Difference between revisions of "Oxygen"
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− | {| | + | {{Element | |
− | | | + | name=Oxygen | |
− | |- | + | symbol=O | |
− | | | + | available=abundant | |
− | | | + | need=critical | |
− | | | + | number=8 | |
− | | | + | mass=15.9994 | |
− | | | + | group=16 | |
− | |- | + | period=2 | |
− | | | + | phase=Gas | |
− | | | + | series=Non-metals | |
− | |} | + | density=1.429 g/L | |
+ | melts=54.36K,<BR/>-218.79°C,<BR/>-361.82°F | | ||
+ | boils=0.20K,<BR/>-182.95°C,<BR/>-297.31°F | | ||
+ | isotopes=16<BR/>17<BR/>18 | | ||
+ | prior=[[Nitrogen|<FONT color="#7F7FFF">N</FONT>]] | | ||
+ | next=[[Fluorine|<FONT color="#7F7FFF">F</FONT>]] | | ||
+ | above=<SMALL><FONT color="#7F7F7F">N/A</FONT></SMALL> | | ||
+ | aprior=<SMALL><FONT color="#7F7F7F">N/A</FONT></SMALL> | | ||
+ | anext=<SMALL><FONT color="#7F7F7F">N/A</FONT></SMALL> | | ||
+ | below=[[Sulfur|<FONT color="#7F7FFF">S</FONT>]] | | ||
+ | bprior=[[Phosphorus|<FONT color="#7F7FFF">P</FONT>]] | | ||
+ | bnext=[[Chlorine|<FONT color="#7F7FFF">Cl</FONT>]] | | ||
+ | radius=60 | | ||
+ | bohr=48 | | ||
+ | covalent=73 | | ||
+ | vdwr=152 | | ||
+ | irad=(-2) 140 | | ||
+ | ipot=13.62 | | ||
+ | econfig=1s<sup>2</sup> <br/>2s<sup>2</sup> 2p<sup>4</sup> | | ||
+ | eshell=2, 6 | | ||
+ | enega=3.44 | | ||
+ | eaffin=1.46 | | ||
+ | oxstat=-2 | | ||
+ | magn=Paramagnetic | | ||
+ | cryst=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. | ||
+ | <BR/><BR/> | ||
− | + | ==Lunar Production and Use== | |
+ | Oxygen production from lunar sources (sometimes referred to as '''LUNOX''') is a critical element of any plan involving long term human presence on Luna. Oxygen is required for both life support and rocket fuel, and as such would be needed in large quantities. Lunar Oxygen production is one category of [[In Situ Resource Utilization]](''ISRU''). | ||
− | + | Oxygen makes up about 45% of the moons crust by weight, and virtually every substance on the moons surface is an oxide. As such, production of nearly anything other than oxygen from lunar resources will produce substantial amounts of oxygen as a byproduct. In addition, free (not bound chemically with other elements) oxygen exists in the lunar soil, albeit in small quantities. | |
− | [[ | + | Processes which produce oxygen from lunar sources include: |
− | + | ||
+ | *Aluminum reduction | ||
+ | *Carbothermal reduction | ||
+ | *[[Volatiles|Volatile Extraction]] | ||
+ | *[[Fluorine reaction]] | ||
+ | *[[Magma electrolysis]] | ||
+ | *[[Ilmenite Reduction]] | ||
+ | *Methane reduction | ||
+ | *hydrogen reduction of glass | ||
+ | *sulfuric acid dissolution/electrolysis | ||
+ | *ion sputtering. | ||
+ | |||
+ | |||
+ | == Related Pages == | ||
+ | *[[In Situ Resource Utilization]] | ||
+ | |||
+ | |||
+ | ==External Links== | ||
+ | |||
+ | *[http://nss.org/settlement/nasa/spaceresvol3/plsoom1.htm lunar oxygen process sequence discussion from Knudson and Gibson (1989)] (note: a good summary of approaches, but somewhat out of date) | ||
+ | *[http://www.moonminer.com/Moondust_index.html Lunar processing links from David Dietzler] | ||
+ | *[http://www.magicdragon.com/ComputerFutures/SpacePublications/llox-footnoted.html 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. | ||
+ | <BR/><BR/> | ||
+ | |||
+ | ==References== | ||
+ | |||
+ | One reference useful as an overview is The Moon: Resources, Future Development, and Colonization, by David Schrunk, Burton Sharpe, Bonnie Cooper and Madhu Thangavelu. | ||
+ | |||
+ | From review by Arthur Smith on ADB: "In particular Appendix E's coverage of oxygen extraction is extremely thorough, and the authors, while finding it somewhat difficult to directly compare techniques, find 4 of the approaches worthy of considerable further research: hydrogen reduction of glass, magma electrolysis, sulfuric acid dissolution/electrolysis, and ion sputtering." | ||
+ | |||
+ | [[Category:Paramagnetic Elements]] | ||
+ | [[Category:Gases]] | ||
+ | [[Category:Non-metals]] | ||
+ | [[Category:Critical and Essential Elements]] | ||
+ | [[Category:Abundant Elements]] | ||
+ | |||
+ | <!-- Generated by a gamma candidate version of Autostub2 (Test 9) --> |
Latest revision as of 07:59, 29 September 2011
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.
Lunar Production and Use
Oxygen production from lunar sources (sometimes referred to as LUNOX) is a critical element of any plan involving long term human presence on Luna. Oxygen is required for both life support and rocket fuel, and as such would be needed in large quantities. Lunar Oxygen production is one category of In Situ Resource Utilization(ISRU).
Oxygen makes up about 45% of the moons crust by weight, and virtually every substance on the moons surface is an oxide. As such, production of nearly anything other than oxygen from lunar resources will produce substantial amounts of oxygen as a byproduct. In addition, free (not bound chemically with other elements) oxygen exists in the lunar soil, albeit in small quantities.
Processes which produce oxygen from lunar sources include:
- Aluminum reduction
- Carbothermal reduction
- Volatile Extraction
- Fluorine reaction
- Magma electrolysis
- Ilmenite Reduction
- Methane reduction
- hydrogen reduction of glass
- sulfuric acid dissolution/electrolysis
- ion sputtering.
Related Pages
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.
References
One reference useful as an overview is The Moon: Resources, Future Development, and Colonization, by David Schrunk, Burton Sharpe, Bonnie Cooper and Madhu Thangavelu.
From review by Arthur Smith on ADB: "In particular Appendix E's coverage of oxygen extraction is extremely thorough, and the authors, while finding it somewhat difficult to directly compare techniques, find 4 of the approaches worthy of considerable further research: hydrogen reduction of glass, magma electrolysis, sulfuric acid dissolution/electrolysis, and ion sputtering."