DISSOLVED OXYGEN IN RESERVOIRS
In most real systems,
circulation and strong surface movement put more dissolved oxygen (DO) into water than air stones do.
The reason comes down to
gas exchange physics. Oxygen enters water mainly at the
airβwater interface. The faster that interface is refreshed and mixed, the faster oxygen dissolves. Surface turbulence continually replaces oxygen-depleted water with fresh water at the surface.
Air stones mainly help by
moving water, not by dissolving much oxygen directly.
Important points:
β’ The bubbles themselves transfer
relatively little oxygen.
β’ Most bubbles
reach the surface before dissolving much Oβ.
β’ Their real value is
circulation and surface agitation created by rising bubbles.
Fine-bubble diffusers improve transfer somewhat, but the effect is still modest compared with aggressive surface mixing.
What actually gives the highest DO?
In descending order of effectiveness (generally):
- Waterfalls / strong surface turbulence
- Venturi injectors or spray bars
- Strong circulation pumps aimed at the surface
- Air stones / bubble diffusers
Important limit
Water can only hold oxygen up to
saturation, which depends mostly on temperature.
Approximate maximum DO at sea level:
| Water temp | Max dissolved Oβ |
|---|
| 68Β°F (20Β°C) | ~9 mg/L |
| 77Β°F (25Β°C) | ~8.3 mg/L |
| 86Β°F (30Β°C) | ~7.5 mg/L |
Warmer water holds
less oxygen, which matters for hydroponics and reservoirs.
I run both a circulation pump and a big air stone for backup, plus my 1/2" feeder line returns back to the res, pushing a good stream.