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Clifford parallel

From Wikipedia, the free encyclopedia
Lines with constant perpendicular distance between them

Inelliptic geometry, two lines areClifford parallel orparatactic lines if theperpendicular distance between them is constant from point to point. The concept was first studied byWilliam Kingdon Clifford inelliptic space and appears only in spaces of at leastthree dimensions. Sinceparallel lines have the property of equidistance, the term "parallel" was appropriated fromEuclidean geometry, although the "lines" of elliptic geometry aregeodesiccurves and, unlike the lines ofEuclidean geometry, are of finite length.

The algebra ofquaternions provides a descriptive geometry of elliptic space in which Clifford parallelism is made explicit.Clifford bundle is a topological construction based onClifford parallel pointed out byHeinz Hopf (1931)[1]

Introduction

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Two Clifford parallelgreat circles on the3-sphere spanned by a twistedannulus. They have a common center point in4-dimensional Euclidean space, and could lie incompletely orthogonal rotation planes.

The lines on 1 in elliptic space are described byversors with a fixed axisr:[2]

{ear: 0a<π}{\displaystyle \lbrace e^{ar}:\ 0\leq a<\pi \rbrace }

For an arbitrary pointu in elliptic space, two Clifford parallels to this line pass throughu.The right Clifford parallel is

{uear: 0a<π},{\displaystyle \lbrace ue^{ar}:\ 0\leq a<\pi \rbrace ,}

and the left Clifford parallel is

{earu: 0a<π}.{\displaystyle \lbrace e^{ar}u:\ 0\leq a<\pi \rbrace .}

Generalized Clifford parallelism

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

Clifford surfaces

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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 aruled surface since every point is on two lines, each contained in the surface.

Given two square roots of minus one in thequaternions, writtenr ands, the Clifford surface through them is given by[2][4]

{earebs: 0a,b<π}.{\displaystyle \lbrace e^{ar}e^{bs}:\ 0\leq a,b<\pi \rbrace .}

History

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Clifford parallels were first described in 1873 by the English mathematicianWilliam Kingdon Clifford.[5]

In 1900Guido Fubini wrote his doctoral thesis onClifford's parallelism in elliptic spaces.[6]

In 1931Heinz Hopf used Clifford parallels to construct theHopf map.[1]

In 2016 Hans Havlicek showed that there is a one-to-one correspondence between Clifford parallelisms and planes external to theKlein quadric.[7]

See also

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Citations

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  1. ^abRoger Penrose;The Road to Reality, Vintage, 2005, pp.334-6. (First published Jonathan Cape, 2004).
  2. ^abGeorges Lemaître (1948) "Quaternions et espace elliptique",ActaPontifical Academy of Sciences 12:57–78
  3. ^Tyrrell & Semple 1971, pp. 5–6, §3. Clifford's original definition of parallelism.
  4. ^H. S. M. CoxeterEnglish synopsis of Lemaître inMathematical Reviews
  5. ^William Kingdon Clifford (1882)Mathematical Papers, 189–93,Macmillan & Co.
  6. ^Guido Fubini (1900) D.H. Delphenich translatorClifford Parallelism in Elliptic Spaces, Laurea thesis, Pisa.
  7. ^Hans Havlicek (2016) "Clifford parallelisms and planes external to the Klein quadric",Journal of Geometry 107(2): 287 to 303MR 3519950

References

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