Guiding Questions Our Star the Sun 1 2 3 Chapter Eighteen An Overview of the Details What is the source of the Sun s energy What is the internal structure of the Sun How can astronomers measure the properties of the Sun s interior 4 How can we be sure that thermonuclear reactions are happening in the Sun s core 5 Does the Sun have a solid surface 6 Since the Sun is so bright how is it possible to see its dim outer atmosphere 7 Where does the solar wind come from 8 What are sunspots Why do they appear dark 9 What is the connection between sunspots and the Sun s magnetic field 10 What causes eruptions in the Sun s atmosphere The Sun s energy is generated by thermonuclear reactions in its core The energy released in a nuclear reaction corresponds to a slight reduction of mass according to Einstein s equation E mc2 Thermonuclear fusion occurs only at very high temperatures for example hydrogen fusion occurs only at temperatures in excess of about 107 K In the Sun fusion occurs only in the dense hot core The Sun s energy is produced by hydrogen fusion not in a single step but in a sequence of thermonuclear reactions in which four hydrogen nuclei combine to produce a single helium nucleus 1 A theoretical model of the Sun shows how energy gets from its center to its surface Solar Model Results Hydrogen fusion takes place in a core extending from the Sun s center to about 0 25 solar radius The core is surrounded by a radiative zone extending to about 0 71 solar radius In this zone energy travels outward through radiative diffusion The radiative zone is surrounded by a rather opaque convective zone of gas at relatively low temperature and pressure In this zone energy travels outward primarily through convection Understanding Hydrostatic Equilibrium Understanding Hydrostatic Equilibrium II 2 How do we know about the solar interior More Model Results By using the Sun s own vibrations Helioseismology is the study of how the Sun vibrates These vibrations have been used to infer pressures densities chemical compositions and rotation rates within the Sun A Subatomic Interlude A Subatomic Interlude II A Subatomic Interlude III 3 A Subatomic Interlude V A Subatomic Interlude IIII Neutrinos are produced in the Weak Interaction for example Neutrinos from the earth natural radioactivity Man made neutrinos accelerators nuclear power plants Astrophysical neutrinos Solar neutrinos Atmospheric neutrinos Relic neutrinos left over from the big bang Neutrino Detection Neutrino Factoids The earth receives about 40 billion neutrinos per second per cm2 from the sun Detecting neutrinos requires a different kind of a detector About 100 times that amount are passing through us from the big bang This works out to about 330 neutrinos in every cm3 of the universe By comparison there are about 0 0000005 protons per cm3 in the universe Our body emits about 340 million neutrinos per day from 40K Neutrinos don t do much when passing through matter Remember it is very difficult to observe neutrinos Neutrinos reveal information about the Sun s core and have surprises of their own Neutrino Detection II The neutrino is observed by detecting the product of its interaction with matter e Electron Muon Neutrinos emitted in thermonuclear reactions in the Sun s core have been detected but in smaller numbers than expected Recent neutrino experiments explain why this is so 4 The Photosphere The Sun is a sphere although it appears as a disk This leads to a phenomenon known as limb darkening the lowest of three main layers in the Sun s atmosphere The Sun s atmosphere has three main layers the photosphere the chromosphere the corona Everything below the solar atmosphere is called the solar interior The visible surface of the Sun the photosphere is the lowest layer in the solar atmosphere The spectrum of the photosphere is similar to that of a blackbody at a temperature of 5800 K Convection in the photosphere produces granules More Convection The Chromosphere characterized by spikes of rising gas Above the photosphere is a layer of less dense but higher temperature gases called the chromosphere Spicules extend upward from the photosphere into the chromosphere along the boundaries of supergranules Cross Sectional View of the Solar Atmosphere 5 The Corona outermost layer of the solar atmosphere made of very hightemperature gases at extremely low density The corona ejects mass into space to form the solar wind The solar corona blends into the solar wind at great distances from the Sun Activity in the corona includes coronal mass ejections and coronal holes Sunspots low temperature regions in the photosphere 6 Sunspot Cycle Sunspots on the move Sunspots are produced by a 22 year cycle in the Sun s magnetic field The Sun s surface features vary in an 11 year cycle the sunspot cycle The average number of sunspots increases and decreases in a regular cycle of approximately 11 years with reversed magnetic polarities from one 11year cycle to the next This is related to a 22 year cycle the solar cycle in which the surface magnetic field increases decreases and then increases again with the opposite polarity Two sunspot cycles make up one 22 year solar cycle The solar magnetic changes are caused by convection and the Sun s differential rotation The magnetic dynamo model suggests that many features of the solar cycle are due to changes in the Sun s magnetic field 7 Rotation of the Solar Interior The Sun s magnetic field also produces other forms of solar activity A solar flare is a brief eruption of hot ionized gases from a sunspot group A coronal mass ejection is a much larger eruption that involves immense amounts of gas from the corona 8 Key Words 22 year solar cycle chromosphere CNO cycle conduction convection convective zone corona coronal hole coronal mass ejection differential rotation filament granulation granule helioseismology hydrogen fusion hydrostatic equilibrium limb darkening luminosity of the Sun magnetic dynamo model magnetogram magnetic reconnection negative hydrogen ion neutrino neutrino oscillation photosphere plage plasma positron prominence 9