Figure 3 - uploaded by Victor F. Medina
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Stratification in a lake, found typically in the summer. Solid line indicates temperature trend while dashed line represents DO. The red region is considered the epilimnion, green thermocline/metalimnion, and blue the hypolimnion defined by the sharp temperature changes/differences between the regions. 

Stratification in a lake, found typically in the summer. Solid line indicates temperature trend while dashed line represents DO. The red region is considered the epilimnion, green thermocline/metalimnion, and blue the hypolimnion defined by the sharp temperature changes/differences between the regions. 

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Technical Report
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Koontz Lake is located in northern Indiana. The lake has had problems with eutrophication, harmful algae, invasive plants, and shallowing due to accumulation of sediment and muck. A study was conducted to assist in evaluating between two ecological restorative options under consideration: aeration and dredging. In this report, both approaches are d...

Contexts in source publication

Context 1
... stratification refers to a condition in which a physical gradient, such as temperature, serves to limit or restrict mixing in the lake. Stratification commonly occurs in summer when solar heating at the surface creates a high temperature region called the epilimnion ( Figure 3). Cooler, denser water is found with depth in the hypolimnion. ...
Context 2
... Lake, like most lakes in the U.S. Midwest, undergoes this stratification pattern. DO levels are closely linked to thermal stratification where the persistence of a thermocline inhibits the atmospheric diffusion of oxygen into the hypolimnion (Figure 3). Furthermore, light-harvesting autotrophs such as phytoplankton release oxygen at or above the thermocline where sunlight is readily available, contributing to a greater oxygen pool in surface waters. ...
Context 3
... natural aeration in lakes tends to be largely at or near the surface (via diffusion, turbulence/mixing, and photosynthetic inputs as mentioned above). Consequently, the near surface tends to have the highest oxygen concentrations (Figure 3). Wind and current mixing can keep oxygen levels relatively high for depth of 1 meter (m) or so, but at increasing depth oxygen diffusion can become more limited, particularly if the lake is highly stratified. ...

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