Difference between revisions of "Terrestrial Air"
(Undo revision 16224 by 81.25.37.219 (talk) removing vandalism) |
m (Fixed Argon abbreviation) |
||
| (One intermediate revision by one other user not shown) | |||
| Line 1: | Line 1: | ||
{{life Stub}}{{Wikify}} | {{life Stub}}{{Wikify}} | ||
| − | <BR>''The | + | <BR>''The percentages by volume of those gases found in relatively constant amounts near sea level are approximately as follows:''<ref>This table is from the 1965 edition of the Aerospace Dictionary.</ref><BR/> |
<TABLE BORDER=1 WIDTH="300" > | <TABLE BORDER=1 WIDTH="300" > | ||
<TR> | <TR> | ||
| Line 19: | Line 19: | ||
<TR> | <TR> | ||
| − | <TD>[[argon]] ( | + | <TD>[[argon]] (Ar)</TD> |
<TD>0.934</TD></TR> | <TD>0.934</TD></TR> | ||
| Line 58: | Line 58: | ||
| − | ''In addition to the above constituents there are many | + | ''In addition to the above constituents there are many that vary. Chief among these is [[water]] vapor, which may vary from zero to volume percentages close to 4 percent. [[Ozone]], [[sulfur dioxide]], [[ammonia]], [[carbon monoxide]], [[iodine]], and other trace [[gases]] occur in small and varying amounts. <BR> The above composition of dry air is true to about 90 kilometers. See [[Upper Atmosphere|upper atmosphere]]. '' |
Latest revision as of 06:37, 29 November 2018
This article is a life support stub. You can help Lunarpedia by expanding it.
|
| This article is not yet properly formatted. You can help Lunarpedia by Editing it. Please remove this template when it is sufficiently well formatted. |
The percentages by volume of those gases found in relatively constant amounts near sea level are approximately as follows:[1]
|
ELEMENT |
% |
| nitrogen (N2) | 78.084 |
| oxygen (O2) | 20.9476 |
| argon (Ar) | 0.934 |
| carbon dioxide (CO2) | 0.0314 (variable) |
| neon (Ne) | 0.001818 |
| helium (He) | 0.000524 |
| methane (CH4) | 0.0002 (variable) |
| krypton (Kr) | 0.000114 |
| hydrogen (H2) | 0.00005 |
| nitruous oxide (N2O) | 0.00005 |
| xenon (Xe) | 0.0000087 |
In addition to the above constituents there are many that vary. Chief among these is water vapor, which may vary from zero to volume percentages close to 4 percent. Ozone, sulfur dioxide, ammonia, carbon monoxide, iodine, and other trace gases occur in small and varying amounts.
The above composition of dry air is true to about 90 kilometers. See upper atmosphere.
References
This article is based on NASA's Dictionary of Technical Terms for Aerospace Use
- ↑ This table is from the 1965 edition of the Aerospace Dictionary.
