropriated from Euclidean geometry, although the "lines" of elliptic geometry are geodesic curves and, unlike the lines of Euclidean geometry, are of finite length.

The algebra of quaternions provides a descriptive geometry of elliptic space in which Clifford parallelism is made explicit.

Clifford bundle is a topological construction based on Clifford parallel pointed out by Heinz Hopf (1931)

Introduction

The lines on 1 in elliptic space are described by versors with a fixed axis ''r'': Georges Lemaître (1948) "Quaternions et espace elliptique", ''Acta'' Pontifical Academy of Sciences 12:57–78
:$\lbrace e^ :\ 0 \le a < \pi \rbrace$

For an arbitrary point ''u'' in elliptic space, two Clifford parallels to this line pass through ''u''.
The right Clifford parallel is
:$\lbrace u e^:\ 0 \le a < \pi \rbrace,$

and the left Clifford parallel is
:$\lbrace e^u:\ 0 \le a < \pi \rbrace.$

Generalized Clifford parallelism

Clifford's original definition was of curved parallel lines, but the concept generalizes to Clifford parallel objects of more than one dimension. In 4-dimensional Euclidean space Clifford parallel objects of 1, 2, 3 or 4 dimensions are related by isoclinic rotations. Clifford parallelism and isoclinic rotations are closely related aspects of the SO(4) symmetries which characterize the regular 4-polytopes.

Clifford surfaces

Rotating a line about another, to which it is Clifford parallel, creates a Clifford surface.

The Clifford parallels through points on the surface all lie in the surface. A Clifford surface is thus a ruled surface since every point is on two lines, each contained in the surface.

Given two square roots of minus one in the quaternions, written ''r'' and ''s'', the Clifford surface through them is given by

:$\lbrace e^e^ :\ 0 \le a,b < \pi \rbrace.$

History

Clifford parallels were first described in 1873 by the English mathematician William Kingdon Clifford.

In 1900 Guido Fubini wrote his doctoral thesis on ''Clifford's parallelism in elliptic spaces''.

In 1931 Heinz Hopf used Clifford parallels to construct the Hopf map.Roger Penrose; ''The Road to Reality'', Vintage, 2005, pp.334-6. (First published Jonathan Cape, 2004).

In 2016 Hans Havlicek showed that there is a one-to-one correspondence between Clifford parallelisms and planes external to the Klein quadric.Hans Havlicek (2016) "Clifford parallelisms and planes external to the Klein quadric", ''Journal of Geometry'' 107(2): 287 to 303

See also

* Clifford torus
*
* Regular 4-polytopes

Citations

References

*
* Laptev, B.L. & B.A. Rozenfel'd (1996) ''Mathematics of the 19th Century: Geometry'', page 74, Birkhäuser Verlag .
* Duncan Sommerville (1914) ''The Elements of Non-Euclidean Geometry'', page 108 Paratactic lines, George Bell & Sons
* Frederick S. Woods (1917
Higher Geometry
"Clifford parallels", page 255, via Internet Archive
{{Refend

Non-Euclidean geometry
Quaternions