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New Members of the Solar System
During the past three years more than two dozen objects of a new
type have
been discovered orbiting the Sun beyond Neptune. These bodies are too
small to
be classified as planets, but are also unlike most asteroids in that
they
inhabit exclusively the outer solar system, and unlike most comets in
that their
orbits are not very eccentric. They are otherwise too faint for much to
be known
other than that they tend to be unusually red in color. Nonetheless,
astronomers
agree that, since so many objects showed up in several deep searches of
very
small areas of the sky, there are estimated to be perhaps 35,000 such
objects
(2-5 per square degree), each at least 100 km across, between 30 and 50
astronomical units from the Sun.
Are They Comets?
The distinction between comets and asteroids has become rather
blurred over
the past decade because no single characteristic uniquely identifies a
body as
either with certainty. For example, debate still rages over whether the
Jupiter
impactor, Shoemaker-Levy 9, was a comet or an asteroid. Despite having
very
different origins in conventional models, comets and asteroids have
continued to
display similar reflectance spectra, albedos, size ranges, etc. Comas
and tails
are the best guides we have to indicate that an object is a comet. But
many
comets display no tails; indeed, virtually all of them beyond Jupiter
do not.
And some comets have lost their comas, becoming completely asteroidal
in
appearance, while some asteroids have suddenly begun to exhibit
comet-like
activity, including the surprise appearance of a tail in one case.
Highly elongated orbits used to be associated exclusively with
comets until
the discovery of some unusual objects without coma or tail that
therefore appear
to be asteroids, yet moving in highly elongated, planet-crossing
orbits. Pholus
is one such object. The object Chiron is another example of the
dilemma, since
it was first assumed to be a large asteroid in a planet-like orbit
crossing the
orbits of Saturn and Uranus. When it was later found to have brightness
variability, many astronomers began to call it a comet.
The trans-Neptunian objects (shall we call them TNOs?) show neither
coma nor
tail, and are therefore completely asteroidal in appearance. But it is
argued
that, at such great distances from the Sun and at such faint
magnitudes, comas
are likely to be invisible. However, all objects designated as comets
heretofore
have displayed visible comas or magnitude variability, even at solar
distances
beyond Saturn, since the coma is generally far brighter than the
nucleus. (For
example, the new Comet Hale-Bopp was photographed pre-discovery in 1993
while
still near the orbit of Uranus, yet had a visible coma.) But the TNOs
show only
point-like nuclei.
The matter of comet versus asteroid would be more difficult to
resolve if the
trans-Neptunian objects had spectra like other comets. But they do not.
TNOs are
quite red. So the only known objects they resemble are the asteroids on
highly
elongated Jupiter-crossing orbits such as Pholus, which likewise happen
to be
highly reddened. Indeed, since those highly elongated asteroid orbits
are
unstable (those that cross Jupiter’s orbit will be eliminated
within
100,000 years), it is a reasonable conjecture that they were recently
perturbed
into their present orbits from the trans-Neptunian population by a
close
encounter with Neptune. Subsequent perturbations by Jupiter would tend
to
quickly eliminate the Neptune-crossing character of the orbit, making
that
origin slightly less obvious today. Chiron, for example, might have
originated
beyond Neptune, but had its orbit subsequently modified by encounters
with first
Neptune, and later Saturn.
Pholus is an interesting case in point. It has a perihelion distance
of 8.7
au and aphelion of 32.3 au. (Neptune is at 30.1 au.) And it had the
reddest
spectrum of any object in the solar system prior to the discovery of
1992 QB1,
the first trans-Neptunian object. It seems safe to bet that Neptune
modified
Pholus’s orbit from Pluto-like to its present condition within
the past
100,000 years; and that Pholus is a sample of the trans-Neptunian
population we
can examine at relatively close proximity. If so, then Pholus gives no
indication of being a comet.
The argument that TNOs are members of the predicted "Kuiper
belt"
of comets is entirely spurious. For example, it is often argued that
short-period comets have small inclinations to the ecliptic plane, in
contrast
to new comets from the "Oort cloud" that have fairly random
inclinations. And this is taken to indicate a different source for the
short-period comets. However, this suggestion overlooks the
consideration that
capture of new comets into short-period orbits by Jupiter is far more
likely for
comets of low inclination because they spend more time near the
ecliptic, and
therefore potentially close to Jupiter. The technical details of the
extensive
arguments against the existence of a Kuiper belt of comets may be found
in
"The Kuiper belt of comets does not exist" by T. Van Flandern
in
Periodic Comets, J.A. Fernandez and H. Rickman, eds.,
Universidad de la
Republic, Montevideo, 75-80 (1992).
Therefore, from what we now know, it seems a likely conjecture that
TNOs are
not comets, but rather are a new class of unusually red asteroids, a
few of
which have been perturbed into temporary orbits that can reach the
inner solar
system.
Another Exploded Planet?
If the trans-Neptunian objects are debris from an exploded planet,
as a great
deal of evidence suggests is the case for main-belt asteroids, then
their
initial orbits would have to exhibit a wide range of eccentricities,
inclinations, and mean distances from the Sun. However, although data
is sparse,
the objects now known are apparently confined to a modest range of
eccentricity
and inclination. But the process used for search and discovery strongly
biases
the discovered objects toward low inclination; and the eccentricities
of many
orbits are not yet well-determined. So one must be cautious about
drawing the
conclusion this early that an exploded planet does not fit the data.
|
Planet |
mean distance |
|
Neptune |
30.1 |
|
Pluto (min) |
29.7 |
|
Pluto (avg) |
39.5 |
|
Pluto (max) |
49.4 |
|
Trans-Neptunian object |
distance |
|
1992 QB1 |
44.4 |
|
1993 FW |
43.9 |
|
1993 RO |
39.3 |
|
1993 RP |
39.3 |
|
1993 SB |
39.3 |
|
1993 SC |
39.3 |
|
1994 ES2 |
46.2 |
|
1994 EV3 |
44.8 |
|
1994 GV9 |
42.3 |
|
1994 JS |
36.6 |
|
1994 JV |
34.2 |
|
1994 JR1 |
35.3 |
|
1994 JQ1 |
43.3 |
There is also a tendency for TNOs to segregate into two ranges of
mean
distance at discovery, one of which is close to the 3-to-2 resonance
with
Neptune that Pluto and its moon Charon occupy. See Table 1. The other
group may
be near that resonance as well if the orbital eccentricities turn out
just
right. For comparison, some outer planet data appears in Table 2.
Again, the
significance of this early data must be judged with caution, both
because of
strong observational selection effects, and because the long-term
gravitational
effects of Neptune are not yet well known. The evolution of
Pluto’s orbit,
for example, has been difficult to study because of its resonance with
Neptune,
and because it can apparently make close approaches to Neptune if one
looks far
enough into the past, of order one billion years. Indeed, it has been
proposed
that only orbits in a 3-to-2 resonance will have long-term stability.
[Icarus 116, 180-185 (1995).]
There are apparently far more "asteroids" over 100 km in
diameter
beyond Neptune than in the main asteroid belt. If the trans-Neptunian
objects
are from a parent body that exploded, the 35,000 number mentioned
earlier can be
combined with a mean diameter of, say, 150 km each to imply a parent
body at
least 5000 km in diameter, the size of Saturn’s moon Titan. But
that would
require a gentle breakup with little mass loss. If most of the mass was
blown
out of the solar system, then the parent body must have been a major
planet. One
possible conjecture is that the parent body was the hypothetical Planet
X, a
trans-Neptunian planet possibly still awaiting discovery that may have
had a
close encounter with Neptune in the distant past [see Dark Matter,
Missing
Planets and New Comets, North Atlantic Books (1993)]. Perhaps the
encounter
somehow destabilized the planet’s interior, leading eventually to
the
explosion. Indeed, this same encounter/destabilization scenario can
readily be
visualized as possibly applicable to the nearest planets to Jupiter,
the parent
bodies of the main asteroid belt, as well.
A Former Neptunian Ring?
In Dark Matter, …, we described evidence indicating
that Pluto
& Charon and the disruption of Neptune’s satellite system may
have
resulted from a past encounter with "Planet X". But in that
study, the
late Robert Harrington and I did not investigate the effect such an
encounter
might have had on any natural rings around Neptune at the time.
However, since
rings are made up of individual bodies that behave dynamically like
individual
satellites, it seems clear that a Neptunian ring could have met the
same fate as
other Neptunian moons – being stripped away from Neptune into an
independent solar orbit that remains Neptune-crossing. Such is the
present
condition for the solar orbit of Pluto and its large moon Charon.
The principal arguments against this are the size of the
trans-Neptunian
objects (too large to be ring pieces), the implied size of the parent
body (much
larger than any existing Neptunian moon), and weak evidence for some
low-eccentricity TNOs that do not come close to crossing
Neptune’s orbit
and therefore could not have originated in this way.
But whatever the origin of the curious new objects, they occupy a
volume of
space so vast that all the 200,000,000,000 stars in our galaxy could
fit within
that volume without touching! This means that the rate of collisions of
smaller
bodies with the larger TNOs is so small that origin by accretion is
ruled out
for a belt with present densities. It therefore may be concluded with
certainty
that something fundamental is missing in conventional models suggesting
accretion of these objects from a primeval solar nebula. [AJ
110,
856-868 (1995).]
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Meta Research Bulletin Volume 4, Number 3 September 15,
1995
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