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Astr 1050     Wed. Feb. 18, 2004
  •    Today:  Chapter 7, the Sun


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Basic Properties of the Sun
  • Radius: R  = 6.96 ´ 105  km    (q=diameter/distance)
  • Mass: M = 1.99 ´ 1030 kg




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Basic Properties of the Sun
  • Surface Temperature 5800 K (from lmax  or  spectral type)
    • Not all that hot by laboratory standards


  • Central Temperature 15 ´ 106 K (explained later)
    • Central temperature IS very high

  • Luminosity (L) 3.8 ´ 1026 J/s ( L = sT4surface ´ 4 p R2sun)
       ( L = Fat Earth   
    ´ 4 p R21 AU)


    • Will be important for understanding energy generation in Sun
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Physical State of material in Sun
  • At these T’s, r’s,  hydrogen will be a gas
    • At high enough T, as pressure (P) increases and r increases,
      you never really get a “liquid”, just a very dense gas.
  • H ionization?
    • On outside, H mostly neutral  (a small fraction is ionized)
      • remember H ionized and Balmer lines gone only above 10,000 K
    • Over most of interior, H completely ionized
      • separate electrons (e-) and protons (p+)
      • Ionized gas called a “plasma”


  • No discrete “surface” – just increasing r, T, P, and “opacity”
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How we determine T, r, P vs depth

  • From theory:
    • Pressure (P) and density (r) must increase with depth
      • Weight of overlying gas compresses lower material -- “Hydrostatic equilibrium”
    • Temperature (T) must increase with depth
      • Energy is flowing out of the sun – and it flows from hot to cold -- so hot inside
    • Numerical modeling of details let us calculate T(r), r(r), P(r)


  • From observations of “oscillations” or “solar seismology”
    • The sun oscillates like a bell (or the air in an organ pipe)
    • The frequency depends upon sound speed, which depends upon T(r), r(r), P(r)
    • Observations from “Global Oscillation Network Group (GONG) telescopes.


  • From interpreting the spectrum using Kirchoff’s laws
    • The Sun looks like continuous emission: Solid or hot dense gas
    • Absorption lines in the spectrum: Cooler gas between us and the dense gas
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How we determine T, r, P vs depth I.

  • From theory:
    • Pressure (P) and density (r) must increase with depth
      • Weight of overlying gas compresses lower material -- “Hydrostatic equilibrium”
    • Temperature (T) must increase with depth
      • Energy is flowing out of the sun – and it flows from hot to cold -- so hot inside
    • Numerical modeling of details let us calculate T(r), r(r), P(r)


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How we determine T, r, P vs depth II


  • From observations of “oscillations” or “solar seismology”
    • The sun oscillates like a bell (or the air in an organ pipe)
    • The frequency depends upon sound speed, which depends upon T(r), r(r), P(r)
    • Observations from “Global Oscillation Network Group (GONG) telescopes.


  • From using Kirchoff’s laws
    • The Sun looks like continuous emission: Solid or hot dense gas
    • Absorption lines in the spectrum: Cooler gas between us and the dense gas
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The “surface” of the Sun

  • No discrete “surface” – just increase r, T, P, and “opacity”
    • “Surface” or photosphere defined by depth from which visible photons can escape.


  • Opacity depends on wavelength, so apparent “surface” will be at different depths for different wavelengths
    • High opacity in absorption lines because these photons easily absorbed/emitted
      • Won’t see very far in at these wavelengths.
    • Low opacity in between absorption lines
      • Can see in deeper at these wavelengths.
    • Eventually  r so high gas opaque at all wavelengths (just as in solid)
    • “surface” high = cool = dark in lines;  deep = hot = bright between lines
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T,r dependence upon depth inside the sun
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Complicated T dependence at the very edge
  • We see emission lines at some wavelengths:
    • Implies very THIN HOT overlying gas at top of atmosphere
    • Gas is so thin it has trouble radiating heat away
    • Sound waves or magnetic fields heat thin gas
      • Chromosphere (“colored region” glows at a few wavelengths)
      • Corona (“crown” seen during solar eclipses)
      • Solar Wind ( escaping wind of tenuous gas)

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Detailed structure of the outer photosphere
  • CONVECTION:
    • Granulation and Supergranulation
    • Heat carried by actual motion of gas
    • Different than radiative transport
      • energy carried by photons
      • dominates deeper in sun


  • SUNSPOTS
    • Darker (and cooler) regions of sun
    • Strong magnetic fields limit convection


    • Come and go in 11 (really 22) year cycle
    • Magnetic energy releases cause “flares”
    • Material ejected causes aurora
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Nuclear forces and nuclear energy
  • What holds protons in the nuclei of atoms?
    • Coulomb (electric) repulsion should make protons fly apart
      • They are packed so close together – must have very strong force to hold them
    • Nuclear “Strong force” attracts nucleons (protons, neutrons)


  • Why doesn’t strong force collapse all atoms into a giant nucleus?
    • Nuclear Strong force is very short range
      • falls off quickly after a few proton radii
    • Coulomb force is long range
      • falling off only as 1/r2
  • At large distances only coulomb force is important Þ repulsion
  • Nuclear Strong Force important only close together
    • Requires very high speed (high temperature) collision for fusion


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The Curve of Binding Energy
  • If you keep adding protons to a nucleus?
    • Coulomb repulsion continues to increase
      • new proton feels repulsion from all other protons
    • Strong force attraction reaches limit
      • new proton can’t feel attraction from protons on far side of a big nucleus


  • Gain energy only up to point where Coulomb repulsion outweighs strong force attraction.
  • Most “stable” nucleus is 56Fe
    (26 protons, 30 neutrons, 56 total)


  • Release energy by fusion of  light nuclei to make heaver ones– up to 56Fe
  • Release energy by fission of heavy nuclei to make lighter ones – down to 56Fe
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The Role of the Nuclear “Weak Force”
  • Why can’t we keep adding neutrons rather than protons?
    • They feel strong force attraction – with no Coulomb repulsion
    • You should be able to get lots of energy by adding neutrons


  • Nuclear Weak Force can (slowly) convert protons to neutrons and back
    • The reactions involve an electron or “positron” to keep charges balanced
    • The reactions produce a new almost massless particle called a neutrino


    • p+ + e- Û n + n p+ is proton
      e- is electron
      n  is neutron
      n is neutrino


    • p+ Û n + e+ + n e+ is positron = antiparticle of electron

      If this second reaction happens then the positron annihilates the next electron it encounters, thereby producing the equivalent of the first reaction.
  • The weak force likes to keep ~equal protons and neutrons in a nucleus
  • The proton repulsion tips the balance towards slightly more neutrons in big nuclei
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The four fundamental forces
  • Gravity Dominates on astronomical scales


  • Electromagnetic Holds atoms together:  Chemistry


  • Strong force Holds nuclei together:   Nuclear energy


  • Weak force n Ûp+, e- Radioactive decay
  • (will also play critical role in solar fusion)
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Fusion in the sun I.
  • Have lots of hydrogen (p+ and e-) – what can we make from it?


  • If  2He (2 protons, 0 neutrons) were stable, fusion would be “easy”
    • Run two protons into each other at fast enough to overcome Coulomb repulsion
    • Once they get close enough strong force takes over, and holds them as nucleus


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Fusion in the sun II.

  • “Unfortunately” 2He isn’t stable
    • To get stable He need to add one or two neutrons to:
      • Increase Strong Force, without increasing Coulomb force
    • Not really “unfortunate” – If 2He were stable:
      • Sun would burn energy way too fast – and would have gone out by now

  • Weak force converts proton to neutron–fusion will be slow
    • In solar fusion no excess neutrons lying around
    • Hydrogen bombs use deuterium: 2H = (p+ n) or tritium:  3H = (p+ n n) to provide it
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The Proton-Proton chain
  • The first step is slow because it relies on two rare events happening simultaneously
    • Two protons collide with enough energy to overcome the Coulomb barrier
    • While they are close the weak force turns one proton into a neutron
      • The resulting combination of a proton and a neutron IS a stable nucleus
    • 1H  +  1H  ®  2H  +  e+  +  n p+  +  p+  ®  (p+ n)  +  e+  +  n


  • The next two steps go quickly because they rely only on the strong force
    • 2H  +  1H  ®  3H (p+ n)     +   p+         ®  (p+ p+ n  )
    • 3H  +  3H  ®  4He  +  1H  +  1H                 (p+ p+ n) + (p+ p+ n) ® (p+ p+ n n) + p+ + p+

  • The net effect is       4  1H ®  4He
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Energy Released?
  • Could work it out “classically” by strength of forces
    • Classical mechanics doesn’t work at this scale – Need quantum mechanics
    • Strength of nuclear forces not originally known


  • Use E=mc2 to do accounting


    • Mass is a measure of the energy stored in a system
    • Loss of mass from a system means release of energy from that system


  • Compare mass of four 1H to mass of one 4He
    • 6.693 ´ 10-27 kg   -  6.645 ´ 10-27 kg   =  0.048 ´ 10-27 kg       drop in mass
    • E = mc2 = 0.048 ´ 10-27 kg ´ (3 ´ 108 m/s)2 =  0.43 ´ 10-11 kg m2/s2 = 0.43 ´ 10-11 J

      (note == a Joule is just shorthand for kg m2/s2)
    • So 4.3 ´ 10-12 J of energy released
      • This is huge compared to chemical energy:  2.2 ´10-18 J to ionize hydrogen
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How long will Sun’s fuel last?
  • Luminosity of sun:  3.8 ´ 1026 J/s


  • H burned rate:


  • H atoms available:


  • Lifetime:



  • In reality not all the atoms we start with are H, and only those near the center are available for fusion.  The structure of the sun will change when about 10% of the above total have been used, so after about 10 billion years.
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Testing solar fusion model
  • Does lifetime of sun make sense?
    • Oldest rocks on earth ~4 billion years old
    • Oldest rocks in meteorites ~4.5 billion years old


  • Other stars with higher/lower luminosity
    • Causes for different luminosity
    • Lifetimes of those stars


  • Look for neutrinos from fusion
    • Complicated story – due to neutrino properties
    • Example of how astronomy presents “extreme” conditions
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Neutrinos
  • Generated by “weak” force during   p+® n + e+ + n
  • “Massless” particles which interact poorly with matter
    • In that first respect, similar to photons
    • Can pass through sun without being absorbed
    • Same property makes them very hard to detect


  • Davis experiment at Homestake Mine in Black Hills
    • 100,000 gallon tank of C2Cl4 dry cleaning fluid
    • in Cl nuclei   n + n ® p+ + e-   so Cl (Z=17) becomes Ar (Z=18)
    • Physically separate out the Ar, then wait for it to radioactively decay
    • Saw only 1/3 the neutrinos predicted
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Missing Neutrino Problem
  • Lack of solar neutrinos confirmed by Kamiokande II detector in Japan.  (Using different detection method)


  • Possible explanation in terms of Neutrino physics
    • 3 different types of Neutrinos:
      • electron, muon, and tau neutrinos
      • Sun generates and Cl detectors see only electron neutrinos
      • Can electron neutrinos can change to another type on way here?
    • These “neutrino oscillations” are possible if neutrino has non-zero mass


    • Kamiokande II evidence of muon neutrinos becoming electron ones


  • Read “Window on Science 7-2”  on “scientific faith”


  • Neutrino mass may have implications for “cosmology”
  • Neutrinos also used to study supernova 1987A
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For Next time

  • Homework #4 is up on WebCT, due Wed.