Book contents
- Frontmatter
- Contents
- Miscellaneous Frontmatter
- Introduction
- Part 1 Genesis of the Sun and Solar Nebula
- Part 2 Emergence of the Sun's Family
- 2 200 000 years: Planetesimals and Protoplanets
- 2–3 million years: Gas Giants and Asteroids
- 3–10 million years: Ice Giants and Comets
- 3–10 million years: Regular Satellites
- 10–100 million years: Terrestrial Planets
- 100–1300 million years: The Heavy Bombardment
- 700–1300 million years: Building the Atmospheres
- 4500 million years? Formation of the Ring Systems
- 4660 million years: The Modern Solar System
- Part 3 Solar System Past and Present
- Part 4 End of an Era
- Glossary
- Index
3–10 million years: Ice Giants and Comets
from Part 2 - Emergence of the Sun's Family
Published online by Cambridge University Press: 10 November 2009
- Frontmatter
- Contents
- Miscellaneous Frontmatter
- Introduction
- Part 1 Genesis of the Sun and Solar Nebula
- Part 2 Emergence of the Sun's Family
- 2 200 000 years: Planetesimals and Protoplanets
- 2–3 million years: Gas Giants and Asteroids
- 3–10 million years: Ice Giants and Comets
- 3–10 million years: Regular Satellites
- 10–100 million years: Terrestrial Planets
- 100–1300 million years: The Heavy Bombardment
- 700–1300 million years: Building the Atmospheres
- 4500 million years? Formation of the Ring Systems
- 4660 million years: The Modern Solar System
- Part 3 Solar System Past and Present
- Part 4 End of an Era
- Glossary
- Index
Summary
By about 3 million years, Jupiter and Saturn had formed and were cooling down. But the protoplanetary disc was still very active. Closer to the Sun, the rocky planetesimals were continuing to gather. And much further from the Sun – twice as far out as Saturn is, and beyond – so too were the last of the icy planetesimals. Despite the abundance of ice there, it took longer for icy protoplanets to accrete to the dimensions where, like Jupiter and Saturn, they could pull in gas directly from the disc, because the orbital speeds there were slower. Eventually, though, two more dominant protoplanets of ice and rock did develop. These would become the outermost giants, Uranus and Neptune.
In time these kernels of rock and ice, each about as massive as the modern Earth, began to stockpile hydrogen and helium, just as the larger cores of the gas giants had done a couple of million years earlier. But they had arrived on the scene too late. The Sun was by now past its T-Tauri phase, and very little gas remained in the protoplanetary disc. For a few more million years Uranus and Neptune seized what little gas they could from the ever-diminishing supply, but their growth ceased after about 10 million years – the exact time remains uncertain. The end result was a pair of planets a little over one-third the diameter of Jupiter and only 5 per cent of its mass. And yet, despite their diminutive statures compared with Jupiter, Uranus and Neptune are each still heavier than 15 Earths. They were more than capable of joining in the game of cosmic billiards demonstrated earlier by Jupiter and Saturn.
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- Information
- The Story of the Solar System , pp. 30 - 31Publisher: Cambridge University PressPrint publication year: 2002