Transcript Document
Physics 681: Solar Physics and Instrumentation – Lecture 4 Carsten Denker NJIT Physics Department Center for Solar–Terrestrial Research Solar Spectrum The spectrum of the Sun: The dashed line is the curve of an ideal blackbody having the Sun’s effective temperature. September 13, 2005 Center for Solar-Terrestrial Research Radiation Field I E d d dtdA cos d J (average intensity) 3 s m sr E d I d dtdA cos d I d dtdA cos sin d I 1 4 I d 1 4 2 0 0 sin d d (m ean intensity) iosotropic radiation field I I isotropic blackbody radiation I B September 13, 2005 Center for Solar-Terrestrial Research Energy Transport Radiation and convection 2 Energy flux (luminosity per unit area): F F R FC L / 4 r Mean free path of photons is small in the solar interior local thermal equilibrium (LTE) Radiative transfer equation cos I B dr Total energy flux F dI 0 F d w ith F w ith B T cos I d Temperature gradient T m 3 L 256 r T September 13, 2005 2 4 3 w ith 1 4 0 2 3 dr dT 0 c dB 1 dB dB 2h e h / kT d d dT Center for Solar-Terrestrial Research 3 1 4 dB dT 3 dT dr Temperature Definitions excitation tem perature N b (Boltzm an equation) Na ionization tem perature N i 1 (S aha equation) Ni gbe gae E b / kT E a / kT gb e ( E b E a / kT ) ga 2 kT Z i 1 2 m e kT 2 Pe Z i h m n v dv n (B oltzm an distribution) 2 kT kinetic tem perature September 13, 2005 and Pe n e kT 3/2 2 e m v / 2 kT 2 2 hc 1 B (T ) hc / kT 5 (P lanck function) e 1 color tem perature 3/2 Center for Solar-Terrestrial Research 4 v dv 2 Opacity Any process that removes photons from a beam of light will be called absorption. dI I ds ( [m d ds 2 1 kg ] absorption coefficient or opacity) (optical depth) s , f ,i d s 0 s 0 ,0 d s 0 September 13, 2005 s 0 ds Center for Solar-Terrestrial Research The optical depth may be thought of as the number of mean free paths from the original position to the surface, as measured along the ray’s path. I I ,0 e (p u re ab so rp tio n ) 1 (gas optically thick) 1 (gas optically thin) September 13, 2005 Center for Solar-Terrestrial Research Radiative Transfer Equation dI j ds ( j [m s 3 1 sr ] em ission coefficient) dI I ds j ds S 1 dI ds j ([J s 1 I dI ds September 13, 2005 1 m j 3 1 sr ] source function) I S (transfer equation) Center for Solar-Terrestrial Research The intensity of the light tends to become equal to the local value of the source function. For the case of thermodynamic equilibrium, the source function is equal to the Planck function S = B. dI ds dI 0 I S 0 intensity decreases w ith distance ds dI ds 0 I approaches S September 13, 2005 Center for Solar-Terrestrial Research Photon Interactions Bound–bound transitions Bound–free absorption Free–free absorption (bremsstrahlung) Electron scattering bf 1.31 10 19 3 m 3 2 8 e 29 2 6.65 10 m 2 3 mec 2 T 1 5 n 500 nm (T hom pson scattering) September 13, 2005 Center for Solar-Terrestrial Research Continuum Opacity Photoionization of H– ions hc 1240 eV nm 1640 nm 0.754 eV , bb ,bf , ff , es (total opacity) The total opacity depends not only on the wavelength of the light being absorbed but also on the composition, density, and temperature of the stellar material. Rosseland mean opacity September 13, 2005 Center for Solar-Terrestrial Research Structure of Spectral Lines W Fc F d (equivalent w idth) Fc natural broadening D oppler broadening pressure broadening September 13, 2005 1 1 2 c t i t f 2 2 2 kT c m 2 1 c t n 2 c 2 kT Center for Solar-Terrestrial Research m Nuclear Reactions http://nobelprize.org/physics/articles/fusion/sun_pp-chain.html September 13, 2005 Center for Solar-Terrestrial Research CNO Cycle http://outreach.atnf.csiro.au/education/senior/astrophysics/stellarevolution_mainsequence.html September 13, 2005 Center for Solar-Terrestrial Research