A POSSIBLE
RELATION BETWEEN PLANETARY DISTANCES
AND THE 160-MINUTE SOLAR PULSATION
V. A. Kotov and S. Koutchmy*
Izvestiya Kryniskoi Astrofizicheskoi Observatorii,
Vol. 72, pp. 199--208, 1985
UDC 523.9--1/8;523.214:530.12
The discovery
of global pulsations on the Sun with period Po
=
160
min
[10]
enables
us to consider a characteristic wavelength for the solar system
L
=cP0=19,24
a.u., where c
is the velocity of light. The planetary distances show a statistically
significant quasicommensurability between
L
and
2pai for the inner planets or between
2ai and
L
for
the outer ones (ai is the major semiaxis of the orbit).
This
L
commensurability leads to a new approach to the Titius-Bode planetary distance
law. The physical mechanism responsible for this
L
commensurability
in the solar system is evidently related to gravitational waves from an external
source of unknown nature.
It is generally
recognized that the distribution of the planets is not random and provides
information on the formation mechanism and evolution of the solar system
[1,2]. In many theories of the origin of the solar system, attempts are made
to derive a planetary-distance law analogous to Bodes law, but none of these
formulations can be taken as satisfactory. Alven and Arrhenius
[3]
criticized
Bodes law but at the same time recognized that the solar system has regular
structure and dynamics; they consider that resonant phenomena must play an
important part in establishing the regularity, which is evidently also reflected
in an exponential law of Bodes type, as well as the commensurability of many
motions within the solar system.
Two average motions are taken as commensurable, or two orbital periods, if
the ratio of them can be represented as the ratio of two quite small integers
[1,2]. In the discussion of the reasons for commensurabi1ity, the main hypothesis
has been that it is due to the direct gravitational interaction of the bodies
during the evolution of the solar system or a result of tides arising on
planets and satellites. Nieto [4] gives strong arguments for dividing the
entire search for a physical basis for the law into two parts: on the one
hand, one has to explain the geometrical progression in the planetary distances,
and on the other,the commensurability. Nieto [4], Dermott
[5],
and
Ovenden
[6]
concluded
that the tidal theory has no basis in explaining the regularity in the planetary
distances, since it requires time to establish commensurability much greater
than the time for which the planetary system has existed. In
[6]
it is
shown that Bodes law reflects the principle of minimal interaction and is
simply a result of the gravitational attraction between the planets, so it
provides no information on the formation conditions. In turn, Hills numerical
calculations
[7]
imply
that commensurability in the periods of rotation around the central body
is the final and most important feature of a system of strongly interacting
bodies, and a state with commensurability is the most stable state out of
all the possible configurations for the orbits; therefore, Bodes law is a
natural expression of the commensurability. However, Hills approach involves
the following difficulty: relaxation in a system of gravitating bodies in
general inevitably leads to unbounded increase in the orbital eccentricities,
which is unrealistic.
According to Molchanov
[8],
the
planetary-distance law follows from simple linear (resonant) relations between
the frequencies of rotation of the planets. However, later
[9]
it was
shown that the set of relationships (correlations) considered in
[8]
is
statistically unreliable.
*Astrophysics Institute, Paris, France.
© 1987
by Allerton Press, Inc.
1.
SOLAR PULSATIONS
In 1974, Severnyi
et al. [10] observed periodic oscillations in the solar photosphere, which
extended to virtually all the visible hemisphere of the Sun and had a period
of about 160 min. This was very shortly afterwards confirmed by others [12-14].
Observations over nine years in the Crimea [15] refined the value of the
period, which is
P0
=
160m,0101±0m,0007.
(1)
The nature
of this oscillations is a difficult problem for the theory. It is possible
to explain it as resonance between gravitational (nonradial) g modes and
certain combinations of them of gi- gk type
for a solar model [16] with low initial heavy-element content Z0
=
0.001
[15].
In [17,18],
it has been suggested that the 160 min period on the Sun is a relict phenomenon,
i.e., has existed for 108-109 yr, namely over a time-scale
comparable with the time of substantial evolution in the solar system. In
that case, it is quite reasonable to suppose that this period may play a
considerable part in establishing the regularity and commensurability in
our system. As regards the physical mechanism, one can evidently envisage
periodic fluctuations in the gravitational field near the Sun accompanying
the 160-min pulsations.
There have
been many suggestions that one could observe gravitational perturbations
(waves) from studies on the entire solar system or some parts of it acting
as trial bodies, in particular from Weber [19], Braginskii [20], and Dicke
[21].
Savin [22]
suggested an important role for a 160 min period in the structure and evolution
of the solar system long before the actual discovery [10] of the global pulsation
on the Sun; in 1946 he said that the period of the natural vibrations of
the Sun, so to say, the period of its infrasound (1/9 day), plays an important
part in the distribution of the outer planets. It is true that now it is
almost impossible to establish how he derived this conclusion on the period
of the Sun of 1/9 day (160 min);it seems that it was an intuitive guess supported
by analysis of the periods of rotation of the planets.
Another important point is the statistically significant commensurability
in the mean periods of axial rotation of the planets and asteroids, period
160 min [18]. This forces one not only to see a physical mechanism for this
preferred synchronization but also other possible signs of the fundamental
periodicity P0 within the solar system.
A discussion
of the possible relationship between this 160 min period and the structure
of the system as a whole leaves on one side the nature of P0
and the physical process that determined the commensurability (of
the axial rotation speeds [18]) with P0. The treatment
is basically statistical and involves the following three major
postulates:
1) the period
P0 =
160.010 min of the Sun is
a relict phenomenon;
2) periodic
perturbations in the gravitational field are, or have been, related to this
period; and
3) these
perturbations have a wavelength
L
determined by P0 and the propagation speed
c, which is equal to the speed of light
(L
= cPo).
The theory
of gravitation and gravitational radiation implies that the equations for
weak gravitational fields are analogous to Maxwells wave equations for the
electromagnetic field. Einstein postulated that gravitational waves propagate
with the speed of light; since then, the speed of light c as a universal
constant has formed the basis of the special theory of relativity and the
theory of gravitation. Correspondingly, we introduce the wavelength
(2)
We further
suppose that
L
is a certain characteristic scale that may be important in
establishing the final dimensions of the system. It is then logical to compare
L
with
the actual distances within the planetary system, which are comparable with
L
as regards order of magnitude.
2. COMPARABILITY
OF
L
AND
THE ORBIT DIMENSIONS
A circular
orbit is the limiting case of an ellipse with eccentricity e tending
to zero. Therefore, the motion of the planets around the central body in
eccentric orbits can be represented as equivalent circular motions occurring
in a certain preferred plane and perturbed by radial oscillations with period
Tn, where
Tn
is the period of rotation
of planet number n around the Sun. The perturbations that transform
a circular orbit into an elliptical one are characterized by the length
zn
~
2pan(an is
the major semiaxis of the orbit). On the basis of resonance, it is reasonable
to assume that
zn
may be commensurable with
L
,
as may be the radius an and the diameter of the orbit
2an.
We now enumerate
all combinations of ratios of the type x1/x2
between these three orbit parameters (an,
2an, and
zn) and
L
:
(3)
To establish
whether x1 and x2 are comparable on average
for the 10 objects in the solar system (the nine planets and the asteroid
belt), we impose three conditions:

where N is the number of objects.

The summation may be taken directly for all 10 objects at once or separately
for the five inner planets (including the asteroid belt) and the five outer
ones. The division of the objects into two groups is quite natural by virtue
of the marked difference in physical characteristics between the planets
of the terrestrial group and the giant ones, as well as the differences in
evolutionary history.
Condition (4)
is obvious, since we are interested in x1/x2
being close to integers; (5) restricts the order of the
commensurability, while (6) is an obvious requirement for the mean multiplicity
(commensurability) between x1 and x2,
where Zn are integers close to
(Xl/X2)n. It is evident from
(3) that
L
does
not show preferred quasicommensurability with any of the three orbital parameters
(an,2an, and
2pan) for all objects taken
simultaneously in accordance with (4)-(6); instead, there is
quasicommensurability only between
L
and
2pan for the five inner planets
or between
L
and 2an for five outer ones; the values of
y are correspondingly 0.118 and 0.217.
The
quasicommensurability is illustrated in more detail in Table 1, which gives
not only the mean distances from the Sun (the an of [23])
for the 10 main objects but also the
L
/2pan for the inner planets and
2an/L
for
the outer ones. All the values are close to small integers (less than 10):
C(x1/x2)n-
Zn
C<1/4,
apart
from Jupiter, for which 2a6
/L
y1/2.
Instead of the major semiaxis an, we can consider the so-called
equivalent radius of the orbit rn, which by definition
is equal to the radius of a circle whose area is equal to that enclosed by
the elliptical orbit:
rn
=
an
(1-e2)1/4
(7)
The average
commensurability of 2prn or
2rn with
L
is then substantially higher than that in Table 1, mainly on
account of the orbital parameters of Mercury and Pluto, which are the two
planets with the largest eccentricities (these correspondingly give
L
/2pr1 = 7,996,
2r10/L
=
4,034).
3.
COMMENSURABILITY SPECTRUM
The main difficulty
in demonstrating any planetary distance law lies in determining the statistical
significance of the approximation for the observed an.
We have 10 values of an and can obtain almost any regularity
with the probability practically equal to one. The values of
L
/2pan
and
2an/L
given
in Table 1 readily give us the probability of obtaining this close correspondence
to integers by accident:
(8)
where
is the number of combinations
of 10 elements taken seven at a time.
In all previous studies on the planetary distances, it has been usual to
find the best approximation to 10 or less values of an
with a parametric function containing two or more constants, whose form is
not known a priori; this is dependent on several untestable and usually
unreliable assumptions. An advantage of our argument is that this
commensurability study is based on the advance assumption of a unique geometrical
scale
L
,
and it will be seen from what follows that this enables us
to evaluate the reliability of the result more or less rigorously, namely
the quasicommensurability of the orbital parameters with
L
.
Table 1 shows
that 2an and
2apn tend to be commensurable
with
L
,
so we are justified in expecting a maximum commensurability
at the frequency f0 =
c/L
=
P0-1. One can calculate the commensurability
function [18] in order to determine whether f0 in fact
corresponds to the best commensurability (i.e., the turning point in a certain
function) and to determine the level of statistical significance for the
maximum.
We assume that the commensurability of the an with
L
(Table 1) is accidental. Then one should assume that in a reasonably chosen
range of wavelengths l(or frequencies
f
=
c/l), there exists certain values
l'that show average quasicommensurability
with the 10 values of an better than the
L
=
19,24
a.u.
(frequency
f0
=
l04.l6
mHz).
We have introduced [18] the commensurability function
F(f) for certain constants
kn with the variable
f
,
which
shows for what values
f
' there
is preferred commensurability for the entire set of
kn,
i.e.,
scope for approximating
kn/f
by integers more or less satisfactorily. The meaning of
F(f) is entirely analogous
to that of the power spectrum of a time-varying signal, so
F(f) is naturally called
the commensurability spectrum.
We construct the following two
F(f) separately for the
planets of the terrestrial group (n 1,...,
5) and the outer ones (n = 6,..., 10):



Here the
Zn are integers closest
to the
x1/x2, while for Jupiter, to retain
the generality, we take 2a6 instead
of a6 (see below on the same on replacing
the real an by random numbers);
l
=
c /
f
,
where
f
is the traveling frequency and b
=
(12)-
1/2
=
0,2887
[18].
Figure 1 shows
F1 calculated in the range of periods
from about 10 to 460 min with a
step
DP
=
2.5
min; there are two
peaks
with
identical amplitudes A
=
0.173
y
2.8s
, which correspond
to periods of about 159 min and about 305 min (±4 min, the error
corresponding to the peak width at the
2s level). The value
of
s is determined here,
as everywhere, by calculating F(
f
) for uniformly
distributed random numbers Rn replacing the actual
an.
Figure 2 shows F2 for the five
outer
planets;
frequency step
D
f
=
2
mHz.
The largest peak with amplitude about
3.5s corresponds to a
period of 163 min
(±3
min),
while the second peak for P
y 82
min has an amplitude less than
3s and is an artefact
of the quasicommensurability for P
y 163
min (see also
[18]).
The two figures
show that there is a single period of about 160 min in the entire frequency
range that gives a dominant and statistically significant quasicommensurability
with the parameters
2pan(n
= 1,...,5) and
2an(n =
6,...,10)
simultaneously. As the amplitudes A of the peaks (about 160 min)
in Figs.
1
and
2 are
>2.3s and
>3.2s, we get the probability
of accidentally finding two peaks at the same frequency simultaneously
as
(11)
Interest also attaches to the form of the average function F = (F1 + F2)/2, which is shown in Fig. 3. The calculations were made for periods from about 56 min to about 1440 min, and for P P 470 min, where F1 is not defined, we took only F2, i.e., here we assumed F = F2. The F(f) is then dominated by quasicommensurability for the period 160 min ( 3 min), peak amplitude about 4.3s and probability of accidental occurrence at that frequency about l0-5.
To illustrate the preferred commensurability with L for 2prn and 2rn. where rn are the equivalent orbital radii, we calculated a function for all 10 planets:

(for Jupiter,
we took 2r6 instead of r6). Figure 14
shows the spectrum, where the largest peak has amplitude
A(160m)y4,3
.


Many calculations have been performed [19-21,25,26] on the energy flux incident on the solar system from a binary one. Consider, for example, a binary system composed of two massive collapsed objects with masses m1 and m2. If the system has a circular orbit with radius r and angular velocity of one component around the other w, the energy flux from gravitational waves near the Sun is [26]
where R
is the distance from the binary system to the Sun. Taking
m1~m2~M@,
w =
p/P0
~ 3,3•104 sec-1 and R
y 10
parsec, we get r ~(GM@ /
w2
)1/3 ~ 1011 cm, and for I we get
the very small value
O2.4.l0-10
erg.cm-2.sec-1. If we assume that the
components in the system are black holes (F. Delache, 1983, personal
communication) with masses about l03 M@ each,
then we get the dimensions of such a system as r
y
1012 cm and I
O2.4
erg.cm-2.sec-1, i.e., comparatively
large. The energy losses by gravitational radiation are
DE
=
4pR2I
~ 3.1040
erg.sec-1, and the lifetime of the system is
t
O2.103
M@c2/DE~4.109
yr, which is comparable with the time of existence of the solar system.
This problem requires a special discussion, which should cover the possibility
of such a massive binary system existing at all near the Sun, its real lifetime
(<t)
and the identification with some peculiar object.
If there is
an external gravitational-radiation source, the observed oscillation with
P0 = 160.010 min is to be considered as a forced oscillation,
which is the more interesting because the region of periods around 160 min
is according to Severnyi et al. [15] the most preferable for the Sun for
resonant interaction and excitation of certain gravitational g modes.
Resonant energy transfer from one mode to another may occur in the presence
of a weak but permanently acting external perturbation at frequency
P0-1, which would lead to appreciable amplification
in this oscillation by comparison with all other g modes.
The authors
are indebted to
A.B. Severnyi for some
critical comments, which led to substantial improvements in the paper, and
we are also indebted to A. Wittman (Gottingen) for a discussion of the
statistical significance of the commensurability found in the solar system,
to A. G. Kosovichev for valuable comments, and to F. Delache (Nice), who
provided some of his results before publication.
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11 November
1983
*Bulletin of
the Crimean Astrophysical Observatory (USSR Academy of Sciences). Available
from Allerton Press, Inc., 150 Fifth Avenue, New York, NY 10011; (212)
924-3950.