Sixth lecture September 21, 2006

Σχετικά έγγραφα
Tutorial problem set 6,

HOMEWORK 4 = G. In order to plot the stress versus the stretch we define a normalized stretch:

Section 8.3 Trigonometric Equations

derivation of the Laplacian from rectangular to spherical coordinates

( y) Partial Differential Equations

Riemannian Curvature

Second Order Partial Differential Equations

Areas and Lengths in Polar Coordinates

Exercises 10. Find a fundamental matrix of the given system of equations. Also find the fundamental matrix Φ(t) satisfying Φ(0) = I. 1.

3.4 SUM AND DIFFERENCE FORMULAS. NOTE: cos(α+β) cos α + cos β cos(α-β) cos α -cos β

Homework 8 Model Solution Section

9.09. # 1. Area inside the oval limaçon r = cos θ. To graph, start with θ = 0 so r = 6. Compute dr

Higher Derivative Gravity Theories

Problem Set 9 Solutions. θ + 1. θ 2 + cotθ ( ) sinθ e iφ is an eigenfunction of the ˆ L 2 operator. / θ 2. φ 2. sin 2 θ φ 2. ( ) = e iφ. = e iφ cosθ.

Section 7.6 Double and Half Angle Formulas

forms This gives Remark 1. How to remember the above formulas: Substituting these into the equation we obtain with

Phys460.nb Solution for the t-dependent Schrodinger s equation How did we find the solution? (not required)

Parallel transport and geodesics

Lecture 2: Dirac notation and a review of linear algebra Read Sakurai chapter 1, Baym chatper 3

b. Use the parametrization from (a) to compute the area of S a as S a ds. Be sure to substitute for ds!

Partial Differential Equations in Biology The boundary element method. March 26, 2013

2 Composition. Invertible Mappings

Example Sheet 3 Solutions

Geometry of the 2-sphere

Cosmological Space-Times

Areas and Lengths in Polar Coordinates

Symmetry. March 31, 2013

SCHOOL OF MATHEMATICAL SCIENCES G11LMA Linear Mathematics Examination Solutions

Geodesic Equations for the Wormhole Metric

A Short Introduction to Tensors

6.1. Dirac Equation. Hamiltonian. Dirac Eq.

If we restrict the domain of y = sin x to [ π, π ], the restrict function. y = sin x, π 2 x π 2

CHAPTER 25 SOLVING EQUATIONS BY ITERATIVE METHODS

Parametrized Surfaces

Section 9.2 Polar Equations and Graphs

C.S. 430 Assignment 6, Sample Solutions

If we restrict the domain of y = sin x to [ π 2, π 2

CRASH COURSE IN PRECALCULUS

Απόκριση σε Μοναδιαία Ωστική Δύναμη (Unit Impulse) Απόκριση σε Δυνάμεις Αυθαίρετα Μεταβαλλόμενες με το Χρόνο. Απόστολος Σ.

Space-Time Symmetries

Chapter 6: Systems of Linear Differential. be continuous functions on the interval

Finite Field Problems: Solutions

The kinetic and potential energies as T = 1 2. (m i η2 i k(η i+1 η i ) 2 ). (3) The Hooke s law F = Y ξ, (6) with a discrete analog

Appendix A. Curvilinear coordinates. A.1 Lamé coefficients. Consider set of equations. ξ i = ξ i (x 1,x 2,x 3 ), i = 1,2,3

ANSWERSHEET (TOPIC = DIFFERENTIAL CALCULUS) COLLECTION #2. h 0 h h 0 h h 0 ( ) g k = g 0 + g 1 + g g 2009 =?

Matrices and Determinants

Concrete Mathematics Exercises from 30 September 2016

Srednicki Chapter 55

1 String with massive end-points

Homework 3 Solutions

Solutions to Exercise Sheet 5

4.6 Autoregressive Moving Average Model ARMA(1,1)

D Alembert s Solution to the Wave Equation

The Simply Typed Lambda Calculus

Approximation of distance between locations on earth given by latitude and longitude

MATH423 String Theory Solutions 4. = 0 τ = f(s). (1) dτ ds = dxµ dτ f (s) (2) dτ 2 [f (s)] 2 + dxµ. dτ f (s) (3)

Orbital angular momentum and the spherical harmonics

Exercise 1.1. Verify that if we apply GS to the coordinate basis Gauss form ds 2 = E(u, v)du 2 + 2F (u, v)dudv + G(u, v)dv 2

Integrals in cylindrical, spherical coordinates (Sect. 15.7)

EE512: Error Control Coding

Reminders: linear functions

You may not start to read the questions printed on the subsequent pages until instructed to do so by the Invigilator.

ECE Spring Prof. David R. Jackson ECE Dept. Notes 2

PARTIAL NOTES for 6.1 Trigonometric Identities

Variational Wavefunction for the Helium Atom

Lecture 26: Circular domains

On a four-dimensional hyperbolic manifold with finite volume

Jesse Maassen and Mark Lundstrom Purdue University November 25, 2013

= {{D α, D α }, D α }. = [D α, 4iσ µ α α D α µ ] = 4iσ µ α α [Dα, D α ] µ.

Chapter 6: Systems of Linear Differential. be continuous functions on the interval

Spherical Coordinates

( ) 2 and compare to M.

Math221: HW# 1 solutions

Numerical Analysis FMN011

Statistical Inference I Locally most powerful tests

Linearized Conformal gravity

DESIGN OF MACHINERY SOLUTION MANUAL h in h 4 0.

CHAPTER 101 FOURIER SERIES FOR PERIODIC FUNCTIONS OF PERIOD

Differential equations

1. (a) (5 points) Find the unit tangent and unit normal vectors T and N to the curve. r(t) = 3cost, 4t, 3sint

ΚΥΠΡΙΑΚΗ ΕΤΑΙΡΕΙΑ ΠΛΗΡΟΦΟΡΙΚΗΣ CYPRUS COMPUTER SOCIETY ΠΑΓΚΥΠΡΙΟΣ ΜΑΘΗΤΙΚΟΣ ΔΙΑΓΩΝΙΣΜΟΣ ΠΛΗΡΟΦΟΡΙΚΗΣ 19/5/2007

Section 8.2 Graphs of Polar Equations

(As on April 16, 2002 no changes since Dec 24.)

6.3 Forecasting ARMA processes

Every set of first-order formulas is equivalent to an independent set

Econ 2110: Fall 2008 Suggested Solutions to Problem Set 8 questions or comments to Dan Fetter 1

Physics 554: HW#1 Solutions

Strain gauge and rosettes

Written Examination. Antennas and Propagation (AA ) April 26, 2017.

ΚΥΠΡΙΑΚΗ ΕΤΑΙΡΕΙΑ ΠΛΗΡΟΦΟΡΙΚΗΣ CYPRUS COMPUTER SOCIETY ΠΑΓΚΥΠΡΙΟΣ ΜΑΘΗΤΙΚΟΣ ΔΙΑΓΩΝΙΣΜΟΣ ΠΛΗΡΟΦΟΡΙΚΗΣ 6/5/2006

Tridiagonal matrices. Gérard MEURANT. October, 2008

Derivation of Optical-Bloch Equations

Problem Set 3: Solutions

Similarly, we may define hyperbolic functions cosh α and sinh α from the unit hyperbola

DERIVATION OF MILES EQUATION FOR AN APPLIED FORCE Revision C

Practice Exam 2. Conceptual Questions. 1. State a Basic identity and then verify it. (a) Identity: Solution: One identity is csc(θ) = 1

Answer sheet: Third Midterm for Math 2339

Example of the Baum-Welch Algorithm

Solutions to the Schrodinger equation atomic orbitals. Ψ 1 s Ψ 2 s Ψ 2 px Ψ 2 py Ψ 2 pz

The challenges of non-stable predicates

Transcript:

Sixth lecture September, 006 Web Page: http://www.colorado.edu/physics/phys7840 NOTE: Next lectures Tuesday, Sept. 6; noon Thursday, Sept. 8; noon Tuesday, Oct. 3; noon Thursday, Oct. 5; noon more???? Today s topics: Bianchi Identities Covariant divergence of Ricci tensor Einstein field equations linearized equations first-order coordinate transformations free space equations gravity waves detection of gravity waves with clocks??

Ricci tensor In General Relativity, the components of the metric tensor (0 independent quantities) are treated as potentials, and one wants to derive field equations that determine these 0 quantities. The Ricci tensor is a candidate, since it is symmetric with respect to exchage of the two indices. There is only one independent way to get a second-rank tensor from the curvature tensor by contraction: R = R α = R σρ σαρ ρσ ( Ricci Tensor)

Bianchi identities One last set of identities is very important in GR. The Bianchi identities state: R R R αβγ ; δ + αγδ ; β + αδβ ; γ = 0. This is the sum of the covariant derivatives of the curvature tensor with last three indices cyclically permuted. To prove this, write out the sum at a point where the Christoffel symbols of the second kind have been reduced to zero by a coordinate transformation: R R R Γ Γ = ; β γ δ β x x x x αγ αβ αβγ ; δ δ β δ γ Γ Γ αδ αγ αγδ ; β = β γ β δ x x x x Γ αβ Γαδ αδβ ; γ = γ δ γ β x x x x ; ; Adding these three equations proves the equation at the top of the page. 3

Scalar curvature One can contract the Ricci tensor further to obtain the scalar curvature α R R = g R α αβ αβ. 4

Example: Surface of a sphere The metric is two-dimensional: ds = a dθ + a sin θdϕ. RicciScalar = a 5

Parallel transport on the surface of a sphere Suppose we take a parallel of latitude at angle θ, and transport a vector parallel to itself around through some angle. The differential equation of parallel transport of the vector is dt = δ t = Γ t dx α σ ασ σ dt α dx + Γ ασt = dλ dλ We consider parallel propagation keeping θ fixed. 0. dt α dϕ + Γ α t = 0; dλ dλ dt α + Γ α t = 0. dϕ We get two coupled equations for the components of the vector: dt = dϕ dt dϕ cosθ sinθ t 0; cosθ sinθ + t = 0; ; 6

Parallel transport on the surface of a sphere The solutions to the differential equations, putting in boundary conditions such that there is only a -component at the start where the azimuthal angle is zero, and also that the vector is normalized, are: t = sin(cos θ ϕ), t = cos(cos θ ϕ). a a sinθ As the vector is transported along the parallel, which is not a geodesic, it rotates. 7

Parallel transport along an arbitrary path path The vector rotates in a retrograde direction; at each point along the path there is a geodesic that is tangent to the curve. During each infinitesimal path increment the tangent vector maintains a constant angle with respect to the local geodesic (great circle)... geodesic 8

Example: Divergence of a gradient The tensor analysis developed so far allows one to construct physically interesting quantities such as the generalization of the Laplacian. This is a second-order differential operator that operates on a scalar. First we take the gradient of a scalar: Φ = Φ x, = Φ ; ; We want to take the divergence of this quantity but first the index has to be raised to get a contravariant vector: g κ Φ, The covariant derivative of this is ( g κ Φ, ) and to get a second-order scalar differential operator, we set λ=κ and sum. ; λ 9

Divergence of a gradient ( ) ( ) g Φ = g Φ + Γ g Φ κ κ κ β, ; κ κ, βκ, κ The contracted quantity Γ βκ occurs often and we shall need an expression for it. κ g κλ Γ = g + g g ( ),,, βκ λβ κ λκ β βκ λ Γ = g g = g x g = det κ κλ κλ βκ λκ, β β λκ ( ) gαβ λ, κ ( ).. ( Cofactor g ) λκ x = det ( g.. ) = ln det ( g.. ) = ln g β β β det g x x x β g λκ. 0

Divergence of a gradient Thus the scalar divergence of a gradient in generalized coordinates is ( ) ( ) g Φ = g Φ + Γ g Φ κ κ κ β, ; κ κ, βκ, ( g ) ( ) = Φ + g g Φ g κ β κ, β, β ( g g, ) = Φ g β This works for any type of orthogonal coordinate system in three dimensions, e.g., spherical polar coordinates: ds = dr + r dθ + r sin θdϕ ;. 0 0 g r g r 0 0 r sin θ ν = 0 0 ; + = sin θ.

Laplacian in spherical polar coordinates 0 0 0 0 g = 0 r 0 ; g = 0 0 ; + g = r sin 0 0 r sin θ 0 0 r sin θ ν ν θ r κ ( g g ) r ( r sinθ r ) Φ = Φ + Φ + Φ g r sinθ r r sin θ r sinθ r sinθ κ, θ θ ϕ ϕ

Einstein Field Equations In Newtonian mechanics and electromagnetic theory, conservation of energy and momentum is expressed by four equations arising from the symmetric stress-energy tensor: T ν =, ν 0. In generalized coordinates in the presence of gravitation, this ought to become T ν = ; ν 0. If we try field equations of the form R = κt ν ν, Then we run into trouble with the Bianchi identities since R ν ; ν 0. 3

Contracting Bianchi identities Let s compute the covariant divergence of the Ricci tensor by contracting the Bianchi identities: R R R αβγ ; δ + αγδ ; β + αδβ ; γ = 0. Set β = and sum, while also raising the index α : R R R α α α γ ; δ + γδ ; + δ ; γ = 0. (We made use of the fact that the covariant derivative of the metric tensor vanishes.) R + R + R = α α α γ ; δ γδ ; δ ; γ R + R R = α α α γ ; δ γδ ; δ ; γ R + R R = α α α γ ; δ γδ ; δ ; γ 0. 0. 0. R = R in last term α α δ δ 4

Contracting the Bianchi identities R R R α α α γ ; δ + γδ ; δ ; γ = 0. R + R R = 0. ( ) α α α γ ; δ δγ ; δ ; γ α = δ Now set and contract: R + R R = R R = 0. α γ ; α γ ; ; γ γ ; ; γ R γ = Thus we conclude that γ ; ; R 0. This can also be written as R δ R = 0. γ ; γ ; 5

Einstein Tensor We define the Einstein Tensor as G R γ = γ δγ R. This has vanishing covariant divergence. The fully covariant form of the Einstein tensor is obtained by lowering the contravariant index: Gβγ = Rβγ gβγ R. This apparently has 0 symmetric components, and second derivatives of the metric tensor enter. It s reasonable to think that the equations determining the metric tensor could be of the form κ G βγ = κt where is a coupling constant. Then conservation laws could be expressed by G βγ ; T γ = κ γ ; = 0,, 6

Einstein Field Equations Einstein pointed out that it is possible another term could enter the field equations, that would also vanish when taking the covariant divergence. The field equations would be Λ G + Λ g = κt βγ βγ βγ where is the cosmological constant. We ll ignore this term even though it is important when discussing dark matter. Also, we ll put off dealing with the actual form of the stress-energy tensor of matter until later, and look for solutions of the field equations in empty space. So for example, for gravitational waves or outside a star, we re interested in G βγ = 0., 7

Does it work??? Linearized coordinate transformations Anticipating needed coordinate transformation equations that will arise a little later, suppose we approximate the metric tensor by small deviations from the Minkowski metric: h ν g = η + h ν ν ν where is not a tensor, but is small enough that terms of second order can be neglected. Let us make a correspondingly small change in coordinates, of the form x = x ' ξ ( x ');, Then x = δ ξ ν x ' ν, ν We ll substitute these expressions in the transformation law for the metric tensor and neglect higher-order terms. 8

Linearized transformation of metric tensor α β x x g ' = η + h' = + h ν x ' x ' ( η ) ν ν ν αβ αβ ( α α )( β β δ )( ) ξ, δν ξ, ν ηαβ hαβ = + η + h δ ξ η δ ξ η α β β α ν ν, ν αβ ν, αβ = η + h η ξ η ξ β α ν ν β, ν αν, h' = h η ξ η ξ. β α ν ν β, ν αν, While we re at it, we raise the index and contract, defining ν ν h ' = η h' ; h = η h. ν ν. β α Then h' = h δ ξ, δ ξ, = h ξ,. β α 9

Getting ready to linearize Anticipating what is going to arise in linearizing the Einstein tensor, we define γδ γδ σ = η hγ, δ ηγ h, δ = η hγ, δ h,. Making the first-order coordinate transformation, γδ σ ' = η h' γ, δ h', γδ α α α = η η ξ η ξ ξ γδ γδ α γδ α α = η h, h, η η ξ, η η ξ, + ξ, But the last two terms cancel: ( hγ, δ α, γδ γα, δ ) ( h,, α ) γ δ α γδ γα δ α γδ α α δ α α α α η η ξ, + ξ, = δ ξ, + ξ, = ξ, + ξ, = 0. γα δ α α δ α α α 0

New coordinate conditions σ ' = η γδ h, h, η γδ η ξ α, γ δ α γδ α ( ) = σ η η ξ γδ α γδ, α But the last term is just the D Alembertian operator applied to ξ ( η ξ ). γδ η ( ξ ), = + + + ξ c t x y z γδ We can therefore choose a coordinate transformation such that γδ ( α η ηαξ ), γδ = σ σ ' = 0 α since solutions of the wave equation with sources has a well-known solution that can be obtained by integration (e.g., see Electromagnetic Theory).

Gauge freedom ( ), σ = η ξ = ξ γδ γδ We can choose ξ so that this equation is satisfied. Further, we can add an arbitrary solution of the wave equation, ξ = ξ σ '. to without changing the value of 0

Linearized Field equations σ So whenever we see a quantity arising in linearizing the field equations, we can say that it can be eliminated by an appropriately chosen coordinate transformation. Now we are finally ready to linearize. We write g = η + h γδ γδ γδ where h is small, and all the calculations are carried only to first order of smallness. The Christoffel symbols involve derivatives of the metric tensor and so will be of first order. For example, Γ = g g + g g h + h h, ( ) η ( ) σ σ αβ σα, β σβ, α αβ, σ σα, β σβ, α αβ, σ. 3

Does it work?? Linearize Then the non-linear terms in the Riemann tensor will be negligible: R = Γ Γ + Γ Γ Γ Γ β β αρσ ρ ασ σ αρ βρ ασ βσ αρ Γ Γ ρ ασ σ αρ κ κ = η + + κ R αρσ = η ( hκσ, αρ hασ, κρ hκρ, ασ + hαρ, κσ ). ( hκα, σρ hκσ, αρ hασ, κρ ) η ( hκα, ρσ hκρ, ασ hαρ, κσ ) ; 4

Linearized Field Equations κ R = η h h h + h ( ),,,, αρσ κσ αρ ασ κρ κρ ασ αρ κσ Construct the Ricci tensor by contraction: ρ =. R = η h h h + h ( ) κ ασ κσ, α ασ, κ κ, ασ α, κσ. And the scalar curvature by raising the index α and contracting: ασ ασ κ R = η R = η η h h h + h ασ κ = η η ( hκσ, α hασ, κ hκ, ασ + hα, κσ ) α = h, h (,,,, ) ασ κσ α ασ κ κ ασ α κσ α 5

Construct the linearized Einstein tensor Gασ = Rασ gασ R κ β = η + ( hκσ, α hασ, κ hκ, ασ hα, κσ ) ηασ ( h, β h) Recall that γδ γδ σ = η hγ, δ ηγ h, δ = η hγ, δ h,. So γδ η h, = σ + h, ; η h, = σ + h, γδ γ δ γ δσ, σ σ We ll rewrite each of the six terms in the linearized Einstein tensor. 6

Rewrite of linearized Einstein tensor η γδ h κ β Gασ = η hκσ α hασ κ hκ ασ + hα κσ ασ h β h ( ) ( ),,,, η, κ η h = σ + h κσ, α σ, α, σα, = σ + h,. γ δσ, σ σ ; κ η hασ, κ = κ κ η hκ, ασ = h, ασ η hα, κσ = σα, σ + h, ασ h ασ ( h β, ) ( γ βδ h, ) γ η, h γ ασ β = ηασ η η γδ β = ηαση σ γ +, γ = ηαση σ γ, ηασ h 4 ηασ = + ( h) η ( ασ h) 7

Linearized Einstein tensor at last! Adding all the contributions: Gασ = σσ, α + h, σα hασ h, ασ σ η η σ η η 4 ( ) γ α, σ + h, ασ ασ γ, ασ h + ασ h Gασ = hασ ηασ h = κtασ These are the linearized field equations. There is also the coordinate condition γδ η hγ, δ h, = 0. 8