The iron-to-calcium abundance ratio in the 20 X 10 to the 6th K plasma of medium and large solar flares

Other

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

16

Calcium, High Temperature Plasmas, Iron, Metallicity, Solar Flares, Solar X-Rays, Abundance, Metal Ions, Resonance Lines, Solar Corona, Solar Maximum Mission

Scientific paper

The iron-to-calcium abundance ratio during several flares observed by instruments on the P78-1 and Solar Maximum Mission spacecraft are determined using the intensity ratio of a dielectronic satellite line of Fe XXIV and the resonance line of Ca XIX. Values of A(Fe)/A(Ca) equal to 6.8 +/- 1.0 and 6.0 +/- 1.5 were derived from these data sets, respectively, the small difference being attributable to errors in the calculated instrument sensitivities. These values fall between two other determinations from X-ray spectra, but are less than the photospheric value. They are fairly constant from flare to flare, contrasting with other recent work which indicates strong flare-to-flare variations.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

The iron-to-calcium abundance ratio in the 20 X 10 to the 6th K plasma of medium and large solar flares does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with The iron-to-calcium abundance ratio in the 20 X 10 to the 6th K plasma of medium and large solar flares, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and The iron-to-calcium abundance ratio in the 20 X 10 to the 6th K plasma of medium and large solar flares will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1334963

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.