lecture 1 - the solar interior

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January 19, 2006 Lecture 1 - The Solar Interior Lecture 1 - The Solar Interior Lecture 1 - The Solar Interior o Topics to be covered: o Solar interior o Core o Radiative zone o Convection zone

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Lecture 1 - The Solar Interior. Topics to be covered: Solar interior Core Radiative zone Convection zone. The Solar Interior - “The Standard Model”. Core Energy generated by nuclear fusion (the proton-proton chain). Radiative Zone Energy transport by radiation. Convective Zone - PowerPoint PPT Presentation

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Page 1: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

Lecture 1 - The Solar InteriorLecture 1 - The Solar Interior

o Topics to be covered:

o Solar interioro Core

o Radiative zone

o Convection zone

Page 2: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

The Solar Interior - “The Standard Model”The Solar Interior - “The Standard Model”

o Coreo Energy generated by

nuclear fusion (the proton-proton chain).

o Radiative Zoneo Energy transport by

radiation.

o Convective Zoneo Energy transport by

convection.

Page 3: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

The Solar InteriorThe Solar Interior

o Christensen-Dalsgaard, J. et al., Science, 272, 1286 - 1292, (1996).

Page 4: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

The Solar CoreThe Solar Core

o R: 0.0 - 0.25 Rsun

o T(r): 15 - 8 MK

(r): 150 - 10 g cm-3

o Temperatures and densities sufficiently high to drive hydrogen burning (H->He).

o Ultimate source of energy in the Sun and Sun-like stars.

Page 5: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

The Solar CoreThe Solar Core

o What is the temperature and pressure in the core?

o Assume hydrostatic equilibrium:

and mass conservation:

o Divide to cancel ’s =>

o Therefore, LHS =>

and RHS =>

dP

dr= −

GMρ

r2

dM

dr= −4πr2ρ

dP

dr/dM

dr=

dP

dM= −

GM

4πr4

−dP

dMdM = PC − PS0

M

GM

4πr4dM

0

M

∫ =GM 2

8πr4

PC = pressure at core PS = pressure at surface

∴PC = PS +GM 2

8πr4

Page 6: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

The Solar CoreThe Solar Core

o Assuming PS << PC and setting r = R,

o Using the Ideal Gas Law

k = Boltzmann’s const

n = number density atoms/cm3

= density = M/4R3

o The core temperature is therefore

PC ~GM 2

8πR4

TC ~GMmH

kR

PC = nkT =ρkT

mH

o Which gives Tc ~ 2.7 x 107 K (actual value is ~1.5 x 107 K).

Page 7: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

The Solar CoreThe Solar Core

o Coulomb barrier between protons must be overcome for fusion to occur.

o To overcome Coulomb barrier, particles must have sufficient thermal kinetic energy to exceed Coulomb repulsion:

o Particles have Maxwell-Boltzmann distribution:

o There is a high-energy tail, but not sufficient … need quantum mechanics.

QuickTime™ and aTIFF (Uncompressed) decompressor

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=1010K!€

3

2kT >

e2

rnuc

=>T >2e2

3krnuc

P(E)dE ∝ Ee−

E

kT dE

Page 8: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

The Solar CoreThe Solar Core

o From Heisenberg Uncertainty Principle a proton of a given (insufficient) energy may be located within nucleus of neighbouring proton.

o Combined with high-energy M-B tail, we get the Gamow Peak.

o So protons in 3-10 keV energy

range can overcome the Coulomb

barrier (i.e., T>15MK).

o Fusion can therefore occur.

(ΔxΔp ≥ h /2)

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Page 9: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

Proton-proton cycleProton-proton cycle

o The p-p cycle occurs in three main steps.

Step 1: 1H + 1H 2H + e+ + (Q = 1.44 MeV)

o Might then expect a 2H + 2H reaction, but because of the large numbers of 1H, the following is more probable:

Step 2: 2H + 1H 3He + (Q = 5.49 MeV)

o 3He can then react with 1H, but the resultant 4Li is unstable (i.e. 3He + 1H 4Li 3He + 1H).

o The final step is then:

Step 3: 3He + 3He 4He + 21H + (Q = 12.86 MeV)

o The net result is: 4 1H 4He + 2e+ + 2 (Q = 26.7 MeV)

Page 10: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

Proton-proton cycle (cont.)Proton-proton cycle (cont.)

o ~99% of the Sun’s energy is produced via the p-p cycle. o The remaining ~1% is produced by the Carbon-Nitrogen-Oxygen (CNO) cycle.o CNO cycle is more important in more massive stars.

Page 11: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

Proton-proton vs. CNOProton-proton vs. CNO

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Page 12: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

The Radiative ZoneThe Radiative Zone

o R: 0.25 - 0.8 Rsun

o T(r): 8 - 0.5 MK

(r): 10 - 0.01 g cm-3

o Hydrogen burning cuts off abruptly at r ~ 0.25 Rsun

.

o Interior becomes optically thin or transparent as density decreases.

o Energy transported radiatively.

o Photons cannot be absorbed in the radiative zone as the temperature are too high to allow atoms to form. Therefore no mechanism for the absorption of photons.

Page 13: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

The Radiative ZoneThe Radiative Zone

o For T = 15MK Wien’s displacement law implies max = 0.19 nm i.e., the center of the Sun is full of X-rays.

o Photons do 3D random walk out of Sun.

o Assume photon moves l between interactions (mean free path) and takes a total number of steps N.

o On average it will have moved a distance

o As tdifusion = N l / c and

=> tdiffusion >104 yrs!

d = l N

R = l N => tdiffusion = R2 / lc

Page 14: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

Solar InteriorSolar Interior

o Total radiative energy inside Sun is: J

where a = 4/c is the radiation constant.

o Can thus estimate solar luminosity from, W

o Which gives, L ~ 3 x 1026 W.

o Actual value is actually 4 x 1026 W.

E = aT 4 4

3πR3 ⎛

⎝ ⎜

⎠ ⎟

L =E

tdiffusion

=16π

3σT 4Rl

Page 15: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

The Convective ZoneThe Convective Zone

o R: 0.8 - 1 Rsun

o T(r): 0.5 MK - 6000 K.

<0.01 g cm-3

o Photons now absorbed as temperature is sufficiently low to allow atoms to form. Gas is optically thick or opaque.

o Continuous absorption of photons by lower layers causes a temperature gradient to build up between the lower and upper layers.

o Plasma become convectively unstable, and large convective motions become the dominant transport mechanism.

TH > TC

TH

TC

r

Page 16: Lecture 1 - The Solar Interior

January 19, 2006 Lecture 1 - The Solar Interior

The Convective ZoneThe Convective Zone

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