Theory of Cosmological Perturbations

Μέγεθος: px
Εμφάνιση ξεκινά από τη σελίδα:

Download "Theory of Cosmological Perturbations"

Transcript

1 1 heory of Cosmological Perturbations Part I gauge-invariant formalism Misao Sasaki PDF files available at

2 1. Formulation Background spacetime Friedmann-Lematre-Robertson-Walker metric K = ±1, 0): ds 2 = dt 2 + a 2 t)dσ 2 K ; dσ 2 K = γ ij dx i dx j = dχ 2 + sinh2 K χ) K dω 2 2) 2 Conformal time coordinate: dη = dt a ds 2 = a 2 η) ) dη 2 + dσk 2 Energy momentum tensor in the perfect fluid form: µν = ρu µ u ν + pg µν + u µ u ν ) ; u ν dx ν = dt = adη. Friedmann equation: G 0 0 = R R = 8πG 0 0) ȧ ) 2 + K a a = 8πG ρ, ρ + 3ȧρ + p) = a ) a 2 + K = 8πG a 3 ρ a2, ρ + 3 a ρ + p) = 0 a ȧ = da ) dt a = da ). dη

3 3 Hereafter, we use the symbols: H = ȧ a, H = a a Spatial harmonics scalar harmonics + k 2 ) Y k = 0 γ ij D i D j ). k 2 K) for K 0 k 2 : continuous) k 2 = nn + 2)K for K > 0 n = 0, 1, 2, ) Examples in the case of K = 0: Y k = e ik x ; k 2 = k 2, or Y k = j l kχ)y lm Ω) ; k = k, l, m).

4 4 vector harmonics index k omitted) scalar type: Y i = k 1 D i Y, vector transverse) type: D i Y 1)i = 0, ) + k 2 Y 1)i = 0 ; + k 2 2K) ) Y i = 0. k 2 = nn + 2) 1)K for K > 0 n = 1, 2, ), k 2 2K) for K 0. tensor harmonics scalar traceless) type: Y ij = k 2 D i D j + 1 ) 3 γ ij Y, + k 2 6K ) Y ij = 0. vector traceless) type with index σ, k): σ = 1, 2): Y 1) ij = 1 ) D i Y 1) j + D j Y 1) i, + k 2 4K ) Y 1) ij = 0. 2k tensor transverse-traceless) type with index σ, k): σ = 1, 2): D j Y 2) ij = Y 2)i i = 0, ) + k 2 Y 2) ij = 0 ; k 2 = nn + 2) 2)K for K > 0 n = 2, 3, ), k 2 3K) for K 0.

5 Perturbation variables scalar type perturbations metric: g 00 = a Aη)Y ), g 0j = a 2 BY j = a 2B ) k D jy, 5 matter: g ij = a 2 [1 + 2H L Y )γ ij + 2H Y ij ] [ ] = a RY )γ ij + 2H k 2D id j Y ; R H L H. µ ν = ρũ µ ũ ν + τ µ ν ; ρ = ρ1 + δ Y ), ṽ i ũi u = v Y i = v ) 0 k Di Y u 0 = a) 1 ũ0 = u 0 1 AY ) from ũ µ ũ µ = 1 ) τ i j = p [ ] δj1 i + π L Y ) + π Y i j

6 geometrical meaning 3 + 1)-decomposition: 6 ds 2 = a 2 η)dŝ 2 ; dŝ 2 = Ñ 2 dη 2 + γ ij dx i + Ñ i dη)dx j + Ñ j dη). ~i N dη xi=const. ~ Ndη η + dη =const. η =const. extrinsic curvature: ñ µ dx µ = Ñdη hypersurface normal : Ñ = 1 + AY lapse function, Ñ i = BY i shift vector. ˆK ij = H kb)y ij = kσ g Y ij σ g 1 k H B shear of η =const. hypersurface.

7 expansion : 7 θ 1 a 4 µ a 3 ñ µ ) = 3 a a 1 + K gy ) = 3H 2 a 1 + K gy ) K g A + H R 1 k ) 3 σ g 3-curvature: In particular, δ s ˆRi jmn = D m δ s Γ i jn D n δ s Γ i jm ; δ s Γ i jm = 1 2 γil D m δγ lj + D j δγ lm D l δγ jm ), s ˆR = 6K + 4k 2 3K) δγ ij = 2H L γ ij + 2H Y ij. H L + 1 ) 3 H Y = 6K + 4k 2 3K)RY. R intrinsic curvature perturbation potential).

8 Gauge transformation properties 8 x x µ x µ = x µ + ξ { µ η = η + Y, x i = x i + LY i. his induces a gauge transformation, x ξ x x=x+ ξ x ḡ µν = g µν ξ µ;ν + ξ ν;µ ) [ ] in general, Q{A} = Q {A} L ξ Q {A}. {A} spacetime indices)

9 metric: ) H = a a 9 Ā = A H lapse ) B = B + L + k H L = H L k σ g = σ g k 3 L H R = R H H = H + kl σ g = 1 ) k H B shear R = H L + 1 ) 3 H curvature matter: δ = δ w)h v = v + L w p ) ρ v B) = v B) k ) π L = π L + 3c w w c w H 2w p ρ π = π ~ Ndη ~i N dη xi=const. v i dη η + dη =const. u µ η =const. v i ~ + N i )d η =v-b )Y idη Blue quantities depend only on the choice of time-slicing.

10 gauge-invariant variables 4 metric variables 2 gauge variables = 2 degrees of freedom) 10 Ψ A 1 ) σ k g + H σ g, σ g = 1 ) k H B Φ R H k σ g. R = H L + 1 ) 3 H s δ + 3 H k 1 + w)σ g V v 1 k H = v B) σ g shear of 4-velocity ũ µ Γ π L c2 w w δ pγ = δp c2 wδρ ) entropy perturbation Π π anisotropic stress perturbation. Ψ = A, Φ = R, s = δ, V = v B on σ g = 0 hypersurface. Shear-free slicing or Newton slicing

11 Other popular choices: 11 R c R H k v B) = Φ H k V, σ g) c = V, A c A 1 k [v B) + Hv B)] = Ψ 1 k [V + H V ] δ + 3 H k 1 + w)v B) = s + 3 H k 1 + w)v, Velocity-orthogonal or comoving slicing v B = 0) ζ R w) δ = R c w) Curvature perturbation on uniform density slices δ = 0) f δ w)r = w)r c = 31 + w)ζ Density perturbation on flat slices R = 0)

12 vector type perturbations 12 Ñ 1) j = B 1) Y 1) j, γ 1) ij = γ ij + 2H 1) Y 1) ij. gauge transformation: ṽ 1)j = aũ [ 1)j = v 1) Y 1)j ], τ 1)i j = p δj i + π 1) Y 1) ij. x j = x j + L 1) Y 1)j gauge-invariant variables: { B1) = B 1) + L 1), H 1) = H 1) + kl 1). v 1) = v 1) + L 1), π 1) = π 1). 2 metric variables 1 gauge variable = 1 degree of freedom) σ 1) g = 1 k H1) B 1), V 1) = v 1) B 1), Π 1) = π1). tensor type perturbations [ ] γ 2) ij = γ ij + 2H 2) Y 2) ij. τ 2)i j = p δj i + π 2) Y 2) ij Both H 2) and π 2) are gauge-invariant by themselves..

13 2. Einstein equations in terms of gauge-invariant variables Scalar type perturbations Einstein equations: δg µ ν = 8πGδ µ ν : δg 0 0 = 2 a 2 [ 3H 2 A + H kσ g 3H R k 2 3K)R ] Y δg 0 j = 2 a [kh A 2 kr + Kσ g ] Y j δg i j = 2 [ ) 2H + H 2 k2 A + H A + k ) σ a g + 2H σ g R 2HR 1 ] 3 k2 3K)R δjy i a 2 [ k 2 A + kσ g + 2Hσ g ) k 2 R ] Y i j δ 0 0 = ρ δ Y, δ 0 j = ρ + p)v B)Y j, δ i j = pγ + c 2 wρ δ)δ i jy + pπ Y i j. N.B. pγ + c 2 wρ δ = δp) he above equations depend only on the choice of time slicing. ie, they are spatially gauge-invariant.

14 Energy-momentum conservation: 14 δ 0 ν ;ν ) = 0 : δ + 3H [ c 2 w w)δ + wγ ] + k1 + w)v B) w)3r kσ g ) = 0. δ j ν ;ν ) = 0 : v B) + H1 3c 2 w)v B) = ka + k c2 wδ + wγ 1 + w 2k 3 hese are also spatially gauge-invariant. w 1 + w 1 3Kk ) π 2. o obtain gauge-invariant equations, it is simplest to set a gauge time-slicing) condition that fixes the time slices completely. gauge-invariance complete gauge-fixing Gauge-invariant quantities are NO necessarily directly related to observables Advantage of gauge-invariant formalism is because one does not have to choose a particular gauge while dealing only with physical degrees of freedom, not because the values of the gauge-invariant variables are physical by themselves.

15 15 Example: choose σ g = 0 Newton slicing), so that A = Ψ, R = Φ, δ = s, v B = V. δg 0 0 = 8πGδ 0 0 : δg 0 j = 8πGδ 0 j : 1 a 2 [ 3HHΨ Φ ) k 2 3K)Φ ] = 4πGρ s, 1) k a 2 [HΨ Φ ] = 4πGρ + p)v, 2) δg i j = 8πGδ i j) traceless : k2 a 2 [Ψ + Φ] = 8πpΠ. 3) δg i j = 8πGδ i j) trace : ) 1 [2H + H 2 k2 Ψ + H Ψ a 2 3 Φ 2HΦ 1 ] 3 k2 3K)Φ = 4πGp [ Γ + c 2 wρ s ]. 4) Combining Eqs. 1) and 2) [Hamiltonian and momentum constraints] gives k 2 3K Φ = 4πGρ [ a 2 s + 3 Hk ] 1 + w)v = 4πGρ. 5) Eqs. 3) and 5) algebraically determine Φ and Ψ in terms of and Π. Combining Eqs. 1), 3) and 4), one can derive 2nd order differential equation for Φ. Alternatively, one may appeal to the energy-momentum conservation laws. contracted Bianchi identities)

16 16 ν δ j ;ν ) = 0 on shear-free Newton) slices : V + H1 3c 2 w)v = kψ + k c2 w s + wγ 1 + w s = 3 Hk ) 1 + w)v 2k 3 w 1 + w 1 3Kk 2 ) π V + H V = kψ + k c2 w + wγ 1 + w 2k w 1 3Kk ) π w 2 6) Ψ = Φ 8πGρ ) a2 w 4πGρ a2 Π k 2, Φ = k 2 3K δ 0 ν ;ν ) = 0 on comoving slices : + 3H [ c 2 w w) + wγ ] w) 3R c + kv ) = 0 ; R c = Φ H ) k V k a [HΨ 2 Φ ] = 4πGρ + p)v, V =, 3wH = 1 3Kk ) [1 + w)kv + 2H wπ 2 ] 7) Combining Eqs. 6) and 7) gives a 2nd order differential equation for.

17 c 2 w 2w) ) H + [ c 2 sk 2 3K) 4πGρa w)1 w) + 6w c 2 w) ) + 34w 3c 2 w)k ] = S c [ ] S c = k 2 δp)c c 2 3K) sδρ) c 2 1 3Kk ) H wπ ρ 2 +2 [3w 2 2w + 3c 2w)H 2 + 4w c 2w)K + c2 wk 2 ] 1 3Kk ) 3 2 Master equation for equation for sound waves) Π In the Newtonian, non-relativistic limit w 1, c 2 s 1), + H + c 2 sk 2 4πGρ a 2) S c, + 2H c 2 + s k 2 ) 4πGρ S c a 2 a 2 dispersion relation: ωeff 2 = c2 sk 2 4πGρ Jeans instability: for c 2 w p /ρ = p/ ρ c 2 s) ) k k gravitationally unstable for a < 4πGρ a c 2 s a 2 J or λ > λ J πc 2 s Gρ

18 Vector type perturbations 18 δg 0 j = 8πGδ 0 j : δg i j = 8πGδ i j : σ g 1) + 2Hσ g 1) k2 2K σ 1) 2a 2 g = 8πG1 + w)ρ V 1). = 8πρa 2w k Π1). Either combining these two or directly from the momentum conservation, For Π 1) δ i µ ;µ ) = 0 : = 0 adiabatic), σ 1) g 1 a 2, V 1) Vorticity Ω: V 1) + 1 3c 2 w)h V 1) = k2 2K 2k 1 ρ1 + w)a 4 1 a 1 3w 1 ρ w/1+w) a his is just the vorticity conservation law. w 1 + w Π1). ) for w = const. Ω µν P α µ u [α;β] P β ν ; P µν = g µν + u µ u ν. Ω ij = a k V 1) Z ij Z ij = 1 ) k D [jy 1) i], Ω ij Ω ij = k2 a 2 V 1) 2 Z ij Z ij ρ w/1+w) S Ω =const. S: area a 2 ).

19 19 ensor type gravitational wave) perturbations For K = 0, Π 2) δg i j = 8πGδ i j : H 2) Ḧ 2) + 2H H 2) + k 2 + 2K)H 2) = 8πG p a 2 Π 2) + 3H Ḣ2) + k2 + 2K H 2) a 2 = 8πG p Π 2) = 0, this is the same as the field equation for a massless minimal scalar: ϕ + 3H ϕ + k2 a 2 ϕ = 0. On superhorizon scales k 2 H 2 a 2 = H 2 ), const. H 2) η dη a 2 growing mode decaying mode tensor perturbation a homogeneous, anisotropic universe On subhorizon scales k 2 H 2 a 2 = H 2 ), H 2) 1 a eikη ρ GW Ḣ2) 2 1 a 4

20 3. Adiabatic perturbations on superhorizon scales Spatially flat universe K = 0) is a good approximation in the early universe. hen, ρ a 3 ) c 2 w)hρ a 3 ) + [c 2sk 2 32 ] 1 + w)h2 ρ a 3 ) = ρ a 3 S c. 20 Here, c 2 w p /ρ, c 2 s p/ ρ) comoving δp) c = c 2 sδρ) c + entropy perturbation Also, all cosmologically relevant scales exceed Hubble horizon. ln L phys λ = 2πa k a, H 1 ρ { 1/2 a 3/2 for dust w = 0) a 2 for radiation w = 1/3) λ for a 0 H 1 k = const. L ~ a) L = 1/H ~ a2 in rad-dom universe) ln a

21 21 For S c = 0 adiabatic perturbation), one general solution in the limit c 2 sk 2 0 is ρ a 3 H 1 a H a = 1 decaying mode 2 H a 3 Using the Wronskian for 2 independent solutions, the other solution is found as ρ a 3 H a η 0 1 H a w)a 2 dη η 0 t 1 + w)a 2 dη = w)adt growing mode H a 3 0 η 2 for w = const. ) Conservation of growing mode amplitude Let us set = C 1 k 2 H a 2 η w)a 2 dη his gives, from the Hamiltonian and momentum constraints, Φ = 3 2 k = C H 1 a 2 H 2 η R c = Φ H k V = C w)a 2 dη, H k V = w)h Φ + H Φ)

22 22 he growing mode amplitude of R c stays constant on superhorizon scales. he condition for the linear perturbation theory to be valid is R c = C 1 1. linear theory is applicable up to t = 0 singularity if only the growing mode is present. For the decaying mode, where = C 2 k 2 H a 2, R c = C 2 ηf η η f = R c = H c2 s + wγ c 1 + w c 2 sk w)a 2dη Γ c δp) c c 2 sδρ) c ρ { for w 1/3 0 finite) for w < 1/3 ) = 0 Decaying mode amplitude for R c is not constant. he standard lore that R c = const. on superhorizon scales is not strictly correct. It is correct only if the decaying mode can be ignored.

23 23 Growing mode solution for several other variables assuming w =const.) a η 2/3w+1) 2 ), H = 3w + 1)η ζ = R c w) C 1 ζ = R on uniform density slice) is also constant. his is true not only for GR but also for any metric theory. Wands et al. 2000) 3w + 1)2 1 + w) 23w + 5) σ g ) c = V 3w + 1 C 1 kη) 2, A c = R c = c2 s 1 + w 3w + 1)2 w 23w + 5) C 1 kη) 2, 3w + 5 C 1 kη, 31 + w) Ψ = Φ 3w + 5 C 61 + w) 1, s 2Φ 3w + 5 C 1 Φ curvature perturbation on Newton slices) or Ψ Newton potential) stays constant for w =const., but the amplitude changes when w changes. In particular, during inflation when w 1, the amplitude of Φ stays very small, but it grows significantly at the end of inflation. During inflation, quasi-nonlinear perturbations C 1 1) can be studied in Newton gauge.

Theory of Cosmological Perturbations

Theory of Cosmological Perturbations 1 heory of Cosmological Perturbations Part I gauge-invariant formalism Misao Sasaki PDF files available at http://www2.yukawa.kyoto-u.ac.jp/~misao/pdf/cp/ 1. Formulation Background spacetime Friedmann-Lematre-Robertson-Walker

Διαβάστε περισσότερα

Cosmological Perturbations from Inflation

Cosmological Perturbations from Inflation Cosmological Perturbations from Inflation Misao Sasaki Kyoto University 1. Introduction 2 Horizon problem ds 2 = dt 2 + a 2 (t)d x 2 + Einstein eqs. ä a = 4πG (ρ + 3p) ρ + 3p > 0 decelerated expansion

Διαβάστε περισσότερα

6.1. Dirac Equation. Hamiltonian. Dirac Eq.

6.1. Dirac Equation. Hamiltonian. Dirac Eq. 6.1. Dirac Equation Ref: M.Kaku, Quantum Field Theory, Oxford Univ Press (1993) η μν = η μν = diag(1, -1, -1, -1) p 0 = p 0 p = p i = -p i p μ p μ = p 0 p 0 + p i p i = E c 2 - p 2 = (m c) 2 H = c p 2

Διαβάστε περισσότερα

Higher Derivative Gravity Theories

Higher Derivative Gravity Theories Higher Derivative Gravity Theories Black Holes in AdS space-times James Mashiyane Supervisor: Prof Kevin Goldstein University of the Witwatersrand Second Mandelstam, 20 January 2018 James Mashiyane WITS)

Διαβάστε περισσότερα

Cosmological Space-Times

Cosmological Space-Times Cosmological Space-Times Lecture notes compiled by Geoff Bicknell based primarily on: Sean Carroll: An Introduction to General Relativity plus additional material 1 Metric of special relativity ds 2 =

Διαβάστε περισσότερα

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

Phys460.nb Solution for the t-dependent Schrodinger s equation How did we find the solution? (not required) Phys460.nb 81 ψ n (t) is still the (same) eigenstate of H But for tdependent H. The answer is NO. 5.5.5. Solution for the tdependent Schrodinger s equation If we assume that at time t 0, the electron starts

Διαβάστε περισσότερα

CHAPTER 25 SOLVING EQUATIONS BY ITERATIVE METHODS

CHAPTER 25 SOLVING EQUATIONS BY ITERATIVE METHODS CHAPTER 5 SOLVING EQUATIONS BY ITERATIVE METHODS EXERCISE 104 Page 8 1. Find the positive root of the equation x + 3x 5 = 0, correct to 3 significant figures, using the method of bisection. Let f(x) =

Διαβάστε περισσότερα

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

Partial Differential Equations in Biology The boundary element method. March 26, 2013 The boundary element method March 26, 203 Introduction and notation The problem: u = f in D R d u = ϕ in Γ D u n = g on Γ N, where D = Γ D Γ N, Γ D Γ N = (possibly, Γ D = [Neumann problem] or Γ N = [Dirichlet

Διαβάστε περισσότερα

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

Lecture 2: Dirac notation and a review of linear algebra Read Sakurai chapter 1, Baym chatper 3 Lecture 2: Dirac notation and a review of linear algebra Read Sakurai chapter 1, Baym chatper 3 1 State vector space and the dual space Space of wavefunctions The space of wavefunctions is the set of all

Διαβάστε περισσότερα

SCHOOL OF MATHEMATICAL SCIENCES G11LMA Linear Mathematics Examination Solutions

SCHOOL OF MATHEMATICAL SCIENCES G11LMA Linear Mathematics Examination Solutions SCHOOL OF MATHEMATICAL SCIENCES GLMA Linear Mathematics 00- Examination Solutions. (a) i. ( + 5i)( i) = (6 + 5) + (5 )i = + i. Real part is, imaginary part is. (b) ii. + 5i i ( + 5i)( + i) = ( i)( + i)

Διαβάστε περισσότερα

Jesse Maassen and Mark Lundstrom Purdue University November 25, 2013

Jesse Maassen and Mark Lundstrom Purdue University November 25, 2013 Notes on Average Scattering imes and Hall Factors Jesse Maassen and Mar Lundstrom Purdue University November 5, 13 I. Introduction 1 II. Solution of the BE 1 III. Exercises: Woring out average scattering

Διαβάστε περισσότερα

Dark matter from Dark Energy-Baryonic Matter Couplings

Dark matter from Dark Energy-Baryonic Matter Couplings Dark matter from Dark Energy-Baryonic Matter Coulings Alejandro Avilés 1,2 1 Instituto de Ciencias Nucleares, UNAM, México 2 Instituto Nacional de Investigaciones Nucleares (ININ) México January 10, 2010

Διαβάστε περισσότερα

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

Απόκριση σε Μοναδιαία Ωστική Δύναμη (Unit Impulse) Απόκριση σε Δυνάμεις Αυθαίρετα Μεταβαλλόμενες με το Χρόνο. Απόστολος Σ. Απόκριση σε Δυνάμεις Αυθαίρετα Μεταβαλλόμενες με το Χρόνο The time integral of a force is referred to as impulse, is determined by and is obtained from: Newton s 2 nd Law of motion states that the action

Διαβάστε περισσότερα

Second Order Partial Differential Equations

Second Order Partial Differential Equations Chapter 7 Second Order Partial Differential Equations 7.1 Introduction A second order linear PDE in two independent variables (x, y Ω can be written as A(x, y u x + B(x, y u xy + C(x, y u u u + D(x, y

Διαβάστε περισσότερα

Inverse trigonometric functions & General Solution of Trigonometric Equations. ------------------ ----------------------------- -----------------

Inverse trigonometric functions & General Solution of Trigonometric Equations. ------------------ ----------------------------- ----------------- Inverse trigonometric functions & General Solution of Trigonometric Equations. 1. Sin ( ) = a) b) c) d) Ans b. Solution : Method 1. Ans a: 17 > 1 a) is rejected. w.k.t Sin ( sin ) = d is rejected. If sin

Διαβάστε περισσότερα

Space-Time Symmetries

Space-Time Symmetries Chapter Space-Time Symmetries In classical fiel theory any continuous symmetry of the action generates a conserve current by Noether's proceure. If the Lagrangian is not invariant but only shifts by a

Διαβάστε περισσότερα

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

Chapter 6: Systems of Linear Differential. be continuous functions on the interval Chapter 6: Systems of Linear Differential Equations Let a (t), a 2 (t),..., a nn (t), b (t), b 2 (t),..., b n (t) be continuous functions on the interval I. The system of n first-order differential equations

Διαβάστε περισσότερα

Srednicki Chapter 55

Srednicki Chapter 55 Srednicki Chapter 55 QFT Problems & Solutions A. George August 3, 03 Srednicki 55.. Use equations 55.3-55.0 and A i, A j ] = Π i, Π j ] = 0 (at equal times) to verify equations 55.-55.3. This is our third

Διαβάστε περισσότερα

Symmetric Stress-Energy Tensor

Symmetric Stress-Energy Tensor Chapter 3 Symmetric Stress-Energy ensor We noticed that Noether s conserved currents are arbitrary up to the addition of a divergence-less field. Exploiting this freedom the canonical stress-energy tensor

Διαβάστε περισσότερα

The Simply Typed Lambda Calculus

The Simply Typed Lambda Calculus Type Inference Instead of writing type annotations, can we use an algorithm to infer what the type annotations should be? That depends on the type system. For simple type systems the answer is yes, and

Διαβάστε περισσότερα

EE512: Error Control Coding

EE512: Error Control Coding EE512: Error Control Coding Solution for Assignment on Finite Fields February 16, 2007 1. (a) Addition and Multiplication tables for GF (5) and GF (7) are shown in Tables 1 and 2. + 0 1 2 3 4 0 0 1 2 3

Διαβάστε περισσότερα

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

= {{D α, D α }, D α }. = [D α, 4iσ µ α α D α µ ] = 4iσ µ α α [Dα, D α ] µ. PHY 396 T: SUSY Solutions for problem set #1. Problem 2(a): First of all, [D α, D 2 D α D α ] = {D α, D α }D α D α {D α, D α } = {D α, D α }D α + D α {D α, D α } (S.1) = {{D α, D α }, D α }. Second, {D

Διαβάστε περισσότερα

wave energy Superposition of linear plane progressive waves Marine Hydrodynamics Lecture Oblique Plane Waves:

wave energy Superposition of linear plane progressive waves Marine Hydrodynamics Lecture Oblique Plane Waves: 3.0 Marine Hydrodynamics, Fall 004 Lecture 0 Copyriht c 004 MIT - Department of Ocean Enineerin, All rihts reserved. 3.0 - Marine Hydrodynamics Lecture 0 Free-surface waves: wave enery linear superposition,

Διαβάστε περισσότερα

Homework 8 Model Solution Section

Homework 8 Model Solution Section MATH 004 Homework Solution Homework 8 Model Solution Section 14.5 14.6. 14.5. Use the Chain Rule to find dz where z cosx + 4y), x 5t 4, y 1 t. dz dx + dy y sinx + 4y)0t + 4) sinx + 4y) 1t ) 0t + 4t ) sinx

Διαβάστε περισσότερα

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)

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) 1. MATH43 String Theory Solutions 4 x = 0 τ = fs). 1) = = f s) ) x = x [f s)] + f s) 3) equation of motion is x = 0 if an only if f s) = 0 i.e. fs) = As + B with A, B constants. i.e. allowe reparametrisations

Διαβάστε περισσότερα

Finite Field Problems: Solutions

Finite Field Problems: Solutions Finite Field Problems: Solutions 1. Let f = x 2 +1 Z 11 [x] and let F = Z 11 [x]/(f), a field. Let Solution: F =11 2 = 121, so F = 121 1 = 120. The possible orders are the divisors of 120. Solution: The

Διαβάστε περισσότερα

6.4 Superposition of Linear Plane Progressive Waves

6.4 Superposition of Linear Plane Progressive Waves .0 - Marine Hydrodynamics, Spring 005 Lecture.0 - Marine Hydrodynamics Lecture 6.4 Superposition of Linear Plane Progressive Waves. Oblique Plane Waves z v k k k z v k = ( k, k z ) θ (Looking up the y-ais

Διαβάστε περισσότερα

Differential equations

Differential equations Differential equations Differential equations: An equation inoling one dependent ariable and its deriaties w. r. t one or more independent ariables is called a differential equation. Order of differential

Διαβάστε περισσότερα

1 String with massive end-points

1 String with massive end-points 1 String with massive end-points Πρόβλημα 5.11:Θεωρείστε μια χορδή μήκους, τάσης T, με δύο σημειακά σωματίδια στα άκρα της, το ένα μάζας m, και το άλλο μάζας m. α) Μελετώντας την κίνηση των άκρων βρείτε

Διαβάστε περισσότερα

Major Concepts. Multiphase Equilibrium Stability Applications to Phase Equilibrium. Two-Phase Coexistence

Major Concepts. Multiphase Equilibrium Stability Applications to Phase Equilibrium. Two-Phase Coexistence Major Concepts Multiphase Equilibrium Stability Applications to Phase Equilibrium Phase Rule Clausius-Clapeyron Equation Special case of Gibbs-Duhem wo-phase Coexistence Criticality Metastability Spinodal

Διαβάστε περισσότερα

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

forms This gives Remark 1. How to remember the above formulas: Substituting these into the equation we obtain with Week 03: C lassification of S econd- Order L inear Equations In last week s lectures we have illustrated how to obtain the general solutions of first order PDEs using the method of characteristics. We

Διαβάστε περισσότερα

Reminders: linear functions

Reminders: linear functions Reminders: linear functions Let U and V be vector spaces over the same field F. Definition A function f : U V is linear if for every u 1, u 2 U, f (u 1 + u 2 ) = f (u 1 ) + f (u 2 ), and for every u U

Διαβάστε περισσότερα

Geodesic Equations for the Wormhole Metric

Geodesic Equations for the Wormhole Metric Geodesic Equations for the Wormhole Metric Dr R Herman Physics & Physical Oceanography, UNCW February 14, 2018 The Wormhole Metric Morris and Thorne wormhole metric: [M S Morris, K S Thorne, Wormholes

Διαβάστε περισσότερα

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

3.4 SUM AND DIFFERENCE FORMULAS. NOTE: cos(α+β) cos α + cos β cos(α-β) cos α -cos β 3.4 SUM AND DIFFERENCE FORMULAS Page Theorem cos(αβ cos α cos β -sin α cos(α-β cos α cos β sin α NOTE: cos(αβ cos α cos β cos(α-β cos α -cos β Proof of cos(α-β cos α cos β sin α Let s use a unit circle

Διαβάστε περισσότερα

Dr. D. Dinev, Department of Structural Mechanics, UACEG

Dr. D. Dinev, Department of Structural Mechanics, UACEG Lecture 4 Material behavior: Constitutive equations Field of the game Print version Lecture on Theory of lasticity and Plasticity of Dr. D. Dinev, Department of Structural Mechanics, UACG 4.1 Contents

Διαβάστε περισσότερα

Section 8.3 Trigonometric Equations

Section 8.3 Trigonometric Equations 99 Section 8. Trigonometric Equations Objective 1: Solve Equations Involving One Trigonometric Function. In this section and the next, we will exple how to solving equations involving trigonometric functions.

Διαβάστε περισσότερα

[Note] Geodesic equation for scalar, vector and tensor perturbations

[Note] Geodesic equation for scalar, vector and tensor perturbations [Note] Geodesic equation for scalar, vector and tensor perturbations Toshiya Namikawa 212 1 Curl mode induced by vector and tensor perturbation 1.1 Metric Perturbation and Affine Connection The line element

Διαβάστε περισσότερα

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

Chapter 6: Systems of Linear Differential. be continuous functions on the interval Chapter 6: Systems of Linear Differential Equations Let a (t), a 2 (t),..., a nn (t), b (t), b 2 (t),..., b n (t) be continuous functions on the interval I. The system of n first-order differential equations

Διαβάστε περισσότερα

4.6 Autoregressive Moving Average Model ARMA(1,1)

4.6 Autoregressive Moving Average Model ARMA(1,1) 84 CHAPTER 4. STATIONARY TS MODELS 4.6 Autoregressive Moving Average Model ARMA(,) This section is an introduction to a wide class of models ARMA(p,q) which we will consider in more detail later in this

Διαβάστε περισσότερα

Solutions to Exercise Sheet 5

Solutions to Exercise Sheet 5 Solutions to Eercise Sheet 5 jacques@ucsd.edu. Let X and Y be random variables with joint pdf f(, y) = 3y( + y) where and y. Determine each of the following probabilities. Solutions. a. P (X ). b. P (X

Διαβάστε περισσότερα

Areas and Lengths in Polar Coordinates

Areas and Lengths in Polar Coordinates Kiryl Tsishchanka Areas and Lengths in Polar Coordinates In this section we develop the formula for the area of a region whose boundary is given by a polar equation. We need to use the formula for the

Διαβάστε περισσότερα

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

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 Lecture 12: Introduction to Analytical Mechanics of Continuous Systems Lagrangian Density for Continuous Systems The kinetic and potential energies as T = 1 2 i η2 i (1 and V = 1 2 i+1 η i 2, i (2 where

Διαβάστε περισσότερα

D Alembert s Solution to the Wave Equation

D Alembert s Solution to the Wave Equation D Alembert s Solution to the Wave Equation MATH 467 Partial Differential Equations J. Robert Buchanan Department of Mathematics Fall 2018 Objectives In this lesson we will learn: a change of variable technique

Διαβάστε περισσότερα

Concrete Mathematics Exercises from 30 September 2016

Concrete Mathematics Exercises from 30 September 2016 Concrete Mathematics Exercises from 30 September 2016 Silvio Capobianco Exercise 1.7 Let H(n) = J(n + 1) J(n). Equation (1.8) tells us that H(2n) = 2, and H(2n+1) = J(2n+2) J(2n+1) = (2J(n+1) 1) (2J(n)+1)

Διαβάστε περισσότερα

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

Exercises 10. Find a fundamental matrix of the given system of equations. Also find the fundamental matrix Φ(t) satisfying Φ(0) = I. 1. Exercises 0 More exercises are available in Elementary Differential Equations. If you have a problem to solve any of them, feel free to come to office hour. Problem Find a fundamental matrix of the given

Διαβάστε περισσότερα

Example Sheet 3 Solutions

Example Sheet 3 Solutions Example Sheet 3 Solutions. i Regular Sturm-Liouville. ii Singular Sturm-Liouville mixed boundary conditions. iii Not Sturm-Liouville ODE is not in Sturm-Liouville form. iv Regular Sturm-Liouville note

Διαβάστε περισσότερα

DESIGN OF MACHINERY SOLUTION MANUAL h in h 4 0.

DESIGN OF MACHINERY SOLUTION MANUAL h in h 4 0. DESIGN OF MACHINERY SOLUTION MANUAL -7-1! PROBLEM -7 Statement: Design a double-dwell cam to move a follower from to 25 6, dwell for 12, fall 25 and dwell for the remader The total cycle must take 4 sec

Διαβάστε περισσότερα

Areas and Lengths in Polar Coordinates

Areas and Lengths in Polar Coordinates Kiryl Tsishchanka Areas and Lengths in Polar Coordinates In this section we develop the formula for the area of a region whose boundary is given by a polar equation. We need to use the formula for the

Διαβάστε περισσότερα

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

Econ 2110: Fall 2008 Suggested Solutions to Problem Set 8  questions or comments to Dan Fetter 1 Eon : Fall 8 Suggested Solutions to Problem Set 8 Email questions or omments to Dan Fetter Problem. Let X be a salar with density f(x, θ) (θx + θ) [ x ] with θ. (a) Find the most powerful level α test

Διαβάστε περισσότερα

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

Every set of first-order formulas is equivalent to an independent set Every set of first-order formulas is equivalent to an independent set May 6, 2008 Abstract A set of first-order formulas, whatever the cardinality of the set of symbols, is equivalent to an independent

Διαβάστε περισσότερα

Statistical Inference I Locally most powerful tests

Statistical Inference I Locally most powerful tests Statistical Inference I Locally most powerful tests Shirsendu Mukherjee Department of Statistics, Asutosh College, Kolkata, India. shirsendu st@yahoo.co.in So far we have treated the testing of one-sided

Διαβάστε περισσότερα

derivation of the Laplacian from rectangular to spherical coordinates

derivation of the Laplacian from rectangular to spherical coordinates derivation of the Laplacian from rectangular to spherical coordinates swapnizzle 03-03- :5:43 We begin by recognizing the familiar conversion from rectangular to spherical coordinates (note that φ is used

Διαβάστε περισσότερα

PARTIAL NOTES for 6.1 Trigonometric Identities

PARTIAL NOTES for 6.1 Trigonometric Identities PARTIAL NOTES for 6.1 Trigonometric Identities tanθ = sinθ cosθ cotθ = cosθ sinθ BASIC IDENTITIES cscθ = 1 sinθ secθ = 1 cosθ cotθ = 1 tanθ PYTHAGOREAN IDENTITIES sin θ + cos θ =1 tan θ +1= sec θ 1 + cot

Διαβάστε περισσότερα

Forced Pendulum Numerical approach

Forced Pendulum Numerical approach Numerical approach UiO April 8, 2014 Physical problem and equation We have a pendulum of length l, with mass m. The pendulum is subject to gravitation as well as both a forcing and linear resistance force.

Διαβάστε περισσότερα

CRASH COURSE IN PRECALCULUS

CRASH COURSE IN PRECALCULUS CRASH COURSE IN PRECALCULUS Shiah-Sen Wang The graphs are prepared by Chien-Lun Lai Based on : Precalculus: Mathematics for Calculus by J. Stuwart, L. Redin & S. Watson, 6th edition, 01, Brooks/Cole Chapter

Διαβάστε περισσότερα

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

b. Use the parametrization from (a) to compute the area of S a as S a ds. Be sure to substitute for ds! MTH U341 urface Integrals, tokes theorem, the divergence theorem To be turned in Wed., Dec. 1. 1. Let be the sphere of radius a, x 2 + y 2 + z 2 a 2. a. Use spherical coordinates (with ρ a) to parametrize.

Διαβάστε περισσότερα

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

ANSWERSHEET (TOPIC = DIFFERENTIAL CALCULUS) COLLECTION #2. h 0 h h 0 h h 0 ( ) g k = g 0 + g 1 + g g 2009 =? Teko Classes IITJEE/AIEEE Maths by SUHAAG SIR, Bhopal, Ph (0755) 3 00 000 www.tekoclasses.com ANSWERSHEET (TOPIC DIFFERENTIAL CALCULUS) COLLECTION # Question Type A.Single Correct Type Q. (A) Sol least

Διαβάστε περισσότερα

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

HOMEWORK 4 = G. In order to plot the stress versus the stretch we define a normalized stretch: HOMEWORK 4 Problem a For the fast loading case, we want to derive the relationship between P zz and λ z. We know that the nominal stress is expressed as: P zz = ψ λ z where λ z = λ λ z. Therefore, applying

Διαβάστε περισσότερα

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

Approximation of distance between locations on earth given by latitude and longitude Approximation of distance between locations on earth given by latitude and longitude Jan Behrens 2012-12-31 In this paper we shall provide a method to approximate distances between two points on earth

Διαβάστε περισσότερα

( ) 2 and compare to M.

( ) 2 and compare to M. Problems and Solutions for Section 4.2 4.9 through 4.33) 4.9 Calculate the square root of the matrix 3!0 M!0 8 Hint: Let M / 2 a!b ; calculate M / 2!b c ) 2 and compare to M. Solution: Given: 3!0 M!0 8

Διαβάστε περισσότερα

Problem Set 3: Solutions

Problem Set 3: Solutions CMPSCI 69GG Applied Information Theory Fall 006 Problem Set 3: Solutions. [Cover and Thomas 7.] a Define the following notation, C I p xx; Y max X; Y C I p xx; Ỹ max I X; Ỹ We would like to show that C

Διαβάστε περισσότερα

General 2 2 PT -Symmetric Matrices and Jordan Blocks 1

General 2 2 PT -Symmetric Matrices and Jordan Blocks 1 General 2 2 PT -Symmetric Matrices and Jordan Blocks 1 Qing-hai Wang National University of Singapore Quantum Physics with Non-Hermitian Operators Max-Planck-Institut für Physik komplexer Systeme Dresden,

Διαβάστε περισσότερα

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

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 Appendix A Curvilinear coordinates A. Lamé coefficients Consider set of equations ξ i = ξ i x,x 2,x 3, i =,2,3 where ξ,ξ 2,ξ 3 independent, single-valued and continuous x,x 2,x 3 : coordinates of point

Διαβάστε περισσότερα

Appendix to On the stability of a compressible axisymmetric rotating flow in a pipe. By Z. Rusak & J. H. Lee

Appendix to On the stability of a compressible axisymmetric rotating flow in a pipe. By Z. Rusak & J. H. Lee Appendi to On the stability of a compressible aisymmetric rotating flow in a pipe By Z. Rusak & J. H. Lee Journal of Fluid Mechanics, vol. 5 4, pp. 5 4 This material has not been copy-edited or typeset

Διαβάστε περισσότερα

6.3 Forecasting ARMA processes

6.3 Forecasting ARMA processes 122 CHAPTER 6. ARMA MODELS 6.3 Forecasting ARMA processes The purpose of forecasting is to predict future values of a TS based on the data collected to the present. In this section we will discuss a linear

Διαβάστε περισσότερα

C.S. 430 Assignment 6, Sample Solutions

C.S. 430 Assignment 6, Sample Solutions C.S. 430 Assignment 6, Sample Solutions Paul Liu November 15, 2007 Note that these are sample solutions only; in many cases there were many acceptable answers. 1 Reynolds Problem 10.1 1.1 Normal-order

Διαβάστε περισσότερα

Exam to General Relativity (Winter term 2011/2012) Prof. V. F. Mukhanov, LMU München Solution! Problem: 1a 1b 1c 1d 1e

Exam to General Relativity (Winter term 2011/2012) Prof. V. F. Mukhanov, LMU München Solution! Problem: 1a 1b 1c 1d 1e Exam to General Relativity Winter term 211/212 Prof. V. F. Mukhanov, LMU München 9.2.212 Solution! Problem: 1a 1b 1c 1d 1e 2 3 4 5 Points: 1 Short Questions In the following questions, mark the correct

Διαβάστε περισσότερα

Dual null formulation (and its Quasi-Spherical version)

Dual null formulation (and its Quasi-Spherical version) filename= dualnull.tex 2003-0403 Hisaaki Shinkai hshinkai@postman.riken.go.jp Dual null formulation (and its Quasi-Spherical version This note is for actual coding of the double null formulation by Hayward

Διαβάστε περισσότερα

Ordinal Arithmetic: Addition, Multiplication, Exponentiation and Limit

Ordinal Arithmetic: Addition, Multiplication, Exponentiation and Limit Ordinal Arithmetic: Addition, Multiplication, Exponentiation and Limit Ting Zhang Stanford May 11, 2001 Stanford, 5/11/2001 1 Outline Ordinal Classification Ordinal Addition Ordinal Multiplication Ordinal

Διαβάστε περισσότερα

3+1 Splitting of the Generalized Harmonic Equations

3+1 Splitting of the Generalized Harmonic Equations 3+1 Splitting of the Generalized Harmonic Equations David Brown North Carolina State University EGM June 2011 Numerical Relativity Interpret general relativity as an initial value problem: Split spacetime

Διαβάστε περισσότερα

Numerical Analysis FMN011

Numerical Analysis FMN011 Numerical Analysis FMN011 Carmen Arévalo Lund University carmen@maths.lth.se Lecture 12 Periodic data A function g has period P if g(x + P ) = g(x) Model: Trigonometric polynomial of order M T M (x) =

Διαβάστε περισσότερα

4.4 Superposition of Linear Plane Progressive Waves

4.4 Superposition of Linear Plane Progressive Waves .0 Marine Hydrodynamics, Fall 08 Lecture 6 Copyright c 08 MIT - Department of Mechanical Engineering, All rights reserved..0 - Marine Hydrodynamics Lecture 6 4.4 Superposition of Linear Plane Progressive

Διαβάστε περισσότερα

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.

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. Chemistry 362 Dr Jean M Standard Problem Set 9 Solutions The ˆ L 2 operator is defined as Verify that the angular wavefunction Y θ,φ) Also verify that the eigenvalue is given by 2! 2 & L ˆ 2! 2 2 θ 2 +

Διαβάστε περισσότερα

Lifting Entry (continued)

Lifting Entry (continued) ifting Entry (continued) Basic planar dynamics of motion, again Yet another equilibrium glide Hypersonic phugoid motion Planar state equations MARYAN 1 01 avid. Akin - All rights reserved http://spacecraft.ssl.umd.edu

Διαβάστε περισσότερα

Non-Gaussianity from Lifshitz Scalar

Non-Gaussianity from Lifshitz Scalar COSMO/CosPA 200 September 27, 200 Non-Gaussianity from Lifshitz Scalar Takeshi Kobayashi (Tokyo U.) based on: arxiv:008.406 with Keisuke Izumi, Shinji Mukohyama Lifshitz scalars with z=3 obtain super-horizon,

Διαβάστε περισσότερα

ST5224: Advanced Statistical Theory II

ST5224: Advanced Statistical Theory II ST5224: Advanced Statistical Theory II 2014/2015: Semester II Tutorial 7 1. Let X be a sample from a population P and consider testing hypotheses H 0 : P = P 0 versus H 1 : P = P 1, where P j is a known

Διαβάστε περισσότερα

Second Order RLC Filters

Second Order RLC Filters ECEN 60 Circuits/Electronics Spring 007-0-07 P. Mathys Second Order RLC Filters RLC Lowpass Filter A passive RLC lowpass filter (LPF) circuit is shown in the following schematic. R L C v O (t) Using phasor

Διαβάστε περισσότερα

8.324 Relativistic Quantum Field Theory II

8.324 Relativistic Quantum Field Theory II 8.324 Relativistic Quantum Field Theory II MIT OpenCourseWare Lecture Notes Hong Liu, Fall 200 Lecture 2 3: GENERAL ASPECTS OF QUANTUM ELECTRODYNAMICS 3.: RENORMALIZED LAGRANGIAN Consider the Lagrangian

Διαβάστε περισσότερα

Matrices and Determinants

Matrices and Determinants Matrices and Determinants SUBJECTIVE PROBLEMS: Q 1. For what value of k do the following system of equations possess a non-trivial (i.e., not all zero) solution over the set of rationals Q? x + ky + 3z

Διαβάστε περισσότερα

ω ω ω ω ω ω+2 ω ω+2 + ω ω ω ω+2 + ω ω+1 ω ω+2 2 ω ω ω ω ω ω ω ω+1 ω ω2 ω ω2 + ω ω ω2 + ω ω ω ω2 + ω ω+1 ω ω2 + ω ω+1 + ω ω ω ω2 + ω

ω ω ω ω ω ω+2 ω ω+2 + ω ω ω ω+2 + ω ω+1 ω ω+2 2 ω ω ω ω ω ω ω ω+1 ω ω2 ω ω2 + ω ω ω2 + ω ω ω ω2 + ω ω+1 ω ω2 + ω ω+1 + ω ω ω ω2 + ω 0 1 2 3 4 5 6 ω ω + 1 ω + 2 ω + 3 ω + 4 ω2 ω2 + 1 ω2 + 2 ω2 + 3 ω3 ω3 + 1 ω3 + 2 ω4 ω4 + 1 ω5 ω 2 ω 2 + 1 ω 2 + 2 ω 2 + ω ω 2 + ω + 1 ω 2 + ω2 ω 2 2 ω 2 2 + 1 ω 2 2 + ω ω 2 3 ω 3 ω 3 + 1 ω 3 + ω ω 3 +

Διαβάστε περισσότερα

From the finite to the transfinite: Λµ-terms and streams

From the finite to the transfinite: Λµ-terms and streams From the finite to the transfinite: Λµ-terms and streams WIR 2014 Fanny He f.he@bath.ac.uk Alexis Saurin alexis.saurin@pps.univ-paris-diderot.fr 12 July 2014 The Λµ-calculus Syntax of Λµ t ::= x λx.t (t)u

Διαβάστε περισσότερα

Cosmology with non-minimal derivative coupling

Cosmology with non-minimal derivative coupling Kazan Federal University, Kazan, Russia 8th Spontaneous Workshop on Cosmology Institut d Etude Scientifique de Cargèse, Corsica May 13, 2014 Plan Plan Scalar fields: minimal and nonminimal coupling to

Διαβάστε περισσότερα

Tutorial problem set 6,

Tutorial problem set 6, GENERAL RELATIVITY Tutorial problem set 6, 01.11.2013. SOLUTIONS PROBLEM 1 Killing vectors. a Show that the commutator of two Killing vectors is a Killing vector. Show that a linear combination with constant

Διαβάστε περισσότερα

Homework 3 Solutions

Homework 3 Solutions Homework 3 Solutions Igor Yanovsky (Math 151A TA) Problem 1: Compute the absolute error and relative error in approximations of p by p. (Use calculator!) a) p π, p 22/7; b) p π, p 3.141. Solution: For

Διαβάστε περισσότερα

Math221: HW# 1 solutions

Math221: HW# 1 solutions Math: HW# solutions Andy Royston October, 5 7.5.7, 3 rd Ed. We have a n = b n = a = fxdx = xdx =, x cos nxdx = x sin nx n sin nxdx n = cos nx n = n n, x sin nxdx = x cos nx n + cos nxdx n cos n = + sin

Διαβάστε περισσότερα

SOLUTIONS TO MATH38181 EXTREME VALUES AND FINANCIAL RISK EXAM

SOLUTIONS TO MATH38181 EXTREME VALUES AND FINANCIAL RISK EXAM SOLUTIONS TO MATH38181 EXTREME VALUES AND FINANCIAL RISK EXAM Solutions to Question 1 a) The cumulative distribution function of T conditional on N n is Pr T t N n) Pr max X 1,..., X N ) t N n) Pr max

Διαβάστε περισσότερα

( y) Partial Differential Equations

( y) Partial Differential Equations Partial Dierential Equations Linear P.D.Es. contains no owers roducts o the deendent variables / an o its derivatives can occasionall be solved. Consider eamle ( ) a (sometimes written as a ) we can integrate

Διαβάστε περισσότερα

Other Test Constructions: Likelihood Ratio & Bayes Tests

Other Test Constructions: Likelihood Ratio & Bayes Tests Other Test Constructions: Likelihood Ratio & Bayes Tests Side-Note: So far we have seen a few approaches for creating tests such as Neyman-Pearson Lemma ( most powerful tests of H 0 : θ = θ 0 vs H 1 :

Διαβάστε περισσότερα

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

1. (a) (5 points) Find the unit tangent and unit normal vectors T and N to the curve. r(t) = 3cost, 4t, 3sint 1. a) 5 points) Find the unit tangent and unit normal vectors T and N to the curve at the point P, π, rt) cost, t, sint ). b) 5 points) Find curvature of the curve at the point P. Solution: a) r t) sint,,

Διαβάστε περισσότερα

NonEquilibrium Thermodynamics of Flowing Systems: 2

NonEquilibrium Thermodynamics of Flowing Systems: 2 *Following the development in Beris and Edwards, 1994, Section 9.2 NonEquilibrium Thermodynamics of Flowing Systems: 2 Antony N. Beris Schedule: Multiscale Modeling and Simulation of Complex Fluids Center

Διαβάστε περισσότερα

Congruence Classes of Invertible Matrices of Order 3 over F 2

Congruence Classes of Invertible Matrices of Order 3 over F 2 International Journal of Algebra, Vol. 8, 24, no. 5, 239-246 HIKARI Ltd, www.m-hikari.com http://dx.doi.org/.2988/ija.24.422 Congruence Classes of Invertible Matrices of Order 3 over F 2 Ligong An and

Διαβάστε περισσότερα

Right Rear Door. Let's now finish the door hinge saga with the right rear door

Right Rear Door. Let's now finish the door hinge saga with the right rear door Right Rear Door Let's now finish the door hinge saga with the right rear door You may have been already guessed my steps, so there is not much to describe in detail. Old upper one file:///c /Documents

Διαβάστε περισσότερα

Lanczos and biorthogonalization methods for eigenvalues and eigenvectors of matrices

Lanczos and biorthogonalization methods for eigenvalues and eigenvectors of matrices Lanzos and iorthogonalization methods for eigenvalues and eigenvetors of matries rolem formulation Many prolems are redued to solving the following system: x x where is an unknown numer А a matrix n n

Διαβάστε περισσότερα

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

You may not start to read the questions printed on the subsequent pages until instructed to do so by the Invigilator. MATHEMATICAL TRIPOS Part III Monday 6 June, 2005 9 to 12 PAPER 60 GENERAL RELATIVITY Attempt THREE questions. There are FOUR questions in total. The questions carry equal weight. The signature is ( + ),

Διαβάστε περισσότερα

Tridiagonal matrices. Gérard MEURANT. October, 2008

Tridiagonal matrices. Gérard MEURANT. October, 2008 Tridiagonal matrices Gérard MEURANT October, 2008 1 Similarity 2 Cholesy factorizations 3 Eigenvalues 4 Inverse Similarity Let α 1 ω 1 β 1 α 2 ω 2 T =......... β 2 α 1 ω 1 β 1 α and β i ω i, i = 1,...,

Διαβάστε περισσότερα

Fourier Series. MATH 211, Calculus II. J. Robert Buchanan. Spring Department of Mathematics

Fourier Series. MATH 211, Calculus II. J. Robert Buchanan. Spring Department of Mathematics Fourier Series MATH 211, Calculus II J. Robert Buchanan Department of Mathematics Spring 2018 Introduction Not all functions can be represented by Taylor series. f (k) (c) A Taylor series f (x) = (x c)

Διαβάστε περισσότερα

Relativistic particle dynamics and deformed symmetry

Relativistic particle dynamics and deformed symmetry Relativistic particle dynamics and deformed Poincare symmetry Department for Theoretical Physics, Ivan Franko Lviv National University XXXIII Max Born Symposium, Wroclaw Outline Lorentz-covariant deformed

Διαβάστε περισσότερα

CHAPTER 48 APPLICATIONS OF MATRICES AND DETERMINANTS

CHAPTER 48 APPLICATIONS OF MATRICES AND DETERMINANTS CHAPTER 48 APPLICATIONS OF MATRICES AND DETERMINANTS EXERCISE 01 Page 545 1. Use matrices to solve: 3x + 4y x + 5y + 7 3x + 4y x + 5y 7 Hence, 3 4 x 0 5 y 7 The inverse of 3 4 5 is: 1 5 4 1 5 4 15 8 3

Διαβάστε περισσότερα

Overview. Transition Semantics. Configurations and the transition relation. Executions and computation

Overview. Transition Semantics. Configurations and the transition relation. Executions and computation Overview Transition Semantics Configurations and the transition relation Executions and computation Inference rules for small-step structural operational semantics for the simple imperative language Transition

Διαβάστε περισσότερα

Sixth lecture September 21, 2006

Sixth lecture September 21, 2006 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????

Διαβάστε περισσότερα