148
Statistical Mechanics of Gravitating Systems ...and some curious history of Chandra’s rare misses! T. Padmanabhan (IUCAA, Pune, INDIA) Chandra Centenary Conference Bangalore, India 8 December 2010

T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

  • Upload
    others

  • View
    3

  • Download
    0

Embed Size (px)

Citation preview

Page 1: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Statistical Mechanics of Gravitating Systems

...and some curious history of Chandra’s rare misses!

T. Padmanabhan

(IUCAA, Pune, INDIA)

Chandra Centenary Conference

Bangalore, India

8 December 2010

Page 2: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Phases of Chandra’s life

[1939] [1942] [1950]

[1961] [1983] [1995]

Page 3: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

)r

Gm2

GRAVITATIONAL N−BODY PROBLEM

)

N particles, mass m, U(r) = −

Page 4: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

)r

Gm2

Non cosmological;no bg. expansion

Cosmological;bg. expansion a(t)

GRAVITATIONAL N−BODY PROBLEM

)

N particles, mass m, U(r) = −

Page 5: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

)r

Gm2

Non cosmological;no bg. expansion

Cosmological;bg. expansion a(t)

CONDENSED MATTER PHYSICS

GRAVITATIONAL N−BODY PROBLEM

PHASE TRANSITIONS

)

N particles, mass m, U(r) = −

Page 6: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

)r

Gm2

Non cosmological;no bg. expansion

Cosmological;bg. expansion a(t)

CONDENSED MATTER PHYSICS

GRAVITATIONAL N−BODY PROBLEM

PHASE TRANSITIONS

POWERTRANSFER

)

UNIVERSAL POWER SPECTRUM,NON−LINEAR SCALING RELATIONS

N particles, mass m, U(r) = −

Page 7: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

)r

Gm2

Non cosmological;no bg. expansion

Cosmological;bg. expansion a(t)

CONDENSED MATTER PHYSICS

GRAVITATIONAL N−BODY PROBLEM

FLUIDTURBULENCE

PHASE TRANSITIONS

POWERTRANSFER

)

UNIVERSAL POWER SPECTRUM,NON−LINEAR SCALING RELATIONS

N particles, mass m, U(r) = −

Page 8: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

)r

Gm2

Non cosmological;no bg. expansion

Cosmological;bg. expansion a(t)

CONDENSED MATTER PHYSICS

GRAVITATIONAL N−BODY PROBLEM

FLUIDTURBULENCE

PHASE TRANSITIONS

RENORMALISATION GROUP

POWERTRANSFER

)

UNIVERSAL POWER SPECTRUM,NON−LINEAR SCALING RELATIONS

N particles, mass m, U(r) = −

Page 9: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

PLAN OF THE TALK

• FINITE SELF-GRAVITATING SYSTEMS OF PARTICLES

– General features

– Mean field description: Isothermal sphere

– Antonov instability

• RELAXATION TIME AND DYNAMICAL FRICTION

– Chandra’s contribution

– Historical background

• GRAVITATING PARTICLES IN EXPANDING BACKGROUND

– General features, Open questions

– Power transfer, Inverse cascade

– Universality

Page 10: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

BASICS OF STATISTICAL MECHANICS

Page 11: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

BASICS OF STATISTICAL MECHANICS

• Density of states:

Γ(E) =

dpdqθD[E −H(p, q)]; g(E) =dΓ(E)

dE

Page 12: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

BASICS OF STATISTICAL MECHANICS

• Density of states:

Γ(E) =

dpdqθD[E −H(p, q)]; g(E) =dΓ(E)

dE

• Microcanonical description: Entropy S(E) = ln g(E) where

T (E) =

(

∂S

∂E

)−1

;P = T

(

∂S

∂V

)

.

Page 13: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

BASICS OF STATISTICAL MECHANICS

• Density of states:

Γ(E) =

dpdqθD[E −H(p, q)]; g(E) =dΓ(E)

dE

• Microcanonical description: Entropy S(E) = ln g(E) where

T (E) =

(

∂S

∂E

)−1

;P = T

(

∂S

∂V

)

.

• Example: Ideal gas with H ∝∑

p2i has:

Γ ∼ V NE3N/2 ∼ g(E); T (E) = (2E/3N); P/T = N/V

Page 14: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

BASICS OF STATISTICAL MECHANICS

• Density of states:

Γ(E) =

dpdqθD[E −H(p, q)]; g(E) =dΓ(E)

dE

• Microcanonical description: Entropy S(E) = ln g(E) where

T (E) =

(

∂S

∂E

)−1

;P = T

(

∂S

∂V

)

.

• Example: Ideal gas with H ∝∑

p2i has:

Γ ∼ V NE3N/2 ∼ g(E); T (E) = (2E/3N); P/T = N/V

• Canonical description:

Z(T ) =

dpdq exp[−βH(p, q)] =

dEg(E) exp[−βE] = e−βF

with

E = −(∂ lnZ/∂β); P = T (∂ lnZ/∂V )

Page 15: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

BASICS OF STATISTICAL MECHANICS

• Density of states:

Γ(E) =

dpdqθD[E −H(p, q)]; g(E) =dΓ(E)

dE

• Microcanonical description: Entropy S(E) = ln g(E) where

T (E) =

(

∂S

∂E

)−1

;P = T

(

∂S

∂V

)

.

• Example: Ideal gas with H ∝∑

p2i has:

Γ ∼ V NE3N/2 ∼ g(E); T (E) = (2E/3N); P/T = N/V

• Canonical description:

Z(T ) =

dpdq exp[−βH(p, q)] =

dEg(E) exp[−βE] = e−βF

with

E = −(∂ lnZ/∂β); P = T (∂ lnZ/∂V )

• If energy is extensive, these descriptions are equivalent for most systems to

O(lnN/N).

Page 16: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

THE TROUBLE WITH GRAVITATING SYSTEMS

Page 17: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

THE TROUBLE WITH GRAVITATING SYSTEMS

• Long range interaction with no shielding. Energy is not

extensive.

Page 18: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

THE TROUBLE WITH GRAVITATING SYSTEMS

• Long range interaction with no shielding. Energy is not

extensive.

• Microcanonical and Canonical descriptions are not

equivalent.

Page 19: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

THE TROUBLE WITH GRAVITATING SYSTEMS

• Long range interaction with no shielding. Energy is not

extensive.

• Microcanonical and Canonical descriptions are not

equivalent.

• The g(E) and S(E) requires short-distance cutoff for

finiteness.

Page 20: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

FINITE GRAVITATING SYSTEMS

– GENERAL DESCRIPTION –

Page 21: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

FINITE GRAVITATING SYSTEMS

– GENERAL DESCRIPTION –

• Typical systems have two natural energy scales: E1 = (−Gm2/a) and

E2 = (−Gm2/R); a ≪ R.

Page 22: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

FINITE GRAVITATING SYSTEMS

– GENERAL DESCRIPTION –

• Typical systems have two natural energy scales: E1 = (−Gm2/a) and

E2 = (−Gm2/R); a ≪ R. Virial theorem gives: 2K + U = 3PV + U0.

Page 23: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

FINITE GRAVITATING SYSTEMS

– GENERAL DESCRIPTION –

• Typical systems have two natural energy scales: E1 = (−Gm2/a) and

E2 = (−Gm2/R); a ≪ R. Virial theorem gives: 2K + U = 3PV + U0.

• For E ≫ E2, gravity is not strong enough and the system behaves like a gas

confined by the container. High temperature phase with positive specific heat;

2K ≈ 3PV .

Page 24: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

FINITE GRAVITATING SYSTEMS

– GENERAL DESCRIPTION –

• Typical systems have two natural energy scales: E1 = (−Gm2/a) and

E2 = (−Gm2/R); a ≪ R. Virial theorem gives: 2K + U = 3PV + U0.

• For E ≫ E2, gravity is not strong enough and the system behaves like a gas

confined by the container. High temperature phase with positive specific heat;

2K ≈ 3PV .

• For E1 ≪ E ≪ E2, the system is unaffected by either the box or the short distance

cutoff; dominated entirely by gravity and has negative specific heat. 2K + U ≈ 0.

Page 25: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

FINITE GRAVITATING SYSTEMS

– GENERAL DESCRIPTION –

• Typical systems have two natural energy scales: E1 = (−Gm2/a) and

E2 = (−Gm2/R); a ≪ R. Virial theorem gives: 2K + U = 3PV + U0.

• For E ≫ E2, gravity is not strong enough and the system behaves like a gas

confined by the container. High temperature phase with positive specific heat;

2K ≈ 3PV .

• For E1 ≪ E ≪ E2, the system is unaffected by either the box or the short distance

cutoff; dominated entirely by gravity and has negative specific heat. 2K + U ≈ 0.

• Since canonical ensemble cannot lead to negative specific heat, microcanonical

and canonical ensembles differ drastically in this range. Canonical ensemble leads

to a phase transition.

Page 26: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

FINITE GRAVITATING SYSTEMS

– GENERAL DESCRIPTION –

• Typical systems have two natural energy scales: E1 = (−Gm2/a) and

E2 = (−Gm2/R); a ≪ R. Virial theorem gives: 2K + U = 3PV + U0.

• For E ≫ E2, gravity is not strong enough and the system behaves like a gas

confined by the container. High temperature phase with positive specific heat;

2K ≈ 3PV .

• For E1 ≪ E ≪ E2, the system is unaffected by either the box or the short distance

cutoff; dominated entirely by gravity and has negative specific heat. 2K + U ≈ 0.

• Since canonical ensemble cannot lead to negative specific heat, microcanonical

and canonical ensembles differ drastically in this range. Canonical ensemble leads

to a phase transition.

• As we go to E ≃ E1, the hard core nature of the particles begins to be felt and

the gravity is again resisted; low temperature phase with positive specific heat.

U ≈ U0.

Page 27: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

FINITE GRAVITATING SYSTEMS

– GENERAL DESCRIPTION –

• Typical systems have two natural energy scales: E1 = (−Gm2/a) and

E2 = (−Gm2/R); a ≪ R. Virial theorem gives: 2K + U = 3PV + U0.

• For E ≫ E2, gravity is not strong enough and the system behaves like a gas

confined by the container. High temperature phase with positive specific heat;

2K ≈ 3PV .

• For E1 ≪ E ≪ E2, the system is unaffected by either the box or the short distance

cutoff; dominated entirely by gravity and has negative specific heat. 2K + U ≈ 0.

• Since canonical ensemble cannot lead to negative specific heat, microcanonical

and canonical ensembles differ drastically in this range. Canonical ensemble leads

to a phase transition.

• As we go to E ≃ E1, the hard core nature of the particles begins to be felt and

the gravity is again resisted; low temperature phase with positive specific heat.

U ≈ U0.

• Increasing R increases the range over which the specific heat is negative.

Page 28: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

GENERIC BEHAVIOUR

T. Padmanabhan, Physics Reports, 188, 285 (1990).

EnsembleMicrocanonical

Page 29: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

GENERIC BEHAVIOUR

T. Padmanabhan, Physics Reports, 188, 285 (1990).

Ensemble

0U ~ U

Low Temperature Phase

Microcanonical

Page 30: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

GENERIC BEHAVIOUR

T. Padmanabhan, Physics Reports, 188, 285 (1990).

Ensemble

0

2K ~ 3PV

HighTemperaturePhase

U ~ U

Low Temperature Phase

Microcanonical

Page 31: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

GENERIC BEHAVIOUR

T. Padmanabhan, Physics Reports, 188, 285 (1990).

Negative SpecificHeat

0

2K + U ~ 0

2K ~ 3PV

HighTemperaturePhase

U ~ U

Low Temperature Phase

MicrocanonicalEnsemble

Page 32: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

GENERIC BEHAVIOUR

T. Padmanabhan, Physics Reports, 188, 285 (1990).

Ensemble

Negative SpecificHeat

0

2K + U ~ 0

2K ~ 3PV

HighTemperaturePhase

U ~ U

Low Temperature Phase

Microcanonical

Canonical EnsemblePhase Transition in the

Page 33: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Mean field description of many-body systems

Page 34: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Mean field description of many-body systems

• A system of N particles interacting through the two-body potential U(x, y). The

entropy S of this system

eS = g(E) =1

N !

d3Nxd3Npδ(E −H) ∝1

N !

d3Nx

[

E −1

2

i,j

U(xi, xj)

]3N2

Page 35: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Mean field description of many-body systems

• A system of N particles interacting through the two-body potential U(x, y). The

entropy S of this system

eS = g(E) =1

N !

d3Nxd3Npδ(E −H) ∝1

N !

d3Nx

[

E −1

2

i,j

U(xi, xj)

]3N2

• Divide spatial volume V be divided into M cells of equal size. Integration over the

particle coordinates (x1, x2, ..., xN)= sum over the number of particles na in the cell

centered at xa (where a = 1, 2, ...,M).

Page 36: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Mean field description of many-body systems

• A system of N particles interacting through the two-body potential U(x, y). The

entropy S of this system

eS = g(E) =1

N !

d3Nxd3Npδ(E −H) ∝1

N !

d3Nx

[

E −1

2

i,j

U(xi, xj)

]3N2

• Divide spatial volume V be divided into M cells of equal size. Integration over the

particle coordinates (x1, x2, ..., xN)= sum over the number of particles na in the cell

centered at xa (where a = 1, 2, ...,M).

• This gives:

eS ≈

∞∑

n1=1

∞∑

n2=1

....

∞∑

nM=1

δ

(

N −∑

a

na

)

expS[{na}]

S[{na}] =3N

2ln

[

E −1

2

M∑

a,b

naU(xa, xb)nb

]

M∑

a=1

na ln

(

naM

eV

)

Page 37: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Mean field description of many-body systems

• A system of N particles interacting through the two-body potential U(x, y). The

entropy S of this system

eS = g(E) =1

N !

d3Nxd3Npδ(E −H) ∝1

N !

d3Nx

[

E −1

2

i,j

U(xi, xj)

]3N2

• Divide spatial volume V be divided into M cells of equal size. Integration over the

particle coordinates (x1, x2, ..., xN)= sum over the number of particles na in the cell

centered at xa (where a = 1, 2, ...,M).

• This gives:

eS ≈

∞∑

n1=1

∞∑

n2=1

....

∞∑

nM=1

δ

(

N −∑

a

na

)

expS[{na}]

S[{na}] =3N

2ln

[

E −1

2

M∑

a,b

naU(xa, xb)nb

]

−M∑

a=1

na ln

(

naM

eV

)

• The mean field approximation: retain in the sum only the term for which the

summand reaches the maximum value∑

{na}

eS[na] ≈ eS[na,max]

Page 38: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Mean field description of self-gravitating systems

Page 39: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Mean field description of self-gravitating systems

• Take the continuum limit with

na,maxM

V= ρ(xa);

M∑

a=1

→M

V

.

gives

ρ(x) = A exp(−βφ(x)); where φ(x) =

d3yU(x, y)ρ(y)

Page 40: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Mean field description of self-gravitating systems

• Take the continuum limit with

na,maxM

V= ρ(xa);

M∑

a=1

→M

V

.

gives

ρ(x) = A exp(−βφ(x)); where φ(x) =

d3yU(x, y)ρ(y)

• In the case of gravitational interaction:

ρ(x) = A exp(−βφ(x)); φ(x) = −G

ρ(y)d3y

|x − y|.

gives the configuration of extremal entropy for a gravitating system

in the mean field limit.

Page 41: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Mean field description of self-gravitating systems

• Take the continuum limit with

na,maxM

V= ρ(xa);

M∑

a=1

→M

V

.

gives

ρ(x) = A exp(−βφ(x)); where φ(x) =

d3yU(x, y)ρ(y)

• In the case of gravitational interaction:

ρ(x) = A exp(−βφ(x)); φ(x) = −G

ρ(y)d3y

|x − y|.

gives the configuration of extremal entropy for a gravitating system

in the mean field limit.

• For gravitational interactions without a short distance cut-off, the

quantity eS is divergent. A short distance cut-off is needed to justify

the entire procedure.

Page 42: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

ANTONOV INSTABILITY

Page 43: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

ANTONOV INSTABILITY

1. Systems with (RE/GM2) < −0.335 cannot evolve into isothermal

spheres. Entropy has no extremum for such systems.

Page 44: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

ANTONOV INSTABILITY

1. Systems with (RE/GM2) < −0.335 cannot evolve into isothermal

spheres. Entropy has no extremum for such systems.

2. Systems with ((RE/GM2) > −0.335) and (ρ(0) > 709 ρ(R)) can exist

in a meta-stable (saddle point state) isothermal sphere

configuration. The entropy extrema exist but they are not local

maxima.

Page 45: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

ANTONOV INSTABILITY

1. Systems with (RE/GM2) < −0.335 cannot evolve into isothermal

spheres. Entropy has no extremum for such systems.

2. Systems with ((RE/GM2) > −0.335) and (ρ(0) > 709 ρ(R)) can exist

in a meta-stable (saddle point state) isothermal sphere

configuration. The entropy extrema exist but they are not local

maxima.

3. Systems with ((RE/GM2) > −0.335) and (ρ(0) < 709 ρ(R)) can form

isothermal spheres which are local maximum of entropy.

Page 46: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

ANTONOV INSTABILITY

1. Systems with (RE/GM2) < −0.335 cannot evolve into isothermal

spheres. Entropy has no extremum for such systems.

2. Systems with ((RE/GM2) > −0.335) and (ρ(0) > 709 ρ(R)) can exist

in a meta-stable (saddle point state) isothermal sphere

configuration. The entropy extrema exist but they are not local

maxima.

3. Systems with ((RE/GM2) > −0.335) and (ρ(0) < 709 ρ(R)) can form

isothermal spheres which are local maximum of entropy.

• Reference:

V.A. Antonov, V.A. : Vest. Leningrad Univ. 7, 135 (1962);

Translation: IAU Symposium 113, 525 (1985).

T.Padmanabhan: Astrophys. Jour. Supp. , 71, 651 (1989).

Page 47: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Isothermal sphere

• Basic equation:

∇2φ = 4πGρce−β[φ(x)−φ(0)]; ρc = ρ(0)

Page 48: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Isothermal sphere

• Basic equation:

∇2φ = 4πGρce−β[φ(x)−φ(0)]; ρc = ρ(0)

• Let

L0 ≡ (4πGρcβ)1/2 , M0 = 4πρcL30, φ0 ≡ β−1 =

GM0

L0

with dimensionless variables:

x ≡r

L0

, n ≡ρ

ρc, m =

M (r)

M0

, y ≡ β [φ− φ (0)] .

Page 49: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Isothermal sphere

• Basic equation:

∇2φ = 4πGρce−β[φ(x)−φ(0)]; ρc = ρ(0)

• Let

L0 ≡ (4πGρcβ)1/2 , M0 = 4πρcL30, φ0 ≡ β−1 =

GM0

L0

with dimensionless variables:

x ≡r

L0

, n ≡ρ

ρc, m =

M (r)

M0

, y ≡ β [φ− φ (0)] .

• Then1

x2

d

dx(x2dy

dx) = e−y; y(0) = y′(0) = 0

Page 50: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Isothermal sphere

• Basic equation:

∇2φ = 4πGρce−β[φ(x)−φ(0)]; ρc = ρ(0)

• Let

L0 ≡ (4πGρcβ)1/2 , M0 = 4πρcL30, φ0 ≡ β−1 =

GM0

L0

with dimensionless variables:

x ≡r

L0

, n ≡ρ

ρc, m =

M (r)

M0

, y ≡ β [φ− φ (0)] .

• Then1

x2

d

dx(x2dy

dx) = e−y; y(0) = y′(0) = 0

• Singular solution:

n =(

2/x2)

,m = 2x, y = 2 lnx

Page 51: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

LANE-EMDEN VARIABLES

• Invariant under the transformation y → y + a ; x→ kx with k2 = ea.

Page 52: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

LANE-EMDEN VARIABLES

• Invariant under the transformation y → y + a ; x→ kx with k2 = ea.

• Reduce the degree by choosing:

v ≡m

x; u ≡

nx3

m=nx2

v.

Page 53: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

LANE-EMDEN VARIABLES

• Invariant under the transformation y → y + a ; x→ kx with k2 = ea.

• Reduce the degree by choosing:

v ≡m

x; u ≡

nx3

m=nx2

v.

u

v

dv

du= −

(u− 1)

(u+ v − 3); v(u = 3) = 0; v′(u = 3) = −

5

3

Page 54: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

LANE-EMDEN VARIABLES

• Invariant under the transformation y → y + a ; x→ kx with k2 = ea.

• Reduce the degree by choosing:

v ≡m

x; u ≡

nx3

m=nx2

v.

u

v

dv

du= −

(u− 1)

(u+ v − 3); v(u = 3) = 0; v′(u = 3) = −

5

3

• The singular point is at: us = 1, vs = 2; corresponding to the

solution n = (2/x2),m = 2x.

Page 55: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

LANE-EMDEN VARIABLES

• Invariant under the transformation y → y + a ; x→ kx with k2 = ea.

• Reduce the degree by choosing:

v ≡m

x; u ≡

nx3

m=nx2

v.

u

v

dv

du= −

(u− 1)

(u+ v − 3); v(u = 3) = 0; v′(u = 3) = −

5

3

• The singular point is at: us = 1, vs = 2; corresponding to the

solution n = (2/x2),m = 2x.

• All solutions tend to this asymptotically for large r by spiralling

around the singular point in the u− v plane.

Page 56: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

LANE-EMDEN VARIABLES

• Invariant under the transformation y → y + a ; x→ kx with k2 = ea.

• Reduce the degree by choosing:

v ≡m

x; u ≡

nx3

m=nx2

v.

u

v

dv

du= −

(u− 1)

(u+ v − 3); v(u = 3) = 0; v′(u = 3) = −

5

3

• The singular point is at: us = 1, vs = 2; corresponding to the

solution n = (2/x2),m = 2x.

• All solutions tend to this asymptotically for large r by spiralling

around the singular point in the u− v plane.

• Finite total mass for the system requires a large distance cut-off at

some r = R.

Page 57: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Chandra (1939) Introduction to the study of stellar structure

Page 58: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 59: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 60: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 61: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 62: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

[D.Lynden-Bell, R. Wood, (1968), MNRAS, 138, p.495.]

Page 63: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Chandra’s comments on Emden’s work

Page 64: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

ENERGY OF THE ISOTHERMAL SPHERE

• The potential and kinetic energies are

U = −

∫ R

0

GM(r)

r

dM

drdr = −

GM20

L0

∫ x0

0

mnxdx

K =3

2

M

β=

3

2

GM20

L0

m(x0) =GM2

0

L0

3

2

∫ x0

0

nx2dx; x0 = R/L0

Page 65: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

ENERGY OF THE ISOTHERMAL SPHERE

• The potential and kinetic energies are

U = −

∫ R

0

GM(r)

r

dM

drdr = −

GM20

L0

∫ x0

0

mnxdx

K =3

2

M

β=

3

2

GM20

L0

m(x0) =GM2

0

L0

3

2

∫ x0

0

nx2dx; x0 = R/L0

• So:

E = K + U =GM2

0

2L0

∫ x0

0

dx(3nx2 − 2mnx)

=GM2

0

2L0

∫ x0

0

dxd

dx{2nx3 − 3m} =

GM20

L0

{n0x30 −

3

2m0}

Page 66: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

ENERGY OF THE ISOTHERMAL SPHERE

• The potential and kinetic energies are

U = −

∫ R

0

GM(r)

r

dM

drdr = −

GM20

L0

∫ x0

0

mnxdx

K =3

2

M

β=

3

2

GM20

L0

m(x0) =GM2

0

L0

3

2

∫ x0

0

nx2dx; x0 = R/L0

• So:

E = K + U =GM2

0

2L0

∫ x0

0

dx(3nx2 − 2mnx)

=GM2

0

2L0

∫ x0

0

dxd

dx{2nx3 − 3m} =

GM20

L0

{n0x30 −

3

2m0}

• The combination (RE/GM2) is a function of (u, v) alone.

λ =RE

GM2=

1

v0

{u0 −3

2}.

Page 67: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

ENERGY OF THE ISOTHERMAL SPHERE

• The potential and kinetic energies are

U = −

∫ R

0

GM(r)

r

dM

drdr = −

GM20

L0

∫ x0

0

mnxdx

K =3

2

M

β=

3

2

GM20

L0

m(x0) =GM2

0

L0

3

2

∫ x0

0

nx2dx; x0 = R/L0

• So:

E = K + U =GM2

0

2L0

∫ x0

0

dx(3nx2 − 2mnx)

=GM2

0

2L0

∫ x0

0

dxd

dx{2nx3 − 3m} =

GM20

L0

{n0x30 −

3

2m0}

• The combination (RE/GM2) is a function of (u, v) alone.

λ =RE

GM2=

1

v0

{u0 −3

2}.

• An isothermal sphere must lie on the curve

v =1

λ

(

u−3

2

)

; λ ≡RE

GM2

Page 68: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

[T. Padmanabhan, Physics Reports, 188, 285 (1990).]

Page 69: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

COLLISIONAL RELAXATION IN GRAVITATING SYSTEMS

Page 70: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

COLLISIONAL RELAXATION IN GRAVITATING SYSTEMS

• Transverse velocity in an encounter:

δv⊥ ≃(

Gm/b2)

(2b/v) = (2Gm/bv)

Page 71: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

COLLISIONAL RELAXATION IN GRAVITATING SYSTEMS

• Transverse velocity in an encounter:

δv⊥ ≃(

Gm/b2)

(2b/v) = (2Gm/bv)

• ”Hard” collisions: ∆v⊥ ≈ v; so b ≤ bc = Gm/v2. The relevant relaxation timescale:

thard ≃1

(nσv)≃

R3v3

N (G2m2)≃NR3v3

G2M2≈ N(R/v)

Page 72: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

COLLISIONAL RELAXATION IN GRAVITATING SYSTEMS

• Transverse velocity in an encounter:

δv⊥ ≃(

Gm/b2)

(2b/v) = (2Gm/bv)

• ”Hard” collisions: ∆v⊥ ≈ v; so b ≤ bc = Gm/v2. The relevant relaxation timescale:

thard ≃1

(nσv)≃

R3v3

N (G2m2)≃NR3v3

G2M2≈ N(R/v)

• More subtle is the effect of ”soft” collisions which is diffusion in the velocity

space in which the (∆v⊥)2 add up linearly with time.

Page 73: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

COLLISIONAL RELAXATION IN GRAVITATING SYSTEMS

• Transverse velocity in an encounter:

δv⊥ ≃(

Gm/b2)

(2b/v) = (2Gm/bv)

• ”Hard” collisions: ∆v⊥ ≈ v; so b ≤ bc = Gm/v2. The relevant relaxation timescale:

thard ≃1

(nσv)≃

R3v3

N (G2m2)≃NR3v3

G2M2≈ N(R/v)

• More subtle is the effect of ”soft” collisions which is diffusion in the velocity

space in which the (∆v⊥)2 add up linearly with time.

〈(δv⊥)2〉total ≃ ∆t

∫ b2

b1

(2πbdb) (vn)

(

G2m2

b2v2

)

=2πnG2m2

v∆t ln

(

b2

b1

)

.

Page 74: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

COLLISIONAL RELAXATION IN GRAVITATING SYSTEMS

• Transverse velocity in an encounter:

δv⊥ ≃(

Gm/b2)

(2b/v) = (2Gm/bv)

• ”Hard” collisions: ∆v⊥ ≈ v; so b ≤ bc = Gm/v2. The relevant relaxation timescale:

thard ≃1

(nσv)≃

R3v3

N (G2m2)≃NR3v3

G2M2≈ N(R/v)

• More subtle is the effect of ”soft” collisions which is diffusion in the velocity

space in which the (∆v⊥)2 add up linearly with time.

〈(δv⊥)2〉total ≃ ∆t

∫ b2

b1

(2πbdb) (vn)

(

G2m2

b2v2

)

=2πnG2m2

v∆t ln

(

b2

b1

)

.

• Take b2 = R= size of the system, b1 = bc. Then

(b2/b1) ≃(

Rv2/Gm)

= N(

Rv2/GM)

≃ N

in virial equilibrium. So

tsoft ≃v3

2πG2m2n lnN≃

(

N

lnN

)(

R

v

)

(

thard

lnN

)

Page 75: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Publication date: 1942

Page 76: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Pages 48 to 73 gives the derivation of TE and TD!

Page 77: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 78: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 79: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 80: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Pages 317 to 320 contain the derivation by Jeans!

Page 81: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 82: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 83: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

First appearance of lnN

Page 84: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 85: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

CHANDRA’S COMMENT ON THE WORK OF JEANS

Page 86: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

SECOND ASPECT OF DIFFUSION IN VELOCITY SPACE

Page 87: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

SECOND ASPECT OF DIFFUSION IN VELOCITY SPACE

• This can’t be the whole story!

Page 88: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

SECOND ASPECT OF DIFFUSION IN VELOCITY SPACE

• This can’t be the whole story!

• We need a dynamical friction to reach steady state with

Maxwellian distribution of velocities.

Page 89: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

SECOND ASPECT OF DIFFUSION IN VELOCITY SPACE

• This can’t be the whole story!

• We need a dynamical friction to reach steady state with

Maxwellian distribution of velocities.

• Chandra seems to have realized this soon after the

publication of the book!!

Page 90: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 91: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 92: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 93: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

DIFFUSION IN VELOCITY SPACE:

A UNIFIED APPROACH

Page 94: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

DIFFUSION IN VELOCITY SPACE:

A UNIFIED APPROACH

• Diffusion current as the source term:

df

dt=∂f

∂t+ v.

∂f

∂x−∇φ.

∂f

∂v= −

∂Jα

∂pα

Page 95: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

DIFFUSION IN VELOCITY SPACE:

A UNIFIED APPROACH

• Diffusion current as the source term:

df

dt=∂f

∂t+ v.

∂f

∂x−∇φ.

∂f

∂v= −

∂Jα

∂pα

• Form of the current can be shown to be:

Jα =B0

2

d l′{

f∂f ′

∂lβ− f ′∂f

∂lβ

}

.

{

δαβ

k−kαkβ

k3

}

where B0 = 4πG2m5L; and L =b2∫

b1

dbb

= ln(

b2b1

)

Page 96: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

TWO FOR THE PRICE OF ONE!

• Current:

Jα =B0

2

d l′{

f∂f ′

∂lβ− f ′ ∂f

∂lβ

}

.

{

δαβ

k−kαkβ

k3

}

Page 97: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

TWO FOR THE PRICE OF ONE!

• Current:

Jα =B0

2

d l′{

f∂f ′

∂lβ− f ′ ∂f

∂lβ

}

.

{

δαβ

k−kαkβ

k3

}

• The term proportional to f gives dynamical friction.

The term proportional to (∂f/∂lβ) increases the velocity

dispersion.

Page 98: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

TWO FOR THE PRICE OF ONE!

• Current:

Jα =B0

2

d l′{

f∂f ′

∂lβ− f ′ ∂f

∂lβ

}

.

{

δαβ

k−kαkβ

k3

}

• The term proportional to f gives dynamical friction.

The term proportional to (∂f/∂lβ) increases the velocity

dispersion.

• The current Jα vanishes for Maxwell distribution, as it

should!

Page 99: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

AN ILLUSTRATIVE TOY MODEL

Page 100: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

AN ILLUSTRATIVE TOY MODEL

• Note that

Jα(l) ≡ aα(l)f(l) −1

2

∂lβ

{

σ2αβf}

where aα = (∂η/∂lα) , σ2αβ = (∂2ψ/∂lα∂lβ)

Page 101: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

AN ILLUSTRATIVE TOY MODEL

• Note that

Jα(l) ≡ aα(l)f(l) −1

2

∂lβ

{

σ2αβf}

where aα = (∂η/∂lα) , σ2αβ = (∂2ψ/∂lα∂lβ)

• Aside:

∇2ψ = η; ∇2l η(l) = ∇2

l

{

2

dl′f(l′)

|l − l′|

}

= −8πf(l)

Page 102: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

AN ILLUSTRATIVE TOY MODEL

• Note that

Jα(l) ≡ aα(l)f(l) −1

2

∂lβ

{

σ2αβf}

where aα = (∂η/∂lα) , σ2αβ = (∂2ψ/∂lα∂lβ)

• Aside:

∇2ψ = η; ∇2l η(l) = ∇2

l

{

2

dl′f(l′)

|l − l′|

}

= −8πf(l)

• Treat the coefficients as constants to understand the structure of

the equation:

∂f(v, t)

∂t=

∂v

{

(αv)f +σ2

2

∂f

∂v

}

≡ −∂J

∂v

Page 103: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

AN ILLUSTRATIVE TOY MODEL

• Note that

Jα(l) ≡ aα(l)f(l) −1

2

∂lβ

{

σ2αβf}

where aα = (∂η/∂lα) , σ2αβ = (∂2ψ/∂lα∂lβ)

• Aside:

∇2ψ = η; ∇2l η(l) = ∇2

l

{

2

dl′f(l′)|l − l′|

}

= −8πf(l)

• Treat the coefficients as constants to understand the structure of

the equation:

∂f(v, t)

∂t=

∂v

{

(αv)f +σ2

2

∂f

∂v

}

≡ −∂J

∂v

• An initial distribution f(v, 0) = δD(v − v0) evolves to:

f(v, t) =

[

α

πσ2(1 − e−2αt)

]1/2

exp

[

−α(v − v0e−αt)2

σ2(1 − e−2αt)

]

Page 104: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

• The mean velocity decays to zero:

< v >= v0e−αt

Page 105: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

• The mean velocity decays to zero:

< v >= v0e−αt

• The distribution tends to Maxwellian limit with velocity dispersion

< v2 > − < v >2=σ2

α(1 − e−2αt) →

σ2

α

Page 106: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

• The mean velocity decays to zero:

< v >= v0e−αt

• The distribution tends to Maxwellian limit with velocity dispersion

< v2 > − < v >2=σ2

α(1 − e−2αt) →

σ2

α

• The interplay between the two effects is obvious.

Page 107: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

HISTORY: OVERLOOKING LANDAU (1936)!

Page 108: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

HISTORY: OVERLOOKING LANDAU (1936)!

Footnote is incorrect; Landau’s expression has both dynamical friction and velocity

dispersion!

Page 109: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 110: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 111: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

GRAVITATIONAL CLUSTERING IN EXPANDING UNIVERSE

– SOME KEY ISSUES –

Page 112: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

GRAVITATIONAL CLUSTERING IN EXPANDING UNIVERSE

– SOME KEY ISSUES –

• If the initial power spectrum is sharply peaked in a narrow band of

wavelengths, how does the evolution transfer the power to other

scales?

Page 113: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

GRAVITATIONAL CLUSTERING IN EXPANDING UNIVERSE

– SOME KEY ISSUES –

• If the initial power spectrum is sharply peaked in a narrow band of

wavelengths, how does the evolution transfer the power to other

scales?

• What is the asymptotic nature of evolution for the self gravitating

system in an expanding background?

Page 114: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

GRAVITATIONAL CLUSTERING IN EXPANDING UNIVERSE

– SOME KEY ISSUES –

• If the initial power spectrum is sharply peaked in a narrow band of

wavelengths, how does the evolution transfer the power to other

scales?

• What is the asymptotic nature of evolution for the self gravitating

system in an expanding background?

• Does the gravitational clustering at late stages wipe out the

memory of initial conditions ?

Page 115: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

GRAVITATIONAL CLUSTERING IN EXPANDING UNIVERSE

– SOME KEY ISSUES –

• If the initial power spectrum is sharply peaked in a narrow band of

wavelengths, how does the evolution transfer the power to other

scales?

• What is the asymptotic nature of evolution for the self gravitating

system in an expanding background?

• Does the gravitational clustering at late stages wipe out the

memory of initial conditions ?

• Do the virialized structures formed in an expanding universe due to

gravitational clustering have any invariant properties? Can their

structure be understood from first principles?

Page 116: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

GRAVITATIONAL CLUSTERING IN EXPANDING UNIVERSE

– SOME KEY ISSUES –

• If the initial power spectrum is sharply peaked in a narrow band of

wavelengths, how does the evolution transfer the power to other

scales?

• What is the asymptotic nature of evolution for the self gravitating

system in an expanding background?

• Does the gravitational clustering at late stages wipe out the

memory of initial conditions ?

• Do the virialized structures formed in an expanding universe due to

gravitational clustering have any invariant properties? Can their

structure be understood from first principles?

• How can one connect up the local behaviour of gravitating systems

to the evolution of clustering in the universe?

Page 117: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

BASIC DEFINITIONS

• Density:

ρ(x, t) =m

a3(t)

i

δD[x − xi(t)]

• Mean density:

ρb(t) ≡

d3x

Vρ(x, t) =

m

a3(t)

(

N

V

)

=M

a3V=ρ0

a3

• Density contrast:

1 + δ(x, t) ≡ρ(x, t)

ρb=V

N

i

δD[x − xi(t)] =

dqδD[x − xT (t, q)].

• Density contrast in Fourier space:

δk(t) ≡

d3xe−ik·xδ(x, t) =

d3q exp[−ik.xT (t, q)] − (2π)3δD(k)

Page 118: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

THE EXACT (BUT USELESS) DESCRIPTION

• Density contrast in Fourier space satisfies:

δk + 2a

aδk = 4πGρbδk + Ak −Bk

with

Ak = 4πGρb

d3k′

(2π)3δk′δk−k′

[

k.k′

k′2

]

Bk =

d3q (k.xT )2 exp [−ik.xT (t, q)]

Page 119: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

THE EXACT (BUT USELESS) DESCRIPTION

• Density contrast in Fourier space satisfies:

δk + 2a

aδk = 4πGρbδk + Ak −Bk

with

Ak = 4πGρb

d3k′

(2π)3δk′δk−k′

[

k.k′

k′2

]

Bk =

d3q (k.xT )2 exp [−ik.xT (t, q)]

• Coupled exact equations:

φk + 4a

aφk = −

1

2a2

d3p

(2π)3φ 1

2k+pφ 1

2k−p

[

(

k

2

)2

+ p2 − 2

(

k.p

k

)2]

+

(

3H20

2

)∫

d3q

a

(

k.x

k

)2

eik.x

x + 2a

ax = −

1

a2∇xφ = −

1

a2

ikφk exp i(k · x);

Page 120: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

“Renormalizability” of gravity

Page 121: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

“Renormalizability” of gravity

• One can then show that: The term (Ak −Bk) receives contribution

only from particles which are not bound to any of the clusters to

the order O(k2R2). (Peebles, 1980)

Page 122: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

“Renormalizability” of gravity

• One can then show that: The term (Ak −Bk) receives contribution

only from particles which are not bound to any of the clusters to

the order O(k2R2). (Peebles, 1980)

• Allows one to ignore contributions from virialised systems and treat

the rest in Zeldovich (-like) approximation. Then one gets:

H20

(

ad2

da2+

7

2

d

da

)

φk = −2

3

d3p(2π)3

φL12

k+pφL1

2k−p

[

(

k

2

)2

(

k.pk

)2]

−1

2

∫ ′ d3p

(2π)3φ1

2k+pφ1

2k−p

[

(

k

2

)2

+ p2 − 2

(

k.p

k

)2]

(T.P, 2002)

Page 123: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Evolution at large scales

Page 124: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Evolution at large scales

• Ignore the terms Ak and Bk. Then:

δk + 2a

aδk = 4πGρbδk

Page 125: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Evolution at large scales

• Ignore the terms Ak and Bk. Then:

δk + 2a

aδk = 4πGρbδk

• For a ∝ t2/3, ρb ∝ a−3, the growing solution is:

δk ∝ a; P (k) = |δk|2 ∝ a2; ξ(a, x) ∝ a2

Page 126: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Evolution at large scales

• Ignore the terms Ak and Bk. Then:

δk + 2a

aδk = 4πGρbδk

• For a ∝ t2/3, ρb ∝ a−3, the growing solution is:

δk ∝ a; P (k) = |δk|2 ∝ a2; ξ(a, x) ∝ a2

• BUT: If δk → 0 for certain range of k at t = t0 (but is

nonzero elsewhere) then (Ak −Bk) ≫ 4πGρbδk and the

growth of perturbations around k will be entirely

determined by nonlinear effects.

Page 127: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Evolution at large scales

• Ignore the terms Ak and Bk. Then:

δk + 2a

aδk = 4πGρbδk

• For a ∝ t2/3, ρb ∝ a−3, the growing solution is:

δk ∝ a; P (k) = |δk|2 ∝ a2; ξ(a, x) ∝ a2

• BUT: If δk → 0 for certain range of k at t = t0 (but is

nonzero elsewhere) then (Ak −Bk) ≫ 4πGρbδk and the

growth of perturbations around k will be entirely

determined by nonlinear effects.

• There is inverse cascade of power in gravitational

clustering! (Zeldovich, 1965)

Page 128: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Bagla, T.P, (1997) MNRAS, 286, 1023

Page 129: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

k3P(k)2a

Lk−1

Page 130: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

k3P(k)2a aP k

4 4

Lk−1

Page 131: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

LINEAR REGIME

QUASI−LINEAR REGIME

Prediction from stable clustering

NON−LINEAR REGIME

Bagla, Engineer, TP (1998), Ap.J.,495, 25

Page 132: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

‘EQUIPARTITION’ OF ENERGY FLOW

Page 133: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

‘EQUIPARTITION’ OF ENERGY FLOW

• If the local power law index is n, then one can show that in the

linear regime:

EL(a, x) ≈ ax−(n+2)

Page 134: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

‘EQUIPARTITION’ OF ENERGY FLOW

• If the local power law index is n, then one can show that in the

linear regime:

EL(a, x) ≈ ax−(n+2)

• In the quasilinear regime:

EQL(a, x) ≈ a2−n

n+4x−2n+5

n+4 ;

Page 135: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

‘EQUIPARTITION’ OF ENERGY FLOW

• If the local power law index is n, then one can show that in the

linear regime:

EL(a, x) ≈ ax−(n+2)

• In the quasilinear regime:

EQL(a, x) ≈ a2−n

n+4x−2n+5

n+4 ;

• In the nonlinear regime:

ENL(a, x) ≈ a1−n

n+5x−2n+4

n+5 ;

Page 136: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

‘EQUIPARTITION’ OF ENERGY FLOW

• If the local power law index is n, then one can show that in the

linear regime:

EL(a, x) ≈ ax−(n+2)

• In the quasilinear regime:

EQL(a, x) ≈ a2−n

n+4x−2n+5

n+4 ;

• In the nonlinear regime:

ENL(a, x) ≈ a1−n

n+5x−2n+4

n+5 ;

• NEW FEATURE: The energy flow is form invariant

(“equipartition”) when n = −1 in QL and n = −2 in the NL regimes!

Then E ∝ a in all three regimes.

Page 137: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

k3P(k)2a aP k

4 4

Lk−1

Page 138: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

k3P(k)2a

aP k−12

aP k4 4

Lk−1

Page 139: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

aP k−12

aP k−22

k3

P(k)

2a

k−1

aP 2

f(k)

Page 140: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Injected initial power spectrum

P(k) ~ k −1

Bagla, T.P, (1997) MNRAS, 286, 1023

Page 141: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Late time power spectra for 3 differentinitial injected spectra

P(k) ~ k −1

Bagla, T.P, (1997) MNRAS, 286, 1023

Page 142: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Asymptotic universality in nonlinear clustering

(T.P., S. Ray, 2006)

Page 143: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪
Page 144: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Summary

Page 145: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Summary

• Chandra pioneered the use of statistical physics in the

study of gravitating systems.

Page 146: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Summary

• Chandra pioneered the use of statistical physics in the

study of gravitating systems.

• His approach to this subject shows the characteristic

rigour employed as a matter of policy rather than out of

necessity.

Page 147: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Summary

• Chandra pioneered the use of statistical physics in the

study of gravitating systems.

• His approach to this subject shows the characteristic

rigour employed as a matter of policy rather than out of

necessity.

• The subject is alive and well and still has several open

questions especially in the context of cosmology.

Page 148: T. Padmanabhan (IUCAA, Pune, INDIA) · FINITE GRAVITATING SYSTEMS – GENERAL DESCRIPTION – • Typical systems have two natural energy scales: E 1 = (−Gm2/a) and E 2 = (−Gm2/R);a≪

Acknowledgements

• D. Lynden-Bell (IOA)

• D. Narasimha (TIFR)

• R. Nityananda (NCRA)

• S. Sridhar (RRI)

• K. Subramanian (IUCAA)