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Chapter 3: Central Forces

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Chapter 3: Central Forces. Introduction Interested in the “2 body” problem! Start out generally, but eventually restrict to motion of 2 bodies interacting through a central force . Central Force  Force between 2 bodies which is directed along the line between them. - PowerPoint PPT Presentation
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Page 1: Chapter 3: Central Forces
Page 2: Chapter 3: Central Forces

Chapter 3: Central ForcesIntroduction

• Interested in the “2 body” problem!Start out generally, but eventually restrict to motion

of 2 bodies interacting through a central force.

• Central Force Force between 2 bodies which is directed along the line between them.

• Important physical problem! Solvable exactly! – Planetary motion & Kepler’s Laws.

– Nuclear forces

– Atomic physics (H atom). Needs quantum version!

Page 3: Chapter 3: Central Forces

Sect. 3.1: Reduction to Equivalent 1-Body Problem

• My treatment differs slightly from text’s. Same results, of course!

• General 3d, 2 body problem. 2 masses m1 & m2: Need 6 coordinates: For example, components of 2 position vectors r1 & r2 (arbitrary origin).

• Assume only forces are due to an interaction potential U. At first, U = any function of the vector between 2 particles, r = r1 - r2, of their relative velocity r = r1 - r2, & possibly of higher derivatives of r = r1 - r2: U = U(r,r,..)– Very soon, will restrict to central forces!

Page 4: Chapter 3: Central Forces

Lagrangian: L = (½)m1|r1|2 + (½)m2|r2|2 - U(r,r, ..)

• Instead of 6 components of 2 vectors r1 & r2, usually transform to (6

components of) Center of Mass (CM) & Relative Coordinates.

• Center of Mass Coordinate: (M (m1+m2))

R (m1r1 +m2r2)(M)

• Relative Coordinate:

r r1 - r2

• Define: Reduced Mass: μ (m1m2)(m1+m2)

Useful relation: μ-1 (m1)-1 + (m2)-1

• Algebra Inverse coordinate relations:

r1 = R + (μ/m1)r; r2 = R - (μ/m2)r

Page 5: Chapter 3: Central Forces

Lagrangian: L = (½)m1|r1|2 + (½)m2|r2|2 - U(r,r, ..) (1)

• Velocities related by

r1 = R + (μ /m1)r; r2 = R - (μ /m2)r (2)

• Combining (1) & (2) + algebra gives Lagrangian in terms of R,r,r: L = (½)M|R|2 + (½)μ|r|2 - U

Or: L = LCM + Lrel . Where: LCM (½)M|R|2

Lrel (½) μ |r|2 - U

Motion separates into 2 parts: 1. CM motion, governed by LCM (½)M|R|2

2. Relative motion, governed by

Lrel (½)μ|r|2 - U(r,r,..)

Page 6: Chapter 3: Central Forces

CM & Relative Motion• Lagrangian for 2 body problem: L = LCM + Lrel

LCM (½)M|R|2 ; Lrel (½)μ|r|2 - U(r,r,..)

Motion separates into 2 parts:

1. Lagrange’s Eqtns for 3 components of CM coordinate

vector R clearly gives eqtns of motion independent of r.

2. Lagrange Eqtns for 3 components of relative

coordinate vector r clearly gives eqtns of motion

independent of R.• By transforming from (r1, r2) to (R,r):

The 2 body problem has been separated into 2 one body problems!

Page 7: Chapter 3: Central Forces

• Lagrangian for 2 body problem

L = LCM + Lrel

Have transformed the 2 body problem

into 2 one body problems!1. Motion of the CM, governed by

LCM (½)M|R|2

2. Relative Motion, governed by

Lrel (½)μ|r|2 - U(r,r,..)

Page 8: Chapter 3: Central Forces

• Motion of CM is governed by LCM (½)M|R|2 – Assuming no external forces.

• R = (X,Y,Z) 3 Lagrange Eqtns; each like:

(d/dt)(∂[LCM]/∂X) - (∂[LCM]/∂X) = 0

(∂[LCM]/∂X) = 0 (d/dt)(∂[LCM]/∂X) = 0

X = 0, CM acts like a free particle!

• Solution: X = Vx0 = constant

– Determined by initial conditions!

X(t) = X0 + Vx0t , exactly like a free particle!

• Same eqtns for Y, Z:

R(t) = R0 + V0t , exactly like a free particle!

CM Motion is identical to trivial motion of a free particle. Uniform translation of CM. Trivial & uninteresting!

Page 9: Chapter 3: Central Forces

• 2 body Lagrangian: L = LCM + Lrel

2 body problem is transformed to 2 one body problems!

1. Motion of the CM, governed by LCM (½)M|R|2

Trivial free particle-like motion!

2. Relative Motion, governed by

Lrel (½)μ|r|2 - U(r,r,..)

2 body problem is transformed to 2 one body problems, one of which is trivial!

All interesting physics is in relative motion part!

Focus on it exclusively!

Page 10: Chapter 3: Central Forces

Relative Motion

• Relative Motion is governed by

Lrel (½)μ|r|2 - U(r,r,..)

– Assuming no external forces.

– Henceforth: Lrel L (Drop subscript)

– For convenience, take origin of coordinates at CM: R = 0

r1 = (μ/m1)r; r2 = - (μ/m2)r

μ (m1m2)(m1+m2)

(μ)-1 (m1)-1 +(m2)-1

Page 11: Chapter 3: Central Forces

• The 2 body, central force problem has been formally reduced to an

EQUIVALENT ONE BODY PROBLEM

in which the motion of a “particle” of mass μ in U(r,r,..) is what is to be determined!

– Superimpose the uniform, free particle-like translation of CM onto the relative motion solution!

– If desired, if get r(t), can get r1(t) & r2(t) from above. Usually, the relative motion (orbits) only is wanted & we stop at r(t).

Page 12: Chapter 3: Central Forces

Sect. 3.2: Eqtns of Motion & 1st Integrals

• System: “Particle” of mass μ (μ m in what follows) moving in a force field described by potential U(r,r,..).

• Now, restrict to conservative Central Forces:

U V where V = V(r)

– Note: V(r) depends only on r = |r1 - r2| = distance of particle from force center. No orientation dependence. System has spherical symmetry

Rotation about any fixed axis can’t affect eqtns of motion.

Expect the angle representing such a rotation to be cyclic & the corresponding generalized momentum (angular momentum) to be conserved.

Page 13: Chapter 3: Central Forces

Angular Momentum• By the discussion in Ch. 2: Spherical symmetry

The Angular Momentum of the system is conserved:

L = r p = constant (magnitude & direction!)

Angular momentum conservation!

r & p (& thus the particle motion!) always lie in a plane L,

which is fixed in space.

Figure:(See text discussion for L = 0)

The problem is effectively

reduced from 3d to 2d

(particle motion in a plane)!

Page 14: Chapter 3: Central Forces

Motion in a Plane• Describe 3d motion in spherical coordinates (Goldstein

notation!): (r,θ,). θ = angle in the plane (plane polar

coordinates). = azimuthal angle. • L is fixed, as we saw. The motion is in a plane. Effectively

reducing the 3d problem to a 2d one!

• Choose the polar (z) axis along L.

= (½)π & drops out of the problem. • Conservation of angular momentum L

3 independent constants of the motion(1st integrals of the motion): Effectively we’ve used 2 of these to limit the motion to a plane. The third (|L| = constant) will be used to complete the solution to the problem.

Page 15: Chapter 3: Central Forces

Summary So Far

• Started with 6d, 2 body problem. Reduced it to 2, 3d 1 body problems, one (CM motion) of which is trivial. Angular momentum conservation reduces 2nd 3d problem (relative motion) from 3d to 2d (motion in a plane)!

• Lagrangian (μ m , conservative, central forces):

L = (½)m|r|2 - V(r)

• Motion in a plane

Choose plane polar coordinates to do the problem:

L = (½)m(r2 + r2θ2) - V(r)

Page 16: Chapter 3: Central Forces

L = (½)m(r2 + r2θ2) - V(r)

• The Lagrangian is cyclic in θ

The generalized momentum pθ is conserved:

p (∂L/∂θ) = mr2 θ

Lagrange’s Eqtn: (d/dt)[(∂L/∂θ)] - (∂L/∂θ) = 0

pθ = 0, pθ = constant = mr2θ

• Physics: pθ = mr2θ = angular momentum about an axis the plane of motion. Conservation of angular momentum, as we already said!

• The problem symmetry has allowed us to integrate one eqtn of motion. pθ a “1st Integral” of motion.

Convenient to define: pθ mr2θ = constant.

Page 17: Chapter 3: Central Forces

L = (½)m(r2 + r2θ2) - V(r)

• In terms of mr2θ = constant, the Lagrangian is:

L = (½)mr2 + [2(2mr2)] - V(r) • Symmetry & the resulting conservation of angular

momentum has reduced the effective 2d problem (2

degrees of freedom) to an effective 1d problem!

1 degree of freedom, one generalized coordinate r!

• Now: Set up & solve the problem using the above Lagrangian. Also, follow authors & do with energy conservation. However, first, a side issue.

Page 18: Chapter 3: Central Forces

Kepler’s 2nd Law • Const. angular momentum mr2θ • Note that could be < 0 or > 0. • Geometric interpretation: = const: See figure:

• In describing the path r(t), in time dt, the radius vector sweeps out an area: dA = (½)r2dθ

Page 19: Chapter 3: Central Forces

• In dt, radius vector sweeps out area dA = (½)r2dθ– Define Areal Velocity (dA/dt)

(dA/dt) = (½)r2(dθ/dt) = dA = (½)r2θ (1)But mr2 θ = constant

θ = (/mr2) (2)• Combine (1) & (2):

(dA/dt) = (½)(/m) = constant! Areal velocity is constant in time!

the Radius vector from the origin sweeps out equal areas in equal times Kepler’s 2nd Law

• First derived by empirically by Kepler for planetary motion. General result for central forces! Not limited to the gravitational force law (r-2).

Page 20: Chapter 3: Central Forces

Lagrange’s Eqtn for r • In terms of mr2θ = const, the Lagrangian is:

L = (½)mr2 + [2(2mr2)] - V(r)

• Lagrange’s Eqtn for r:

(d/dt)[(∂L/∂r)] - (∂L/∂r) = 0

mr -[2(mr3)] = - (∂V/∂r) f(r)

(f(r) force along r)

Rather than solve this directly, its easier to use Energy Conservation. Come back to this later.

Page 21: Chapter 3: Central Forces

Energy • Note: Linear momentum is conserved also:

– Linear momentum of CM.

Uninteresting free particle motion

• Total mechanical energy is also conserved since the central force is conservative:

E = T + V = constant

E = (½)m(r2 + r2θ2) + V(r) • Recall, angular momentum is:

mr2θ = const

θ = [(mr2)]

E = (½)mr2 + (½)[2(mr2)] + V(r) =const

Another “1st integral” of the motion

Page 22: Chapter 3: Central Forces

r(t) & θ(t) E = (½)mr2 + [2(2mr2)] + V(r) = const

• Energy Conservation allows us to get solutions to the eqtns of motion in terms of r(t) & θ(t) and r(θ) or θ(r) The orbit of the particle!– Eqtn of motion to get r(t): One degree of freedom

Very similar to a 1 d problem!

• Solve for r = (dr/dt) :

r = ({2/m}[E - V(r)] - [2(m2r2)])½

– Note: This gives r(r), the phase diagram for the relative coordinate & velocity. Can qualitatively analyze (r part of) motion using it, just as in 1d.

• Solve for dt & formally integrate to get t(r). In principle, invert to get r(t).

Page 23: Chapter 3: Central Forces

r = ({2/m}[E - V(r)] - [2(m2r2)])½

• Solve for dt & formally integrate to get t(r):

t(r) = ∫dr({2/m}[E - V(r)] - [2(m2r2)])-½

– Limits r0 r, r0 determined by initial condition

– Note the square root in denominator!

• Get θ(t) in terms of r(t) using conservation of angular momentum again: mr2θ = const

(dθ/dt) = [(mr2)]

θ(t) = (/m)∫(dt[r(t)]-2) + θ0

– Limits 0 t

θ0 determined by initial condition

Page 24: Chapter 3: Central Forces

• Formally, the 2 body Central Force problem has been reduced to the evaluation of 2 integrals:

(Given V(r) can do them, in principle.)

t(r) = ∫dr({2/m}[E - V(r)] - [2(m2r2)])-½

– Limits r0 r, r0 determined by initial condition

θ(t) = (/m)∫(dt[r(t)]-2) + θ0

– Limits 0 t, θ0 determined by initial condition

• To solve the problem, need 4 integration constants:

E, , r0 , θ0

Page 25: Chapter 3: Central Forces

Orbits • Often, we are much more interested in the path in the r, θ

plane: r(θ) or θ(r) The orbit. • Note that (chain rule):

(dθ/dr) = (dθ/dt)(dt/dr) = (dθ/dt)(dr/dt)

Or: (dθ/dr) = (θ/r)

Also, mr2θ = const θ = [/(mr2)]

Use r = ({2/m}[E - V(r)] - [2(m2r2)])½

(dθ/dr) = [/(mr2)]({2/m}[E - V(r)] - [2(m2r2)])-½

Or:

(dθ/dr) = (/r2)(2m)-½[E - V(r) -{2(2mr2)}]-½

• Integrating this will give θ(r) .

Page 26: Chapter 3: Central Forces

• Formally:

(dθ/dr) = (/r2)(2m)-½[E - V(r) -{2(2mr2)}]-½

• Integrating this gives a formal eqtn for the orbit:

θ(r) = ∫ (/r2)(2m)-½[E - V(r) - {2(2mr2)}]-½ dr• Once the central force is specified, we know V(r) & can, in principle, do

the integral & get the orbit θ(r), or, (if this can be inverted!) r(θ).

This is quite remarkable! Assuming only a central force law & nothing else:

We have reduced the original 6 d problem of 2 particles to a 2 d problem with only 1 degree of freedom. The solution for the orbit can be obtained simply by doing the above (1d) integral!


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