1 Solar Energy Lecture #8 16 February 2015 HNRT 228 Spring 2015 Energy and the Environment.

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Presentation transcript:

1 Solar Energy Lecture #8 16 February 2015 HNRT 228 Spring 2015 Energy and the Environment

2 Chapter 4 Summary Energy from the Sun – This lecture will focus on this only Passive solar systems Solar Thermal Systems – Electric power generation indirectly Photovoltaic systems – Making electricity directly Solar cooling systems

3 Guiding Questions 1. What is the source of the Sun’s energy? 2. What is the internal structure of the Sun? 3. 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?

4 An Overview of the Details

5 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 = mc 2 Thermonuclear fusion occurs only at very high temperatures; for example, hydrogen fusion occurs only at temperatures in excess of about 10 7 K In the Sun, fusion occurs only in the dense, hot core

6 iClicker Question The release of energy from the Sun is accompanied by a very slight Aincrease in the Sun's gravitational attraction on the planets Bincrease in the Sun's rotation rate Cdecrease in the mass of the Sun Dall of the above are true Enone of the above are true

7 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

8

9

10

11 iClicker Question The proton-proton reaction in the core of the sun is a multi-step process in reality, but it can be summarized as which of the following? A1 x 4 He  4 x 1 H + energy B4 x 1 He  1 x 4 H + energy C4 x 1 H + energy  1 x 4 He D4 x 1 H  1 x 4 He + energy Eall of the above are equivalent.

12 A theoretical model of the Sun shows how energy gets from its center to its surface 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

13 iClicker Question Which of the following is true of Hydrogen conversion into Helium? – AIt absorbs more energy than it creates. – BIt only takes place in stars more massive than the Sun. – CIt takes place throughout the interior of the Sun. – DIt takes place only in the core of the Sun. – EAll of the above are true regarding Hydrogen conversion into Helium.

14 Understanding Hydrostatic Equilibrium

15 Understanding Hydrostatic Equilibrium II

16 iClicker Question Most of the Sun's energy is produced in Asupergranules Bthe convection zone Cthe photosphere Dthe chromosphere Ethe core

17 iClicker Question Energy generation in the Sun results from Afission of uranium Bfission of hydrogen Cgravitational contraction Dthe Sun isn't generating energy; it's just cooling Efusion of hydrogen

18 How do we know about the solar interior? 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

19 Solar Model Results

20

21 iClicker Question The fraction of the Sun that is comprised of hydrogen and helium is roughly A98% B90% C50% D10% E2%

22 A Subatomic Interlude

23 A Subatomic Interlude II

24 A Subatomic Interlude III

25 A Subatomic Interlude IV 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.

26 Neutrino Factoids The earth receives about 40 billion neutrinos per second per cm 2 from the sun. – About 100 times that amount are passing through us from the big bang.  This works out to about 330 neutrinos in every cm 3 of the universe!  By comparison there are about protons per cm 3 in the universe. Our body emits about 340 million neutrinos per day from 40 K. Neutrinos don’t do much when passing through matter. Remember, it is very difficult to observe neutrinos.

27 Neutrino Detection The neutrino is observed by detecting the product of its interaction with matter. nene Electron nmnm Muon

28 Neutrinos reveal information about the Sun’s core—and have surprises of their own 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

29 iClicker Question Which of the following are most likely to get to Earth from the core of the Sun, before any of the others? Aprotons Belectrons Cphotons Dneutrinos Eall of the above will arrive at about the same time

30 The Photosphere - 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

31 The Sun is a sphere, although it appears as a disk. This leads to a phenomenon known as limb darkening.

32 iClicker Question The correct order of the layers of the Sun from innermost to outermost is: Acore, chromosphere, photosphere Bcore, convective layer, radiative layer Cradiative layer, convective layer, core Dconvective layer, core, radiative layer Ecore, radiative layer, convective layer

33 Convection in the photosphere produces granules

34 More Convection

35 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

36 Cross Sectional View of the Solar Atmosphere

37 The solar corona blends into the solar wind at great distances from the Sun The Corona – outermost layer of the solar atmosphere, made of very high-temperature gases at extremely low density

38 The corona ejects mass into space to form the solar wind

39 iClicker Question The highest temperatures found in the Sun’s atmosphere is located in the Achromosphere Bcorona Cphotosphere Dcore Ecytosphere

40 Activity in the corona includes coronal mass ejections and coronal holes [below is an x-ray image of the Sun]

41 iClicker Question The solar wind is mostly composed of Aoxygen Bdust grains Cneutrinos Dphotons Echarged particles

42 Sunspots - low-temperature regions in the photosphere

43 iClicker Question Sunspots are Aareas obscured by higher layers of clouds Bashes of nuclear burning brought to the surface by convection Choles in the photosphere that allow us to see deeper regions Dregions which are cooler and darker than surrounding material Ecausing global warming

44 Sunspot Cycle - Sunspots on the move

45 Sunspots are produced by a 22-year cycle in the Sun’s magnetic field – solar magnetic cycle

46 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 11-year 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

47 The magnetic-dynamo model suggests that many features of the solar cycle are due to changes in the Sun’s magnetic field

48 iClicker Question During the sunspot cycle the position of new sunspots on the Sun Achanges from mid-latitudes to the equator Bchanges from mid-latitudes to the poles Cchanges from the equator to the mid- latitudes Dchanges from the equator to the poles Edoes not change in any predictable manner

49 iClicker Question Sunspot cycles are, on the average, what length? A22 years B11 years C5.5 years D1 year E3 years

50 The solar magnetic changes are caused by convection and the Sun’s differential rotation

51 iClicker Question The solar cycle is determined by the change in the Asolar constant Bsunspot location and number Csolar radiance flux measurements Dsolar electric field changes Esolar magnetic field polarity

52 iClicker Question During a sunspot cycle Aeach sunspot increases in size and then decreases in size Bthe material composing a spot makes one complete rotation Cthe spots move from one of the Sun's polar regions to the other Dthe number of spots rises to maximum and then decreases to a minimum Ethe Sun and the spots on it make one complete rotation

53

54 Picture of Sun from Mason Observatory

55 iClicker Question Coronal mass ejections are Alarge bits of the sun that blow out into interplanetary space Bcharged particles from the sun accelerated/guided by magnetic field lines Cricher in heavier elements than other mass ejections Dnothing to be feared by spacecraft and humans in space Enever going to achieve escape velocity

56

57 Rotation of the Solar Interior

58 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

59 Jargon 22-year solar (magnetic) cycle 11-year sunspot 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