Dynamics of Collisionless Systems Summer Semester 2005, ETH Zürich

Dynamics of Collisionless Systems Summer Semester 2005, ETH Zürich

Dynamics of Collisionless Systems Summer Semester 2005, ETH Zürich Frank C. van den Bosch Useful Information TEXTBOOK: Galactic Dynamics, Binney & Tremaine Princeton University Press Highly Recommended WEBPAGE: http://www.exp-astro.phys.ethz.ch/ vdbosch/galdyn.html LECTURES: Wed, 14.45-16.30, HPP H2. Lectures will be in English EXERSIZE CLASSES: to be determined HOMEWORK ASSIGNMENTS: every other week EXAM: Verbal (German possible), July/August 2005 GRADING: exam (2=3) plus homework assignments (1=3) TEACHER: Frank van den Bosch ([email protected]), HPT G6 SUBSTITUTE TEACHERS: Peder Norberg ([email protected]), HPF G3.1 Savvas Koushiappas ([email protected]), HPT G3 Outline Lecture 1: Introduction & General Overview Lecture 2: Cancelled Lecture 3: Potential Theory Lecture 4: Orbits I (Introduction to Orbit Theory) Lecture 5: Orbits II (Resonances) Lecture 6: Orbits III (Phase-Space Structure of Orbits) Lecture 7: Equilibrium Systems I (Jeans Equations) Lecture 8: Equilibrium Systems II (Jeans Theorem in Spherical Systems) Lecture 9: Equilibrium Systems III (Jeans Theorem in Spheroidal Systems) Lecture 10: Relaxation & Virialization (Violent Relaxation & Phase Mixing) Lecture 11: Wave Mechanics of Disks (Spiral Structure & Bars) Lecture 12: Collisions between Collisionless Systems (Dynamical Friction) Lecture 13: Kinetic Theory (Fokker-Planck Eq. & Core Collapse) Lecture 14: Cancelled Summary of Vector Calculus I A~ B~ = scalar = A~ B~ cos = A B (summation convention) · j j j j i i A~ B~ = vector = ~e A B (with the Levi-Civita Tensor) × ijk i j k ijk Useful to Remember A~ A~ = 0 × A~ B~ = B~ A~ × − × A~ (A~ B~ ) = 0 · × A~ (B~ C~ ) = B~ (C~ A~) = C~ (A~ B~ ) · × · × · × A~ (B~ C~ ) = B~ (A~ C~ ) C~ (A~ B~ ) × × · − · (A~ B~ ) (C~ D~ ) = (A~ C~ )(B~ D~ ) (A~ D~ )(B~ C~ ) × · × · · − · · ~ =vector operator= ( @ ; @ ; @ ) r @x @y @z ~ S = gradS = vector r ~ A~ = divA~ = scalar r · ~ A~ = curlA~ = vector r × Summary of Vector Calculus II 2 2 2 Laplacian: 2 = ~ ~ = scalar operator = @ + @ + @ r r · r @x2 @y2 @z2 2S = ~ (~ S) = scalar r r · r 2A~ = (~ ~ )A~ = vector r r · r ~ (~ A~) = 2A~ = vector r r · 6 r ~ (~ S) = 0 curl(gradS) = 0 r × r ~ (~ A~) = 0 div(curl A~) = 0 r · r × ~ (~ A~) = ~ (~ A~) 2A~ r × r × r r · − r ~ (ST ) = S ~ T + T ~ S r r r ~ (SA~) = S(~ A~) + A~ ~ S r · r · · r ~ (SA~) = S(~ A~) A~ ~ S r × r × − × r ~ (A~ B~ ) = B~ (~ A~) A~ (~ B~ ) r · × · r × − · r × Integral Theorems I Gradient Theorem: Let γ be a curve running from ~x0 to ~x1, d~l is the directed element of length along γ, and φ(~x) is a scalar field then: ~x1 ~x1 ~ φ d~l = dφ = φ(~x ) φ(~x ) r · 1 − 0 ~x0 ~x0 R R It follows that ~ φ d~l = 0 r · Divergence Theorem (Gauss’H Theorem): Let V be a 3D volume bounded by a 2D surface S, and let A~(~x) be a vector field, then: ~ A~ d3~x = A~ d2S~ V r · S · Curl Theorem (Stokes’R Theorem): LetRS be a 2D surface bounded by a 1D curve γ, and let A~(~x) be a vector field, then: (~ A~) d2S~ = A~ d~l S r × γ · R H Integral Theorems II NOTE: Since a conservative force F~ can always be written as the gradient of a scalar field φ, we have from the gradient theorem that F~ d~l = 0 · From the curl theorem we immediatelH y see that ~ F~ = 0 r × We immediately infer that a conservative force is curl free, and that the amount of work done (dW = F~ d~r) is independent of the path taken. · From the divergence theorem we infer that φ~ A~ d3~x = φA~ d2S~ A~ ~ φ d3x~ V r · S · − V · r R R R which is the three-dimensional analog of integration by parts u dv dx = d(uv) v du dx dx − dx R R R Curvi-Linear Coordinate Systems I In addition to the Cartesian coordinate system (x; y; z), we will often work with cylindrical (R; φ, z) or spherical (r; θ; φ) coordinate systems Let (q1; q2; q3) denote the coordinates of a point in an arbitrary coordinate system, defined by the metric tensor hij . The distance between (q1; q2; q3) and (q1 + dq1; q2 + dq2; q3 + dq3) is 2 ds = hij dqi dqj (summation convention) We will only consider orthogonal systems for which hij = 0 if i = j, so 2 2 2 6 that ds = hi dqi with @~x hi hii = ≡ j @qi j The differential vector is @~x @~x @~x d~x = dq1 + dq2 + dq3 @q1 @q2 @q3 The unit directional vectors are @~x @~x 1 @~x ~ei = = = @qi j @qi j hi @qi 3 so that d~x = hi dqi ~ei and d ~x = h1h2h3dq1dq2dq3. i P Curvi-Linear Coordinate Systems II The gradient: 1 @ ~ = ~ei r hi @qi The divergence: 1 @ @ @ ~ A~ = (h2h3A1) + (h3h1A2) + (h1h2A3) r · h1h2h3 @q1 @q2 @q3 h i The curl (only one component shown): 1 @ @ (~ A~)3 = (h2A2) (h1A1) r × h1h2 @q1 − @q2 h i The Laplacian: 1 @ h h @ @ h h @ @ h h @ 2 = 2 3 + 3 1 + 1 2 r h1h2h3 @q1 h1 @q1 @q2 h2 @q2 @q3 h3 @q3 h i Cylindrical Coordinates For cylindrical coordinates (R; φ, z) we have that x = R cos φ y = R sin φ z = z The scale factors of the metric are: hR = 1 hφ = R hz = 1 and the position vector is ~x = R~eR + z~ez Let A~ = AR~eR + Aφ~eφ + Az~ez an arbitrary vector, then A = A cos φ A sin φ R x − y A = A sin φ + A cos φ φ − x y Az = Az _ Velocity: ~v = R_ ~eR + R~eR + z_~ez = R_ ~eR + Rφ_~eφ + z_~ez Gradient & Laplacian: ~ A~ = 1 @ (RA ) + 1 @Aφ + @Az r · R @R R R @φ @z 2 2 2 = 1 @ R @ + 1 @ + @ r R @R @R R2 @φ2 @z2 Spherical Coordinates For spherical coordinates (r; θ; φ) we have that x = r sin θ cos φ y = r sin θ sin φ z = r cos θ The scale factors of the metric are: hr = 1 hθ = r hφ = r sin θ and the position vector is ~x = r~er Let A~ = Ar~er + Aθ~eθ + Aφ~eφ an arbitrary vector, then Ar = Ax sin θ cos φ + Ay sin θ sin φ + Az cos θ A = A cos θ cos φ + A cos θ sin φ A sin θ θ x y − z A = A sin φ + A cos φ φ − x y _ Velocity: ~v = r_~er + r~er = r_~er + rθ~_eθ + r sin θφ_~eφ Gradient & Laplacian: ~ A~ = 1 @ (r2A ) + 1 @ (sin θA ) + 1 @Aφ r · r2 @r r r sin θ @θ θ r sin θ @φ 2 2 = 1 @ r2 @ + 1 @ sin θ @φ + 1 @ r r2 @r @r r2 sin θ @θ @θ r2 sin2 θ @ 2 Introduction COLLISIONLESS DYNAMICS: The study of the motion of large numbers of point particles orbiting under the influence of their mutual self-gravity EAMPLES OF COLLISIONLESS SYSTEMS Galaxies (ellipticals & disk galaxies) N 106 1011 • ∼ − Globular clusters N 104 106 • ∼ − Galaxy clusters N 102 103 • ∼ − Cold Dark Matter haloes N 1050 • MAIN GOALS • Infer mass distribution from observed kinematics. Comparison with light distribution learn about dark matter and black holes ) • Understand observed structure of galaxies: 1. Galaxies formed this way learn about Galaxy Formation ) 2. Galaxies evolved this way learn about Stability of galaxies ) Newtonian Gravity Newton’s First Law: A body acted on by no forces moves with uniform velocity in a straight line Newton’s Second Law: ~ d~v dp~ (equation of motion) F = m dt = dt Newton’s Third Law: F~ = F~ (action = reaction) ij − ji m m Newton’s Law of Gravity: ~ i j Fij = G ~x ~x 3 (~xi ~xj ) − j i− j j − 11 2 2 9 1 2 1 G = 6:67 10− Nm kg− = 4:3 10− ( km s− ) M − Mpc × × Gravity is a conservative Force. This implies that: scalar field V (~x) (potential energy), so that F~ = ~ V (~x) • 9 −r The total energy E = 1 mv2 + V (~x) is conserved • 2 Gravity is a curl-free field: ~ F~ = 0 • r × Gravity is a central Force. This implies that: The moment about the center vanishes: ~r F~ = 0 • × ~ Angular momentum J~ = m~r ~v is conserved: ( dJ = ~r F~ = 0) • × dt × The Gravitational Potential Potential Energy: F~(~x) = ~ V (~x) −r Gravitational Potential: V (~x) Φ(~x) = m ~ Gravitational Field: ~g(~x) = F (~x) = ~ Φ(~x) m −r From now on F~ is the force per unit mass so that F~(~x) = ~ Φ(~x) −r For a point mass at : GM M x~0 Φ(~x) = ~x ~x − j − 0j 0 ρ(~x ) 3 For a density distribution : 0 ρ(~x) Φ(~x) = G ~x ~x d ~x0 − j − j R The density distribution ρ(~x) and gravitational potential Φ(~x) are related to each other by the Poisson Equation 2Φ = 4πGρ r For ρ = 0 this reduces to the Laplace equation: 2Φ = 0. r see B&T p.31 for derivation of Poisson Equation Gauss’s Theorem & Potential Theorem If we integrate the Poisson Equation, we obtain 4πG ρ d3x~ = 4πGM = 2Φ d3x~ = ~ Φd2~s V r S r R R R Gauss’s Theorem: ~ Φ d2~s = 4πGM S r Gauss’s Theorem statesRthat the integral of the normal component of the gravitational field [~g(~r) = ~ Φ] over any closed surface S is equal to 4πG r times the total mass enclosed by S. cf. Electrostatics: E~ ~n d2~s = Qint S · 0 R For a continuous density distribution ρ(~x) the total potential energy is: 1 3 W = 2 ρ(~x) Φ(~x) d ~x R (see B&T p.33 for derivation) NOTE: Here we follow B&T and use the symbol W instead of V .

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