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Astron. Astrophys. 327, 867-889 (1997)
Appendix A: continuity and nondifferentiability implies scale-divergence
One can demonstrate
(Nottale 1993a,
1996a) that the length of a
continuous and nowhere differentiable curve is dependent on resolution
, and, further, that
when , i.e. that this curve is fractal (we used
the word "fractal" in this extended meaning throughout this paper).
The scale divergence of continuous and almost nowhere differentiable
curves is a direct consequence of Lebesgue's theorem, which states
that a curve of finite length is almost everywhere
differentiable.
Consider indeed a continuous but nondifferentiable function
between two points A
and A in the Euclidean plane. Since f
is non-differentiable, there exists a point A1 of
coordinates with , such
that is not on the segment A0 A
. Then the total length
. We can now iterate the argument and find two
coordinates and with
and , such that
. By iteration we finally construct successive
approximations of
whose lengths increase monotonically when the
"resolution" tends to zero. In other words,
continuity and nondifferentiability implies a monotonous scale
dependence of f on resolution . Now,
Lebesgue's theorem states that a curve of finite length is almost
everywhere differentiable (see e.g. Tricot 1993).
Therefore, if f is continuous and almost everywhere
nondifferentiable, then when the resolution
; namely f is not only scale-dependent,
but even scale-divergent. This theorem is also demonstrated in
(Nottale 1993a, p.82) by using non-standard analysis.
What about the reverse proposition: Is a continuous function whose
length is scale-divergent between any couple of points (such that
finite), i.e., when
, nondifferentiable? The answer is as follows:
(i) If the length diverges as fast as a power law, i.e.
, or faster than a power law (e.g., exponential
divergence , etc...), then the function is
certainly nondifferentiable. It is interesting to see that the
standard (self-similar, power-law) fractal behavior plays a critical
role in this theorem: it gives the limiting behavior beyond which
non-differentiability is ensured.
(ii) In the intermediate domain of slower divergences (for example,
logarithmic divergence, , etc...), the function
may be either differentiable or nondifferentiable.
This can be demonstrated by looking at the way the length increases
and the slope changes under successive zooms of a constant factor
. There are two ways by which the divergence
can occur: either by a regular increase of the length (due to the
regular appearance of new structures at all scales that continuously
change the slope), or by the existence of jumps (in this case,
whatever the scale, there will always exist a smaller scale at which
the slope will change). The power law corresponds to a continuous
length increase, , then to a continuous and
regular change of slope when : therefore the
function is nondifferentiable in this case. Divergences slower than
power laws may correspond to a regular length increase, but with a
factor which becomes itself scale-dependent:
with when
. In this case, some functions can be
differentiable, if they are such that new structures indeed appear at
all scales (and could then be named "fractal" under the general
definition initially given by Mandelbrot 1975 to this word), but these
structures become smaller and smaller with decreasing scale, so that a
slope can finally be defined in the limit .
Some other functions diverging slower than power laws are not
differentiable, e.g. if there always exists a scale smaller than any
given scale such that an important change of slope occurs: in this
case, the slope limit may not exist in the end.
Appendix B: special and generalized scale-relativity
B.1. Special scale relativity
It is well known that the Galileo group of motion is only a
degeneration of the more general Lorentz group. The same is true for
scale laws. Indeed, if one looks for the general linear scale laws
that come under the principle of scale relativity, one finds that they
have the structure of the Lorentz group (Nottale 1992). Therefore, in
special scale relativity, we have suggested to substitute to the
Galilean laws of dilation the more general
Lorentzian law
(Nottale 1992,
1993a):
![[EQUATION]](img352.gif)
This expression is yet uncomplete, since under this form the scale
relativity symmetry remains unbroken. Such a law corresponds, at the
present epoch, only to the null mass limit. It is expected to apply in
a universal way during the very first instants of the Universe. This
law assumes that, at very high energy, no static scale and no space or
time unit can be defined, so that only pure contractions and dilations
have physical meaning. The corresponding physics is a physics of pure
numbers. In Eq. (B1), there appears a universal, purely numerical
constant , which plays the role of a maximal
possible dilation. We have found that the value of
is about
(Nottale 1993a,
1995d,
1996a): its existence yields an explanation to the
Eddington-Dirac large number hypothesis, and connects the cosmological
constant to the Planck scale. A more detailed study of these questions
will be presented in a forthcoming work
(Nottale 1997).
However, the effect of the spontaneous scale symmetry breaking
which arises at some scale is to yield a new
law in which the invariant is no longer a dilation
, but becomes a length-time scale
. In other words, there appears in the theory a
fundamental scale that plays the role of an unpassable resolution,
invariant under dilations
(Nottale 1992). Such a scale of length and
time is an horizon for scale laws, in a way similar to the status of
the velocity of light for motion laws. The new law of composition of
dilations and the scale-dimension now write respectively (in the
scale-dependent domains, i.e. only below the transition scale in
microphysics and beyond it in the cosmological case):
![[EQUATION]](img358.gif)
![[EQUATION]](img359.gif)
A fractal curvilinear coordinate becomes now scale-dependent in a
covariant way, namely . One of the main new
feature of special scale relativity with respect to the previous
fractal or scale-invariant approaches is that the scale-dimension
, which was previously constant, is now
explicitly varying with scale (see Fig. 5) and even diverges when
resolution tends to the new invariant scales. In the microphysical
domain, the invariant length-scale is naturally identified with the
Planck scale, , that now becomes impassable and
plays the physical role that was previously devoted to the zero point
(Nottale 1992,
1993a). The same is true in the cosmological domain,
with once again an inversion of the scale laws. We have identified the
invariant maximal scale with the scale of the cosmological constant,
. The consequences of this new interpretation
of the cosmological constant have been considered in
(Nottale 1993a,
1995d,
1996a)
and will be developed further in a forthcoming work
(Nottale 1997).
![[FIGURE]](img364.gif) |
Fig. 5. Schematic representation of the three domains of the present era, (quantum microscopic, classical and cosmological) in the case of special scale-relativistic (Lorentzian) laws.The variation of the effective fractal dimension is given in terms of the logarithm of resolution. It is constant and equal to the topological dimension in the classical, scale-independent domain. It jumps fastly to towards small and large scales (Galilean regime), then it increases continuously in the Lorentzian regime (Eq. (A.2.2). The (relative) transitions are given by the Compton length at small scale and (presumably) by the Emden radius at large scale.
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Note that special scale-relativistic laws (Nottale 1992) have also
recently been considered by Dubrulle (1994) and Dubrulle and Graner
(1996) for the description of turbulence, with a different
interpretation of the variables.
It is also noticeable that recent developments in string theories
(Witten 1996) have reached conclusions that are extraordinarily
similar to those of scale relativity. One finds that there is a
smallest circle in string theory (whose radius is about the Planck
length), and that strings are characterized by duality symmetries. Two
of these dualities are especially relevant to our approach, since they
make already part of it in a natural way. The first is the quantum /
classical duality, which we recover in terms of our scale / motion
duality. The second is a microscopic / macroscopic duality: it has
been found that strings do not distinguish small spacetime scales from
large ones, relating them through an inversion. But scale inversion is
a transformation which is naturally included in the scale-relativistic
framework (see Sect. 2.5), since this is nothing but the symmetric
element of the scale group ( in the Galilean
case). Therefore it has recently been claimed by Castro (1996) that
scale relativity is the right framework in which the newly discovered
string structures will take their full physical meaning. The string
duality between the small and large scales adds a new argument to our
main conclusion: namely, that the laws of physics take again a
quantum-like form at very large spacetime scales.
B.2. From scale dynamics to general scale relativity
The whole of our previous discussion indicates to us that the scale
invariant behavior corresponds to freedom in the framework of a scale
physics. However, in the same way as there exists forces in nature
that imply departure from inertial, rectilinear uniform motion, we
expect most natural fractal systems to also present distorsions in
their scale behavior respectively to pure scale invariance. Such
distorsions may be, as a first step, attributed to the effect of a
scale "dynamics", i.e. to "scale-forces". (Caution: this is only an
analog of "dynamics" which acts on the scale axis, on the
internal structures of a given point at this level of
description, not in space-time. See Sect. B.3 for first hints about
the effects of coupling with space-time displacements). In this case
the Lagrange scale-equation takes the form of Newton's equation of
dynamics:
![[EQUATION]](img367.gif)
where is a "scale-mass", which measures the
way the system resists to the scale-force.
B.2.1. Constant scale-force
Let us first consider the case of a constant scale-force. Eq. (B4)
writes
![[EQUATION]](img368.gif)
where constant. It is easily integrated in
terms of the usual parabolic solution (where
:
![[EQUATION]](img371.gif)
![[EQUATION]](img372.gif)
However the physical meaning of this result is not clear under this
form. This is due to the fact that, while in the case of motion laws
we search for the evolution of the system with time, in the case of
scale laws we search for the dependence of the system on resolution,
which is the directly measured observable. We find, after redefinition
of the integration constants:
![[EQUATION]](img373.gif)
![[EQUATION]](img374.gif)
The scale dimension becomes a linear
function of resolution (the same being then true of the fractal
dimension ), and the
relation is now parabolic rather than linear as in the standard
power-law case. There are several physical situations where, after
careful examination of the data, the power-law models were clearly
rejected since no constant slope could be defined in the
plane. In the several cases where a clear
curvature appears in this plane (e.g., turbulence, sand piles,...),
the physics could come under such a "scale-dynamical" description. In
these cases it might be of the highest interest to identify and study
the scale-force responsible for the scale distorsion (i.e., for the
deviation to standard scaling).
B.2.2. Harmonic oscillator
Another interesting case of scale-potential is that of a repulsive
harmonic oscillator. It is solved as
![[EQUATION]](img377.gif)
For it gives the standard Galilean case
, but its large-scale behavior is particularly
interesting, since it does not permit the existence of resolutions
larger than a scale . Such a behavior could
provide a model of confinement in QCD (Nottale 1997).
More generally, we shall be led to look for the general non-linear
scale laws that satisfy the principle of scale relativity (see also
Dubrulle and Graner 1997). As remarked in
(Nottale 1994b,
1996a), such
a generalized framework implies working in a five-dimensional fractal
space-time. The development of such a "general scale-relativity" lies
outside the scope of the present paper and will be considered
elsewhere (Nottale 1997).
B.3. Scale-motion coupling and gauge invariance
The theory of scale relativity also allows to get new insights
about the physical meaning of gauge invariance
(Nottale 1994b,
1996a).
In the previous scale laws, only scale transformations at a given
point were considered. But we must also wonder about what happens to
the structures in scale of a scale-dependent object when it is
displaced. Consider anyone of these structures, lying at some
(relative) resolution (such that
, where is the
fractal/nonfractal transition) for a given position of the particle.
In a displacement of the object, the relativity of scales implies that
the resolution at which this given structure appears in the new
position will a priori be different from the initial one. In other
words, is now a function of the space-time
coordinates, , and we expect the occurrence of
dilatations of resolutions induced by translations, which
read:
![[EQUATION]](img382.gif)
where a four-vector must be introduced
since is itself a four-vector and
a scalar (in the case of a global dilation).
This behavior can be expressed in terms of a new scale-covariant
derivative:
![[EQUATION]](img386.gif)
However, if one wants such a "field" to be
physical, it must be defined whatever the initial scale from which we
started. Starting from another scale (we
consider only Galilean scale-relativity here, see
Nottale 1994b,
1996a
for the additional implications of special scale-relativity), we
get
![[EQUATION]](img388.gif)
so that we obtain:
![[EQUATION]](img389.gif)
which depends on the relative "state of scale",
. However, if one now considers translation
along two different coordinates (or, in an equivalent way,
displacement on a closed loop), one may write a commutator
relation:
![[EQUATION]](img391.gif)
This relation defines a tensor field which,
contrarily to , is independent of the initial
scale. One recognizes in the analog of an
electromagnetic field, in , that of an
electromagnetic potential, in e that of the electric charge,
and in Eq. (B14) the property of gauge invariance which, in accordance
with Weyl's initial ideas (Weyl 1918), recovers its initial status of
scale invariance. However, Eq. (B14) represents a progress compared
with these early attempts and with the status of gauge invariance in
today's physics. Indeed the gauge function, which has, up to now, been
considered as arbitrary and devoid of physical meaning, is now
identified with the logarithm of internal resolutions. In Weyl's
theory, and in its formulation by Dirac (1973), the metric element
ds (and consequently the length of any vector) is no longer
invariant and can vary from place to place in terms of some
(arbitrary) scale factor. Such a theory was excluded by experiment,
namely by the existence of universal and unvarying lengths such as the
electron Compton length (i.e., by the existence of particle masses).
In scale relativity, we are naturally led to introduce two "proper
times", the classical one ds which remains invariant, and the
fractal one , which is scale-divergent and can
then vary from place to place (its variation amounting to a scale
transformation of resolution). In Galilean scale-relativity, the
fractal dimension of geodesics is , so that the
scale-dependence of writes
. Therefore we have ,
and we recover the basic relation of the Weyl-Dirac theory, in the
asymptotic high energy domain . Another
advantage with respect to Weyl's theory is that we are now allowed to
define four different and independent dilations along the four
space-time resolutions instead of only one global dilation. The above
U(1) field is then expected to be embedded into a larger field, in
agreement with the electroweak theory, and the charge e to be
one element of a more complicated, "vectorial" charge (Nottale 1997).
Moreover, when combined with the Lorentzian structure of dilations of
special scale relativity, our interpretation of gauge invariance
yields new relations between the charges and the masses of elementary
particles
(Nottale 1994b,
1996a).
© European Southern Observatory (ESO) 1997
Online publication: April 6, 1998
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