The geodesic equation can be derived using the action S0 = ∫dτ√−˙xμ⋅˙xμ
Let's find the eom in Minkowski space: 0=˙pμ=ddτ(−˙xμ√−˙xμ˙xμ+2λ˙xμ)
The square root in the first equation equals 1. So pμ=(2λ−1)˙xμ.
In the case λ≠12 this simply gives the old eom ¨x=0. However in the case λ=12 there is no restriction to ¨x.
I don't understand where this case λ=12 comes from. How do I deal with it? Can I simply neglect it? Or have I forgotten something?
Answer
First of all, we should stress that what OP calls τ is not† proper time off-shell but just some world-line (WL) parameterization. However, the constraint ˙xμ˙xμ ≈ −1
will imply that the WL parameter τ is the proper time on-shell.Since the EOM depends on the first derivative dλdτ of the Lagrange multiplier, we should specify a single condition, e.g. an inertial condition (IC) for λ. If we choose the IC different from 1/2, we avoid the problem when λ is 1/2.
The nature of the λ=1/2 pathology is a degeneracy of the constraint force/missing rank issue. To see this more clearly note that we can get an equivalent action ˜S = ∫τfτidτ(√1+λ(˙xμ˙xμ+1))
by inserting the constraint (A) into the first term in OP's action (4). If we repeat OP's calculation for the equivalent action ˜S we will see that the trouble has shifted to λ=0. Clearly, the case λ=0 corresponds to a degenerate case where the stationary action principle (B) is ill-defined.
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† If the WL parameter τ is proper time off-shell as well, it would mean that OP's action (4) is just S=τf−τi, which is fixed by boundary conditions (BC). In other words, the action would not depend on the WL, i.e. the variational problem would be ill-defined.
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