Up to 70% of a wastewater plant’s energy budget is spent powering their aeration system. For years, these aeration systems were controlled by manually changing the airflow set point, valve positions or speed of the motor because membrane DO sensors were unreliable. LDO allows the systems to automatically control the aeration to a certain DO set point, allowing the blowers to respond to the loading in real time and saving 30 to 60% in energy costs.
Dissolved oxygen is necessary to many forms of life including fish, invertebrates, bacteria and plants. These organisms use oxygen in respiration, like organisms on land. Fish and crustaceans obtain oxygen for respiration through their gills, while plant life and phytoplankton require dissolved oxygen for respiration when there is no light for photosynthesis. The amount of DO needed varies from creature to creature. Bottom feeders, crabs, oysters and worms need minimal amounts of oxygen (1-6 mg/L), while shallow water fish need higher levels (4-15 mg/L). Bacteria and fungi also require dissolved oxygen. These organisms use DO to decompose organic material at the bottom of a body of water. Microbial decomposition is an important contributor to the nutrients cycle. However, if there is an excess of decaying organic material (from dying algae and other organisms) in a body of water with infrequent or no turnover (also known as stratification), the oxygen at lower water levels will be used up quicker.
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.
Dissolved oxygen concentration will increase as pressure increases. This is true of both atmospheric and hydrostatic pressures. Water at lower altitudes can hold more DO than water at higher altitudes. This relationship also explains the potential for "supersaturation" of waters below the thermocline. At greater hydrostatic pressures, water can hold more DO without it escaping and therefore, dictate lower DO saturation at the same concentration. Gas saturation decreases by ~10% per meter increase in depth due to hydrostatic pressure, given the water temperature is constant. This means that DO at the same concentration can be at 100% air saturation at the surface and it would only be at 70% air saturation 3 meters below the surface.
Two bodies of water that are both 100% air-saturated do not necessarily have the same concentration of DO. The amount of dissolved oxygen (in mg/L) will vary depending on temperature, pressure and salinity.