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They call me Emilia. Years ago we moved to North Dakota and I adore every day living right here. He used to be unemployed but now he is a meter reader. Body developing is one of the things I love most.<br><br>Feel free to visit my site: [http://www.breda.nl/users/noeliadfebdftijfsdnt std testing at home]
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{{Expert-subject|Physics|date=February 2009}}
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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 force|tidal gravitational force]] will cause the trajectories to bend towards or away from each other, producing a relative [[acceleration]] between the objects.<ref name="ohanian">{{cite book|last1=Ohanian|first1=Hans|title=Gravitation and Spacetime|edition=1st|year=1976|pages=271&ndash;6}}</ref>
 
Mathematically, the tidal force in general relativity is described by the [[Riemann curvature tensor]],<ref name="ohanian" /> 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 field|Jacobi equation]].
 
== Geodesic deviation equation ==
 
To quantify geodesic deviation, one begins by setting up a family 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<sub>''s''</sub>(''t'') as ''t'' varies is a geodesic with affine parameter. If ''x''<sup>μ</sup>(''s'',&nbsp;''t'') are the coordinates of the geodesic  γ<sub>''s''</sub>(''t''), then the [[tangent vector]] of this geodesic is
 
:<math>T^\mu = \frac{\partial x^\mu(s, t)}{\partial t}.</math>
 
One can also define a ''deviation vector'', which is the displacement of two objects travelling along two infinitesimally separated geodesics:
 
:<math>X^\mu = \frac{\partial x^\mu(s, t)}{\partial s}.</math>
 
The ''relative acceleration'' ''A''<sup>μ</sup> of the two objects is defined, roughly, as the second derivative of the separation vector ''X''<sup>μ</sup> as the objects advance along their respective geodesics. Specifically, ''A''<sup>μ</sup> is found by taking the directional [[covariant derivative]] of ''X'' along ''T'' twice:
:<math> A^\mu = T^\alpha \nabla_\alpha (T^\beta \nabla_\beta X^\mu).</math>
 
The geodesic deviation equation relates ''A''<sup>μ</sup>, ''T''<sup>μ</sup>, ''X''<sup>μ</sup>, and the Riemann tensor ''R''<sup>μ</sup><sub>νρσ</sub>:<ref name="carroll">{{cite book|last=Carroll|first=Sean|title=Spacetime and Geometry|year=2004|pages=144&ndash;6}}</ref>
:<math> A^\mu = {R^\mu}_{\nu\rho\sigma} T^\nu T^\rho X^\sigma.</math>
 
An alternate notation for the directional covariant derivative <math>T^\alpha \nabla_\alpha</math> is <math>D/dt</math>, so the geodesic deviation equation may also be written as
:<math>\frac{D^2 X^\mu}{dt^2} = {R^\mu}_{\nu\rho\sigma} T^\nu T^\rho X^\sigma.</math>
 
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.{{Clarify|date=September 2009}} The Lagrangian approach has two advantages. First it allows various formal approaches of [[Quantization (physics)|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).{{Citation needed|date=September 2009}}
 
==See also==
*[[Bernhard Riemann]]
*[[Curvature]]
*[[Glossary of Riemannian and metric geometry]]
 
==References==
{{reflist}}
 
*{{Citation|title=General relativity - an introduction to the theory of the gravitation field|first=Hans|last=Stephani|publisher=Cambridge University Press|year=1982|isbn=0-521-37066-3}}.
*{{Citation | last1=Wald | first1=Robert M. | author1-link=Robert Wald | title=[[General Relativity (book)|General Relativity]] | isbn=978-0-226-87033-5 | year=1984}}.
 
==External links==
*[http://www.arXiv.org/abs/gr-qc/0404094 General Relativity and Quantum Cosmology]
*[http://www.mth.uct.ac.za/omei/gr/chap6/node11.html Tensors and Relativity: Geodesic deviation]
 
{{DEFAULTSORT:Geodesic Deviation Equation}}
[[Category:Geodesic (mathematics)]]
[[Category:Riemannian geometry]]
[[Category:Equations]]

Revision as of 02:14, 21 January 2014

Template:Multiple issues

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.[1]

Mathematically, the tidal force in general relativity is described by the Riemann curvature tensor,[1] 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 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 γs(t) as t varies is a geodesic with affine parameter. If xμ(st) are the coordinates of the geodesic γs(t), then the tangent vector of this geodesic is

Tμ=xμ(s,t)t.

One can also define a deviation vector, which is the displacement of two objects travelling along two infinitesimally separated geodesics:

Xμ=xμ(s,t)s.

The relative acceleration Aμ of the two objects is defined, roughly, as the second derivative of the separation vector Xμ as the objects advance along their respective geodesics. Specifically, Aμ is found by taking the directional covariant derivative of X along T twice:

Aμ=Tαα(TββXμ).

The geodesic deviation equation relates Aμ, Tμ, Xμ, and the Riemann tensor Rμνρσ:[2]

Aμ=RμνρσTνTρXσ.

An alternate notation for the directional covariant derivative Tαα is D/dt, so the geodesic deviation equation may also be written as

D2Xμdt2=RμνρσTνTρXσ.

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.Template:Clarify 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).Potter or Ceramic Artist Truman Bedell from Rexton, has interests which include ceramics, best property developers in singapore developers in singapore and scrabble. Was especially enthused after visiting Alejandro de Humboldt National Park.

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References

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