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Astron. Astrophys. 324, 381-394 (1997)
Fe XVII X-ray lines in solar coronal and laboratory plasmas
K.J.H. Phillips 1,
C.J. Greer 2,
A.K. Bhatia 3,
I.H. Coffey 2,
R. Barnsley 4 and
F.P. Keenan 2
1 Astrophysics Division, Rutherford Appleton Laboratory,
Chilton, Didcot, Oxon. OX11 0QX, UK (phillips@solg2.bnsc.rl.ac.uk)
2 Department of Physics, The Queen's University, Belfast
BT7 1NN, Northern Ireland, UK
3 Laboratory for Astronomy and Solar Physics, NASA Goddard
Space Flight Center, Greenbelt, MD 20771, USA
4 Department of Physics and Astronomy, Leicester
University, Leicester LE1 7RH, UK
Received 27 September 1996 / Accepted 2 January 1997
Abstract
Theoretical intensities of the Fe XVII X-ray
lines due to transitions (near 15 Å)
and (near 17 Å) are presented, and
compared with solar flare and active region spectra. The ratio of the
15 Å lines to the 17 Å lines is a function of
temperature , but for solar spectra this is not
of practical use because of the resonance scattering of the intense
15.015 Å line. Instead we use the ratio of a nearby
Fe XVIII line to obtain . We
find very satisfactory correspondence between solar spectra and
synthetic spectra based on calculated line intensities with
appropriately chosen apart from the
15.015 Å line, which is sometimes less intense than its
theoretical value, apparently owing to resonance scattering. Spectra
emitted by DITE and JET tokamak plasmas with measured
and are also considered. A
predicted density variation of the ratio of the
Fe XVII lines at 17.051 Å and
17.096 Å is confirmed, and using Abel inversion techniques
applied to a sequence of DITE spectra with different radial distances
good agreement is found between the theoretical temperature variation
of the line ratio and that derived from these
spectra. We conclude that our calculated Fe XVII
line intensities are very reliable and may therefore be used in future
analysis.
Key words: atomic
data
atomic
processes
Sun: activity
Sun: flares
Sun: X-rays, gamma rays
Send offprint requests to: K.J.H. Phillips
Contents
© European Southern Observatory (ESO) 1997
Online publication: May 26, 1998
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