High Refractive Index Materials of Iron Sulfides and Poly(ethylene oxide)
- 1 August 1997
- journal article
- Published by Springer Nature in Journal of Materials Research
- Vol. 12 (8) , 2198-2206
- https://doi.org/10.1557/jmr.1997.0294
Abstract
High refractive index composites of iron sulfides and poly(ethylene oxide) (PEO) have been prepared by co-precipitation from aqueous solution. Several reaction parameters were varied: inorganic reactants, reactant ratios, reaction temperatures, and reaction times. Selected samples were characterized with organic microelemental analysis, x-ray fluorescence spectroscopy, x-ray diffraction, DSC, and TEM. The nanocomposites with the highest refractive indices have been prepared using PEO, Mohr's salt, and H2S or NaHS. The analyses indicate that the iron sulfides in these materials consist of finely dispersed mackinawite and greigite (“amorphous” FeS) and, partially, also pyrite. The refractive indexes of the resulting composites are clearly above 2 at 632.8 and 1295 nm and can assume values between 2.5 and 2.8.Keywords
This publication has 22 references indexed in Scilit:
- Iron Sulfide for PhotovoltaicsMRS Bulletin, 1993
- Research/ResearchersMRS Bulletin, 1993
- Mechanisms of pyrite and marcasite formation from solution: III. Hydrothermal processesGeochimica et Cosmochimica Acta, 1991
- An XPS study of gold deposition at low temperatures on sulphide minerals: Reducing agentsGeochimica et Cosmochimica Acta, 1989
- The chemistry of the hydrogen sulfide and iron sulfide systems in natural watersEarth-Science Reviews, 1987
- Marcasite precipitation from hydrothermal solutionsGeochimica et Cosmochimica Acta, 1986
- An XPS and SEM study of gold deposition at low temperatures on sulphide mineral surfaces: Concentration of gold by adsorption/reductionGeochimica et Cosmochimica Acta, 1985
- On the conversion of mackinawite to greigiteJournal of Inorganic and Nuclear Chemistry, 1979
- Sedimentary pyrite formationAmerican Journal of Science, 1970
- The chemistry of pyrite formation in aqueous solution and its relation to the depositional environmentMineralium Deposita, 1969