Stellar structure and evolution II
SPAT0045
Marc-Antoine Dupret
Associate Professor
email: ma.dupret@ulg.ac.be tel: 04 3669732
Bât. B5c, 1er flour
Stellar formation
Stellar formation
1) Molecular clouds
• Mass : ~ 104 – 105 M¯ . • Size : ~ 1 – 50 pc
•Temperature : ~ 10 – 15 K° • Number density : ~ 108 - 1010 part./m3
3 types of interstellar clouds
H
2mainly
2) Atomic clouds : HI regions
•Temperature : ~ 30 – 80 K°
Atomic H mainly
• Number density : ~ 107 - 109 m-3
3) Ionized clouds : HII regions
•Temperature : ~ 8000 K°
H
+mainly
• Number density :
~ 102 - 106 m-3 10-25 air
Most abundant but most difficult to detect (21 cm line)
• If the cloud density is high enough ( ) , the atoms can form molecules
³ / 10
10m
pm
Molecular clouds
We have a molecular cloud
• Most abundant molecule :
H
2Problem : not easy to detect !!
Radio waves from CO
• Organic molecules mainly
•Mass : ~ 50 000 M
¯.
•Size : ~ 40 light years
Stellar formation
• The clouds do not collapse immediately because : - Force due to interstellar magnetic field - Internal pressure gradient
- Centrifugal force
But this equilibrium is not eternal
• Factors breaking the equilibrium : - Entering into a high density zone.
- Shock wave due to supernova explosion
Barnard 68, un globule de Bok composé de gaz et de poussière. Les forces de gravitéet de pression
sont encore en équilibre, mais le nuage risque à tout moment de s'effondrer
Gravitational contraction
Cloud collapse
Instability of a proto-stellar cloud (H
2) Jeans criterion : the cloud is unstable if :
Isothermal sound speed
If ff vs < , during the free fall time ff, the pressure does not increase enough to counterbalance the increasing weight
collapse
Size of
perturbation vs2 = P/ ~ T/
Dispersion relation :
A slightly more rigorous approach :
How does the cloud reacts to a plane wave perturbation ?
w2 < 0 : unstable w2 > 0 : stable
Cloud collapse
Instability of the proto-stellar cloud (H
2)
~ 10-24 g/cm3, T ~ 10 K , =2
MJ ~ 400 M0
MJ
Fragmentation
Jeans criterion : the cloud is unstable if :
Isothermal sound speed
Size of
perturbation vs2 = P/ ~ T/
Cloud collapse
Step 1 : Isothermal collapse
Free fall time ~ (G)-1/2 ~ 106 years
>>
Thermal adjustment time scale
The isothermal collapse stops when ff ~ th
Isothermal collapse
0.018
Mass of smallest fragments ~ 0.03 M0 >> planetary masses
Cloud collapse
Fragmentation Step 2 : Adiabatic collapse
When M ~ M¯: free fall time scale ~ thermal adjustment time scale : Adiabatic collapse Tc, Pc
Supersonic collapse speed near the center
Appearance of a shock wave
“Hydrostatic equilibrium” below
Cloud collapse
Step 1 : Isothermal collapse
: no longer fragmentation
When Tc ~ 2000 K Dissociation : H2 H + H
New collapse
New « hydrostatic equilibrium » below
107 R0
5UA
Appearance of a 2nd shock wave Endothermic reaction 1 = ln P/ ln|s
Dynamical instability
Step 2 : Adiabatic collapse
Cloud collapse
à 107 R¯ !
5UA
Cloud collapse
Step 2 : Adiabatic collapse
Dissociation : H2 H + H
New collapse
1 = ln P/ ln|s Dynamical instability
New hydrostatic equilibrium below
Appearance of a 2nd shock wave
Lignes de naissance
L ~ 2 R
2
sv
3accThe kinetic energy of the accreted matter is converted into infrared radiation.
The accretion disk
Initially, the star is entirely hidden by its accretion disk
Stationnary equatorial accretion disk:
Near the axis: Gravitational force >> Centrifugal force
- Matter is accreted near the poles where the angular momentum is low - The magnetic field acts against star-disk differential rotation
The accretion disk ensures the evacuation of angular momentum
jcloud ~ 1021-1022 cm2s-1 >> jT Tauri ~ 1016-1017 cm2s-1 >> jSun ~ 1015 cm2s-1 Angular momentum per unit mass:
Gravitational force Centrifugal force=
(weak pressure gradient)
The accretion disk
The Hayashi track :
entirely convective models
) 2
, ( 4
1
r P T dm
dr
= 4
4 r m G dm
dP
−
= P
T r Gm dm
dT
ad 4
- 4
= 3 differential equations :
3 unknown functions : r(m), P(m), T(m) 2 parameters to be fixed : M et L
3 boundary conditions (1 at the center, 2 at the photosphere):
0 ) 0 ( = r
For fixed M and L One solution 1 point in the HR diag.
Fixed M, variable L one family of solutions curve in the HR diag.
This is the Hayashi track
of mass MGeneral definition :
The Hayashi track of mass M is the curve in the HR diagram corresponding to the stellar models of mass M
entirely convective and in hydrostatic equilibrium (but not necessarily in
thermal equilibrium)
Hayashi tracks
of different masses
The Hayashi track:
entirely convective models
P ad
ln d
T ln
d
Same mathematical question but with :
Forbidden region
Too strong Convection (Lc too large) Allowed region
Partially radiative model
Forbidden region Allowed
region
Right and left of the Hayashi track
P ad
ln d
T ln
d
P ad
ln d
T ln
d
Gravitational contraction
maintaining hydrostatic equilibrium Virial theorem
Total gravitational energy
4 r4
m G m
P = −
4 2
1 r m
r =
Hydrostatic
equilibrium Mass
Monoatomic perfect gas, degenerated or not,
non-relativistic
Ei = s0M u dm
E
g= - 2 E
iIntegration by part
Total internal energy :
(Perfect gas)
E
g= - 2 E
iHelmholtz – Kelvin time : HK = GM2 / (R L)
E
tot= E
i+ E
gTotal energy :
Conservation of total energy without internal production
No nuclear reactions !
L = - dEtot /dt = – d Ei / dt – dEg / dt
= dEi /dt = -(1/2) dEg / dt
L - s dm
With nuclear reactions, replace L by
During the contraction, half of the released gravitational potential energy is converted into internal energy, the other half is radiated.
Gravitational contraction
maintaining hydrostatic equilibrium
Virial theorem
Simplified case : evolution at constant (low) mass
When a star becomes visible, it is entirely convective.
It goes down the Hayashi track
Gravitational contraction
maintaining hydrostatic equilibrium
Helmholtz – Kelvin time :
HK= GM
2/ (R L)
Gravitational contraction
maintaining hydrostatic equilibrium
Minimal luminosity
, why ?(Kramers) and Tc
cAppearance of a radiative core
As long as the star is entirely convective : descent along the
Hayashi track
16 4
3
GmT ac
L P
rad
=
~ 0T-3.5
Gravitational contraction
maintaining hydrostatic equilibrium
Minimal luminosity
Appearance of the radiative core when:
Next :
Crossing of the HR diagram towards the left
Henyey track
Gravitational contraction
maintaining hydrostatic equilibrium
Pre-main sequence
1.5 – 4 M
Entirely convective
Entirely radiative
If M > 1.5 M
sun, the star becomes nearly entirely
radiative when T
eff> 6000-6500 K
Birthline
dM/dt ~ 10-5 M0/year
Gravitational contraction
maintaining hydrostatic equilibrium
But, in reality, the mass of the star is not constant during this phase !
Typical 2 steps modeling:
1. Evolution with constant accretion rate
(typically 10-5M0/ year)
The star moves on a
« birthline » of given accretion rate
2. Evolution with constant mass : 2.1 Hayashi track : low masses only 2.2 Henyey track
But, in reality, the mass of the star is not constant during this phase !
Typical 2 steps modeling:
1. Evolution with constant accretion rate
(typically 10-5M0/ year)
The star moves on a
« birthline » of given accretion rate
2. Evolution with constant mass : 2.1 Hayashi track : low masses only 2.2 Henyey track
Gravitational contraction
maintaining hydrostatic equilibrium
Starting or not of nuclear reactions ?
Role of electronic degeneracy
Question : During the gravitational contraction, is Tc always increasing ? Virial theorem : P/ increases
Ideal gas : P/ / T Yes for a non-degenerated ideal gas But … No for a degenerated gas
r r’ = x r = r + dr = (1+dr/r) r
’ = /x3
P=Weight P’ = Weight’
= P/x4
d/ = ’(m)/(m) – 1
= 1/(1+dr/r)3 - 1 = – 3 dr/r dP/P = P’(m)/P(m) – 1
= 1/(1+dr/r)4 - 1 = – 4 dr/r Homologous contraction
dr/r = x-1 = cst
Equation of state : d/ = dP/P - dT/T
dT/T = (/) dP/P - (1/) d/
= (4-3)/(3) d/ dP/P = (4/3) d/ r r’ = x r = r + dr = (1+dr/r) r
’ = /x3
P P’ = P/x4
d/ = ’(m)/(m) – 1
= 1/(1+dr/r)3 - 1 = – 3 dr/r dP/P = P’(m)/P(m) – 1
= 1/(1+dr/r)4 - 1 = – 4 dr/r Homologous contraction
dr/r = x-1 = cst
Starting or not of nuclear reactions ?
Role of electronic degeneracy
dT/T = (4 -3)/(3 ) d /
For a non-degenerated = 1 , = 1 dT/T = (1/3) d/ ideal gas
For a degenerated = 3/5 , = 0 dT/T = - ∞ d/
non-relativistic gas
d/ = dP/P - dT/T
T
T
The gravitational energy released during the contraction is not
sufficient to accelerate the degenerated electrons (Fermi energy ).
The missing energy is drawn from the kinetic energy of the non- degenerated ions, so that the temperature decreases.
Starting or not of nuclear reactions ?
Role of electronic degeneracy
Degenerated : dT/T = - d/ non-relativistic gas
: Degeneracy parameter
Non-degenerated gas dT/T = (1/3) d/
Cas général : dT/T = (4-3)/(3) d/
Slope 1/3
Slope 2/3
T-3/2 = cte
General case : dT/T = (4-3)/(3) d/
Starting or not of nuclear reactions ?
r r’ = x r = r + dr = (1+dr/r) r
Homologous expansion with change of mass :
Fixed density: d/ = 0 dr/r = 1/3 dm/m dP/P = 2/3 dm/m Ideal gas: dT/T = dP/P - d/ = dP/P = 2/3 dm/m
The larger the mass, the larger the central temperature (at fixed density)
= dm/(4 r2dr)
dP/P = (1+dm/m)2/(1+dr/r)4 - 1 = 2 dm/m – 4 dr/r P = smM Gm/(4 r4)dm
m(r) m’(r’) = q m(r) = (1+dm/m) m(r)
‘ = dm’/dr’ (1/(4r’2)) = (q/x)dm/dr (1/(4x2r2)) = (q/x3)
d/ = (1+dm/m)/(1+dr/r)3 – 1 = dm/m – 3 dr/r P’ = smM Gm’/(4 r’4)dm’ = (q2/x4) P
Cas général : dT/T = (4-3)/(3) d/
Evolution of T
cas a function of
cdT/T= 2/3 dm/m
Non-degenerated gas
dT/T = (1/3) d/ Degenerated : dT/T = - d/ non-relativistic gas
Effect of the mass on the (
c, T
c) trajectory
Required temperature for hydrogen burning :
T
c~ 10
7K
Critical mass : M = 0.08 M
0If M < 0.08 M
¯, the star never reaches
the temperature required to initiate hydrogen burning (because of electron degeneracy)
Brown dwarf
Starting or not of
nuclear reactions ?
Total gravitational energy Ei, tot = ∫0M u dm = 3/2 ∫0M (P/) dm
E
g= - 2 E
i, tot-1/2 dE
g/dt = L = dE
i/dt
Cooling of brown and white dwarfs
Total internal energy
Virial theorem
The internal energy increases during the contraction !!
-1/2 E
g= E
i,tot Ei, tot : Internal energy (ions + electrons) Eg : Gravitational energyVirial theorem :
Ee : Electrons internal energy
Eions << Ee The whole released gravitational energy
increases the electrons kinetic energy
/
= cst.
= - 3 dr/r
Eg = - 2 Ei, tot
Cooling of brown and white dwarfs
L = - dEtot /dt = - d Eions /dt – d Ee /dt – d Eg /dt
= - d Eions /dt
The whole radiated energy is drawn from the ions kinetic energy.
Decoupling Hydrostatic pressure, gravity :
electron gas Thermal aspects : ion gas
Temperature decreases
Cooling of brown and white dwarfs
The whole released gravitational energy increases the electrons kinetic energy.
L = - d E
ions/dt = - c
vM dT
0/dt E
ions= ∫
0Mu
ionsdm = c
vT
0M
Isothermal core
(very efficient electronic conduction)
The temperature decreases slowly
Cooling of brown and white dwarfs
The whole radiated energy is drawn from the ions kinetic energy.
Homologous contraction or expansion, maintaining hydrostatic equilibrium
dT/T = (4-3)/(3) d/ Non-deg. gas : dT/T = (1/3) d/
State eq. : d/ = dP/P - dT/T
Gaz parfait
Non-degenerated ideal fully ionized gas : dQ = - cv dT !!!
Degenerated gas : contraction is blocked : dQ = cv dT
Gravothermal specific heat
Provided heat
Heat is supplied to the star, how does it react ? …
How does the star react to the onset
of nuclear reactions ?
Gaz parfait
When heat is supplied, the temperature decreases ! Why ?
The provided heat leads to a double expansion work (to maintain the hydrostatic equilibrium).
The remainder of required energy to produce this work is drawn from the internal energy reservoir
The temperature decreases Local Virial theorem
Gravothermal specific heat
Heat is supplied to the star, how does it react ? …Homologous contraction or expansion in hydrostatic equilibrium Non-degenerated ideal fully ionized gas : dQ = - cv dT !!!
How does the star react to the onset
of nuclear reactions ?
Why ?
The ion and electron gas are decoupled.
The degenerated electron gas freezes the star
(because the mass-radius relation of a degenerated sphere is stable).
The provided heat increases the kinetic energy of the ions The temperature increases
Degenerated gas, the star is “frozen” : dQ = cv dT
Homologous contraction or expansion in hydrostatic equilibrium
Gravothermal specific heat
How does the star react to the onset
of nuclear reactions ?
Loop
1) Contraction u T
2) dQ>0 (nuclear reactions) T P expansion 3) Pdv > dQ du < 0 T
4) dQ<0 contraction 5) Thermal equilibrium
How does the star react to the onset
of nuclear reactions ?
Expansion of the core
T
c|dT/dm|
-1/2 dEg/dt = L - ∫ dm< 0
L
The starting of nuclear reactions leads to an expansion of the core, a decrease of the central
temperature and of the luminosity and a decrease of the total stellar radius.
How does the star react to the onset
of nuclear reactions ?
C12, O16 -> N14 Towards
CNO equilibrium
Towards P-P equilibrium
If M > 1.2 M0, 2 steps : 1)
2) Cycle reaches equilibrium C12, O16 N14
2 hooks in the HR diag.
Henyey track
The onset of nuclear reactions leads to an expansion of the core,
a decrease of the central temperature and of the luminosity and a decrease of the
total stellar radius.
Concrete example : Pre-Main- Sequence evolution of a 2 M 0 star
ZAMS
When the core becomes radiative, T ds/dt = du/dt + P dv/dt = - dL/dm < 0 its contraction is accelerated and L
But the contraction of the envelope is stopped
Radiative zone Convective zone
ZAMS
Nuclear reactions (CNO) Appearance of a convective core
and drop of L, 2 hooks in the HR diag.
Radiative zone Convective zone
Concrete example : Pre-Main-
Sequence evolution of a 2 M 0 star
ZAMS
g = -T ds/dt = -dQ/dt = -du/dt - P dv/dt = dL/dm - nucg < 0 expansion work, g > 0 contraction (released gravitational energy)
Concrete example : Pre-Main-
Sequence evolution of a 2 M 0 star
2 observational cases :
T Tauri stars
- Low masses ( < 2-3 M
0) - On the Hayashi track
- Highly variable and active (X, radio), winds - Accretion disk (one half)
Herbig Ae/Be stars
- Larger masses ( 1.5 - 8 M
0) - On the Henyey track
- Circumstellar gas emission lines
Secular stability
At thermal equilibrium: dQ/dt = 0, dT/dt = 0, s dm = L
The thermal equilibrium is broken, maintaining hydrostatic equilibrium, does the star come back to its initial state ?
At disequilibrium (small perturbation % equilibrium) :
Homologous perturbation : d(X/X)/dr = 0 (X=T, , L, , , , … )
T T’ = T + T
’ = +
L L’ = L + L
’ = +
Is the onset of nuclear reactions a
thermally stable process ?
Non-degenerated ideal gas
T ~ 5 (p-p)
~ 15 (CNO)
Degenerated gas
~ 1
~ 1
T ~ -3.5 (Kramers)
c
*= - c
vStable c
*= c
vUnstable
(conduction)T ~ 2The thermal equilibrium is broken, maintaining hydrostatic equilibrium, does the star come back to its initial state ?
Is the onset of nuclear reactions a thermally stable process ?
Secular stability
The Zero Age Main Sequence (ZAMS)
Location of models in thermal equilibrium for core H burning, with a fixed chemical composition
Duration of the main sequence phase:
~ (Q
pp/4) N
av(M/10) / L
~ 10 £ 10
9years (sun)
Qpp ~ 25 Mev
>>
HK = G M2/(2RL)Thermal equilibrium From now on, stellar evolution is due
to changes of the internal chemical composition ( essentially).
Mass-Luminosity relation
Low masses
Intermediate masses
Very large masses
The Zero Age Main Sequence (ZAMS)
Mass-Luminosity relation, consequences :
1) M L
2) M Lifetime
The Zero Age Main Sequence (ZAMS)
Typical internal structures
The size increases with the mass
< 0
The density decreases with the mass
> 0
The temperature slightly increases with the mass
Slope of the main sequence
The Zero Age Main Sequence (ZAMS)
Evolution: Main sequence phase
Evolution of the global parameters
Assuming increases everywhere homologous transformation
increases
Structural changeThe luminosity increases during the evolution
Nuclear reactions control: R
So that T and thus L do not increase too much
> 0
But in reality, increases only in the core
Solution : contraction of the core and expansion of the envelope The core must contract, but without too large increase of
the pressure and thus the temperature.
Contraction : Weight
Expansion : Weight
Evolution: Main sequence phase
Evolution of the global parameters
Low masses, p-p (M < 1.2 M0)
High masses, CNO (M > 1.2 M0)
~ 6 , ~ X2T6:
L , R , Teff ?
~ 15 , ~ X T15:
L , R , Teff
increases in the core contraction of the core
and expansion of the envelope
Evolution: Main sequence phase
Evolution of the global parameters
Effect of the metallicity
Z in the envelope, the core does not change much.
|dT/dm| Teff
M=1.4 M0 M=1.45 M0
M=1.4 M0 M=1.45 M0
Z=0.01 Z=0.02
M=1.4 M0 M=1.45 M0
M=1.4 M0 M=1.45 M0
Z=0.01 Z=0.02
M=1.6 M0
Evolution: Main sequence phase
Convective envelopes (low masses)
Difficulty : Modeling of the super-adiabatic zone (r >> rad)
r - r
ad3D MLT
Mixing-length theory
l = Hp
: mixing-length parameter
|dT/dm| Teff
MZC
rZC Convective zone base :
T ~ cst. TZC ~ cst.
Fc = cp Vc,rT (enthalpy flux)
~ cpT (P/)1/22(r - rad)3/2
Hp = |dr/dln P|
Mixing-length:
Evolution: Main sequence phase
Energy transfer 3D simulation
of convection
Convective cores (high masses)
Very efficient convection
F
c/ l
2c
pT (r - r
ad)
3/2 CpTr ~ r
adEvolution of the convective core’s mass :
The larger the mass, the larger the convective core’s mass
Most of the time,
the mass of the convective core decreases as the star evolves, leaving above a -gradient zone
T
r
radX+1
16
43
GmT ac
L P
rad
Evolution: Main sequence phase
Convective cores and envelopes
Convective core Convective
envelope
Convective cores (high masses)
If the mass of the convective core increases as the star evolves because : - Starting of the CNO cycle (around 1.3 M0)
- rad because PR (very massive stars) X discontinuity 1+Xe > 1+Xi
e>
i
Evolution: Main sequence phase
Discontinuity of X 1+Xe > 1+Xi
e>
i
r
rad> r
adSemi-convection
Partial Mixing
Evolution: Main sequence phase
Convective cores (high masses)
If the convective core mass increases (starting of CNO cycle or massive star)
Where is the convective zone boundary ??
Convective penetration – overshooting
When a convective bubble
enters in a radiative zone:
r < r
ad Deceleration, not sudden stop ! Convective penetrationzone where:
T < 0 Fc < 0
Cooling r ~ rad Growth of the adiabatic
mixed (chemically homogeneous) region
Convective cores (high masses)
Evolution: Main sequence phase
Very well constrained by asteroseismology !
Overshooting at the top of convective cores
Simple parameterization :
r
ov=
ovH
p ov : overshooting parameter Typical values :ov = 0.1 – 0.2
Increases : - Duration of the main sequence - Luminosity
Very well constrained by asteroseismology !
Evolution: Main sequence phase
Differential rotation in stars
Conservation of angular momentum:
If does not depend on
Global :
Local :
is constant over time
Evolution: Main sequence phase
Differential rotation
Rotational mixing
Evolution: Main sequence phase
Turbulence due to the shear
Meridional circulation due to Thermal imbalance (Von Zeipel paradox) Exchange of angular momentum due to
winds, tidal interactions, accretion, … Transport of angular momentum
Transport of chemicals Diffusive process
Gratton-öpik circulation cell
Rotational mixing
Turbulence (shear) + meridional circulation
Partial mixing
~ Diffusive process
Convective overshooting versus rotational mixing Convective overshooting
Inertia of
convective bubbles
Growth of the mixed adiabatic zone
Depends on rotation rate Independent of rotation
Evolution: Main sequence phase
Les étoiles peuvent tourner vite ) force centrifuge:
La Rotation
rP/ = -r + 2 r sin es ) Déformation de l’étoile ) Toutes les grandeurs (T, P, , F, …) dépendent
de 2 dimensions spatiales (r, ) ) bcp. plus lourd à résoudre Vitesse critique : si Veq = r > Vcrit ¼ (GM/R)1/2 ,
la force centrifuge dépasse la gravité ) enveloppe éjectée Pour certaines étoiles (étoiles Be, …), on n’en est pas loin !
Influence de la rotation
Affecte la structure et l’évolution de l’étoile:
- Structure 2D
- Processus de transports
Affecte les observables spectro- et photométriques (Teff , …),
car à la photosphère: F(), ge()
La baroclinité:
r£ (rP/) = -(1/2) r£r P = (1/2) r(2) £ r(r2 sin2) Rotationel de l’équation d’équilibre rP/ = -r + 2 r sin es
r sin es = (1/2) r(r2 sin2)
Pour une rotation solide ou cylindrique ((r sin)): r£rP = 0 Isobares = Iso-densité = Isothermes : P(), (), T(), …
= Potentiel total = (Rot. solide)
1
2
3
Sinon (rotation différentielle plus complexe):
Isobares Iso-densité Isothermes
Baroclinité
La Rotation
Le paradoxe de Von Zeipel:
Considérons la zone radiative d’une étoile en rotation solide P(), (), T(), …
1
2
3
Non-constant sur les équipotentielles
Quel que soit T(), il est impossible d’avoir r¢ (Frad) = 0 partout ! Déséquilibre thermique :
Cas stationaire : V ¢ rS 0
Circulation méridienne
La Rotation
Circulation méridienne
Mécanisme de transport à grande échelle:
1) Transport du moment cinétique
2) Transport des
éléments chimiques
Temps caractéristique associé à son établissement:
temps d’Eddington-Sweet:
Ensuite, la circulation s’adapte pour assurer le transport du moment angulaire requis par les conditions aux limites (vents, accrétion,
effet de marée dans les binaires proches, …)
r¢F/(T) = - V ¢ rS < 0 r¢F/(T) =
- V ¢ rS > 0
La Rotation
La rotation différentielle dans les étoiles
- Rompt la symétrie sphérique
- Varie en fonction de la profondeur - Crée un déséquilibre thermique
Si conservation du moment angulaire :
Si ne dépend pas de
Globale : Locale :
Circulation méridienne
est constant avec le temps
Evolution: Phase de séquence principale
Evolution: Phase de séquence principale
La rotation interne dans les étoiles
Conservation locale du moment angulaire
Mais en réalité, il existe de nombreux mécanismes de transports et pertes de moment angulaire (champs magnétique, circulation méridienne, turbulence, ondes
internes …)
L’astérosismologie nous permettra d’en savoir plus !
The heaviest elements go down The lightest elements go up
Microscopic diffusion
Evolution: Main sequence phase
Gravitational settling
Very quick near the surface, very slow deep in the star
High cross-section pushed up Low cross section go down
Radiative forces
Example: Iron, Nickel, … T = E/k ~ 2£105 K :
e- transitions from layer M
Opacity peak Accumulation of Iron
Diffusion
No diffusion Helium
Hydrogen
Processus non-standards: Diffusion microscopique
1) Les forces entrant en jeu
Pression partielle sur les particules i :
1.1 Les collisions
Force moyenne exercée sur la particule i par collisions :
En l’absence de r P , évolution vers l’homogénisation
1.2 La gravité
Force exercée sur la particule i par l’attraction gravifique :
Gravité + collisions
Les particules les plus lourdes sombrent, les plus légères flottent.
Processus non-standards: Diffusion microscopique
1) Les forces entrant en jeu
1. 3 Forces radiatives
Impulsion fournie / u. de vol. , de fréq. et de temps par les photons sur les ions i :
« Accélération » (force / u. de masse) de la particule i :
Processus non-standards: Diffusion microscopique
1) Les forces entrant en jeu
Contribution de toutes les forces sur la particule i :
2) Vitesses de diffusion
3) Evolution des abondances
Conservation des particules i :
Libre parcours moyen: = ( n)-1 Vitesse thermique
Si élément minoritaire (ci << 1)
Processus non-standards: Diffusion microscopique
4) Diffusion et gradients de température
Le libre parcours moyen dépend de la température car / T-2 (ions), vT / T1/2 augmente avec T déplacement des régions chaudes vers les régions froides
Très approximatif, le signe peut être opposé dans certains cas !
The Sun
Central temperature
~ 15 106 K
Proton-proton chain
15 millions °
5800°
T°K
ppI dominates
ppIII negligible T6
c2/c2
Very well constrained by helioseismology
Sound speed : c
2= P
1/ ~ T/
Rotation
:Convective envelope :
Differential rotation in latitude Radiative core : rigid rotation !!
Because of angular momentum
transport by gravitational waves ?
The sun
Different neutrino energies
PPII
0
0 7
3 0
1 7
4
Be +
−e → Li + PPIII
58B →
48Be +
01e +
ePPI H + H → H +
0e +
e1 2
1 1
1 1
1 E = 0.263 Mev
E = 0.8 Mev E = 7.2 Mev
The solar neutrino problem
T6
The flux of neutrinos at different energies is an excellent indicator of the temperature !
The sun
Spectre des neutrinos solaires
Exercice : Calculer la quantité d’hydrogène consommé en une seconde
L
= 3.9 10
33erg/s = M c
2 M = 3.9 10
33/(3 10
10)
2= 4.33 10
12g
Chaque seconde, 4.33 10
6tonnes de matière disparaît
m = m(4p) – m(He) = (4.031280-4.002603) uma
= 0.028677 uma = 7.1136‰ de m(4p)
La masse de 4.33 10
6tonnes représente donc 7.1136‰
de la masse d’hydrogène transformée
Masse totale d’hydrogène transformée par seconde
609 millions de tonnes
Exercice : Calculer le nombre de neutrinos reçus sur Terre (par cm
2et par seconde)
Chaque seconde, 609 millions de tonnes d’hydrogène sont transformées en hélium
Nombre de protons = 6.09 10
14/1.66 10
-24N
p= 3.67 10
38Chaque fois que 4 protons sont transformés, 2 neutrinos sont émis
Nombre de neutrinos = N
p/2 = 1.83 10
38/s
Surface de la sphère à la distance d de la Terre = 4 d
2(d = 150 10
6km) = 2.83 10
27cm
2Nombre de neutrinos par seconde et par cm
265 milliards
Un être humain S~0.5 m2360 mille milliards par seconde
Homestake
(R. Davis, 1968-…) 380 000 l C
2Cl
437
Cl +
e
37Ar + e
Cl*= 35 jours E
> 0.814 Mev 1
e/ 2.5 jours !
37
Ar + e
37Cl
*+
e37
Cl
*
37Cl + photon
2 km sous terre
Détection sur terre des neutrinos
Homestake
(R. Davis, 1968-…)
37
Cl +
e
37Ar + e
Cl*= 35 jours E
> 0.814 Mev 1
e/ 2.5 jours !
37
Ar + e
37Cl
*+
e37
Cl
*
37Cl + photon
1 SNU = 10
-36captures / sec. / atome de Cl
Modèles théoriques prédisent:
8-10 SNU
Résultats de l’expérience:
4 SNU
Détection sur terre des neutrinos
Gallex (1992-…)
E
> 0.233 Mev
Tous les neutrinos pp,
7Be,
8B
71
Ga +
e
71Ge + e
Ga*= 11.5 jours
71
Ge + e
71Ga
*+
e71
Ga
*
71Ga + photon
Détection sur terre des neutrinos
SuperKamiokande (M. Koshiba 1996-…) 50 000 m
3eau très pure
Diamètre 40 m – Hauteur 40 m 11 000 photodétecteurs (50 cm)
Effet Cerenkov Directionnel
Temps réel E
> 6 Mev
25
e/ jour !
1000 tonnes D
2O
12 m diameter Acrylic Vessel
18 m diameter support structure; 9500 PMTs (~60% photocathode coverage) 1700 tonnes inner shielding H2O
5300 tonnes outer shielding H2O
Sudbury Neutrino Observatory (1998-…)
Tous types de neutrinos
e,
,
Photo, Courtesy of Sudbury Neutrino Observatory
1 Kton of D2O 9500 PM tubes
The flux of detected electronic neutrinos is 2-3 times smaller than what it should be in a standard solar model !!
Neutrinos are oscillating ! If we consider all kinds of neutrinos, the total detected flux is in agreement with the solar model
Evolution : phase de séquence principale
Evolution de la composition chimique
Faibles masse : Chaîne P-P
La majorité des éléments « minoritaires » : D, L
i, B
e, B est brulée au cœur lors de la phase pré-séquence principale
TLi ~ 2 106 K , TBe ~ 3 106 K, TB ~ 5 106 K
Valeurs d’équilibre
(suffisemment profond)
0 0 7
3 0
1 7
4
Be +
−e → Li +
+
→
+ H Be
Li
84 1
1 7
3
+
→ + H B Be
11 587 4
1. Chaîne proton-proton (T > 10
7K)
Temps de réaction très court :
pd ¼ 1 sec.
+
→
+ H He H
12 231 1
Combustion du deuterium
Sur terre : D/H = 1.5 £ 10-4 Première phase de combustion du
Deuterium initial, puis équilibre.
Evolution de la composition chimique
Phénomène de spaliation
1. Chaîne proton-proton (T > 10
7K)
Combustion He3 + He3
Deuterium à l’équilibre
H He
He
He 23 24 11
3
2 + → +2
Au début, réaction très lente !!
Décroit quand T
Pour T trop petit, He3 n’a jamais le temps d’atteindre sa valeur d’équilibre,
donc bosse
Evolution de la composition chimique
1. Chaîne proton-proton
Combustion He3 + He3 H He
He
He 23 24 11
3
2 + → +2
Evolution de la composition chimique
Décroit quand T
eq (années) Soleil
Problème du Lithium
Mécanismes hydrodynamiques non-standards de transport des régions profondes vers la surface : diffusion, circulation méridienne, ondes internes, …
L’abondance de Lithium à la surface du Soleil est 140 * plus
petite que sa valeur initiale PPII
37Li +
11H →
48Be +
L’étude d’amas jeunes (Hyades, …) montre que l’abondance en surface
diminue au cours du temps TLi ~ 2 106 K
1. Chaîne proton-proton
Evolution de la composition chimique
2. Cycle CNO T > 15 10
6K
1. C12 N14
O16 N14 (beaucoup plus lent)
2. Evolution complexe car :
- Présence d’un coeur convectif qui homogénise et dont la taille change - Certains constituants n’atteignent
jamais la valeur d’équilibre
Evolution de la composition chimique
Au départ :
C12 : N14 : O16 = 5.5 : 1 : 9.5 A l’équilibre (typiquement) : C12 : N14 : O16 = 0.15 : 15 : 0.3
12
C
14
N
Post main sequence evolution
Step 1:The whole star contracts due to the thermal imbalance (Virial theorem)
After all hydrogen has been consumed in the core:
Step 2: Hydrogen burning starts in a shell above the helium core
H He He
I fix the mass Mc of the isothermal core and let the radius Rc vary.
For each Rc , I have one solution and thus one value of the pressure P0 at the top of the core.
The curve P0 (Rc) behaves as follows, with a maximum :
Post main sequence evolution:
Evolution of the helium core
Assumption (maybe wrong!): the helium core is in thermal equilibrium No energy production below the H-burning shell.
dL/dm = = 0 et L(0) = 0 L = 0 dT/dr = 0
The helium core is isothermal Question : is the helium core able
to support the envelope above it ?
The helium core: Schönberg – Chandrasekhar limit of the relative core mass q=M
c/M
Post main sequence evolution
Virial theorem for the helium core (P > 0 at the top !):
Isothermal helium core
Mc : Helium core mass M : Total mass
Envelope
The isothermal core is not always able to support the envelope!!
Support condition:
Schönberg – Chandrasekhar limit of the relative core mass
The helium core: Schönberg – Chandrasekhar limit of the relative core mass q=M
c/M
Post main sequence evolution
Mc : Helium core mass M : Total mass
Isothermal helium core
If P0, max > Weight of the envelope (Pe), a solution Rc exists such that P0(Rc) = Pe This is so when Mc / Mtot < qsc ~ 0.1
qsc ~ 0.1 is thus a mass ratio limit beyond which an isothermal core cannot support the envelope above it. What happens in this case ?
The core cannot be in thermal equilibrium : dT/dr < 0 fast contraction of the core
Evolution of the helium core :
Schönberg – Chandrasekhar limit of the relative core mass
Support condition: The curve P0 (Rc) has a maximum :
If P0, max < Weight of the envelope (Pe), there is no solution whatever Rc This is so when Mc / Mtot > qsc ~ 0.1