Book contents
- Frontmatter
- Contents
- Foreword
- Note on the expression of planetary masses
- 1 Introduction
- 2 The internal structure of the Earth
- 3 Methods for the determination of the dynamical properties of planets
- 4 Equations of state of terrestrial materials
- 5 The Moon
- 6 Mars, Venus and Mercury
- 7 High pressure metals
- 8 Jupiter and Saturn, Uranus and Neptune
- 9 Departures from the hydrostatic state
- 10 Conclusion
- Appendix 1 Limits and conditions on planetary models
- Appendix 2 Combination of effects of small departures from a uniform distribution of density
- Appendix 3 The physical librations of the Moon
- References
- Index
- Frontmatter
- Contents
- Foreword
- Note on the expression of planetary masses
- 1 Introduction
- 2 The internal structure of the Earth
- 3 Methods for the determination of the dynamical properties of planets
- 4 Equations of state of terrestrial materials
- 5 The Moon
- 6 Mars, Venus and Mercury
- 7 High pressure metals
- 8 Jupiter and Saturn, Uranus and Neptune
- 9 Departures from the hydrostatic state
- 10 Conclusion
- Appendix 1 Limits and conditions on planetary models
- Appendix 2 Combination of effects of small departures from a uniform distribution of density
- Appendix 3 The physical librations of the Moon
- References
- Index
Summary
The lesser objects of the solar system
So far in our studies, no notice has been taken of the smaller bodies in the solar system, i.e. Pluto, the asteroids and the satellites of Mars and the major planets, for their properties are but poorly known on the whole and it is not very rewarding to apply to them the type of analysis that was applied in the foregoing parts of this book to the greater objects. Yet, in considering the solar system as a whole, their existence and such information as we have of them cannot be ignored.
Pluto, the outermost known planet, is in a highly eccentric orbit highly inclined to the ecliptic, and, in consequence, although it comes on occasion within the orbit of Neptune, it never approaches Neptune closely, and detailed studies have shown the outer solar system to be stable. Pluto is a very small object as seen from the Earth. Its diameter is estimated from the brightness and supposed reflectivity. The latter has recently been redetermined from infra-red spectroscopy and the diameter of Pluto is consequently now estimated to lie between 2800 and 3300 km (Cruickshank, Pilcher and Morrison, 1976). The mass of Pluto was originally estimated from the perturbations of the orbits of Uranus and Neptune, but a satellite has now been detected (Christy and Harrington, 1978) with a period of 6.4 d, from which the mass of Pluto is estimated to be about 0.002 times that of the Earth (Meadows, 1980).
- Type
- Chapter
- Information
- Interiors of the Planets , pp. 302 - 308Publisher: Cambridge University PressPrint publication year: 1980