The Carbotek/Shimizu process to produce oxygen from lunar soils has been successfully demonstrated on actual lunar samples in laboratory facilities at Carbotek with Shimizu funding and support. Apollo sample 70035 containing approximately 25 percent ilmenite (FeTiO3) was used in seven separate reactions with hydrogen varying temperature and pressure: FeTiO3 + H2 yields Fe + TiO2 + H2O. The experiments gave extremely encouraging results as all ilmenite was reduced in every experiment. The lunar ilmenite was found to be about twice as reactive as terrestrial ilmenite samples. Analytical techniques of the lunar and terrestrial ilmenite experiments performed by NASA Johnson Space Center include iron Mossbauer spectroscopy (FeMS), optical microscopy, SEM, TEM, and XRD. The Energy and Environmental Research Center at the University of North Dakota performed three SEM techniques (point count method, morphology determination, elemental mapping), XRD, and optical microscopy.
First oxygen from lunar basalt
1993-01-01
Aufsatz (Konferenz)
Keine Angabe
Englisch
Kinetic Interpretations of First Reactivity Experiments on Lunar Basalt Samples
British Library Conference Proceedings | 1994
|Separation of lunar ilmenite - Basalt vs. regolith
NTRS | 1990
|Shock metamorphism of basalt and the lunar samples
NTRS | 1970
|