You have requested a machine translation of selected content from our databases. This functionality is provided solely for your convenience and is in no way intended to replace human translation. Neither SPIE nor the owners and publishers of the content make, and they explicitly disclaim, any express or implied representations or warranties of any kind, including, without limitation, representations and warranties as to the functionality of the translation feature or the accuracy or completeness of the translations.
Translations are not retained in our system. Your use of this feature and the translations is subject to all use restrictions contained in the Terms and Conditions of Use of the SPIE website.
1 February 1994Reflective coating of 834 Å for imaging O+ ions
Imaging upflowing O+ ions of ionospheric origin and plasmaspheric O+ can be achieved through solar resonance scattering at 834 Å. Unfortunately, several strong background emissions, including the ones at 1025 and 1216 Å due to geocoronal hydrogen atoms, pose serious problems. Most common optical coatings have higher reflectivity at 1025 and 1216 Å than at 834 Å. After examining a number of options, e have designed a multiple-layer coating that selectively reflects 834-Å radiation and suppresses 1025- and 1216-Å radiation. The structure of the coating material consists of a very thin (50 to 150 Å) metal (nickel) layer on top of a semitransparent dielectric material (magnesium fluoride) over an aluminum substrate. Three such coatings were produced at NASA Goddard Space Flight Center using an existing coating facility that is not optimized for thin coatings. In spite of such fabrication difficulties, we have obtained encouraging results.
The alert did not successfully save. Please try again later.
Supriya Chakrabarti, Jerry Edelstein, Ritva A. M. Keski-Kuha, Felix T. Threat, "Reflective coating of 834 Å for imaging O+ ions," Opt. Eng. 33(2) (1 February 1994) https://doi.org/10.1117/12.155927