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The formation of stars and planets

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Title: The formation of stars and planets


1
The formation of stars and planets
  • Day 2, Topic 2
  • Self-gravitating
  • hydrostatic
  • gas spheres
  • Lecture by C.P. Dullemond

2
B68 a self-gravitating stable cloud
Bok Globule
Relatively isolated, hence not many external
disturbances
Though not main mode of star formation, their
isolation makes them good test-laboratories for
theories!
3
Hydrostatic self-gravitating spheres
  • Spherical symmetry
  • Isothermal
  • Molecular

From here on the material is partially based on
the book by Stahler Palla Formation of Stars
4
Hydrostatic self-gravitating spheres
Spherical coordinates
5
Hydrostatic self-gravitating spheres
Spherical coordinates
6
Hydrostatic self-gravitating spheres
Numerical solutions
7
Hydrostatic self-gravitating spheres
Numerical solutions
Exercise write a small program to integrate
these equations, for a given central density
8
Hydrostatic self-gravitating spheres
Numerical solutions
9
Hydrostatic self-gravitating spheres
Plotted logarithmically (which we will usually
do from now on)
Numerical solutions
Bonnor-Ebert Sphere
10
Hydrostatic self-gravitating spheres
Different starting ?o a family of solutions
Numerical solutions
11
Hydrostatic self-gravitating spheres
Numerical solutions
Singular isothermal sphere (limiting solution)
12
Hydrostatic self-gravitating spheres
Boundary condition Pressure at outer edge
pressure of GMC
Numerical solutions
13
Hydrostatic self-gravitating spheres
Another boundary condition Mass of clump is given
Numerical solutions
One boundary condition too many!
14
Hydrostatic self-gravitating spheres
  • Summary of BC problem
  • For inside-out integration the paramters are ?c
    and ro.
  • However, the physical parameters are M and Po
  • We need to reformulate the equations
  • Write everything dimensionless
  • Consider the scaling symmetry of the solutions

15
Hydrostatic self-gravitating spheres
All solutions are scaled versions of each other!
16
Hydrostatic self-gravitating spheres
A dimensionless, scale-free formulation
17
Hydrostatic self-gravitating spheres
A dimensionless, scale-free formulation
Lane-Emden equation
18
Hydrostatic self-gravitating spheres
A dimensionless, scale-free formulation
Boundary conditions (both at ?0)
Numerically integrate inside-out
19
Hydrostatic self-gravitating spheres
A dimensionless, scale-free formulation
A direct relation between ?o/?c and ?o
20
Hydrostatic self-gravitating spheres
  • We wish to find a recipe to find, for given M and
    Po, the following
  • ?c (central density of sphere)
  • ro (outer radius of sphere)
  • Hence the full solution of the Bonnor-Ebert
    sphere
  • Plan
  • Express M in a dimensionless mass m
  • Solve for ?c/?o (for given m)
  • (since ?o follows from Po ?ocs2 this gives
    us ?c)
  • Solve for ?o (for given ?c/?o)
  • (this gives us ro)

21
Hydrostatic self-gravitating spheres
22
Hydrostatic self-gravitating spheres
23
Hydrostatic self-gravitating spheres
Dimensionless mass
Recipe Convert M in m (for given Po), find ?c/?o
from figure, obtain ?c, use dimless solutions
to find ro, make BE sphere
24
Stability of BE spheres
  • Many modes of instability
  • One is if dPo/dro gt 0
  • Run-away collapse, or
  • Run-away growth, followed by collapse
  • Dimensionless equivalent dm/d(?c/?o) lt 0

25
Stability of BE spheres
26
Bonnor-Ebert mass
  • Ways to cause BE sphere to collapse
  • Increase external pressure until MBEltM
  • Load matter onto BE sphere until MgtMBE

27
Bonnor-Ebert mass
Now plotting the x-axis linear (only up to ?c/?o
14.1) and divide y-axis through BE mass
Hydrostatic clouds with large ?c/?o must be very
rare...
28
BE Sphere Observations of B68
Alves, Lada, Lada 2001
29
Magnetic field support / ambipolar diff.
As mentioned in previous chapter, magnetic fields
can partly support cloud and prevent collapse.
Slow ambipolar diffusion moves fields out of
cloud, which could trigger collapse.
  • Models by Lizano Shu (1989) show this
    elegantly
  • Magnetic support only in x-y plane, so cloud is
    flattened.
  • Dashed vertical line is field in beginning,
    solid after some time. Field moves inward
    geometrically, but outward w.r.t. the matter.
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