Extrinsic Curvature as Geodesics Deviation
Extrinsic Curvature as Geodesics Deviation
Extrinsic Curvature as Geodesics Deviation
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References<br />
[1] R. M. Wald, “General Relativity,” (The University of Chicago Press, Chicago and London,<br />
1984), Chapter 10.<br />
[2] C. Misner, K. Thorne and J. A. Wheeler, “Gravitation,” (Freeman, San Francisco, 1973),<br />
Chapter 21.<br />
expressed explicitly by its coefficients and b<strong>as</strong>is. Thus equation (26) is written <strong>as</strong><br />
∇ a (I) n = (I) K b<br />
a e b +<br />
C∑<br />
J=1,J≠I<br />
where e a are b<strong>as</strong>is vectors of Σ. And equation (29) can be rewritten <strong>as</strong><br />
( )<br />
K = h ab e b ⊗ ∇ (1)<br />
a n ∧ (2) n ∧ ... ∧ (C) n = h ab e b ⊗<br />
Now combine above two equations, we have<br />
K =h ab e b ⊗<br />
=e a ⊗<br />
C∑<br />
I=1<br />
C∑<br />
I=1<br />
C∑<br />
I=1<br />
(J) ɛ (J) n (IJ) B δ , (30)<br />
(<br />
( )<br />
)<br />
(1) n ∧ (2) n ∧ ... ∧ ∇ (I) a n ∧ ... ∧ (C) n . (31)<br />
(<br />
)<br />
(I) Ka<br />
c (1) n ∧ (2) n ∧ ... ∧ e c ∧ ... ∧ (C) n<br />
(<br />
)<br />
(I) K (1) ab n ∧ (2) n ∧ ... ∧ e b ∧ ... ∧ (C) n , (32)<br />
where we have defined e a ≡ h ab e b and in the above sum, e c (e b ) occupies the Ith position and (I) n is removed.<br />
Equation (32) shows clearly there is an one-to-one correspondence between K and (I) K ab .<br />
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