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Liouville surface

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In the mathematical field of differential geometry a Liouville surface (named after Joseph Liouville) is a type of surface which in local coordinates may be written as a graph in R

z = f ( x , y ) {\displaystyle z=f(x,y)}

such that the first fundamental form is of the form

d s 2 = ( f 1 ( x ) + f 2 ( y ) ) ( d x 2 + d y 2 ) . {\displaystyle ds^{2}={\big (}f_{1}(x)+f_{2}(y){\big )}\left(dx^{2}+dy^{2}\right).}

Sometimes a metric of this form is called a Liouville metric. Every surface of revolution is a Liouville surface.

Darboux gives a general treatment of such surfaces considering a two-dimensional space ( u , v ) {\displaystyle (u,v)} with metric

d s 2 = ( U V ) ( U 1 2 d u 2 + V 1 2 d v 2 ) , {\displaystyle ds^{2}=(U-V)(U_{1}^{2}\,du^{2}+V_{1}^{2}\,dv^{2}),}

where U {\displaystyle U} and U 1 {\displaystyle U_{1}} are functions of u {\displaystyle u} and V {\displaystyle V} and V 1 {\displaystyle V_{1}} are functions of v {\displaystyle v} . A geodesic line on such a surface is given by

U 1 d u U α V 1 d v α V = 0 {\displaystyle {\frac {U_{1}\,du}{\sqrt {U-\alpha }}}-{\frac {V_{1}\,dv}{\sqrt {\alpha -V}}}=0}

and the distance along the geodesic is given by

d s = U U 1 d u U α V V 1 d v α V . {\displaystyle ds={\frac {UU_{1}\,du}{\sqrt {U-\alpha }}}-{\frac {VV_{1}\,dv}{\sqrt {\alpha -V}}}.}

Here α {\displaystyle \alpha } is a constant related to the direction of the geodesic by

α = U sin 2 ω + V cos 2 ω , {\displaystyle \alpha =U\sin ^{2}\omega +V\cos ^{2}\omega ,}

where ω {\displaystyle \omega } is the angle of the geodesic measured from a line of constant v {\displaystyle v} . In this way, the solution of geodesics on Liouville surfaces is reduced to quadrature. This was first demonstrated by Jacobi for the case of geodesics on a triaxial ellipsoid, a special case of a Liouville surface.

Notes

  1. Liouville 1846
  2. Darboux 1894, §§583-584
  3. Jacobi 1839

References

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