THE
SINGLE BODY BREAKUP HYPOTHESIS FOR THE SOLAR SYSTEM
NOTE: The subject matter and conclusions of the
paper “Further Study of the Major Satellites of the Solar System and of the
Lesser Bodies Triton, Pluto, and Charon – A Revision
of Ideas of Origin”, dated May to September, 2004 supersedes any mathematics
and conclusions reached in this earlier paper when the mathematics and
conclusions are on properties treated in both papers.
PAPER C
The
Major Satellites and Mars (but Triton excluded)
It is the intention in this paper to look at
the major satellites and Mars to compare some of their major physical
properties and to suggest a possible (probable?) mode of formation. Why is Mars
included with the satellites? Because it has characteristics of
both planets and satellites. But its origin can be shown to be linked
more closely to the satellites, as will be illustrated below.
It was suggested in paper B that, excluding
Saturn, the planets and satellites once formed a "protoJupiter",
the structure of which was a Mercury core surrounded by a series of shells
composed successively outwards of the mass and volume of Venus, Earth, Mars,
"silicate" satellites, Pluto group, "medium icy"
satellites, "light icy" satellites, Neptune, Uranus, and Jupiter. It
was further suggested that this protoJupiter began to
break up internally and the matter to be ejected from the body by a series of
impulse forces. Paper A gives the breakup stage immediately prior to the
ejection of Earth and Uranus.
Initial internal breakup was the separation
of the gaseous component of the core (Neptune/Uranus) and the
silicate/"icy" component. There is little difficulty in arguing or
comprehending that before the terrestrial planets could be formed the
surrounding less competent satellite shells had first to be removed. As this is
an outline paper and not a rigid treatise, satellite removal prior to planet
removal will be assumed; and it will be assumed that "onion skin"
stripping of the core was the mode of separation followed by impulse force
ejection. Should such not have been so then some (perhaps all) of the following
relationships would not appear and the assumptions would have been wrong.
mx = (MpJ 100) x
1.23n
where mx = mass of the
satellite
MpJ = sum of the masses of all the planets and satellites
LESS Saturn;
n = -46.5 for Ganymede, -47 Titan, -48 Callisto, -49 Io, -50 Moon, -52 Europa,
and Triton –56.
Mars does not fit this sequence very
well -n = -39 gives a +7.13% difference from the measured mass - and more
nearly fits the formula for the terrestrial planets of,
mx = (MJ 100) x 1.23n
where MJ = mass of Jupiter
and n = -39 (-2.65% different).
S.G. = 2 x 0.981n
where n is an integer.
For the "icy" satellites, n = -2
for Triton, +2 Ganymede, +4 Titan, and +6 Callisto.
For the "silicate" satellites and uncompressed terrestrial planets, n
= -22 for Europa, -27 Moon, -30 Io, -33 Mars, ---.
The above formulae suggest a close
relationship between the satellites and the terrestrial planets groups, and
there are other suggestive relationships not touched on here.
Consider, now, the separation of the
"medium icy" and "silicate" satellites from the silicate
core. Assume that the silicate/"icy" sphere lay beside the
Neptune/Uranus sphere and that the "icy" shell peeled off in layers
to form the three major "icy" satellites in line and touching one
another and the silicate/"silicate" satellite core as in the
following figure – from left to right Callisto,
Titan, and Ganymede, "silicate"/"silicate satellite"
sphere.

This was then almost certainly followed by a
similar stripping of four satellites – Charon,
"Asteroid", Pluto, and Triton - followed by the "silicate" satellites
Europa, Moon, Io, and Mars as below.

The central four satellites are outside this
discussion and can be ignored.
(c ) Radii Comparison of the Satellites
There are various ways of comparing the two strings of satellites, e.g. within
each string, between each string, and each string to the enclosing body, but
only two will be given here as suggestive support for the breakup as outlined.
(c1) The radii in km of the satellites are:
Mars 3398, Io 1829, Moon 1738, Europa 1560,
Ganymede 2640, Titan 2560, Callisto 2400.
(c1a) Taking ratios of successive couples
between the two groups gives:
Mars/Ganymede = 1.28712, within 4.64% of
1.23;
Io/Titan = 0.71436, within 1.32% of 0.724;
Moon/Callisto =
0.72417, within 0.02% of 0.724;
which suggests a relationship.
(c1b) More interestingly, taking ratios of
successive couples from Triton to Ganymede to Mars and on into the terrestrial
planets gives:
Titan/Callisto =
1.06667, within 1.29% of 1.231/4 (= 1.066671);
Ganymede/Titan = 1.03125, within 0.49% of
1.231/8 (= 1.063481/2);
Europa/Ganymede = 0.59091, no fit;
Moon/Europa =
1.11410, within 0.46% of 1.231/2;
Io/Moon = 1.05236, within 0.07% of 1.231/4;
Mars/Io = 1.85785, within 2.62% of 0.724-2;
Earth/Mars = 1.87699, within 1.61% of 0.724-2;
Venus/Earth = 0.94857, within 0.10% of 1.23-1/4;
Mercury/Venus = 0.40314, no fit.
The Mercury/Venus value can be ignored as
Mercury is the remainder of the sequence breakup. Then the bodies within the
three groups "icy", "silicate", planet show 1.23
relationships, Europa/Ganymede shows no fit (another
group – the Pluto group - lies here), and Mars shows an inverse relationship
between Io (1.857851) and Earth (1.87699-1). Mars thus
shows a relationship to both satellites and planets; it is not clearly one or
the other.
The pattern of the ratios clearly points to
an intimate relationship between the bodies and the groups of bodies.
Development was not unconnected or random. The single body breakup hypothesis gives
one to expect such an intimate relationship.
(d1) On the basis that the impulsive force
reduced as a straight line variation from the centre of the system outwards
along the internal bodies’ alignment, the impulse pressures per unit cross
sectional area on the four bodies must plot as a straight line variation
when the impulse pressure is plotted on the y-axis against distances equal to
the centre points of the touching spheres on the x-axis.
Assuming the velocities of ejection of the
four bodies were translated directly into linear orbit speeds, then for Io and Europa:
impulse pressure = impulse force divided by cross-sectional
area = mx.vx/prx2,
where m, v, and r have their usual meanings in dynamics.
The ejection velocity of Mars would have been
its present velocity about the Sun less the velocity of the composite body (=
12.9 km.sec-1 at 5.3 AU), i.e.(24.1 - 12.9)
= 11.2 km.sec-1, and so its impulse pressure, too, can be
calculated. Plotting the three impulse pressure values gives the following
graph.

A near straight line curve results. This
suggests that the development as given above could have taken place. In turn it
also suggests that the Moon, in the sequence as given, had had induced on it at
commencement of its outward movement an impulse pressure of 1.24x1017
kg.km.sec-1 (measured off the graph). By inserting this value in the
impulse formula we obtain for the Moon a velocity of ejection of 16.01 km.sec-1.
It is an empirical fact that the formula d =
2 x 0.724n gives approximately the distance of each major satellite
of Jupiter from Jupiter measured in Jupiter radii (RJ), where n = -3
for Io, n = -5 for Europa, n = -6 for Ganymede, and n
= -8 for Callisto. But note that when n = -4 is
inserted in the formula a value of 7.28RJ is obtained and a body at
this distance from Jupiter would have an orbit velocity about Jupiter of
approximately 16.0 km.sec-1. That is to say, the velocity of
ejection and consequently orbit speed about Jupiter of the Moon (if it went
into orbit) as determined by impulse pressure closely approximates the orbit
velocity determined by the distance formula for n = -4. This suggests that the
Moon was part of the series of satellites given, originally lay in the order
given within protoJupiter, and was ejected into an
orbit of about 7.3RJ about protoJupiter.
Turning to the "medium icy"
satellites, assume a similar formation and ejection sequence took place as
argued for the "silicate" satellites and prior to them. The bodies
developed would have lain on a common diameter and touched in the order Callisto, Titan, Ganymede, silicate core. They would then
have suffered an impulse force which drove them out of protoJupiter.
Knowing the velocities of orbit of Ganymede
and Callisto we can calculate their bodies’ impulse
pressures. For Titan, since captured by Saturn, we can make a calculated guess
of its ejection velocity in the same way as was done for the Moon, above. In
the formula d = 2 x 0.724n the Moon was placed between Io and Europa at the vacant n = -4 position. There is a vacant
position at n = -7, between Ganymede and Callisto
where Titan must be placed to give the correct satellite sequence. Assuming
this position to be correctly filled it is possible to determine the
satellite’s impulse pressure because its orbit velocity can be calculated.
Plotting the impulse pressures against spacing of the three satellites as for
the "silicate" satellites gives the following graph,

and it is seen that an almost straight line curve is
obtained. This leads to the conclusion - in conjunction with the
"silicate" satellite curve - that the satellites were formed as two
groups and were ejected by two separate impulses, one immediately after each
group formed.
(d2) Further evidence of such an ejection
will appear if the impulse force acted at a slight angle to the diameter on
which the satellites lay immediately after formation. The rotation axes of the
bodies (Yes! They would have been rotating.) would
have been tilted by the component of the impulse force at right angles to the
join line of the body centres. It is a mathematical
fact that the ratio of any two obliquities of the rotation axes (here called
for brevity, tilts) must ideally equal the ratio of the radii of the same two
bodies. The ideal is unlikely to be realised but the
two ratios should be approximately equal.
Only the tilts of Mars and the Moon have been
measured. Tilts for the other satellites have been "theoretically"
calculated using assumptions but because of rotation lock by Jupiter none have
been actually measured. Thus this tilt test can only be applied to Mars and the
Moon in the "silicate" satellite group. Applying the test, the ratio
for the radii of Mars and Moon = 1.96.
The tilts of the two bodies must be taken at
(very closely) the location of Jupiter. Not considering refinements and
possible variations (see Lee; Jan., 1998) the ratio of the tilts is about:
= (24.98 + 1.85 - 1.31)o/(11.233
+ 1.309)o = 2.03,
i.e. the two ratios differ by 3.7% and the dynamic
requirement obtains. The origin of the two bodies as suggested above is thus
supported.
Conclusions The
tests based on the assumption of the origin of the satellites deriving from the
internal breakup of a protoJupiter accompanied by
intermittent impulsive ejection of the bodies as described have been:
All have supported the contention that
development of the satellites came about in the early stages of the internal
breakup of a protoJupiter body. None of the five
relationships can be explained by the Nebula Theory, which requires random
formation of the bodies and unrelated points of origin for the non-Galilean
bodies.