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–1– Order of Magnitude Astrophysics - a.k.a. Astronomy 111 Photon Opacities in Matter If the cross section for the relevant process that scatters or absorbs radiation given by σ and the number density of scatters is n, then the mean free path of a photon is given by l = (nσ)−1 . In the case of radiation, it is conventional to define a quantity κ (called opacity) such that α ≡ nσ ≡ ρκ (1) where ρ is the mass density of the scatterers. The optical depth of a system of size R is defined to be τ ≡ αR = R . l (2) The opacity for the photons is provided mainly by three different processes: (1) scattering by free electrons; (2) the free-free absorption of photons, and (3) the bound-free transitions induced by matter by the photons that are passing through it. Electron Scattering The simplest case is the one in which the charged particle is accelerated by an electromagnetic wave that is incident upon it. Consider a charge q placed on an electromagnetic wave of amplitude E. The wave will induce an acceleration a ≈ (qE/m), causing the charge to radiate. The power radiated will be P= 2q2 a2 2q4 2 = E . 3c3 3m2 c3 (3) –2– Because the incident power in the electromagnetic wave is S = cE 2 /(4π), the scattering cross section (for electrons with m = me ) is P 8π q2 σT ≡ = S 3 me c2 !2 ≈ 6.7 × 10−25 cm−2 , (4) which is the Thomson scattering cross section. This cross section governs the basic scattering phenomena between charged particles and radiation. The corresponding mean free path for photons through a plasma is lT = (ne σT )−1 , and the Thomson scattering opacity, defined to be κ ≡ (ne σT /ρ), is ne κT = np ! ! σT = 0.4 cm2 g−1 mp (5) for ionized hydrogen with ne = n p . Random Walks A particular useful way of looking at scattering, which leads to important order-of-magnitude estimates, is by means of random walks. It is possible to view the processes of absorption, emission, and propagation in probabilistic terms for a single photon rather than the average behavior of large number of photons. For example, the exponential decay of a beam of photons has the interpretation that the probability of a photon traveling an optical depth τ before absorption is e−τ . Similarly, when radiation is scattered isotropically we can say that a single photon has equal probabilities of scattering into equal solid angles. In this way we can speak of a typical or sample path of a photon, and the measured intensities can be interpreted as statistical averages over photons moving in such paths. Now consider a photon emitted in an infinite, homogenous scattering region. It travels a displacement r1 before being scattered, then travels in a new direction over a displacement r2 before being scattered, and so on. The net displacement of the photon after N free paths is R = r1 + r2 + r3 + · · · + rN (6) –3– We would like to find a rough estimate of the distance | R | traveled by a typical photon. Simple averaging of equation [6] over all sample paths will not work, because the average displacement, being a vector, must be zero. Therefore, we first square equation [6] and then average. This yields the mean square displacement traveled by the photon: l∗2 ≡ hR2 i = hr21 i + hr22 i + · · · + hr2N i + +2hr1 · r2 i + 2hr1 · r3 i + · · ·+ · · ·. (7) Each term involvement the square of a displacement averages to the mean square of the free path of a photon, which is denoted l2 . To within a factor of order unity, l is simply the mean free path of a photon. The cross terms in equation [7] involve averaging the cosine of the angle between the directions before and after scattering, and this vanishes for isotropic scattering. (It also vanishes for any scattering with front-back symmetry, as in Thomson or Rayleigh scattering.)Therefore l∗2 = Nl2 , √ l∗ = Nl. (8) (9) The quantity l∗ is the root mean square net displacement of the photon, and it increases as the square root of the number of scatterings. This result can be used to estimate the mean number of scattering in a finite medium. Suppose a photon is generated somewhere within the medium; then the photon will scatter until it escapes completely. For regions of large optical depth the number of scatterings required to do this is roughly determined by setting l∗ ∼ L, the typical size of the medium. From equation [9] we find N≈ L2 . l2 (10) Since l is of the order of the mean free path, L/l is approximately the optical thickness of the medium τ. Therefore, we have N ≈ τ2 , (τ 1). (11) –4– For regions of small optical thickness the mean number of scatterings is small, of order 1 − e−τ ≈ τ; that is N ≈ τ, (τ 1). (12) For most order-of-magnitude estimates it is sufficient to use N ≈ τ2 + τ or N ≈ max(τ, τ2 ) for any optical thickness.