# DE2410: Learning Objectives. SOLAR SYSTEM Formation, Evolution and Death. Solar System: To Size Scale. Learning Objectives : This Lecture

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1 DE2410: Learning Objectives SOLAR SYSTEM Formation, Evolution and Death To become aware of our planet, solar system, and the Universe To know about how these objects and structures were formed, are evolving and will die To become aware of life of the Universe Dr. Rohan Munasinghe BSc, MSc, PhD, MIEEE Department of Electronic and Telecommunication Engineering Faculty of Engineering University of Moratuwa To become a broad-minded, complete human by knowing about the Universe and Life in it. Solar System: To Size Scale Learning Objectives : This Lecture What constitutes the solar system Scale model of the solar system Origin of the Sun and planets Fate of the Sun and Planets

2 Sun Members of the Solar System Eight planets More than 130 satellites of the planets A large number of small bodies Comets, asteroids, and asteroid belt Interplanetary medium Kuiper belt and Oort cloud Solar System s Whereabouts The Solar System is in the Milky Way galaxy on its Orionis spiral arm, some 30,000 light years from the galactic centre. Its speed is about 220 km/s, thus, completes one revolution around the galactic centre in million years. Since its formation, the Solar System has completed at least 18 such revolutions Solar System s Whereabouts Solar System: 1/Billion Model Solar system is at least 4.6 billion years old (meteorite radiometric dating) 1 parsec = light years 1 light year = km What is the size of the Sun? 1.5m What is the size of the Earth? How far is the Sun from the Earth? How far is the Moon from the Earth? How big is the Jupiter? How far is Jupiter from the Sun How far is the Saturn from the Sun How far are the Uranus/Neptune from the Sun How far is the nearest star from the Sun? 1.3cm (a grape) 150m 30cm 15cm 750m 1500m 3km/4.5km 40km

3 Origin of the Solar System NEBULAE HYPOTHESIS Nebulae Theory: A STRONG THEORY Gravitational collapse of a small part of a giant molecular cloud Most of the collapsing mass collected in the centre, forming the Sun Rest flattened into a protoplanetary disc planets, moons, asteroids, and other small solar system bodies were formed Hubble image of protoplanetary discs in the Orion nebula, a light-years-wide "stellar nursery" Originated in the 18 th century P-S. Laplace Emanuel Swedenborg, Immanuel Kant, and Pierre- Simon Laplace Serious consideration in the space age in the 1950s 1980s: Acceptance with the observation of young stars being surrounded by cool discs of dust and gas 1990s: Strengthened by the discovery of extra-solar planets Theory has been refined based on the observations Nebulae Hypothesis: PROTOPLANETARY DISC Nebulae Hypothesis: STABLE SUN and ACCRETION DISC Nebula spun faster as it collapsed As the nebulae collapsed, the atoms began to collide with increasing frequency, converting their kinetic energy into heat Gravity, gas pressure, magnetic fields, and rotation caused the contracting nebula to flatten into a spinning protoplanetary disc with a diameter of 200 AU and form a hot, dense protostar (a star in which hydrogen fusion has not yet begun) at the centre. Within 50 million years, the temperature and pressure at the core of the Sun became so great that its hydrogen began to fuse, creating an internal source of energy to counter the gravitational contraction Sun became stable (hydrostatic equilibrium) Dust grains around the central Proto-Sun formed into clumps on 1-10km size by direct contact, which in turn collided to form larger bodies

4 Inner Solar System: Rocky Dwarf Inner Solar System Rocky dwarfs Rock and metal Relatively high densities Slow rotation Solid surfaces No rings Few satellites Near the newborn Sun, temperature was so high that only the materials of high melting point could stay and form planets Such as Fe, Ni, Al and rocky silicates Only comprise 0.6% of the nebulae mass Thus small planetesimals were formed near the Sun Moon-Mars size bodies The main asteroid belt lies between the orbits of Mars and Jupiter Solar wind (T-Tauri stage) of the new Sun swept away gasses to distant areas Within 100million years: inner solar system planetasimals collided and merged to form terrestrial planets Mercury, Venus, Earth, and Mars Frost Line and Outer Solar System Outer Solar System: Gas Giants Beyond a distance from the Sun, temperature was low enough for gasses to condense and form planets Gasses were the most abundant (99% of mass), thus, bigger planets were formed far away from the Sun Jupiter, Saturn, Uranus, Neptune Jupiter (5AU) was just outside the frost-line, and accumulated huge amount of vapor released from infalling materials Jovian or gas giants Hydrogen and helium Low densities Rapid rotation Deep atmospheres Rings Lots of satellites Saturn was formed later, thus, accumulated less amount of gasses than Jupiter

5 Uranus and Neptune Uranus, and Neptune are too big and too quick to be accreted at their distances from the Sun, thus, believed to have formed closer (between Jupiter and Saturn) and later moved outward After 3-10 million years almost all gas had been swept into interstellar space. Planet formation ceased Asteriod Belt With the formation of Jupiter and Saturn (3-4 million years), their gravity caused orbital resonance of nearby planetisimals that disturbed planet formation in the vicinity Planetisimals in 2-4 AU couldn t accrete into planets Planetary embryos and small planetesimals of the asteroid belt might have thrown out by Jupiter. And, some may have fallen on the Earth, bringing water here. Otherwise, water is too volatile to have been present at Earth's formation. Orbital Resonance: Jupiter and Saturn Kuiper Belt Jupiter and Saturn underwent orbital changes and eventually reached 2:1 orbital resonance Galilean Moons Jupiter and Saturn caused Neptune to move outward, and also ejected planetisimals from the Kuiper belt and scattered planetary disc Formed the Oort cloud

6 Oort Cloud Verification of Nebulae Theory: Extra Solar Planets First confirmation: Orbiting pulsars PSR B (1992) and PSR B (1993) The first extra-solar planet orbiting a normal star 51 Pegasi was discovered in 1995 At present, there are 281 planets listed 277 orbiting normal stars 63 in multiple planet systems 214 in single planet systems 4 around orbiting pulsars Extra-Solar Planet Discoveries Destiny of the Planets Planets' orbits are chaotic over longer timescales In all cases this means that the position of a planet along its orbit ultimately becomes impossible to predict with any certainty After next few billion years Mars's eccentricity may grow to around 0.2, such that it lies on an Earth-crossing orbit, leading to a potential collision with the Earth. Mercury's eccentricity may grow even further, and a close encounter with Venus could theoretically eject it from the Solar System altogether

7 Earth-Moon Dynamics Why do we always see the same side of the Moon? 1:1 lock at present: Moon always shows one side towards Earth Moon and Tides Moon revolves (27days) around the Earth slower than the Earth s rotation (24hrs) causing gravitational bulge on Earth s seas to lead ahead of the Moon Momentum transfers from Earth to Moon Slows down the spin of the Earth Speeds up the Moon, causing it to spiral out and recede from us After 50B years, both the Earth and Moon will show one side to the other Near Side (visible) Far Side (not visible) Planet-Moon Dynamics Neptune and Triton Seen by Voyager2 When a moon is revolving around a planet faster than the planet rotates, the tidal bulge lags behind the moon in its orbit Momentum transfers from the moon to planet Planet speeds up its rotation Moon slows down and spiral in to the planet, reach the Roche limit, tears apart and fall, or form a ring system Phobos of Mars (within 30 to 50 million years) Triton of Neptune (in 3.6 billion years) Metis and Adrastea of Jupiter at least 16 small satellites of Uranus and Neptune. Planet-Moon Dynamics: Tidal-lock Tidal bulge stays directly under the moon, there is no transfer of angular momentum, and the orbital period will not change Pluto and Charon are an example of this type of configuration

8 Saturn s Rings Gravitational interactions with Saturn's moons were expected to gradually sweep the rings' outer edge toward the planet However, data from the Cassini mission led scientists to revise that early view. Observations revealed 10 km-wide icy clumps of material that repeatedly break apart and reform, keeping the rings fresh Fate of the Solar System changes in the Solar System will come from changes in the Sun itself as it ages As the Sun burns its hydrogen fuel, it gets hotter, and burns the remaining fuel even faster. As a result, the Sun is growing brighter at a rate of 10% every 1.1 billion years Backlit Saturn shows two new faint rings and Earth (Cassini mission, 2007) Fate of the Solar System Around 5.4 billion years from now, all of the hydrogen in the core of the Sun will have fused into helium. The core will loose its counter action against gravitational collapse and will begin to contract This heats up the shell around the core until hydrogen starts burning there. This will cause the outer layers of the star to expand greatly, bringing the Sun to the red giant stage Fate of the Solar System 7.5 billion years, the Sun will expanded to a radius of 1.2 AU 250 times its current size Sun's surface will be much cooler, about 2600 K than now and its luminosity much higher up to 2700 times current solar luminosity Sun will have a strong stellar wind which will carry away around 33% of its mass As the Sun expands, it will most likely swallow the planets As the Sun expands, it will most likely swallow the planets Mercury and Venus. Earth's fate is less clear, but a 2008 study suggests that Earth will likely be swallowed up as a result of tidal interactions with the Sun's weakly bound outer envelope Sun: as at present and when it is a red giant

9 Fate of the Solar System He flash Hydrogen burning in the shell around the solar core will increase the mass of the core until it reaches about 45% of the present solar mass, at which point the density and temperature will become so high that the fusion of helium into carbon will begin, leading to a helium flash; the Sun will shrink from times its present radius. Consequently, its luminosity will decrease from times its current level, and its surface temperature will increase to about 2600 K 4770 K The Sun will keep burning helium in its core in a stable fashion much like it burns hydrogen today. The heliumfusing stage will last only 100 million years Fate of the Solar System: Second Expansion As the core depletes with He, the Sun will burn the reserves of hydrogen and helium in its outer layers and will expand for a second time. Here the luminosity of the Sun will increase again, reaching about 2100 times of the present luminosity, and it will cool to about 3500 K. This phase will last about 30 million years Fate of the Solar System: Planetary Nebulae Over the course of a further 100,000 years, the Sun's remaining outer layers will fall away, ejecting a vast stream of matter into space and forming a halo known (misleadingly) as a planetary nebula The ejected material will contain the helium and carbon produced by the Sun's nuclear reactions, continuing the enrichment of the interstellar medium with heavy elements for future generations of stars The Ring nebula, a planetary nebula similar to what the Sun will become

10 Fate of the Solar System: White Dwarf Sun's loss of mass could send the orbits of the surviving planets into chaos, causing some to collide, others to be ejected from the Solar System, and still others to be torn apart by tidal interactions Afterwards, all that will remain of the Sun is a white dwarf, an extraordinarily dense object, 54% its original mass but only the size of the Earth Initially, this white dwarf may be 100 times as luminous as the Sun is now. It will consist entirely of degenerate carbon and oxygen, but will never reach temperatures hot enough to fuse these elements. Thus the white dwarf Sun will gradually cool, growing dimmer and dimmer Fate of the Solar System: Black Dwarf As the Sun dies, its gravitational pull on the orbiting bodies such as planets, comets and asteroids will weaken due to its mass loss. All remaining planets' orbits will expand; if Earth still exists, its orbit will lie at about 1.85 AU. And, all the remaining planets will become dark Carbon and oxygen in the Sun's core will freeze, with over 90% of its remaining mass assuming a crystalline structure Eventually, after billions more years, the Sun will finally cease to shine altogether, becoming a black dwarf

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