Pseudosphere

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In geometry, a pseudosphere is a surface in 3. It is the most famous example of a pseudospherical surface. A pseudospherical surface is a surface piecewise smoothly immersed in 3 with constant negative Gaussian curvature. A "pseudospherical surface of radius R" is a surface in 3 having curvature −1/R2 at each point. Its name comes from the analogy with the sphere of radius R, which is a surface of curvature 1/R2. Examples include the tractroid, Dini's surfaces, breather surfaces, and the Kuen surface.

The term "pseudosphere" was introduced by Eugenio Beltrami in his 1868 paper on models of hyperbolic geometry.[1]

Tractroid

Tractroid

By "the pseudosphere", people usually mean the tractroid. The tractroid is obtained by revolving a tractrix about its asymptote. As an example, the (half) pseudosphere (with radius 1) is the surface of revolution of the tractrix parametrized by[2]

t(ttanht,secht),0t<.

It is a singular space (the equator is a singularity), but away from the singularities, it has constant negative Gaussian curvature and therefore is locally isometric to a hyperbolic plane.

The name "pseudosphere" comes about because it has a two-dimensional surface of constant negative Gaussian curvature, just as a sphere has a surface with constant positive Gaussian curvature. Just as the sphere has at every point a positively curved geometry of a dome the whole pseudosphere has at every point the negatively curved geometry of a saddle.

As early as 1693 Christiaan Huygens found that the volume and the surface area of the pseudosphere are finite,[3] despite the infinite extent of the shape along the axis of rotation. For a given edge radius R, the area is R2 just as it is for the sphere, while the volume is 2/3πR3 and therefore half that of a sphere of that radius.[4][5]

The pseudosphere is an important geometric precursor to mathematical fabric arts and pedagogy.[6]

Line congruence

A line congruence is a 2-parameter families of lines in 3. It can be written asX(u,v,t)=x(u,v)+tp(u,v)where each pick of u,v picks a specific line in the family.

A focal surface of the line congruence is a surface that is tangent to the line congruence. At each point on the surface,det(uX,vX,p)=0The above equation expands to a quadratic equation in t:det(ux(u,v)+tup(u,v),vx(u,v)+tvp(u,v),p(u,v))=0Thus, for each (u,v)2, there in general exists two choices of t1(u,v),t2(u,v). Thus a generic line congruence has exactly two focal surfaces parameterized by t1(u,v),t2(u,v).

For a bundle of lines normal to a smooth surface, the two focal surfaces correspond to its evolutes: the loci of centers of principal curvature.

In 1879, Bianchi proved that if a line congruence is such that the corresponding points on the two focal surfaces are at a constant distance 1, that is, |t1(u,v)t2(u,v)|=1, then both of the focal surfaces have constant curvature -1.

In 1880, Lie proved a partial converse. Let X be a pseudospherical surface. Then there exists a second pseudospherical surface X^ and a line congruence such that X and X^ are the focal surfaces of . Furthermore, X^ and may be constructed from X by integrating a sequence of ODEs.

Universal covering space

The pseudosphere and its relation to three other models of hyperbolic geometry

The half pseudosphere of curvature −1 is covered by the interior of a horocycle. In the Poincaré half-plane model one convenient choice is the portion of the half-plane with y ≥ 1.[7] Then the covering map is periodic in the x direction of period 2π, and takes the horocycles y = c to the meridians of the pseudosphere and the vertical geodesics x = c to the tractrices that generate the pseudosphere. This mapping is a local isometry, and thus exhibits the portion y ≥ 1 of the upper half-plane as the universal covering space of the pseudosphere. The precise mapping is

(x,y)(v(arcoshy)cosx,v(arcoshy)sinx,u(arcoshy)),

where

t(u(t)=ttanht,v(t)=secht)

is the parametrization of the tractrix above.

Hyperboloid

Deforming the pseudosphere to a portion of Dini's surface. In differential geometry, this is a Lie transformation. In the corresponding solutions to the sine-Gordon equation, this deformation corresponds to a Lorentz Boost of the static 1-soliton solution.

In some sources that use the hyperboloid model of the hyperbolic plane, the hyperboloid is referred to as a pseudosphere.[8] This usage of the word is because the hyperboloid can be thought of as a sphere of imaginary radius, embedded in a Minkowski space.

Relation to solutions to the sine-Gordon equation

Pseudospherical surfaces can be constructed from solutions to the sine-Gordon equation.[9] A sketch proof starts with reparametrizing the tractroid with coordinates in which the Gauss–Codazzi equations can be rewritten as the sine-Gordon equation.

On a surface, at each point, draw a cross, pointing at the two directions of principal curvature. These crosses can be integrated into two families of curves, making up a coordinate system on the surface. Let the coordinate system be written as (x,y).

At each point on a pseudospherical surface there in general exists two asymptotic directions. Along them, the curvature is zero. Let the angle between the asymptotic directions be θ.

A theorem states thatxxθyyθ=sinθIn particular, for the tractroid the Gauss–Codazzi equations are the sine-Gordon equation applied to the static soliton solution, so the Gauss–Codazzi equations are satisfied. In these coordinates the first and second fundamental forms are written in a way that makes clear the Gaussian curvature is −1 for any solution of the sine-Gordon equations.

Then any solution to the sine-Gordon equation can be used to specify a first and second fundamental form which satisfy the Gauss–Codazzi equations. There is then a theorem that any such set of initial data can be used to at least locally specify an immersed surface in 3.

This connection between sine-Gordon equations and pseudospherical surfaces mean that one can identify solutions to the equation with surfaces. Then, any way to generate new sine-Gordon solutions from old automatically generates new pseudospherical surfaces from old, and vice versa.

A few examples of sine-Gordon solutions and their corresponding surface are given as follows:

See also

References

  1. Beltrami, Eugenio (1868). "Saggio sulla interpretazione della geometria non euclidea" (in it). Gior. Mat. 6: 248–312. 

    (Republished in Beltrami, Eugenio (1902). Opere Matematiche. 1. Milan: Ulrico Hoepli. XXIV, Template:Pgs.  Translated into French as Beltrami, Eugenio (1869). "Essai d'interprétation de la géométrie noneuclidéenne". Annales Scientifiques de l'École Normale Supérieure. Ser. 1 6: 251–288. doi:10.24033/asens.60. Template:EuDML.  Translated into English as "Essay on the interpretation of noneuclidean geometry" by John Stillwell, in Stillwell 1996, pp. 7–34.)

  2. Bonahon, Francis (2009). Low-dimensional geometry: from Euclidean surfaces to hyperbolic knots. AMS Bookstore. p. 108. ISBN 978-0-8218-4816-6. https://books.google.com/books?id=YZ1L8S4osKsC. , Chapter 5, page 108
  3. Stillwell, John (2010). Mathematics and Its History (revised, 3rd ed.). Springer Science & Business Media. p. 345. ISBN 978-1-4419-6052-8. https://books.google.com/books?id=V7mxZqjs5yUC. , extract of page 345
  4. Le Lionnais, F. (2004). Great Currents of Mathematical Thought, Vol. II: Mathematics in the Arts and Sciences (2 ed.). Courier Dover Publications. p. 154. ISBN 0-486-49579-5. https://books.google.com/books?id=pCYDhbhu1O0C. , Chapter 40, page 154
  5. Weisstein, Eric W.. "Pseudosphere". http://mathworld.wolfram.com/Pseudosphere.html. 
  6. Roberts, Siobhan (15 January 2024). "The Crochet Coral Reef Keeps Spawning, Hyperbolically". The New York Times. https://www.nytimes.com/2024/01/15/science/mathematics-crochet-coral.html. 
  7. Thurston, William, Three-dimensional geometry and topology, 1, Princeton University Press, p. 62 .
  8. Hasanov, Elman (2004), "A new theory of complex rays", IMA J. Appl. Math. 69 (6): 521–537, doi:10.1093/imamat/69.6.521, ISSN 1464-3634, http://imamat.oxfordjournals.org/cgi/reprint/69/6/521 
  9. Wheeler, Nicholas. "From Pseudosphere to sine-Gordon equation". https://www.reed.edu/physics/faculty/wheeler/documents/Miscellaneous%20Math/Geometric%20Origin%20of%20Sine-Gordon/Pseudosphere%20to%20Sine-Gordon.pdf.