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Astron. Astrophys. 357, 767-776 (2000) 2. TheoryThe spectral emission from a plasma is governed by two sets of coupled equations, namely the radiative transfer equations and the equations of statistical balance. These may be written as (McWhirter 1965) Here where where Using the relation between the Einstein A and B-coefficients, Eqs. 1 and 2 become where the spatial dependances have been put in explicitly. The terms in the brackets are markedly similar, the only difference
being in the specification of the intensity terms. In the radiative
transfer case the intensity term Eqs. 5 and 6 can be re-written as follows:
g is identical to what Irons (1979) calls the transmission
coefficient but is called here the escape probability since the point
r is outwith the emitting plasma.
2.1. The escape probabilityThe escape probability, as introduced by Holstein (1947), has subsequently been considered by many authors (eg. McWhirter 1965; Irons 1979; Kastner & Kastner 1990). Holstein showed that assuming a constant source function and that spectral lines are purely doppler broadened, the escape probability may be written as From Eq. 7 the solution of the equation of radiative transfer may be written as where where From this follows a simple idea, which was introduced by Jordan (1967), for extracting optical depth from observations of intensity ratios of spectral lines arising from a common upper level. Such ratios may be written as In optically thin conditions this ratio reduces to that of the Einstein A-coefficients and opacity is the only mechanism that can modify it from this value. The transitions that are most significantly affected are those with large and long lived lower level populations - i.e. metastables. However, such populations are themselves not significantly modified due to their large value and are collisionally controlled. Thus the ratio of optical depths of two optically thick lines arising from a common upper level is constant - i.e. where This equation provides the route for extracting optical depth from observations. Once the optical depth is known for one line, those of all the other lines of the same ion whose lower levels are metastable can be obtained via Eq. 16. Assuming the other lines of the same ion (those whose lower levels are not metastable) are optically thin, the opacities of all the lines of an ion can be obtained from the single extracted value. In Paper I this analysis was performed for lines of C II and C III using SUMER data to assess which lines should be rejected or intensity adjusted in a DEM analysis. 2.2. Absorption factorsThe two principle effects of opacity are
The absorption of a photon by an atom or ion results in an electron excitation which can lead to either a re-emission of a photon in the reverse process or a collisional de-excitation. It is conventional within radiative transfer theory to distinguish between these two cases since the former (scattering) leads to no thermal coupling between the emitting and the absorbing plasma, whereas the latter case (pure absorption) does. Furthermore this distinction is useful in dealing with a third effect of opacity, namely partial frequency redistribution in which the emission profiles are modified due to scattering. This distinction is not always so clear in escape probability literature. However, as described above, it influences the populations and emergent intensities via the effect of partial frequency redistribution and as yet this effect has not been included within an escape probability model. The escape probability takes account of the loss of photons out of the line of sight due to both scattering and absorption. However, this quantity is not sufficient in describing the effects of opacity on spectral emission. Along the line of sight photons are absorbed from all directions leading to an enhanced upper level population and consequently an increase in emission in the line of sight. This is described by some authors as scattering into the line of sight (e.g. Kastner & Bhatia 1992). In essence Kastner & Bhatia formulate the problem as follows: where ` where where Jordan noted that in the case of intensity ratios of lines arising from a common upper level the denominator cancels and thus the population modification does not influence these ratios. The problem with this approach is that it does not take full account of the indirect effects on the population structure. In the formulation of Eq. 19, Jordan considered emission in line i from a point to be characterised by an optically thin population structure. She then considered the ultimate fate of those emitted photons allowing them to be absorbed in line i , subsequently re-emitted in any line stemming from the same upper level, subsequently re-absorbed again, and so on and so forth. However, this does not take account of the contribution to line i of photons initially emitted in lines other than i , but from the same upper level, that are re-absorbed leading to emission in line i . This contribution is of particular importance for lines that are relatively thin if there exist thick lines stemming from the same upper level. In addition if there is some line blending then photons emitted in
one line in the blend may be absorbed by the other line. The indirect
effects of this situation are complex and can effectively increase the
optical depth of a line from a population modification point of view,
whilst decreasing it from an emergent flux perspective and vice versa.
If blending exists then the denominator of Eq. 20 will, in
principle, not cancel. Furthermore it is not clear how the
Following Bhatia & Kastner (1999), we choose to formulate the problem as follows: where The use of absorption factors, or indeed escape factors, in the
statistical balance equations to calculate an optically thick
population structure has been considered by a number of authors (eg.
McWhirter 1965; Kastner & Bhatia 1989; Bhatia & Kastner 1992,
1999; Brooks et al. 2000). The escape factor - the escape probability
averaged over every line of sight through the layer - is often used in
this context as it was shown by Irons (1979) that this quantity is
equivalent to the absorption factor averaged throughout the layer.
Bhatia & Kastner (1999) calculated optically thick populations
iteratively starting from an optically thin solution and assuming that
the source function (
If we assume a stratified atmosphere where
where From the lower level models described below, absorption factors
were calculated throughout the layer. These were calculated
iteratively assuming an initial optically thin solution since the
evaluation of Interestingly, upon iteration the optically thick upper level
distributions of the levels of interest here (see Fig. 1b) tend
to If this assumption is made then Eq. 21 reduces to Eq. 13 as follows: A similar argument shows that in making the assumption of Eq.
23, This quantity was derived in Paper I. 2.3. Line blendingAs discussed in Sect. 2.2, the overlap of spectral lines in
frequency space influences both the emergent intensities and the
population structure. Emitted photons may be absorbed by any line
whose absorption profile overlaps at the nominal frequency.
Furthermore the intensity term, Blending may be included trivially within the expressions for
g, Fig. 3a shows the C II 2s22p 2P - 2s2p2 2P multiplet for the case where the optical depth of the 3/2-1/2 component at 904.143 Å is 10, calculated using Eqs. 29 and 31, in comparison with the optically thin case. Fig. 3b shows the same in comparison with the thick multiplet calculated using Eqs. 14 and 28. These show that there is a clear difference in both intensity and line shape when blending is included. Note that the multiplet components are labelled by their J quantum numbers.
© European Southern Observatory (ESO) 2000 Online publication: June 5, 2000 ![]() |