Difference between revisions of "Oxygen"
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*[[Magma electrolysis]] | *[[Magma electrolysis]] | ||
*Methane reduction | *Methane reduction | ||
| + | *hydrogen reduction of glass | ||
| + | *sulfuric acid dissolution/electrolysis | ||
| + | *ion sputtering. | ||
In any Lunox production sequence, it is necessary that all reactants are returned to the initial state. | In any Lunox production sequence, it is necessary that all reactants are returned to the initial state. | ||
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*[http://www.magicdragon.com/ComputerFutures/SpacePublications/llox-footnoted.html LLOX automated production summary (1990)] | *[http://www.magicdragon.com/ComputerFutures/SpacePublications/llox-footnoted.html LLOX automated production summary (1990)] | ||
<BR/><BR/> | <BR/><BR/> | ||
| − | + | * ''The Moon: Resources, Future Development, and Colonization'' by David Schrunk, Burton Sharpe, Bonnie Cooper and Madhu Thangavelu - appendix E covers a wide range of oxygen extraction methods. | |
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{{Autostub}} | {{Autostub}} | ||
Revision as of 06:10, 15 June 2007
| Oxygen | |
|---|---|
| O | |
| In situ availability: | abundant |
| Necessity: | critical |
| Atomic number: | 8 |
| Atomic mass: | 15.9994 |
| group: | 16 |
| period: | 2 |
| normal phase: | Gas |
| series: | Non-metals |
| density: | 1.429 g/L |
| melting point: | 54.36K, -218.79°C, -361.82°F |
| boiling point: | 0.20K, -182.95°C, -297.31°F |
| N/A ← N/A → N/A | |
| N ← O → F | |
| P ← S → Cl | |
| Atomic radius (pm): | 60 |
| Bohr radius (pm): | 48 |
| Covalent radius (pm): | 73 |
| Van der Waals radius (pm): | 152 |
| ionic radius (pm): | (-2) 140 |
| 1st ion potential (eV): | 13.62 |
| Electron Configuration | |
| 1s2 2s2 2p4 | |
| Electrons Per Shell | |
| 2, 6 | |
| Electronegativity: | 3.44 |
| Electron Affinity: | 1.46 |
| Oxidation states: | -2 |
| Magnetism: | Paramagnetic |
| Crystal structure: | Cubic |
Oxygen is a Non-metal in group 16.
It has a Cubic crystalline structure.
This element has 3 stable isotopes: 16, 17, and 18.
LUNOX is short for Lunar Oxygen, which is oxygen harvested from resources available on the moon. Oxygen is a major requirement for sustaining any human presence on the lunar surface, useful both for life support and also as a major component of rocket fuel. Lunar Oxygen production is one category of In Situ Resource Utilization, or ISRU.
Methods of LUNOX Production
Most of the methods of lunar oxygen production envision the reduction of lunar regolith or rocks to liberate oxygen, although another possible method of harvesting oxygen is to free small amounts of trapped gas from soil by heating. Reduction methods include:
- Aluminum reduction
- Carbothermal reduction
- Fluorine reaction
- Ilmenite Reduction
- Magma electrolysis
- Methane reduction
- hydrogen reduction of glass
- sulfuric acid dissolution/electrolysis
- ion sputtering.
In any Lunox production sequence, it is necessary that all reactants are returned to the initial state.
External Links
- lunar oxygen process sequence discussion from Knudson and Gibson (1989) (note: a good summary of approaches, but somewhat out of date)
- Lunar processing links from David Dietzler
- LLOX automated production summary (1990)
- The Moon: Resources, Future Development, and Colonization by David Schrunk, Burton Sharpe, Bonnie Cooper and Madhu Thangavelu - appendix E covers a wide range of oxygen extraction methods.
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