Riemann curvature tensor derivation

weio
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Hey,

when calculating the Riemann curvature tensor, you need to calculate the commutator of some vector field V, ie like this :-

[\bigtriangledown_a, \bigtriangledown_b] = \bigtriangledown_a\bigtriangledown_b - \bigtriangledown_b\bigtriangledown_a = V;_a_b - V;_b_a

But why does this difference of antisymmtery give us the Riemman tensor?

thanks
 
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weio said:
Hey,

when calculating the Riemann curvature tensor, you need to calculate the commutator of some vector field V, ie like this :-

[\bigtriangledown_a, \bigtriangledown_b] = \bigtriangledown_a\bigtriangledown_b - \bigtriangledown_b\bigtriangledown_a = V;_a_b - V;_b_a

But why does this difference of antisymmtery give us the Riemman tensor?

thanks

In addition to the commutator of the covariant derivatives, you need the commutator of the basis vectors too. Ignore torsion.

Think of your covariant derivative as a change along your basis. In a coordinate basis (defined by vanishing basis commutators) two different basis vectors span a plane. Think of a small quadrilateral spanned by the two basis vectors. When the vector V is carried around this quadrilateral your commutator of covariant derivatives gives the change in V. It's length can't change, but its direction does. So with R the full Riemann curvature:
[grada , gradb] V = R(.,V,a,b) . Riemann set up his geometry so it would look flat in the small. However, he was amazed that this difference resulting from taking a vector to nearby points could be described by an object (the full curvature tensor) that lived solely at the base point. This made him realize the importance of the curvature tensor and gave substance to his geometry.
 
Hey

So far this is how I understand it, though I know I could be very wrong. If you have two geodesics parallel to each other, with tangents V and V' , in which the coordinate x^\alpha point along both geodesics. There is some connecting vector w^\alpha between them. Let the affine parameter on the geodesics be \lambda

Riemman tensor calculates the acceleration between these two geodesics. so you calculate the acceleration at some point A, A' on each geodesic , and subtract them. this gives you an expression telling how the components of w^\alpha change.

\frac{d^2w^\alpha} {d\lambda^2} = \frac{d^2x^\alpha} {d\lambda^2} | A' - \frac {d^2x^\alpha} {d\lambda^2} | A = - \Gamma^\alpha_0_0_\beta w^\beta

After that you calculate the full 2nd covariant derivative along V, ie , you get something like
\bigtriangledown v \bigtriangledown v w^\alpha = (\Gamma^\alpha_\beta_0_0 - \Gamma^\alpha_0_0,\beta) w^\beta
= R^a_0_0\beta w^\beta
= R^a_u_v_\beta V^u V^v w^\beta

That's where the tensor arises. so basically it's a difference in acceleration as geodesics don't maintain their separation in curved space.
 
weio said:
Hey

So far this is how I understand it, though I know I could be very wrong. If you have two geodesics parallel to each other, with tangents V and V' , in which the coordinate x^\alpha point along both geodesics. There is some connecting vector w^\alpha between them. Let the affine parameter on the geodesics be \lambda

Riemman tensor calculates the acceleration between these two geodesics. so you calculate the acceleration at some point A, A' on each geodesic , and subtract them. this gives you an expression telling how the components of w^\alpha change.

\frac{d^2w^\alpha} {d\lambda^2} = \frac{d^2x^\alpha} {d\lambda^2} | A' - \frac {d^2x^\alpha} {d\lambda^2} | A = - \Gamma^\alpha_0_0_\beta w^\beta

After that you calculate the full 2nd covariant derivative along V, ie , you get something like
\bigtriangledown v \bigtriangledown v w^\alpha = (\Gamma^\alpha_\beta_0_0 - \Gamma^\alpha_0_0,\beta) w^\beta
= R^a_0_0\beta w^\beta
= R^a_u_v_\beta V^u V^v w^\beta

That's where the tensor arises. so basically it's a difference in acceleration as geodesics don't maintain their separation in curved space.

Yes it arises there and in many other places, including the one you asked about and that I told you about.
 
Thanks!

I understand the derivation now. I found a simple one which fully explains it. for the curious, here is the link :- http://www.anasoft.co.uk/physics/gr/reimann/reimann.html

weio
 
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