Theoretical intensities of the Fe XVII X-ray lines due to transitions
2p(6) - 2p(5)3d (near 15 Angstrom) and 2p(6) - 2p(5)3s (near 17 Angstr
om) are presented, and compared with solar flare and active region spe
ctra. The ratio of the 15 Angstrom lines to the 17 Angstrom lines is a
function of temperature T-e, but for solar spectra this is not of pra
ctical use because of the resonance scattering of the intense 15.015 A
ngstrom line. Instead we use the ratio of a nearby Fe XVIII line to ob
tain T-e. We find very satisfactory correspondence between solar spect
ra and synthetic spectra based on calculated line intensities with app
ropriately chosen T-e apart from the 15.015 Angstrom line, which is so
metimes less intense than its theoretical value, apparently owing to r
esonance scattering. Spectra emitted by DITE and JET tokamak plasmas w
ith measured T-e and N-e, are also considered. A predicted density var
iation of the ratio of the Fe XVII lines at 17.051 Angstrom and 17.096
Angstrom is confirmed, and using Abel inversion techniques applied to
a sequence of DITE spectra with different radial distances good agree
ment is found between the theoretical temperature variation of the I(1
5.015 Angstrom)/I(16.776 Angstrom) line ratio and that derived from th
ese spectra. We conclude that our calculated Fe XVII line intensities
are very reliable and may therefore be used in future analysis.