The Sun: Our Star How does the Sun work ? What is the energy source for the Sun ? The Planets Lecture 15 © 2005
Download ReportTranscript The Sun: Our Star How does the Sun work ? What is the energy source for the Sun ? The Planets Lecture 15 © 2005
The Sun: Our Star How does the Sun work ? What is the energy source for the Sun ? The Planets Lecture 15 © 2005 Pearson Education Inc., publishing as Addison-Wesley The Sun Homework • Read Chapter 14: The Sun • MasteringAstronomy: Assignment Chapter 14 Due Friday, Oct 24, 6pm © 2005 Pearson Education Inc., publishing as Addison-Wesley Partial Solar Eclipse Meet on grass area across from Pimentel Hall Thursday 2:30-4:00pm Questions about The Sun 1. 2. 3. 4. 5. 6. 7. 8. 9. What is the Sun made of? What produces the enormous light energy ? How many years will the Sun continue shining? Is the Sun’s light output constant, or variable? What doesn’t the Sun contract, due to its gravity? How did the Sun form ? What are sunspots? And those loops on the surface? What is the “sunspot cycle”? Does the Sun have layers inside, like the Earth? © 2005 Pearson Education Inc., publishing as Addison-Wesley Answers about The Sun 1. What produces the enormous light energy ? Nuclear reactions: 4H He : Fusion 2. How many years will the Sun continue shining? 5 Billion years 3. Is the Sun’s light output constant, or variable? Constant! Within 0.1% 4. What doesn’t the Sun contract due to its gravity? Gas Pressure pushes outward. 5. How did the Sun form ? A massive gas cloud collapsed by its own gravity. 6. What are sunspots? Dark regions with strong magnetic fields. . © 2005 Pearson Education Inc., publishing as Addison-Wesley Observable Properties of the Sun Distance: 1.5 x 108 km = 1 A.U. Luminosity: 3.8 x 1026 watts Light spreads out spherically Mass = 300,000 x Earth Radius = 110 x Earth Density = 1.4 g/cm3 ~ 40% more than Water 1 sec of Luminosity supplies 500,000 yrs of energy for humanity. © 2005 Pearson Education Inc., publishing as Addison-Wesley Quiz: Each person uses roughly 1000 Watts (i.e., 10 100-Watt light bulbs). How much energy per second do humans use in the entire world? a) 7x108 W b) 7x1012 W Approach: Find approximate answer 9) • 7 billion people (7 x 10 c) 7x1016 W • 1000 watts per person d) 7x1020 W • Total power: 7 x 10129 x 1000 = 7x10 Watts © 2005 Pearson Education Inc., publishing as Addison-Wesley Quiz: How much energy, in Joules, do all humans use in one year? a) 2x108 W b) 2x1012 W c) 2x1016 W Approach:12Find approximate answer • 7 x 10 Watts d) 2x1020 W X • One year = • 365 days x 24 hour/day x 3600 sec/hour = 3 x 107 seconds Total Energy = 7 x 1012 Watts x 3 x 107 sec = 21 x 1019 Joules © 2005 Pearson Education Inc., publishing as Addison-Wesley Quiz: How much energy, in Joules, do humans use in one year? a) 2x108 J b) 2x1012 J Approach: Find approximate answer c) 2x1016 J • 7 x 1012 Watts d) 2x1020 J • One year = • 365 days x 24 hour/day x 3600 sec/hour = 3 x 107 seconds Total Energy = 7 x 1012 Watts x 3 x 107 sec = 21 x 1019 Joules © 2005 Pearson Education Inc., publishing as Addison-Wesley Properties of the Sun Density: 1.4 g/cm3 ~ 40% more than Water Implies: Sun is Gaseous compressed by gravity No hard surface © 2005 Pearson Education Inc., publishing as Addison-Wesley Composition of the Sun Dark spectral lines are caused by absorption of light by atoms in the Sun’s atmosphere. Magnesium Calcium Sodium Iron You can measure the amount of different atoms from darkness of the absorption lines. © 2005 Pearson Education Inc., publishing as Addison-Wesley Composition of the Sun (by Mass) C, N, O, Ne, Fe, Others: 2% He 28% Hydrogen 70% Representative of the Universe as a whole: Hydrogen and Helium Dominate. (But not for Earth.) © 2005 Pearson Education Inc., publishing as Addison-Wesley H He O 0.3% C 0.2% Fe Gravity Balanced by Pressure • Gas pressure supports the star against the inward force of gravity. • At Sun’s center, pressure is huge. (Weight of material above is huge.) • Huge Pressure Huge temperature and densities at Sun’s center. © 2005 Pearson Education Inc., publishing as Addison-Wesley Center of the Sun Computer models (balancing gravity with pressure) show: Temperature = 15 Million K Collisions between atoms so violent: • electrons removed from atoms: Atoms are Ionized • leaving bare nucleus of each atom. Nuclei of atoms collide & react Nuclear Reactions Fusion of Hydrogen to Helium © 2005 Pearson Education Inc., publishing as Addison-Wesley Fusion occurs only in the Sun’s core • Nuclear fusion • a reaction where Hydrogen combines (fuses) to form Helium nuclei. + + • Electric force: nuclei repel each other. • Nuclei have positively charged protons • For fusion to occur, nuclei must be moving fast enough to overcome electric repulsion • This requires high temperatures At low speeds, electric repulsion prevents protons from coming close. + + • When nuclei touch, the nuclear force binds them together At high speeds, protons overcome electric repulsion. Come close. Nuclear reaction! © 2005 Pearson Education Inc., publishing as Addison-Wesley Neutrons Neutrons are not stable! They do not exist alone for long! + e + ¯ e - n p+ p+ n + e+ + e (inverse -decay) (-decay) e is a neutrino ---- a weakly interacting particle which has almost no mass and travels at nearly the speed of light. e- = electron e+ = positron (anti-electron) © 2005 Pearson Education Inc., publishing as Addison-Wesley Note: Charge conserved. Energy Generation: Nuclear Fusion in the Sun: Proton-Proton Chain IN: 6 H, (2 e-) OUT: He, 2 H, 2 e, 4 4 H nuclei are converted into 1 He nucleus and energy is released. © 2005 Pearson Education Inc., publishing as Addison-Wesley Energy Generation: Nuclear Fusion in the Sun: Proton-Proton Chain IN: 6 H, (2 e-) OUT: He, 2 H, 2 e, 4 4 H nuclei are converted into 1 He nucleus and energy is released. © 2005 Pearson Education Inc., publishing as Addison-Wesley Quiz • a) b) c) d) Which particle has the greatest mass? helium electron proton deuterium © 2005 Pearson Education Inc., publishing as Addison-Wesley Proton - proton Reaction makes Deuterium P+P D + positron + neutrino D = 2H = Deuterium = proton+neutron 2H: © 2005 Pearson Education Inc., publishing as Addison-Wesley “2” is number of Protons + neutrons D+P 3He + photon © 2005 Pearson Education Inc., publishing as Addison-Wesley 3He + 3He © 2005 Pearson Education Inc., publishing as Addison-Wesley He + 2P © 2005 Pearson Education Inc., publishing as Addison-Wesley Quiz What is this object? a) deuterium b) tritium c) helium d) 2H © 2005 Pearson Education Inc., publishing as Addison-Wesley Quiz What is this object? a) deuterium b) tritium c) helium d) 2H © 2005 Pearson Education Inc., publishing as Addison-Wesley Mass Accounting Mass Input: 4 p + 2 eMass Output: 1 He (2p + 2n) Look up Masses of particles: Mass Input > Mass Output Mass Input = 1.007 Mass Output Mass is missing ! Mass is not conserved! Converted to Energy: 2 E = mc 8 m/s. Where c is speed of light, 3x10 © 2005 Pearson Education Inc., publishing as Addison-Wesley Nuclear Reactors on Earth work by Fission A heavy nucleus, such a Uranium 235 is split apart by a fast-moving neutron. The resulting nuclei have lower energy. The extra energy comes out as fast-moving particles, notably neutrons that provide the energy of the reactor, heating the material to high temperatures. Fission: http://www.youtube.com/watch?v=G1jtWR_tcX4&feature=elated © 2005 Pearson Education Inc., publishing as Addison-Wesley The Solar Thermostat Suppose the Sun Heats Up at little accidentally Is there a negative feedback to bring temperature back ? • Higher Temp causes faster collisions: - Nuclear reactions proceed faster. - More energy is produced. • Added energy heats Sun to higher temperature. The Sun expands ! • Expansion causes gas density to be lower. • So, atoms are farther apart. • Nuclear reaction rate declines. • Sun cools - - - Back to normal Temp. Sun’s energy output (luminosity) remains stable: Thermostat © 2005 Pearson Education Inc., publishing as Addison-Wesley The Solar Luminosity has Risen 30% in Past 4 Billions years • During the past 4.6 billion years: • 4 Hydrogen atoms fused into Helium • Core now has fewer atoms. Lower pressure: the Sun’s core contracts, causing it to heat up • The fusion rate increases (until higher pressure balances gravity) • A new equilibrium is reached at a higher energy output • Thus, the Sun’s luminosity increases. • Computer Models indicate the Sun’s luminosity has increased 30% since it formed 4.6 billion years ago. • From 2.9 x 1026 watts to today’s 3.8 x 1026 watts © 2005 Pearson Education Inc., publishing as Addison-Wesley Core • T = 15 million K; Depth = inner 1/4 of Sun • Where the Sun’s energy is generated. Interior Zones • Energy is transported from center outward. • The interior is divided into two zones: • Radiation Zone (energy carried by light) • Convection Zone (energy carried by rising hot gas) • Boundary between them is at: • T = 2 x 106 K; Distance from center: 0.70 RSun © 2005 Pearson Education Inc., publishing as Addison-Wesley Layers of the Sun Solar Wind photosphere Convective Zone Core © 2005 Pearson Education Inc., publishing as Addison-Wesley Radiative Zone Photon Transport of Energy “Radiation Transport” © 2005 Pearson Education Inc., publishing as Addison-Wesley Energy Transport by Photons (Light) • Radiation Zone • Energy travels as photons of light, which continually collide with particles • Photons scatter, changing direction (random walk), and change wavelengths • This is called radiative diffusion Path of photon, scattered by electrons and atoms. © 2005 Pearson Education Inc., publishing as Addison-Wesley • This is a slow process! • It takes about 1 million years for energy to travel from the core to the surface. Layers of the Sun Solar Wind Convective Zone Core © 2005 Pearson Education Inc., publishing as Addison-Wesley Radiative Zone Convective Transport of Energy Wait 10 sec For flame © 2005 Pearson Education Inc., publishing as Addison-Wesley Convective Energy Transport • Convection: Hot air rises; carries heat with it. • The bottom of the convection zone is heated … hot gas rises to the top • cooler gas sinks to the bottom…similar to boiling a pot of water! • Energy is brought to the surface via bulk motions of matter © 2005 Pearson Education Inc., publishing as Addison-Wesley Convection in the Sun: Hot gases rise, cool gases fall © 2005 Pearson Education Inc., publishing as Addison-Wesley Layers of the Sun Solar Wind photosphere Convective Zone Core © 2005 Pearson Education Inc., publishing as Addison-Wesley Radiation Zone Photosphere • T = 5,800 K; depth = 400 km • This is the yellow “surface” that we see. © 2005 Pearson Education Inc., publishing as Addison-Wesley The Photosphere: Visible Surface of the Sun • Photosphere: opaque “surface” human eye sees. • Granulation (convection) • Sunspots © 2005 Pearson Education Inc., publishing as Addison-Wesley The Sun: 1 Hour Ago Sun in Visible Light Nov 19, 2013 4pm (PST) © 2005 Pearson Education Inc., publishing as Addison-Wesley http://sdo.gsfc.nasa.gov/data/ http://www.spaceweather.com/ Solar Magnetic Activity • The photosphere of the Sun is covered with sunspots. • Sunspots are not constant; they appear & disappear. • They appear and disappear in a cycle, lasting 11 years. • Sun’s magnetic field switches polarity (N-S) every 11 yrs • So the entire cycle repeats every 22 yrs © 2005 Pearson Education Inc., publishing as Addison-Wesley Sunspots: Cool, Magnetic Regions © 2005 Pearson Education Inc., publishing as Addison-Wesley Sunspots: Umbra and Penumbra Umbra Penumbra © 2005 Pearson Education Inc., publishing as Addison-Wesley Partial Solar Eclipse Thursday 2:30-4:00pm Meet on grass area across from Pimentel Hall Partial Solar Eclipse The Sun: Our Star End of Lecture 20 © 2005 Pearson Education Inc., publishing as Addison-Wesley Extra Slides Neutrinos from the Sun • Neutrinos are created in the proton-proton reaction. • We have detected them, proving that the theory of nuclear fusion reactions is correct! • But we only detect about 30% of the neutrinos predicted by theoretical models. • Reason: Three types of neutrinos: • electron (e), muon (), and tau () • our neutrino detectors can register only electron neutrinos • Neutrinos can change type after being created, allowing us to detect only 1/3 of them © 2005 Pearson Education Inc., publishing as Addison-Wesley “Observing” the Solar Interior • The Sun’s interior is opaque… • we can not see directly into it with light • We can construct mathematical computer models of it. • the models are a grid of temperature, pressure, & density vs. depth • these values are calculated using known laws of physics • they are tested against the Sun’s observable quantities • We can directly measure sound waves moving through the interior • we observe “sunquakes” in the photosphere by using Doppler shifts • motion of sound waves can be checked against interior conditions predicted by models • There is another way to see directly into the core…neutrinos! © 2005 Pearson Education Inc., publishing as Addison-Wesley