Mooring cables, typically made of stainless steel, are attached to anchors either on the lake bottom or a nearby shoreline. The recommended cable length is at least five times the water depth, using three or four cables for stability.
Limnetics recommends a minimum anchor weight of 300 pounds per motor horsepower to ensure proper stability of the system.
The Limnetics OX pontoons and frame can be used as a barge to lift, transport, and lower the anchors into position at the lake or pond bottom.
The electrical cord is typically laid along the bottom from the Limnetics OX to just offshore, and then buried underground to reach the onshore control panel.
An outdoor-rated power cord runs from the motor junction box to a fused disconnect or motor starter panel. Limnetics recommends using a strain relief cord grip on the motor and PVC conduit for any buried sections of the cable.
To prevent freeze-up, common vegetable oil can be poured into the driveshaft housing. The oil, which is lighter than water, floats to the top and forms a soft paste when frozen. This displaces water below the freeze level and helps protect the driveshaft during winter conditions.
No. The pontoons are made of UV-stabilized polyethylene, and all other wetted parts are constructed from 304 stainless steel. For more demanding environments, 316 stainless steel is available as an option.
Yes, a washdown option is available. Contact Limnetics for detailed specifications and pricing information.
Usually not. The system’s low water velocities and broad flow area help prevent scouring, so pond liners are generally unnecessary.
Shallow, fertile (eutrophic) lakes with mucky or silty bottoms are most susceptible to winterkill. Lakes between 5 and 15 feet deep are ideal candidates for winter aeration. Lakes shallower than 5 feet usually require an external oxygen source, like a stream, to sustain game fish. Lakes deeper than 15 feet often retain enough oxygen from fall through the spring thaw.
Most game fish are at risk when dissolved oxygen levels fall below 2 milligrams per liter. Hardy species like carp and bullhead may survive at levels below 1 milligram per liter.
At room temperature and atmospheric pressure, clean fresh water can dissolve approximately 9.09 milligrams of oxygen per liter. That means it takes 2,095 gallons of water to dissolve just one ounce of oxygen.
You can measure dissolved oxygen using inexpensive chemical test kits or electronic meters. Test kits are widely available from environmental supply companies, while electronic meters typically range from $300 to $3,000. Both methods are effective for determining aeration needs.
Oxygen transfer occurs at the air-water interface. The greater the surface area, the more oxygen is transferred. While thousands of bubbles may provide only about one square foot of surface area, an acre of open water provides 43,560 square feet—excluding waves, which increase it even more.
Yes. Fish will naturally move to areas with higher oxygen concentrations if they aren't isolated by shallow sections. Additionally, the Limnetics OX creates currents that help circulate oxygenated water under ice, improving lake-wide oxygen levels even from a single site.
The anoxic bottom layer (hypolimnion) is recharged with oxygen-rich surface water (epilimnion). This oxygen helps bind manganese, iron, and phosphorus into solid forms in the sediment, preventing their release. Harmful anoxic decomposition and hydrogen sulfide production are replaced by beneficial aerobic processes.
Operating a 3 HP motor 24 hours per day typically costs about $10 per day or $300 per month, based on standard electricity rates.
Speed reducer oil should be changed every 2,500 hours of operation.
For complete destratification, the unit should be installed over the deepest part of the lake.
Continuous 24-hour operation is recommended during the stratified season, typically from May through September.
The best time to start operation is in late winter or early spring when oxygen levels are high. Initial operation may stir sediment, temporarily affecting water quality.
Removal is not required in areas with little to no ice. However, large bodies of water with shifting ice may cause damage, so removal may be advisable in those conditions.
The unit can be launched from a trailer at a boat ramp or placed by crane. It is anchored with three or four weights (400–700 lbs each). The Destratifier's own frame can be used as a barge for anchor placement. A flexible power cord rests on the lake bottom.
Water is densest at 38°F. In summer, cooler, heavier water sinks, causing stratification. The upper layer (epilimnion) is oxygen-rich, while the lower layer (hypolimnion) becomes isolated, oxygen-poor, and accumulates decomposing organic matter.
Oxygen is consumed through respiration by aquatic animals and by aerobic bacteria decomposing organic material.
Oxygen is replenished via diffusion from the atmosphere and by photosynthesis from plants and algae during daylight, especially in the afternoon when sunlight is strongest.
Bottom water in a stratified lake is cut off from air and sunlight. It does not mix with upper layers and receives no photosynthetic oxygen. Meanwhile, decomposing material uses up the available oxygen.
Oxygen depletion in the hypolimnion can eliminate game fish habitat and reduce zooplankton refuge. It also releases phosphorus, manganese, and iron from sediments, promoting algae blooms and generating hydrogen sulfide gas.
The Limnetics Destratifier circulates water to prevent or reduce stratification, especially in sheltered lakes. It stops cold, dense water from settling at the bottom by maintaining circulation throughout the lake.
A fountain circulates a small volume of water at high speed in a small area. In contrast, the Destratifier moves a much larger volume of water gently, using less energy and creating long-distance horizontal flows for effective whole-lake circulation.
A diffused air bubbler lifts water using rising bubbles, but this method uses more energy than the propeller-driven flow of the Destratifier. Like fountains, bubblers often create small circular flow zones rather than wide, lake-spanning currents.
Oxygen is transferred through photosynthesis and at the air-water surface. Moving large volumes of oxygen-poor water to the surface maximizes contact area, making oxygen transfer more efficient than using small bubbles alone.