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Gravity and Strings

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7.1 Schwarzschild’s solution 191<br />

where p α =−mdx α /dτ is the observer’s four-momentum, τ is the observer’s<br />

proper time, <strong>and</strong> we have set ξ = cτ. Onthe other h<strong>and</strong>, since the Schwarzschild<br />

metric admits a timelike Killing vector k µ = δ µ0 , the observer’s motion<br />

has an associated conserved momentum p(k) ≡ p 0 given by Eq. (3.266) that<br />

we can identify with the observer’s total energy<br />

E =−p 0 c. (7.10)<br />

To simplify the calculations, we assume that the observer has only radial motion<br />

(i.e. zero angular momentum) so pθ = pϕ = 0. Then, using the conservation of<br />

the energy, the mass-shell constraint becomes a simple equation for pr , which<br />

is a differential equation for r,<br />

2 <br />

dr E<br />

=<br />

cdτ mc2 2 − W, (7.11)<br />

that can be integrated to give the total proper time:<br />

where<br />

τ = 1<br />

r2<br />

dr<br />

c r1<br />

R0 =<br />

RS<br />

r<br />

RS<br />

1 − [E/(mc 2 )] 2<br />

1<br />

−<br />

RS<br />

2<br />

− , (7.12)<br />

R0<br />

(7.13)<br />

is the value of the radial coordinate r for which the speed of the observer is zero<br />

<strong>and</strong> E = mc2 .<br />

We can use the above expression to calculate how long it takes for the freefalling<br />

observer to go from r = R0 > RS to the curvature singularity at r = 0,<br />

going through the surface r = RS. The answer is, surprisingly, finite:<br />

τ = π<br />

2c R0<br />

1<br />

R0<br />

2<br />

RS<br />

. (7.14)<br />

This confirms that nothing unphysical happens at r = RS <strong>and</strong> that the singularity<br />

is only a problem of Schwarzschild’s coordinates. It should, then, be possible<br />

to find a coordinate system which is not singular there. 10<br />

This is essentially the idea on which the Eddington–Finkelstein coordinates<br />

{v,r,θ,ϕ} are based [345, 394]. In these coordinates the Schwarzschild solution<br />

takes the form<br />

ds 2 = Wdv 2 − 2dvdr − r 2 d 2 (2) , (7.15)<br />

where the coordinate v is related to t <strong>and</strong> r in the region r > RS by<br />

v = ct + r + RS ln |W |, (7.16)<br />

10 There is, of course, another issue: whether the tidal forces at the horizon are big or small. For big enough<br />

Schwarzschild BHs they are small, but this might not be a universal behavior of BHs [555, 556].

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