Spectral Line Broadening Hubeny & Mihalas Chap. 8 Gray Chap. 11

Slides:



Advertisements
Similar presentations
Introduction to Astrophysics Lecture 4: Light as particles.
Advertisements

Molecular Bonds Molecular Spectra Molecules and Solids CHAPTER 10 Molecules and Solids Johannes Diderik van der Waals (1837 – 1923) “You little molecule!”
Chapter 1 Electromagnetic Fields
- + Hydrogen Lines in DA White Dwarfs: Improved Stark Broadening E Pier-Emmanuel Tremblay & Pierre Bergeron Université de Montréal.
METO 621 Lesson 6. Absorption by gaseous species Particles in the atmosphere are absorbers of radiation. Absorption is inherently a quantum process. A.
Bound – Bound Transitions. Bound Bound Transitions2 Einstein Relation for Bound- Bound Transitions Lower State i : g i = statistical weight Lower State.
Spectroscopy Spectral lines The Fraunhofer spectrum Charlotte Moore Sitterly –Multiplet table –Rowland table Formalism of spectroscopy 1990 Bruce Gold.
Natural Broadening From Heisenberg's uncertainty principle: The electron in an excited state is only there for a short time, so its energy cannot have.
Line Transfer and the Bowen Fluorescence Mechanism in Highly Ionized Optically Thick Media Masao Sako (Caltech) Chandra Fellow Symposium 2002.
Microphysics of the radiative transfer. Numerical integration of RT in a simplest case Local Thermodynamical Equilibrium (LTE, all microprocesses are.
Sub-THz Component of Large Solar Flares Emily Ulanski December 9, 2008 Plasma Physics and Magnetohydrodynamics.
March 4, 2011 Turn in HW 5; Pick up HW 6 Today: Finish R&L Chapter 3 Next: Special Relativity.
Physics 681: Solar Physics and Instrumentation – Lecture 10 Carsten Denker NJIT Physics Department Center for Solar–Terrestrial Research.
Introduction to radiative transfer
METO 621 Lesson 5. Natural broadening The line width (full width at half maximum) of the Lorentz profile is the damping parameter, . For an isolated.
LESSON 4 METO 621. The extinction law Consider a small element of an absorbing medium, ds, within the total medium s.
Suprit Singh Talk for the IUCAA Grad-school course in Inter-stellar medium given by Dr. A N Ramaprakash 15 th April 2KX.
Stellar Atmospheres: Emission and Absorption 1 Emission and Absorption 
Nonlinear Optics Lab. Hanyang Univ. Chapter 3. Classical Theory of Absorption 3.1 Introduction Visible color of an object : Selective absorption, Scattering,
Ch. 5 - Basic Definitions Specific intensity/mean intensity Flux
Solid State Physics Bands & Bonds. PROBABILITY DENSITY The probability density P(x,t) is information that tells us something about the likelihood of.
Solar Physics Course Lecture Art Poland Modeling MHD equations And Spectroscopy.
Stellar Atmospheres II
SCATTERING OF RADIATION Scattering depends completely on properties of incident radiation field, e.g intensity, frequency distribution (thermal emission.
Gas Absorption Line Broadening April 6. Summary in Words of Gas Transitions 3 types of quantized transitions important to us: Electronic (highest energy:
Average Lifetime Atoms stay in an excited level only for a short time (about 10-8 [sec]), and then they return to a lower energy level by spontaneous emission.
B.SC.II PAPER-B (OPTICS and LASERS)
Solution Due to the Doppler effect arising from the random motions of the gas atoms, the laser radiation from gas-lasers is broadened around a central.
Radiation In astronomy, the main source of information about celestial bodies and other objects is the visible light or more generally electromagnetic.
Absorption and Emission of Radiation:
Atoms in stellar atmospheres are excited and ionized primarily by collisions between atoms/ions/electrons (along with a small contribution from the absorption.
Ch ; Lecture 26 – Quantum description of absorption.
Atoms in stellar atmospheres are excited and ionized primarily by collisions between atoms/ions/electrons (along with a small contribution from the absorption.
1 Nature of Light Wave Properties Light is a self- propagating electro- magnetic wave –A time-varying electric field makes a magnetic field –A time-varying.
Substitute Lecturer: Jason Readle Thurs, Sept 17th, 2009
1 Introduction to Atomic Spectroscopy Lecture 10.
Chapter 28:Atomic Physics
Spectroscopy Spectral lines The Fraunhofer spectrum Charlotte Moore Sitterly (Allen!) –Multiplet table –Rowland table Formalism of spectroscopy 1990 Bruce.
Introduction to materials physics #4
The Boltzmann Distribution allows Calculation of Molecular Speeds Mathematically the Boltzmann Distribution says that the probability of being in a particular.
LINE-BROADENING MECHANISMS
Spectroscopy Spectral lines The Fraunhofer spectrum Charlotte Moore Sitterly (Allen!) –Multiplet table –Rowland table Formalism of spectroscopy.
Chapter 38C - Atomic Physics © 2007 Properties of Atoms Atoms are stable and electrically neutral.Atoms are stable and electrically neutral. Atoms have.
Lecture 8 Optical depth.
1.1 What’s electromagnetic radiation
Chapter – 7 Line Width Line Width (natural) Oscillator strength
REVIEW OF QUANTUM MECHANICS IMRANA ASHRAF ZAHID DEPARTMENT OF PHYSICS QUAID-I-AZAM UNIVERSITY ISLAMABAD, PAKISTAN.
Quantum theory Electron Clouds and Probability. Bohr’s model of the atom is unable to describe electron (e - ) behavior in an atom Problem: multiple spectral.
Spectral Line Transfer Hubeny & Mihalas Chap. 8 Mihalas Chap. 10 Definitions Equation of Transfer No Scattering Solution Milne-Eddington Model Scattering.
Line Broadening Chap 9, part 9.3. ‘Natural’ Line Width For quantum-mechanical reasons (which we can express in terms of the Heisenberg uncertainty principle),
Lyα Forest Simulation and BAO Detection Lin Qiufan Apr.2 nd, 2015.
Spectral Line Formation
MOLECULAR SPECTROSCOPY
Chapter 13 Cont’d – Pressure Effects More curves of growth How does the COG depend on excitation potential, ionization potential, atmospheric parameters.
Shanxi University Atomic Physics Chapter 7 The interaction of atoms with radiation Atomic Physics.
Summary Blackbody radiation Einstein Coefficients
Einstein’s coefficients represent a phenomenological description of the matter-radiation interaction Prescription for computing the values of the A and.
Saturation Roi Levy. Motivation To show the deference between linear and non linear spectroscopy To understand how saturation spectroscopy is been applied.
The Interaction of Light and Matter: a and n
The Solar System Lesson2 Q & A
Maxwell's Equations and Light Waves
Maxwell's Equations & Light Waves
Chapter 13 – Behavior of Spectral Lines
The Classical Damping Constant
Really Basic Optics Instrument Sample Sample Prep Instrument Out put
Chapter 7. Emission and Absorption and Rate Equations
Lecture 3 Radiative Transfer
Stars and Galaxies Lesson2 Q & A
Bound – Bound Transitions
Equation of Transfer (Hubeny & Mihalas Chapter 11)
Presentation transcript:

Spectral Line Broadening Hubeny & Mihalas Chap. 8 Gray Chap. 11 Natural Broadening Doppler Broadening Collisional Broadening: Impact, Statistical, Quantum Theories

Broadening of Absorption Profile Natural – energy uncertainty due to finite lifetime Doppler – thermal motion of gas Pressure – perturbations in energy levels due to collisions (encounters) with charged particles [important in transfer equation] Stellar rotation – Doppler shifts across disk Stellar turbulence – Doppler shifts from motion [important in line synthesis] Instrumental – projected slit of spectrograph [always important]

Natural Broadening Uncertainty principle level j depopulated by spontaneous emission, rate Aji (Einstein coeff.) Lifetime for j to i Lifetime for all downward transitions FWHM j i

Natural Broadening Damping constant Lorentzian profile Small, important in low density gas

Doppler Broadening by Thermal Motion Profile at Doppler shifted frequency by speed ξ Integrate over Maxwellian velocity distribution along the line of sight

Doppler Broadening by Thermal Motion Substitute Then final profile has form H(a,V) = Voigt profile

Voigt Profile Gaussian in core and Lorentzian in wings IDL version: IDL> u=findgen(201)/40.-2.5 IDL> v=voigt(0.5,u) IDL> plot,u,v

Collisional Broadening: Classical Impact – Phase Shift Theory Suppose encounter happens quickly and atom emits as an undisturbed oscillator between collisions but ceases before and after Frequency content of truncated wave from FT Power spectrum (observed)

Collisional Broadening: Classical Impact – Phase Shift Theory Probability number occurring in time dT at T where T0 = average time between collisions Mean energy spectrum is then Lorentzian profile damping constant Γ=2/T0

Collisional Broadening: Classical Impact – Phase Shift Theory Frequency of collisions = 1/T0 Suppose collisions occur if particles pass within distance = impact parameter ρ0 N = #perturbers/cm3, v = relative velocity cm/s Then damping parameter is

Weisskopf approximation perturber is a classical particle path is a straight line no transitions caused in atom interaction creates a phase shift or frequency shift given by

p exponents of astronomical interest p = 2 linear Stark effect (H + charged particle) p = 3 resonance broadening (atom A + atom A) p = 4 quadratric Stark effect (non-hydrogenic atom + charged particle) p = 6 van der Waals force (atom A + atom B) Cp from experiment or quantum theory

Weisskopf approximation Total phase shift Atom r(t) t = 0 v=constant p ψp 2 π 3 4 π/2 6 3π/8 perturber path

Weisskopf approximation Assume that only collisions that produce a phase shift > η0 are effective in broadening Weisskopf assumed η0 =1 , yields damping depends on ρ, T Ignores weak collisions η < η0

Better Impact Model: Lindholm-Foley Includes effects of multiple weak collisions, which introduce a phase shift Δω0 ; ΓLF > ΓW Impact theory fails for: small ρ, large broadening time overlap of collisions nonadiabatic collisions p 3 4 6 Γ 2π2C3N 11.37 C42/3 v1/3 N 8.08 C62/5 v3/5 N Δω0 9.85 C42/3 v1/3 N 2.94 C62/5 v3/5 N

Statistical Theory for Collisional Broadening: Nearest Neighbor Approximation Imagine atom sitting in a static sea of perturbers (OK for slow moving ions) that produces a relative probability of perturbing electric field and Δω Close to atom, consider probability that nearest neighbor is located at a distance in the range (r,r+Δr) = W(r) dr Corresponding frequency profile

Statistical Theory for Collisional Broadening: Nearest Neighbor Approximation Probability proportional to (1) % that do not occur at <r (2) increasing numbers at increasing distance Differentiate wrt r

Statistical Theory for Collisional Broadening: Nearest Neighbor Approximation Consider frequency shifts relative to that for mean interparticle distance r0 #particles x volume for each = total volume Insert into expression W(r) Express with relative frequency shift

Statistical Theory for Collisional Broadening: Nearest Neighbor Approximation Replace W(r) with W(Δω) Probability that atom will experience a perturbing field to give a frequency shift Δω

Apply to Linear Stark effect p=2 Express in terms of normal field strength Change of variables

Apply to Linear Stark effect p=2 Then probability in terms of field strength is [note missing minus sign in Hubeny & Mihalas] Final expression for profile

Holtsmark Statistical Theory Ensemble of perturbers instead of single more particles, more chances for strong field e- attracted to ions, reduce perturbation by Debye shielding in stellar atmospheres density is low, number of perturbers is large, and Holtsmark distribution is valid

Hydrogen: Linear Stark Effect each level degenerate with 2n2 sublevels perturbing field will separate sublevels observed profile is a superposition of components weighted by relative intensities and shifted by field probability function

Hydrogen: Linear Stark Effect each component shifted by profile is a sum over all components density dependent shift (N) statistical theory OK for interactions H + protons impact theory ~OK for interactions H + electron, but electron collisions are non-adiabatic

Quantum Calculations for the Linear Stark effect of Hydrogen unified theory for electron and proton broadening for Lyman and Balmer series: Vidal, Cooper, & Smith 1973, ApJS, 25, 37 IR series Lemke 1997, A&AS, 122, 285 Model Microfield Method (not static for ions) Stehle & Hutcheon 1999, A&AS, 140, 93

Summary final profile is a convolution of all the key broadening processes convolution of Lorentzian profiles: Γtotal=ΣΓi convolution of Lorentzian and Doppler broadening yields a Voigt profile convolution of Stark profile with Voigt (for H) calculate as a function of depth in atmosphere because broadening depends on T, N (Ne)