Lakes and Reservoirs

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Lakes and Reservoirs

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If people had to pick their favorite water body, they might choose a crystal-clear lake nestled in the mountains. Not all lakes are clear or are near mountains, though. The world is full of lakes of all types and sizes.

A lake really is just another component of Earth's surface water. A lake is where surface-water runoff (and maybe some groundwater seepage) have accumulated in a low spot, relative to the surrounding countryside. It's not that the water that forms lakes get trapped, but that the water entering a lake comes in faster than it can escape, either via outflow in a river, seepage into the ground, or by evaporation. And if humans live nearby, then water levels can be affected by water withdrawals for human needs.

A reservoir is the same thing as a lake in many peoples' minds. But, in fact, a reservoir is a manmade lake that is created when a dam is built on a river. River water backs up behind the dam creating a reservoir.

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Lakes come in many varieties

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The Earth has a tremendous variety of freshwater lakes, from fishing ponds to Lake Baikal in Siberia. Lake Baikal is the world's oldest, largest, and deepest freshwater lake. Nearly a mile deep and holding over 23,000 cubic kilometers water, it would require the total volume of all the Great Lakes to fill it up if it were ever drained. (Source: NASA)

Most lakes contain fresh water, but some, especially those where water cannot escape via a river, can be classified as saline lakes. In fact, some lakes, such as the Great Salt Lake in Utah, are saltier than the oceans. Most lakes support a lot of aquatic life, but not all. The Dead Sea in the Middle East isn't called "Dead" for nothing — it is too salty for aquatic life! Lakes formed by the erosive force of ancient glaciers, such as the Great Lakes, can be thousands of feet deep. Some very large lakes may be only a few dozen feet deep — Lake Pontchartrain in Louisiana has a maximum depth of only about 15 feet.

Some of the salty lakes were formed in ancient times when they were connected to seas and when rainfall may have been heavier. These lakes have been shrinking since the last ice age. The ancient Lake Bonneville in the United States was once as big as Lake Michigan, and the Great Salt Lake was once about 14 times larger than it is now.

People use (and abuse) lakes

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Lakes are highly valued for their recreational, aesthetic, scenic, and water-supply qualities, and the water they contain is one of the most treasured of our natural resources. Lakes constitute important habitats and food resources for a diverse array of fish, aquatic life, and wildlife. But lake ecosystems are fragile. Lake ecosystems can undergo rapid environmental changes, often leading to significant declines in their aesthetic, recreational, and aquatic ecosystem functions. Exposed to external effects from the atmosphere, their watersheds, and groundwater, lakes are subject to change through time. Human activities can further accelerate the rates of change. If the causes of the changes are known, however, human intervention (lake-management practices) sometimes can control, or even reverse, detrimental changes.

Urban lakes, like this one in Seattle, Washington, are highly valued by local residents. Where urban lakes exist, you'll find lots of walkers and joggers, people enjoying canoeing and swimming, picnickers, and, of course, lots of dogs and ducks. The water can sometimes be used for water supply for a city's needs, also. Urban lakes do have special needs, though. Water quality must be monitored constantly; it would not be good for the mayor of a town to become ill from swimming in polluted water. The inflow of nutrients, such as phosphorus and nitrogen from fertilizers, must be restricted in order to prevent the overgrowth of algae. And, where there is wildlife, such as ducks, around, there is the chance of bacteria problems.

Characteristics of lakes

The following are some of the most important basic factors that give unique character to each lake ecosystem.

• Climate: Temperature, wind, precipitation, and solar radiation all critically affect the lake's hydrologic and chemical characteristics, and indirectly affect the composition of the biological community. Precipitation is the main factor affecting runoff and the delivery of nutrients and sediments.
• Atmospheric inputs: Precipitation, such as acid rain, and dry particles can be major sources of certain contaminants to a lake. Each lake also receives indirect atmospheric inputs by way of the runoff from its watershed.
• Underground rock and soils in the watershed: The soil type affects the potential for runoff and erosion. The physical characteristics of the underground rock determine the extent, nature, and quality of groundwater inflows and outflows.
• Physiography: The area, surface topography, existence of upstream lakes and wetlands, altitude, and land slope of the lake's watershed affect surface-water runoff and the amount and nature of chemicals and sediments entering the lake. Interactions with land use by people can greatly change how these factors affect runoff and the export of nutrients and sediment.
• Land use: The type, location, extent, and history of land cover/land use (such as agriculture, rural, and urban developed areas) can greatly affect the quantity of surface-water and groundwater inflows and outflows, as well as the amounts and types of sediment, nutrients and chemicals (natural or synthetic) that are transported into the lake from the watershed.
• Lake morphometry: Size, shape, and depth characteristics of a lake are critical in determining currents and mixing of the lake, as well as its thermal and chemical stratification characteristics.
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Common environmental problems in lakes and probable causes

Lakes are subject to a variety of problems that can diminish their aesthetic beauty, recreational value, water quality, and habitat suitability. Among the most common lake problems is eutrophication, which is the process of physical, chemical, and biological changes ("aging") associated with nutrient, organic matter, and silt enrichment of a lake. Eutrophic conditions can be exhibited with the following conditions:

• Algal blooms
  
  Extensive and rapid growth of planktonic (floating and suspended) algae, caused by an increased input of nutrients (primarily phosphorus, but sometimes nitrogen), is a common problem in lakes. Lakes normally undergo aging over centuries, but the process can be accelerated rapidly by human activities that cause increases in sedimentation and nutrient inflow to the lake. Accelerated eutrophication and excessive algal growth reduces water clarity, inhibits growth of other plants, and can lead to extensive oxygen depletion, accumulation of unsightly and decaying organic matter, unpleasant odors, and fish kills.
  
   
• Sedimentation/turbidity
  
  Increases of sediments can harm water quality and the habitat for many aquatic species. Such events usually are caused by heavy rains that produce erosion and intense runoff.
  
   
• Oxygen depletion
  
  Decreases in dissolved oxygen to less than 3 mg/L (milligrams per liter) in the water can be harmful or lethal to aquatic life. Oxygen can get used up due to organic decomposition. Prolonged low oxygen concentrations can lead to fish kills.
  
   
• Growth of aquatic plants
  
  Normal plant growth generally is beneficial for the lake ecosystem; among other benefits, the plants provide refuge for fish and other organisms. However, in some lakes, the growth of aquatic plants ("weeds") can become excessive and create a serious nuisance for lake users, interfering with swimming, boating, and other recreational activities. Other causes of excessive plant growth include increased nutrients in the water, invasion of exotic species, and accumulation of organic sediment.
  
   
• Water-level changes
  
  Wide fluctuations in stage (lake level) can create major hardships for lakeside residences, marinas, and businesses. These changes most commonly are linked to weather anomalies (extended periods of abnormally high or low precipitation), but also may be associated with human activities such as withdrawals for water use.
  
   
• Species shifts
  
  Populations of desirable animal and plant species might decline sharply or disappear, to be replaced by other less-desirable species. Species shifts can be caused by introduction of invasive species that may have little or no natural controls on their population growth.

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