
5.2 Mathematical properties of the world function 77
This relation stems from the requirement that the connector preserves the scalar
product. Along any curve connecting points
P
0
and P
1
we have
(u ·v)
0
=(ˇu · ˇv)
1
, (5.16)
with u, v ∈ T
P
0
(M) and ˇu, ˇv ∈ T
P
1
(M).
Let us conclude this brief summary by recalling the concept of geodesic on the
manifold. A curve γ connecting
P
0
to P
1
is geodesic if
Γ(s
0
,s
1
; γ)˙γ
(0)
= f(s
1
)˙γ
(1)
, (5.17)
where f(s) is a differentiable function on γ. As stated, a geodesic can always be
reparameterized with s
(s) so that f(s
(s)) = 1; in this case the parameter s
is
termed affine. An affine parameter is defined up to linear transformations.
5.2 Mathematical properties of the world function
The world function behaves as a scalar at each of its end-points and can be
differentiated at each of them separately; in this case it generates new functions
which may behave as a scalar at one point and a vector or 1-form at the other,
or as a 1-form at the first point and as a vector at the other, and so on. To
define the derivatives of a world function we shall consider only those whose end-
points are connected by a geodesic. If we further restrict our analysis to normal
neighborhoods then the geodesic connecting any two points is unique. The world
function can be written as
Ω(s
0
,s
1
;Υ)=
1
2
(s
1
− s
0
)
2
X · X, (5.18)
where X =
˙
Υ denotes the tangent vector to the unique geodesic Υ joining
P
0
to P
1
and parameterized by s. We shall now deduce the derivatives of Ω with respect to
variations of its two end-points. Let
P
0
and P
1
belong to smooth curves ˜γ
0
and ˜γ
1
,
parameterized by t,andletΥ
t
≡ Υ
˜γ
0
(t)→˜γ
1
(t)
be the geodesic connecting points
of ˜γ
0
to points of ˜γ
1
. We then require that the curve connecting the points P
0
and P
1
as they vary independently on the curves ˜γ
0
and ˜γ
1
is the unique geodesic
Υ
P
0
→P
1
. In this case the points we are considering belong also to the geodesic
Υ
t
so they can be referred to as P
0
=Υ
t
(s
0
)andP
1
=Υ
t
(s
1
). This situation
is depicted in Fig. (5.1). We then have a one-parameter family of geodesics C
X
with connecting vector Y =
˙
˜γ, namely £
X
Y = 0. By definition we have
DX
ds
=0,
DX
dt
=
DY
ds
. (5.19)
To pursue our task let us write
d
dt
Ω(Υ
t
(s
0
), Υ
t
(s
1
); Υ
t
)=
∂Ω
∂x
α
0
Y
α
0
+
∂Ω
∂x
α
1
Y
α
1
=(s
1
− s
0
)
2
DX
dt
· X
, (5.20)