In a stable body of water with no stratification, DO will remain at 100% air saturation. The 100% air saturation means that the water is holding as many dissolved gas molecules at it can in equilibrium. At equilibrium, the percentage of each gas in the water would be equivalent to the percentage of that gas in the atmosphere, which is known as its partial pressure.
The water will slowly absorb oxygen and other gases from the atmosphere until it reaches equilibrium at complete saturation. This process is sped up by aeration. It is possible for DO to exceed 100% air saturation in water by biological means.
The post What is Dissolved Oxygen saturation? first appeared on Pathfinder Instruments.
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