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Table
of Contents
The
Solar System
Planetary
Data
Terminology
Formation Theory Parameters
Magnetic Fields
Angular Momentum
Solar System Formation
Questions
Intro
to Astronomy
Misconceptions
Archaeoastronomy
Equitorial Coordinates
Understanding the Seasons
Time & Its Measurement
Telescopes
Solar
& Lunar Eclipses
The Earth
The Moon
Mecury,
Venus, Mars
The
Outer Planets
Solar
System Debris
The
Sun
Evolution
of Stars
Intersteller
Matter
Sky
Literacy
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Characteristics which must
be explained by a successful theory of Solar System formation
- The sun contains over 99 percent of the mass of the solar system.
- The rotational axis of the sun is nearly perpendicular (within 7
degrees) to the plane of the planetary orbits, i.e., the ecliptic.
Stated in another way, planetary orbits lie near the plane of the
sun's equator.
- Planetary orbits all lie near the plane of the ecliptic.
- Planetary orbits are nearly circular.
- The planets revolve around the sun in the same direction.
- Planetary rotations are all direct (counterclockwise) and axial
tilts are perpendicular to the plane of the planets' orbits. (Venus,
Uranus, and Pluto are exceptions to this rule).
- Satellite systems mimic the planetary systems. Most of the satellites
revolve in the same direction that their primaries rotate and revolve.
Their orbital planes lie near or in the plane of the equators of the
planets which they revolve around. (Neptune's Triton is the best exception
to this rule. Its orbit is retrograde).
- Planetary distances can be mathematically stated through a simple
formula known as the Titius-Bode law (1772)--Johann E. Bode and Johann
D. Titius. The distances given below are stated in AUs.
| |
Mer |
Ven |
Ear |
Mar |
Ast |
Jup |
Sat
|
Uran |
Nept |
Pluto |
| Bode- |
0.0
|
0.3
|
0.6
|
1.2
|
2.4
|
4.8
|
9.6
|
19.2
|
38.4
|
76.8
|
| Titus |
0.4
|
0.4
|
0.4
|
0.4
|
0.4
|
0.4
|
0.4
|
0.4
|
0.4
|
0.4
|
| Law |
0.4
|
0.7
|
1.0
|
1.6
|
2.8
|
5.2
|
10.0
|
19.6
|
38.8
|
77.2
|
| |
|
|
|
|
|
|
|
|
|
|
| Actual |
0.4
|
0.7
|
1.0
|
1.5
|
2.8
|
5.2
|
9.5
|
19.2
|
30.1
|
39.4
|
- There are two major classifications of planets in the solar system:
the terrestrials (earth like) and the Jovians (Jupiter like). Between
these two groups there are distinct size, mass, density and compositional
differences.
- Jupiter and Saturn contain 99 percent of the angular momentum of
the solar system (the momentum is predominantly orbital). The sun
contains only one percent the angular momentum of the solar system.
- Comets, asteroids, and meteoroids form distinct classes of objects
within the solar system which must be explained. Their orbital eccentricities
and inclinations are higher than the planets, while their sizes are
smaller.
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