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Article

Discontinuous Normals in Non-Euclidean Geometries and Two-Dimensional Gravity

by
Emmanuele Battista
1,* and
Giampiero Esposito
2
1
Department of Physics, University of Vienna, Boltzmanngasse 5, A-1090 Vienna, Austria
2
Dipartimento di Fisica “Ettore Pancini” and INFN Sezione di Napoli, Complesso Universitario di Monte S. Angelo, Via Cintia Edificio 6, 80126 Napoli, Italy
*
Author to whom correspondence should be addressed.
Symmetry 2022, 14(10), 1979; https://doi.org/10.3390/sym14101979
Submission received: 8 August 2022 / Revised: 14 September 2022 / Accepted: 16 September 2022 / Published: 21 September 2022
(This article belongs to the Special Issue Symmetry in Gravity Research)

Abstract

:
This paper builds two detailed examples of generalized normal in non-Euclidean spaces, i.e., the hyperbolic and elliptic geometries. In the hyperbolic plane we define a n-sided hyperbolic polygon P , which is the Euclidean closure of the hyperbolic plane H , bounded by n hyperbolic geodesic segments. The polygon P is built by considering the unique geodesic that connects the n + 2 vertices z ˜ , z 0 , z 1 , , z n 1 , z n . The geodesics that link the vertices are Euclidean semicircles centred on the real axis. The vector normal to the geodesic linking two consecutive vertices is evaluated and turns out to be discontinuous. Within the framework of elliptic geometry, we solve the geodesic equation and construct a geodesic triangle. Additionally in this case, we obtain a discontinuous normal vector field. Last, the possible application to two-dimensional Euclidean quantum gravity is outlined.

1. Introduction

Suppose we want to measure the perimeter of a plane curve and we only have at our disposal a ruler, but not a wire that would perfectly match the boundary [1]. How are we going to evaluate the perimeter? One can indeed look for polygons whose sides are measurable with the help of the ruler, and one can “approximate” the shape of the curve by means of such polygons, asking ourselves the question by how much such polygons are close to the figure whose perimeter we want to evaluate. Within this framework, the very fruitful idea of Caccioppoli [2,3] was to “measure” the distance between the polygon and the figure by means of the area of the difference set. In order to gain an idea of the perimeter, we have to take a sequence of polygons, such that the area of the difference set becomes smaller, and they will provide a sequence of approximate values of the perimeter. However, the area-type approximation of the figure can be obtained also by means of polygons having a perimeter unnecessarily large (for example, if we curl a polygon, we can achieve a very large perimeter). Thus, among all sequences of polygons which approximate a geometric figure, we must take, among the limits of their perimeters, the smallest value, i.e., the minimal limit of perimeters of the approximating polygons.
The development of geometric measure theory [2,3,4,5,6,7,8,9,10,11,12] therefore led to the discovery of many important concepts including, in particular, finite-perimeter sets with their reduced boundary (see definitions in Appendix A), two concepts that play an important role in modern mathematics. With hindsight, one can say that the divergence theorem does not hold on the topological boundary of a finite-perimeter set, but only on the reduced boundary, which is therefore the truly important concept of the boundary. Let us here review some key aspects of this framework, which provide a motivation of our research.
If E R n is a finite-perimeter set, the De Giorgi structure theorem ensures that its reduced boundary * E can be written in the form
* E = l = 1 K l N 0 ,
where the K l are disjoint compact sets, and N 0 is a set having vanishing ( n 1 ) -dimensional Hausdorff measure. The sets K l are contained in ( n 1 ) -dimensional manifolds M l of class C 1 . If the point x belongs to K l , one finds that the generalized normal to E, denoted by ν E , can be obtained by the equation
ν E ( x ) = ν M l ( x ) .
This means that the normal ν E at x is given by the normal existing at x on the manifold M l (for this purpose, it is of crucial importance that the manifold M l should be of class C 1 ). Thus, the generalized normal is evaluated from the usual normal to a countable infinity of compact portions K l of smooth manifolds M l .
However, despite this profound result, the actual evaluation of the generalized normal may turn out to be impossible in some cases. In order to understand this feature, one can consider a dense sequence q k of points of R n . If the points q k are vectors with n components which have rational coordinates
q k 1 , q k 2 , , q k n ,
then within each ball B 1 k ( q k ) centred at the point q k R n and having radius 1 k one can find infinitely many points, and the same is true outside such a ball. The desired set E is in this case
E = k = 1 B 1 k ( q k ) ,
and its volume can be majorized as follows:
Vol ( E ) k = 1 Vol B 1 k ( q k ) = Vol ( B 1 ) k = 1 1 k n < ,
where B 1 is the ball of unit radius. We have therefore defined a finite-volume set. Although no picture can be drawn, one can think of E as consisting of infinitely many balls about the points q k of R n , which are dense in R n .
The topological boundary E of E coincides with the whole of R n minus E. In fact, given a point x of R n , one can find a sequence of points with rational coordinates, extracted from the sequence q k considered previously. Such an extracted sequence tends to x R n because the points with rational coordinates are dense. This means that x R n is an accumulation point for E. Thus x belongs to the closure E ¯ of E. In turn, since E is an open set (being formed by a countable union of open balls), the closure of E is given by
E ¯ = E E ,
and hence
E = R n E Vol ( E ) = + .
Let us now prove that E is a finite-perimeter set, despite the fact that its topological boundary has infinite volume. Indeed, by definition, the perimeter P ( E ) is given by
P ( E ) sup E div T d x : T L 1 , T C c 1 ( R n , R n ) ,
where the integral over E is a volume integral, and the defining conditions mean that T is a vector field of L norm never bigger than 1, of class C 1 on R n and having compact support on R n . By virtue of the definition (3), one can write the volume integral of the divergence of T in the form
E div T d x = lim m k = 1 m B 1 k ( q k ) div T d x .
The union of a finite number of balls B 1 k ( q k ) gives rise to an irregular set, because the balls do not have smooth intersections. Nevertheless, on such a set the divergence theorem holds, since such a set is piecewise smooth. One can therefore write, by virtue of the divergence theorem:
lim m k = 1 m B 1 k ( q k ) div T d x = lim m k = 1 m B 1 k ( q k ) T · ν d H n 1 ,
where ν is the normal to the topological boundary of the union of open balls, and d H n 1 is a surface measure. By virtue of (8) and (9), one finds the majorization ( H n 1 being the measure of the surface given by the topological boundary of the union of open balls B 1 k ( q k ) )
E div T d x lim m H n 1 k = 1 m B 1 k ( q k ) lim m k = 1 m H n 1 B 1 k ( q k ) ,
where, on the first line, we have exploited the majorization of the L norm of T and the unit norm of ν , while on the second line we have exploited the property
k = 1 m B 1 k ( q k ) k = 1 m B 1 k ( q k ) .
This latter condition means that the topological boundary of the union of balls B 1 k ( q k ) is in general smaller than the union of the various topological boundaries of such balls. Furthermore, we can re-express the majorization (10) as follows:
E div T d x lim m H n 1 B 1 k = 1 m 1 k n 1 M , if n 3 .
Indeed, if n 3 , one can find a constant M for which
k = 1 m 1 k n 1 M .
By virtue of (12), a real number M exists such that
E div T d x M P ( E ) M ,
i.e., the set E has a finite perimeter.
To sum up, the set E defined in Equation (3) is a finite-perimeter set of finite volume, while its topological boundary has infinite volume. Moreover, another consequence of De Giorgi’s structure theorem is that, if E is a finite-perimeter set and if T is a vector field of class C 1 , then
E div T = * E T · ν E d H n 1 .
Thus, the divergence theorem holds for a finite-perimeter set, but it does not involve the whole of the topological boundary E (because E might contain parts that are too irregular to see the divergence of T). The divergence theorem involves therefore only the reduced boundary * E , which represents the truly useful part of the topological boundary E . With hindsight, this is the ultimate meaning of De Giorgi’s structure theorem and of the concept of reduced boundary. The finite-perimeter sets are therefore the most general objects for which the divergence theorem still holds.
In the example we have investigated it is impossible to explicitly evaluate the generalized normal. Nevertheless, by virtue of De Giorgi’s structure theorem, we know some qualitative properties of great value: the reduced boundary is given by the countable union of pieces of manifolds of class C 1 , and the generalized normal is given by the normal to such manifolds. In such an example the reduced boundary is given by the countable union of pieces K l of smooth manifolds, and such pieces are represented by awkward-looking pieces of spherical surfaces. One can also prove, for this example, the inclusion property
* E k = 1 B 1 k ( q k ) ,
i.e., the reduced boundary is a subset of the countable union of the topological boundaries of all open balls centred at q k and having radius 1 k .
It is therefore clear that every explicit construction of generalized normal is a challenging task, which is nevertheless necessary if one wants to go beyond the purely qualitative properties. The following sections are devoted to two original examples, motivated by the desire to study geometric measure theory in non-Euclidean spaces. In particular, in Section 2 we deal with hyperbolic geometry, whereas the case of elliptic geometry is investigated in Section 3. The physical relevance of our framework is discussed in Section 4, where we consider possible applications to the action principle for two-dimensional Euclidean quantum gravity. In particular, we deal with the Euclidean two-dimensional Callan–Giddings–Harvey–Strominger (hereafter referred to as CGHS) dilaton gravity model [13,14,15] (see also Refs. [16,17,18,19]). As we will show, a two-dimensional model makes it possible to overcome the issue regarding the definition of the normal vector in higher-dimensional theories such as general relativity (for recent reviews of general relativity and beyond, see, e.g., Refs. [20,21,22] and references therein). Last, the concluding remarks are made in Section 5.

2. An Example of Generalized Normal in the Hyperbolic Plane

The hyperbolic (or Lobachevsky) plane [23,24,25] is defined as the upper half-plane H in the complex plane C
H = { z C : Im ( z ) > 0 } ,
endowed with the metric
g a b d x a d x b = d x d x + d y d y y 2 , ( a , b = 1 , 2 ) .
Geodesics (or hyperbolic lines) in H are defined in terms of Euclidean objects in C , being represented either by (the intersection of H with) Euclidean segments in C perpendicular to the real axis R = { z C : Im ( z ) = 0 } or by (the intersection of H with) Euclidean circles (strictly speaking, we should distinguish between a circle and the associated circumference) in C having Euclidean centre on R and Euclidean radius r. Any two points in H can be joined by a unique geodesic. Let φ : I R H be the piecewise differentiable path
φ = { z ( t ) = x ( t ) + i y ( t ) H : t I } ,
defining a geodesic in H . Bearing in mind (17), one finds that the geodesic (18) satisfies the following system of ordinary differential equations [26]:
{ (19a) y 2 = 0 , (19b) y ÿ + 2 ( ) 2 ( ) = 0 ,
where x ˙ ( t ) d x ( t ) d t and y ˙ ( t ) d y ( t ) d t . When x ˙ ( t ) = 0 t I , the solution of (19) is given by
z ( t ) = a , b e ± t , a R , b > 0 ,
representing a vertical line in H . On the other hand, if x ˙ ( t ) is nonvanishing, the system (19) leads to
z ( t ) = r tanh t + c , r cosh t , r > 0 , c R ,
which describes a Euclidean positive semicircle with an Euclidean centre at ( c , 0 ) and Euclidean radius r, since z ( t ) = ( x ( t ) , y ( t ) ) satisfies
x ( t ) c 2 + y 2 ( t ) = r 2 .
It is not difficult to show that the Euclidean center ( c , 0 ) and the Euclidean radius r of the Euclidean circle through p , q H can be written as [24]
c = 1 2 | p | 2 | q | 2 Re ( p ) Re ( q ) ,
r = | c p | = | c q | .
The hyperbolic length H ( γ ) of a piecewise differentiable path
γ = { z ( t ) = x ( t ) + i y ( t ) H : t I R } ,
is given by
H ( γ ) = I d t y ( t ) d z ( t ) dt .
The hyperbolic distance ρ H ( z , w ) between two points z , w H is defined by the formula
ρ H ( z , w ) = inf H ( γ ) ,
where the infimum is taken over all paths γ joining z , w H . Equation (26) defines a distance function on H , since it is non-negative, symmetric, and satisfies the triangle inequality [23]. Moreover, it can be shown that for any z , w H [23] (when the points z , w H are such that Re z = Re w , their hyperbolic distance reads as [23,24]
ρ H ( z , w ) Re z = Re w = log Im w Im z , Im w > Im z ) .
ρ H ( z , w ) = log | z w ¯ | + | z w | | z w ¯ | | z w | .
The hyperbolic distance ρ H ( z , w ) can also be written in terms of the Euclidean radius r and the Euclidean center ( c , 0 ) of the geodesic connecting z , w H as [24]
ρ H ( z , w ) = log w ( c + r ) z ( c r ) w ( c r ) z ( c + r ) .
The group of all isometries of H is isomorphic to the space PS L ( 2 , R ) , which is defined as follows:
PSL ( 2 , R ) z T ( z ) = ( a z + b ) ( c z + d ) | ( a d b c = 1 ) .
This is equivalent to expressing PSL ( 2 , R ) as the quotient space SL ( 2 , R ) / Z 2 because, if we change sign to all matrix entries, both T ( z ) and the determinant condition are preserved. Besides being a group, PSL ( 2 , R ) is also a topological space in which the fractional linear transformation T ( z ) can be identified with the point ( a , b , c , d ) of R 4 . More precisely, as a topological space, SL ( 2 , R ) can be identified with the following subset of R 4 :
X ( a , b , c , d ) R 4 : a d b c = 1 .
If one defines
δ ( a , b , c , d ) ( a , b , c , d ) ,
the map δ : X X is therefore a homeomorphism, and we can write that
PSL ( 2 , R ) = SL ( 2 , R ) / δ ,
which is a more precise expression of the quotient space formula involving Z 2 . Therefore PSL ( 2 , R ) is a topological group, and the fractional linear maps T have a norm induced from R 4 given by
T a 2 + b 2 + c 2 + d 2 .
A hyperbolic n-sided polygon P is a closed set of H R { } (i.e., the Euclidean closure of H ) bounded by n hyperbolic geodesic segments. The vertices of P , defined as the points of intersection of two line segments, can lie in R { } , although no segment of R can belong to P [23].
An example that makes it possible for us to display an explicit expression for the dual normal can be constructed as follows. Let
z ˜ = 0 , 1 ,
z 0 = 1 , 1 ,
z 1 = 1 + 1 3 , 1 2 ,
z 2 = 1 + 1 3 + 1 9 , 1 4 ,
z n 1 = 1 + 1 3 + 1 9 + + 1 3 n 1 , 1 2 n 1 ,
z n = 1 + 1 3 + 1 9 + + 1 3 n 1 + 1 3 n , 1 2 n
denote the n + 2 vertices of a hyperbolic ( n + 2 ) -sided polygon P . Such a polygon can be constructed by considering the unique geodesic connecting the following pairs of points: z ˜ and z 0 , z 0 and z 1 , z 1 and z 2 , …, z n 1 and z n , and eventually z n and z ˜ . Since the points occurring in Equation (29) have different real parts, all the aforementioned geodesics will be Euclidean positive semicircles with a centre on the real axis R . The generic geodesic φ n joining z n 1 and z n will be defined by
φ n = { z H : f ( z ) | z c n | 2 r n 2 = 0 } ,
where, from Equation (19), we have
c n = 1 2 | z n 1 | 2 | z n | 2 Re z n 1 Re z n ,
r n = | c n z n 1 | = | c n z n | .
Therefore, we find that
c n = 1 3 n j = 1 n 3 j + α n ,
r n = α n 2 + 1 2 2 n 2 ,
where
α n 2 2 n 3 2 n + 1 3 n 2 2 n + 1 .
The unit normal vector N ( n ) to the geodesic (30) will be
N ( n ) = N ( n ) 1 , N ( n ) 2 = y r n x c n , y , ( n N ) ,
with x , y subjected to the conditions x c n 2 + y 2 = r n 2 and y > 0 .
We note that
lim n c n = 3 2 , lim n r n = 0 ,
which define an Euclidean degenerate circle. From the above equation jointly with formula (28), we find that
ρ H z n 1 , z n n 0 .
We note that the above result cannot be obtained by employing Equation (27), since
z n n 3 2 , 0 ,
meaning that z n does not belong to H when n (see Appendix B for further details). In this limit, Equation (27) would lead to a meaningless result.
The geodesic φ ˜ connecting z ˜ and z 0
φ ˜ = { z H : f ( z ) | z c ˜ | 2 r ˜ 2 = 0 } ,
will have a Euclidean centre at ( c ˜ , 0 ) and Euclidean radius r ˜ , whereas for the geodesic φ ^ through z n and z ˜
φ ^ = { z H : f ( z ) | z c ^ | 2 r ^ 2 = 0 } ,
the Euclidean centre lies at ( c ^ , 0 ) and the Euclidean radius is r ^ . From Equation (23), we find
c ˜ = 1 2 , r ˜ = 5 2 ,
and
c ^ = 3 4 1 1 3 n + 1 + 3 n 1 2 2 n 2 2 n 3 n + 1 1 , r ^ = c ^ 2 + 1 .
In the limit of large n, we obtain
lim n c ^ = 5 12 , lim n r ^ = 13 12 ,
which agree with Equation (39) (cf. also Equation (37)).
The unit normal vector to the geodesic (40) will be
N ˜ = N ˜ 1 , N ˜ 2 = y r ˜ x c ˜ , y ,
x , y satisfying the conditions x c ˜ 2 + y 2 = r ˜ 2 and y > 0 , whereas the unit normal vector to (41) is
N ^ = N ^ 1 , N ^ 2 = y r ^ x c ^ , y ,
where x , y are such that the relations x c ^ 2 + y 2 = r ^ 2 and y > 0 are fulfilled.
The polygon P having vertices (29) has thus a generalized normal represented by Equations (36), (45), and (46), i.e.,
ν E = N ( n ) , N ˜ , N ^ , ( n N ) .
It follows from the above equation that the n-th segment of the polygon P admits a normal vector which differs from the one of the ( n + 1 ) -th segment. In other words, the generalized normal (47) defines a discontinuous vector field and, in the limit of large n, assumes an infinite number of values. Furthermore, we note that in our example the reduced boundary * E of the polygon P has a form that agrees with the De Giorgi structure theorem (cf. Equation (1)).

3. An Example of Generalized Normal in Elliptic Geometry

In Euclidean geometry, given a line and a point that does not lie on this line, there exists one and only one line that passes through the given point and is parallel to the given line. On the other hand, in hyperbolic geometry, which we have considered in the previous section, infinitely many distinct parallel lines can be found. A third option, where no parallel lines exist, gives rise to elliptic geometry [27] and will be considered here. The most common model of elliptic geometry is represented by the surface of a sphere (however, it should be noted that in elliptic geometry two lines are usually assumed to intersect at a single point, while in spherical geometry two great circles intersect at two points, which is why spherical geometry is said to be a doubly elliptic geometry). Another relevant example of (two-dimensional) elliptic geometry is Klein’s conformal model of the elliptic plane [27].
In this section, we consider an example of two-dimensional elliptic geometry having a squared line element [28]
d s 2 = d x 2 + d y 2 + x d y y d x 2 1 + x 2 + y 2 2 .
The resulting connection coefficients read as
Γ x x x x = 2 x 1 + x 2 + y 2 , Γ x x y x = y 1 + x 2 + y 2 , Γ y x y y = x 1 + x 2 + y 2 , Γ y y y y = 2 y 1 + x 2 + y 2 ,
and hence the geodesic equations take the form
{ (50a) x = 2 x ( 1 + x 2 + y 2 ) ( x x + y y ) , (50b) y = 2 y ( 1 + x 2 + y 2 ) ( x x + y y ) ,
, where the prime denotes differentiation with respect to the affine parameter τ . If we eliminate the factor ( x x + y y ) / ( 1 + x 2 + y 2 ) from the second equation and substitute it in the first, we get
d d τ log x y = 0 ,
which leads to
x ( τ ) = α 1 y ( τ ) + α 2 , ( α 1 0 , α 2 R ) .
Then, from Equations (50b) and (52) we obtain the geodesic solutions
x ( τ ) = α 2 + α 1 1 + α 1 2 + α 2 2 tan c 1 τ + c 2 1 + α 1 2 + α 2 2 1 + α 1 2 ,
y ( τ ) = α 1 α 2 + 1 + α 1 2 + α 2 2 tan c 1 τ + c 2 1 + α 1 2 + α 2 2 1 + α 1 2 ,
where c 1 and c 2 are integration constants.
We note that the system (50) is not affected if we interchange the role of x and y, i.e., it is invariant under the transformation
x y .
This means that
x 2 ( τ ) = α ˜ 1 α ˜ 2 + 1 + α ˜ 1 2 + α ˜ 2 2 tan c ˜ 1 τ + c ˜ 2 1 + α ˜ 1 2 + α ˜ 2 2 1 + α ˜ 1 2 ,
y 2 ( τ ) = α ˜ 2 + α ˜ 1 1 + α ˜ 1 2 + α ˜ 2 2 tan c ˜ 1 τ + c ˜ 2 1 + α ˜ 1 2 + α ˜ 2 2 1 + α ˜ 1 2 ,
is a solution of Equation (50), where c ˜ 1 , c ˜ 2 are real-valued integration constants and
y 2 ( τ ) = α ˜ 1 x 2 ( τ ) + α ˜ 2 , ( α ˜ 1 0 , α ˜ 2 R ) .
We can now set up a geodesic triangle T by means of Equations (52)–(54). Let
A ( 0 , 1 ) , B ( 1 , 0 ) , C ( 0 , 1 ) ,
be the vertices of T (see Figure 1).
Then, the side T A B of T connecting A and B is parametrized by
T A B : x A B ( τ ) = 1 2 1 + 3 tan 2 3 3 + τ , y A B ( τ ) = 1 2 1 + 3 tan 2 3 3 + τ , τ 1 τ τ 2 ,
where
τ 1 6 3 + π / 6 2 3 , τ 2 6 3 π / 6 2 3 ,
and the functions x A B ( τ ) and y A B ( τ ) can be obtained from Equations (53) and (54), respectively, by setting
α 1 = α 2 = 1 ,
c 1 = 2 ,
c 2 = 3 .
The side T B C , which links the vertices B and C, is defined by
T B C : x B C ( τ ) = 1 2 1 3 tan 2 3 3 + τ , y B C ( τ ) = 1 2 1 + 3 tan 2 3 3 + τ , τ 1 τ τ 2 .
The functions x B C ( τ ) and y B C ( τ ) can be read off from Equations (53) and (54), respectively, with
α 1 = α 2 = 1 ,
c 1 = 2 ,
c 2 = 3 .
Last, T C A can be obtained from
T C A : x C A ( τ ) = 0 , y C A ( τ ) = tan 2 3 + τ , τ 3 τ τ 4 ,
with
τ 3 1 2 6 π / 4 , τ 4 1 2 6 + π / 4 ,
the functions x C A ( τ ) and y C A ( τ ) stemming from Equations (53) and (54), respectively, when
α 1 = α 2 = 0 ,
c 1 = 2 ,
c 2 = 3 .
It should be noted that the solution having α 1 = 0 can be regarded as a “limiting” case of Equations (52)–(54).
At this stage, we are ready to evaluate the normal vector field to the geodesic triangle T . Given the curve y = f ( x ) , it is known that the equation of its normal to a generic point with the coordinates ( X , Y ) is [29]
y Y = 1 f ( X ) x X ,
the prime denoting differentiation with respect to the x variable. In our example, the geodesics can be equivalently described by means of (cf. Equation (52))
y ( x ) = x α 1 α 2 α 1 , ( α 1 0 , α 2 R ) ,
which means that, recalling Equation (62a), the equation of the side T A B reads also as (it is clear that Equation (70) can also be obtained from Equation (60))
T A B : y A B x = x 1 , x [ 0 , 1 ] ,
and hence by virtue of Equation (68) the normal vector field N A B to T A B is defined by
N A B : y n A B x = x + x ¯ + y ¯ ,
where ( x ¯ , y ¯ ) are the coordinates of a generic point belonging to T A B . As a consequence of (64a) (or, equivalently, Equation (63)), we have for the side T B C
T B C : y B C x = x + 1 , x [ 0 , 1 ] ,
from which we derive the form of its normal vector field N B C
N B C : y n B C x = x x ^ + y ^ ,
( x ^ , y ^ ) being the coordinates of a point lying on T B C . As pointed out previously, the side T C A cannot be obtained directly from (69). Indeed, its equation is
T C A : x C A = 0 , 1 y 1 ,
which means that N C A is
N C A : y n C A = k , 1 k 1 .
Likewise the hyperbolic example discussed in Section 2, Equations (71), (73), and (75) give rise to a discontinuous normal vector field.

4. Application to Two-Dimensional Euclidean Quantum Gravity

As far as we know, the kind of thinking used so far in our paper has been lacking in the literature on fundamental interactions in physics. In recent times, much work in the mathematical literature has been devoted to the investigation of geometric measure theory in non-Euclidean spaces [30]. Within such a framework, the occurrence of discontinuous normal vector fields has to be considered [10], and our original explicit examples in Section 2 and Section 3 can be of interest.
On the other hand, the examples of Section 2 and Section 3 have a clear mathematical motivation, but they do not have an impact on theoretical physics. For this purpose, we are currently considering the case of Euclidean quantum gravity [31,32,33,34,35,36,37,38,39,40]. Within this framework, a prescription for functional integration is necessary, and we propose to consider only finite-perimeter sets that match the assigned data on their reduced boundary. We arrive at this prescription upon bearing in mind that measurable sets belong to two families: either they have finite perimeter, or they do not. The restriction to finite-perimeter sets might be severe, but it leads to mathematical properties which are under control and hence merits a careful assessment.
A second choice is also in order, and it has to do with the dimension of such finite-perimeter sets. In higher dimensions a problem arises, i.e., how to define a vector that plays the role of normal. Even just for a straight line in three-dimensional Euclidean space, what is defined is the plane orthogonal to such a line, but there is no coordinate-independent way of selecting two linearly independent normal vector fields to the line. Thus, a four-dimensional analogue of our Section 2 and Section 3 is not conceivable, as far as we can see. We have therefore resorted to two-dimensional Euclidean quantum gravity, by focusing on the Euclidean two-dimensional CGHS dilaton gravity model [13,14,15] (see also e.g., Ref. [41] for a general framework pertaining to Euclidean dilaton gravity in two dimensions). This example will clarify the role of the discontinuous normal ν E occurring in the divergence theorem (14).
The Euclidean CGHS action reads as
I E = 1 2 π d 2 x g e 2 ϕ R + 4 μ ϕ μ ϕ + 4 Λ 2 ,
g denoting the metric determinant, R the Ricci scalar, ϕ the dilaton field, and Λ 2 a cosmological constant. Bearing in mind the recipes of Ref. [42] (see also Refs. [43,44]), we can write the variations of the Lagrangian L E occurring in Equation (76) as
δ g L E = g 2 π E g μ ν δ g μ ν + E ϕ δ ϕ + α Θ α ,
where
E g μ ν = 0 , E ϕ = 0 ,
are the metric and the dilaton field equations, respectively, and Θ α is referred to as the symplectic potential current density. By virtue of Equation (76), we find
E g μ ν = 2 e 2 ϕ g μ ν ( α ϕ ) ( α ϕ ) Λ 2 α α ϕ + μ ν ϕ ,
E ϕ = 2 e 2 ϕ R + 4 α α ϕ + 4 Λ 2 4 α ϕ α ϕ ,
Θ α = e 2 ϕ [ 8 α ϕ δ ϕ μ δ g μ α + g μ ν α δ g μ ν 2 μ ϕ δ g μ α + 2 α ϕ g μ ν δ g μ ν ] .
We aim at evaluating the integral
1 2 π C d 2 x g α Θ α ,
where C is a two-dimensional region having finite perimeter. For this purpose, we find it more convenient to consider an off-shell calculation, i.e., for metric and dilaton field which do not obey the Euclidean field equations. In such a way, we may choose an example as close as possible to the ones developed in the theory of finite-perimeter sets in n-dimensional Euclidean space [11], while avoiding the difficult task of solving the coupled partial differential equations for metric and dilaton.

Preparing the Ground for Evaluating the Integral

In order to prepare the ground for investigating the integral (80), let us consider the following example of two-dimensional finite-perimeter set [11], which provides a slight modification of the case discussed in Section 1 (which we recall is valid in R n with n 3 , see Equation (12)). Consider in R 2 the set E defined by
E = k = 1 B r k ( x k )
where, as before, B r k ( x k ) denotes the Euclidean open ball centred at the point x k R 2 and having small positive radius r k , which is supposed to satisfy
r k < ε , k N ,
such that
2 ω 2 k = 1 r k 1 ,
with
ω 2 = Γ ( 1 / 2 ) 2 Γ ( 1 ) = π ,
Γ ( n ) being the Euler Γ -function. The perimeter of B r k ( x k ) is
P B r k ( x k ) = H 1 B r k ( x k ) = 2 ω 2 r k ,
H 1 denoting the one-dimensional Hausdorff measure. Starting from Equation (85), it can be shown [11] that for every N N , the set
E N = k = 1 N B r k ( x k ) ,
has finite perimeter since, by virtue of Equation (83),
P ( E N ) k = 1 N P B r k ( x k ) 2 ω 2 k = 1 r k 1 .
Therefore, as | E | ω 2 < ( | E | being the volume of E), we have E N E as N and hence
P ( E ) 1 ,
which means that E has finite perimeter. Furthermore, it is possible to prove that | E | ω 2 ε , which implies as a consequence H 1 ( E ) = [11].
We can now extend the previous example to a two-dimensional analytic Riemannian manifold M . For this reason, let us consider the two-dimensional geodesic ball B r G ( p ) having small positive radius r and centred at the point p M . The volume V r ( p ) of B r G ( p ) can be written by means of the power series [45]
V r ( p ) = ω 2 r 2 [ 1 R 24 r 2 + r 4 8640 ( 3 R μ ν ρ σ R μ ν ρ σ + 8 R μ ν R μ ν + 5 R 2 18 μ μ R ) + O r 6 ] p ,
whereas the volume S r ( p ) of B r G ( p ) reads as [45]
S r ( p ) = 2 ω 2 r [ 1 R 12 r 2 + r 4 2880 ( 3 R μ ν ρ σ R μ ν ρ σ + 8 R μ ν R μ ν + 5 R 2 18 μ μ R ) + O r 6 ] p .
If the trace R of the Ricci tensor is positive, then it follows from Equations (89) and (90) that, for sufficiently small r,
V r ( p ) < ω 2 r 2 ,
and
S r ( p ) < 2 ω 2 r ,
respectively.
At this stage, we have the necessary ingredients to generalize the previous example to the case when the manifold M admits a positive trace R of Ricci. Indeed, along the same lines as before, let
C = k = 1 B r k G ( x k ) ,
be a surface of M constructed in terms of the geodesic balls B r k G ( x k ) whose radius r k is subject to the condition (83). Bearing in mind Equation (92), we have
P B r k G ( x k ) = H 1 B r k G ( x k ) < 2 ω 2 r k ,
which makes it possible for us to prove that the set
C N = k = 1 N B r k G ( x k ) ,
has finite perimeter, since, similarly to Equation (87),
P ( C N ) k = 1 N P B r k ( x k ) < 2 ω 2 k = 1 r k 1 .
Therefore, the set C , which can be obtained from C N in the limit N , has finite perimeter with
P ( C ) < 1 ,
although H 1 ( C ) = .

5. Concluding Remarks

By means of the methods presented in our paper, it is possible to evaluate the integral (80) over the finite-perimeter set C , and we hope to have outlined the good potentialities of geometric measure theory for a fresh look at the unsolved problems of traditional formulations of Euclidean quantum gravity.
The next task wil be the rigorous proof of existence theorems of Euclidean functional integrals for gravity in two and higher dimensions, when restricted to finite-perimeter sets. If it were possible to accomplish this, the associated reduced boundary construction might open a new era in quantum gravity and quantum cosmology.

Author Contributions

The authors have given equal weight contributions to the conceptual and technical parts of their paper. All authors have read and agreed to the published version of the manuscript.

Funding

Austrian Science Fund (FWF) grant P32086.

Data Availability Statement

All calculations are reproducible by hand, and hence no data have been stored.

Acknowledgments

E.B. is grateful to Nicola Fusco for invaluable discussions regarding many relevant topics of geometric measure theory. The authors thank Marco Abate for the enlightening correspondence. This work is supported by the Austrian Science Fund (FWF) grant P32086. G.E. dedicates this research to Margherita.

Conflicts of Interest

The authors declare no conflict of interest.

Appendix A. Finite-Perimeter Sets and Their Reduced Boundary

On denoting by φ ( x , E ) the characteristic function of a set E R n (by definition, φ ( x , E ) equals 1 at points x E , and 0 otherwise) and by * the convolution product of two functions defined on R n :
f * h ( x ) f ( x ξ ) h ( ξ ) d ξ ,
De Giorgi defined [4,5,7] for all integer n 2 and for all λ > 0 the function
φ λ : x φ λ ( x ) ( π λ ) n 2 exp k = 1 n ( x k ) 2 λ * φ ( x , E ) ,
and, as a next step, the perimeter of the set E R n
P ( E ) lim λ 0 R n k = 1 n φ λ x k 2 d x .
The perimeter defined in Equation (A3) is not always finite. A necessary and sufficient condition for P ( E ) to be finite is the existence of a set function of vector nature completely additive and bounded, defined for any set B R n and denoted by a ( B ) , verifying the generalized Gauss–Green formula
E D h d x = R n h ( x ) d a .
If Equation (A4) holds, the function a is said to be the distributional gradient of the characteristic function φ ( x , E ) . A polygonal domain is every set E R n that is, the closure of an open set and whose topological boundary E is contained in the union of a finite number of hyperplanes of R n . The sets approximated by polygonal domains having finite perimeter were introduced by Caccioppoli [2,3] and coincide with the collection of all finite-perimeter sets [7]. This is why finite-perimeter sets are said to be Caccioppoli sets.
If E is a finite-perimeter set of R n , its reduced boundary * E is the collection of all points ξ for which:
(i)
The integral of the norm of the gradient of the characteristic function, when taken over the ball (our ball is called open hypersphere by De Giorgi) centred at ξ and of radius ρ , is always positive, i.e.,
B ρ ( ξ ) grad φ ( x , E ) > 0 ρ > 0 ,
(ii)
The limit defining the normal vector exists, i.e.,
lim ρ 0 B ρ ( ξ ) grad φ ( x , E ) B ρ ( ξ ) grad φ ( x , E ) = ν ( ξ ) ,
(iii)
The resulting normal vector has the unit Euclidean norm.

Appendix B. Calculation of the Hyperbolic Distance in the Limit of Large n

In Section 2, we evaluated the large-n limit of the hyperbolic distance ρ H z n 1 , z n between the vertices z n 1 and z n of the ( n + 2 ) -sided hyperbolic polygon P , defined by Equation (29), by employing Equation (28). The final result of this computation is displayed in Equation (38). In this appendix, we show how the application of Equation (27) for this calculation would have led to a misleading result.
Bearing in mind Equations (29e) and (29f), from Equation (27) we obtain
ρ H z n 1 , z n = log 1 + 2 2 n + 3 2 n 2 2 n + 3 2 n + 2 1 2 2 n + 3 2 n 2 2 n + 3 2 n + 2 ,
and hence, in the limit of large n, the above equation yields
lim n ρ H z n 1 , z n = log 1 + 1 9 1 1 9 = log 2 .
Therefore, in Equation (A8) we recover a different result from the one given in Equation (38). As pointed out before, this is due to the fact that the vertices z n 1 and z n of the polygon P do not belong, in the limit of large n, to the hyperbolic plane H , and hence Equation (27) becomes meaningless under this hypothesis.

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Figure 1. The geodesic triangle T having vertices (59) and parametrized by Equations (60), (63), and (65).
Figure 1. The geodesic triangle T having vertices (59) and parametrized by Equations (60), (63), and (65).
Symmetry 14 01979 g001
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Battista, E.; Esposito, G. Discontinuous Normals in Non-Euclidean Geometries and Two-Dimensional Gravity. Symmetry 2022, 14, 1979. https://doi.org/10.3390/sym14101979

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Battista, Emmanuele, and Giampiero Esposito. 2022. "Discontinuous Normals in Non-Euclidean Geometries and Two-Dimensional Gravity" Symmetry 14, no. 10: 1979. https://doi.org/10.3390/sym14101979

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Battista, E., & Esposito, G. (2022). Discontinuous Normals in Non-Euclidean Geometries and Two-Dimensional Gravity. Symmetry, 14(10), 1979. https://doi.org/10.3390/sym14101979

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