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Astron. Astrophys. 347, 401-408 (1999) 3. ResultsAn example of the total emissivity curve as resulting from the
present version of the Arcetri Code calculation is displayed in
Fig. 1. It has been evaluated assuming
Fig. 2 shows the contribution of the most abundant elements to the total emissivity curve. Hydrogen is responsible for nearly all the radiative losses at chromospheric temperatures, while iron provides most of the output energy at high temperature. Continuum radiation may be neglected for all temperatures lower than a few million degrees, but at very high temperature free-free continuum radiation dominates the total emissivity.
Figs. 3 and 4 display the total emissivity for some of the most abundant elements in astrophysical plasmas together with the strongest lines of each of the element's ions. For some temperatures the total emissivity of some elements is dominated by the emission of a very small number of very strong lines; these are some of the strongest spectral features observed in solar and stellar spectra.
3.1. Effect of the electron densityBoth continuum and line radiation may be electron density dependent, and this may cause the radiative losses and the total emissivity curve to be density dependent as well. As in literature the total emissivity curve is usually given as a function of temperature only, it is important to check the density dependence of this curve. Continuum radiation electron density dependence stems from the
two-photons continuum process: the populations of the H-like
However, in the literature ion fractions are usually reported as a function of electron temperature only, so in the present work it is not possible to check the effects of their density dependence on the total emissivity curve due to ionization balance. In order to assess the density dependence due to level population
we have performed the theoretical calculation of this curve assuming
four different values of the electron density:
Fig. 5 displays the percentual difference
(with
The maximum at coronal temperatures is given by the presence of a host of strong density dependent lines formed in quiet corona, mainly from Fe, Mg and Si ions. The high temperature tail is dominated by strong, density insensitive lines and free-free continuum; the low temperaure tail is dominated by density insensitive transition region and chromospheric lines and for this reason there are small differences between computations carried out assuming different density values. 3.2. Effect of different datasets and approximations in level population computationLevel populations are strongly sensitive to any change or problem in the atomic parameters, collision strengths and transition probabilities as well as in the approximation adopted for their calculations, and this affects line radiation. It is therefore important to check the effects of different transition probabilities datasets on the resulting total emissivity curve. As big improvements have been done in the present version of the Code versus the older version described in Landini & Monsignori Fossi 1990, we have performed a comparison between the present results and those obtained using the 1990 version of the Arcetri Code. The adopted element abundances are from Allen 1973. There are three main differences between the two versions of the Arcetri Code: (a) the old 1990 Code calculated all line intensities using the Coronal Model Approximation , (b) the collision rates were calculated using Gaunt factors and (c) radiative data came from different literature sources than in the present version of the Code. Thus, the present comparison allows to check also the effects of different assumptions in level population calculations on the resulting total plasma emissivity. Fig. 6 displays the percentual difference
between the two versions of the Code as a function of electron temperature. It is possible to see that rather high differences (up to 60%) are found at transition region temperatures, and smaller discrepancies occur at coronal temperatures. In the positive section of Fig. 6 the older version of the Arcetri Code has higher total emissivity than the more recent version at transition region temperatures. This is due to the presence of few very bright transitions from [ O iv], [ O v], [ C iv] whose emissivities have very different values in the two versions of the Code; their difference is due both to the use of different datasets and to the different approximations used in level population calculation leading to an overestimation of line emissivity for these transitions in the old version of the Code. The negative section of the diagram is due to the much larger number of lines included in the new version.
3.3. Effect of ionization equilibriumIon fractions are necessary to both line and continuum calculation and any difference in their values are usually reflected into the total emissivity curve. We have checked the changes between curves calculated adopting different ion fractions datasets. All these calculations have been carried out assuming ionization equilibrium, and ion fractions come from Shull & Steenberg 1982 (SS, but with H and He ion fractions coming from Arnaud & Rothenflug 1985), Arnaud & Rothenflug 1985 (RO), Arnaud & Rothenflug 1985 plus Arnaud & Raymond 1992 for the Fe ions (RA), Mazzotta et al. 1998 (MA). Fig. 7 displays the percentual differences
between the results obtained adopting RA ion fractions and those obtained with the other three datasets. The overall differences are smaller than 40%, and the greater differences are found with RO ion fractions. These are due to Fe ion fractions, dominating the high temperature tail of the total emissivity curve (the other elements' ion fractions being the same). Differences with the SS and MA results are much smaller.
On the overall, the effect of the use of different ion fractions
onto the total emissivity curve may rise up to a maximum of 40%, and
are smaller than 20% at transition region and chromospheric
temperatures below 3.4. Effect of element abundancesVariation of the chemical composition of the emitting plasma may change the total emissivity curve by very large amounts. It has been long acknowledged that element abundances change in
solar plasmas, and their values seem to be associated to magnetic
structures in the solar atmosphere (see the reviews of Feldman et al.
1992, Feldman 1992, Mason 1995). These variations seem to be related
to the First Ionization Potential (FIP) of the emitting elements (e.g.
Haisch et al. 1996). Cook et al. 1989 determined the radiative loss
function using photospheric, chromospheric and coronal abundaces and
found huge differences in the Also B The importance of abundance changes pointed out by these authors has led us to check the effect of different element abundance values on the resulting total emissivity curve. As this curve is dominated by the emission of some elements, these effects are expected to be very large. In order to check these effects total emissivities have been calculated assuming several different sets of element abundances: Allen 1973 (AL), Feldman 1992 (FE), Grevesse & Anders 1991 (GA), Meyer 1985 (ME) and Waljeski et al. 1994 (WA). Fig. 8 displays the percentual differences
found between the emissivity curve calculated using FE abundances and those calculated adopting the other datasets. There are huge variations (up to a factor 2.5) between FE and WA total emissivities, while differences up to 70% are found between FE and the other three sets of abundance values.
Considering the results shown in Fig. 8, and that differences up to factor 9 have been observed in the solar atmosphere between distinct structures very close to each other (e.g. Young & Mason 1997), abundance variations are a key factor for the evaluation of total plasma emissivity and need to be carefully chosen in order to be able to properly determine the plasma radiative losses.
© European Southern Observatory (ESO) 1999 Online publication: June 18, 1999 ![]() |