Pond and People Management

Reader Contribution by Kenneth Rust
Published on November 18, 2013
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I enjoy speaking on pond management and teaching its fundamentals. One of the ways I begin my talks is to

let people know: It’s not always pond management, it’s often people management. People, their effects on the input to the pond, and their expectations of what the pond can do for them are the things I deal with the most. Contrasting uses for a pond can result in frustration. Actions have reactions, and finding out the root causes for a pond’s behavior is the key.

Ponds aren’t mysterious; they are behaving exactly as they should, based on their circumstances, and are actually pretty predictable. As with a lot of things, there are fundamentals to any subject and focusing on them as you begin is a good idea. A few “big picture” fundamentals on pond behavior:

Ponds are aging and trying to turn into land. As a part of natural succession, ponds generally are filling and losing volume to plant life and organic material. Some are doing this slowly, but some ponds seem to be transforming rapidly before our eyes on a seasonal basis. Each season ponds receive input from the watershed and environment: leaves, grass clippings, thatch, water runoff, erosion, and manure from fish, waterfowl, and livestock. The ecosystem digests this liquid compost, but generally not to completion each year, leaving residual organic sludge in your pond. As the volume of sludge builds over the years, it provides a bank of nutrients for the ecosystem, and creates chemical and biological demands on oxygen in the pond.

Pond ecology needs oxygen. There are two sources: mixing from weather, and photo synthesis. Submerged plants and algae provide oxygen through photosynthesis during daylight hours and respire at night, consuming some of the day’s oxygen and producing carbon dioxide. Wind, and rain and the resulting energy from wave action help to mix ponds and bring water in contact with the atmosphere for some healthy “breathing action.”

Ponds make well-defined temperature layers in the warm season. In warmer months, sunlight heats water near the surface. In addition, sunlight has limited penetration into the water column, and increases the production of single cell algae, called phytoplankton, darkening the surface water to a familiar green tint. The dark water further limits the penetration of sunlight.

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