Oxygen the water can hold–
Root oxygen demand vs 20 °C–
Root zone–
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Oxygen falls as water warms

The oxygen readout uses a standard curve fit for fresh water at sea level: DO = 14.652 minus 0.41022 T plus 0.007991 T squared minus 0.000077774 T cubed, with T in degrees Celsius. It gives about 9 mg/L at 20 °C and about 7.4 mg/L at 30 °C.

That is the most the water can hold when fully mixed with air. Real tanks run a little below it, which is why bubbling never stops.

Try it: slide the temperature from 18 to 30 °C. The water's oxygen capacity drops by nearly 2 mg/L while root demand roughly doubles, and the plants start to yellow. Many growers chill the solution to the high teens or low 20s for this reason.

Demand rises too

Root respiration speeds up with temperature. Biologists often use a Q10 of about 2, meaning the rate doubles for every 10 °C rise. The demand readout uses that rule of thumb relative to 20 °C, so it is a simplified teaching model rather than a measurement.

How to cite this model

Avid Solutions International. (2026, November 11). Why deep water culture needs bubbles [Interactive 3D model]. Avid Field Lab. https://avidsolutionsintl.com/explore/deep-water-culture

Last updated November 11, 2026

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