This section from Randy H. Farley's article on seawater explains saturation levels and athospheric gas levels in seawater :
Dissolved Atmospheric Gases
<hr align="left" size="1px" width="75%" color="#006699"><table align="right" width="43%" cellpadding="2" cellspacing="2"> <tbody><tr> <td> <table align="right" bgcolor="#E8FAFF" border="2" width="300"> <tbody><tr bgcolor="#006699"> <td colspan="2">
[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1] Table 4. Atmospheric gases in seawater at 25°C when in equilibrium with air.[/SIZE][/FONT]
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Gas[/SIZE][/FONT]</td> <td width="139">
[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1]Concentration[/SIZE][/FONT]
</td> </tr> <tr> <td width="143">[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1]
Carbon dioxide (as HCO<sub>3</sub><sup>-</sup> and CO<sub>3</sub><sup>--</sup>)[/SIZE][/FONT]</td> <td width="139">
[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1] 100 ppm of CO<sub>2</sub>[/SIZE][/FONT]
</td> </tr> <tr> <td width="143">[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1]
Nitrogen (N<sub>2</sub>)[/SIZE][/FONT]</td> <td width="139">
[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1] 10.7 ppm[/SIZE][/FONT]
</td> </tr> <tr> <td width="143">[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1]
Oxygen (O<sub>2</sub>)[/SIZE][/FONT]</td> <td width="139">
[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1] 6.6 ppm[/SIZE][/FONT]
</td> </tr> <tr> <td width="143">[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1]
Argon (Ar)[/SIZE][/FONT]</td> <td width="139">
[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1] 0.40 ppm[/SIZE][/FONT]
</td> </tr> <tr> <td width="143">[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1]
Neon (Ne)[/SIZE][/FONT]</td> <td width="139">
[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1] 0.13 ppb[/SIZE][/FONT]
</td> </tr> <tr> <td width="143">[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1]
Helium (He)[/SIZE][/FONT]</td> <td width="139">
[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1] 0.0066 ppb[/SIZE][/FONT]
</td> </tr> <tr> <td width="143">[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1]
Krypton (Kr)[/SIZE][/FONT]</td> <td width="139">
[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1] 0.185 ppb[/SIZE][/FONT]
</td> </tr> <tr> <td width="143">[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1]
Xenon (Xe)[/SIZE][/FONT]</td> <td width="139">
[FONT=Georgia, Times New Roman, Times, serif][SIZE=-1] 0.038 ppb[/SIZE][/FONT]
</td> </tr> </tbody></table> </td> </tr> </tbody></table>
Any gas present in the atmosphere will be present in seawater. Many of these are unimportant to reef aquarists, but two are of critical importance: oxygen and carbon dioxide. Aside from carbon dioxide, all of the gases have lower solubility in seawater as the temperature and salinity are raised. Table 4 shows the concentration of the most common gases in seawater at 25°C.
Oxygen is generally most highly concentrated near the ocean's surface. In the top 50 meters or so, oxygen's concentration is controlled largely by exchange with the atmosphere, and is usually close to equilibrium with the air. Between 50 and 100 meters, the O[SIZE=-1]2[/SIZE] level often rises due to photosynthesis. Below about 100 meters in the open ocean the oxygen level drops steadily for the next 1000 meters or so due to biological processes that consume it. It then sometimes rises again in the deeper oceans as oxygen there is replenished by sinking cold ocean water that is rich in oxygen. The importance of dissolved oxygen in seawater and reef aquaria has been discussed in a series of previous articles:
The Need to Breathe in Reef Tanks: Is it a Given Right?
http://www.reefkeeping.com/issues/2005-06/eb/index.php
The Need to Breathe, Part 2: Experimental Tanks
http://www.reefkeeping.com/issues/2005-07/eb/index.php
The Need to Breathe, Part 3: Real Tanks and Real Importance
http://reefkeeping.com/issues/2005-08/eb/index.php
Carbon dioxide is a special case. It hydrates on contact with water to form carbonic acid, which can then ionize (break apart) to from hydrogen ions, bicarbonate and carbonate, as shown below.
CO<sub>2</sub> + H<sub>2</sub>O ßà H<sub>2</sub>CO<sub>3</sub> ßà H<sup>+</sup> + HCO<sub>3</sub><sup>-</sup> ßà 2H<sup>+</sup> + CO<sub>3</sub><sup>--</sup>
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[SIZE=-1]Table 5. Fate of carbon dioxide in the ocean after 1000 years.[/SIZE]
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Form/Location[/SIZE]
</td> <td width="125">
[SIZE=-1]Percentage[/SIZE]
</td> </tr> <tr> <td width="157">[SIZE=-1]
CO<sub>2</sub> in the atmosphere[/SIZE]</td> <td width="125">
</td> </tr> <tr> <td width="157">[SIZE=-1]
CO<sub>2</sub>/H<sub>2</sub>CO<sub>3</sub> in the ocean[/SIZE]</td> <td width="125">
</td> </tr> <tr> <td width="157">[SIZE=-1]
HCO<sub>3</sub><sup>-</sup> in the ocean[/SIZE]</td> <td width="125">
</td> </tr> <tr> <td width="157">[SIZE=-1]
CO<sub>3</sub><sup>--</sup> in the ocean[/SIZE]</td> <td width="125">
</td> </tr> <tr> <td width="157">[SIZE=-1]
Organics on land[/SIZE]</td> <td width="125">
</td> </tr> <tr> <td width="157">[SIZE=-1]
Organics in the ocean[/SIZE]</td> <td width="125">
</td> </tr> </tbody></table> </td> </tr> </tbody></table>
For this reason, carbon dioxide is much more soluble in seawater than is any other atmospheric gas. It is more soluble than all the other gases combined, in fact, with a total solubility of about 100 ppm of carbon dioxide. An interesting question to ask is, "What happens to carbon dioxide that is mixed into the ocean?" After 1000 years, it is thought that it ends up in the forms shown in Table 5.
Additional discussion of carbonate and bicarbonate in seawater is provided in subsequent sections of this article.
Many other gases are dissolved in seawater, but it is beyond the scope of this article to describe all of them. Many have biological significance, including hydrogen sulfide (H[SIZE=-1]2[/SIZE]S), methane (CH[SIZE=-1]4[/SIZE]) and other organic gases, carbon monoxide (CO), hydrogen (H[SIZE=-1]2[/SIZE]) and nitrous oxide (N[SIZE=-1]2[/SIZE]O).
The complete article can be found here:
http://reefkeeping.com/issues/2005-11/rhf/index.php#8