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arXiv math/0406225math.DGmath.SG

允许环面可积测地流的3维流形

3-Manifolds admitting toric integrable geodesic flows

Christopher R. Lee

AI总结:

本文利用余球面丛在环面可积时具有的接触环面流形结构,通过比较Betti数,得到紧连通3维流形上测地流环面可积的必要条件。

摘要:

紧流形 $Q$ 上黎曼度量的测地流,如果完全可积,且运动的首次积分在去掉零截面的余切丛 $T^*Q\setminus{Q}$ 上生成齐次环面作用,则称为环面可积的。若测地流环面可积,余球面丛具有接触环面流形的结构。通过比较接触环面流形与余球面丛的 Betti 数,我们能够给出紧、连通的3维流形上测地流环面可积的必要条件。

英文摘要:

The geodesic flow of a Riemannian metric on a compact manifold $Q$ is said to be toric integrable if it is completely integrable and the first integrals of motion generate a homogeneous torus action on the punctured cotangent bundle $T^*Q\setminus{Q}$. If the geodesic flow is toric integrable, the cosphere bundle admits the structure of a contact toric manifold. By comparing the Betti numbers of contact toric manifolds and cosphere bundles, we are able to provide necessary conditions for the geodesic flow on a compact, connected 3-dimensional manifold to be toric integrable.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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