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翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Geodesic deviation ： ウィキペディア英語版 Geodesic deviation In general relativity, geodesic deviation describes the tendency of objects to approach or recede from one another while moving under the influence of a spatially varying gravitational field. Put another way, if two objects are set in motion along two initially parallel trajectories, the presence of a tidal gravitational force will cause the trajectories to bend towards or away from each other, producing a relative acceleration between the objects. Mathematically, the tidal force in general relativity is described by the Riemann curvature tensor,〔 and the trajectory of an object solely under the influence of gravity is called a ''geodesic''. The ''geodesic deviation equation'' relates the Riemann curvature tensor to the relative acceleration of two neighboring geodesics. In differential geometry, the geodesic deviation equation is more commonly known as the Jacobi equation. == Geodesic deviation equation == To quantify geodesic deviation, one begins by setting up a family of closely spaced geodesics indexed by a continuous variable ''s'' and parametrized by an affine parameter ''t''. That is, for each fixed ''s'', the curve swept out by γ''s''(''t'') as ''t'' varies is a geodesic with affine parameter. If ''x''μ(''s'', ''t'') are the coordinates of the geodesic γ''s''(''t''), then the tangent vector of this geodesic is :$T^\backslash mu\; =\; \backslash frac.$ One can also define a ''deviation vector'', which is the displacement of two objects travelling along two infinitesimally separated geodesics: :$X^\backslash mu\; =\; \backslash frac.$ The ''relative acceleration'' ''A''μ of the two objects is defined, roughly, as the second derivative of the separation vector ''X''μ as the objects advance along their respective geodesics. Specifically, ''A''μ is found by taking the directional covariant derivative of ''X'' along ''T'' twice: :$A^\backslash mu\; =\; T^\backslash alpha\; \backslash nabla\_\backslash alpha\; (T^\backslash beta\; \backslash nabla\_\backslash beta\; X^\backslash mu).$ The geodesic deviation equation relates ''A''μ, ''T''μ, ''X''μ, and the Riemann tensor ''R''μνρσ: :$A^\backslash mu\; =\; \_\; T^\backslash nu\; T^\backslash rho\; X^\backslash sigma.$ An alternate notation for the directional covariant derivative $T^\backslash alpha\; \backslash nabla\_\backslash alpha$ is $D/dt$, so the geodesic deviation equation may also be written as :$\backslash frac\; =\; \_\; T^\backslash nu\; T^\backslash rho\; X^\backslash sigma.$ The geodesic deviation equation can be derived from the second variation of the point particle Lagrangian along geodesics, or from the first variation of a combined Lagrangian. The Lagrangian approach has two advantages. First it allows various formal approaches of quantization to be applied to the geodesic deviation system. Second it allows deviation to be formulated for much more general objects than geodesics (any dynamical system which has a one spacetime indexed momentum appears to have a corresponding generalization of geodesic deviation). 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Geodesic deviation」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.