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Lentic Systems

Lentic Systems. Lakes and Ponds. Formation of Lakes. Glacier lakes Oxbow lakes Playas Man-made lakes. Glacier Lakes. Carved out by glaciers (glaciation), which fill with water Northern U.S. and Canada. How Does Glaciation Work?.

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Lentic Systems

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  1. Lentic Systems Lakes and Ponds

  2. Formation of Lakes • Glacier lakes • Oxbow lakes • Playas • Man-made lakes

  3. Glacier Lakes • Carved out by glaciers (glaciation), which fill with water • Northern U.S. and Canada

  4. How Does Glaciation Work? • As the glaciers move they act as scouring pads on the ground underneath them. • Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat • A retreating glacier often left behind large deposits of ice in hollows between hills which later melted to create lakes. • Rocks are eroded and mineral deposits become sediments at the bottom of the lake • Some suspended minerals are used by algae for growth, making the water appear green

  5. The Great Lakes in northern U.S. are the largest glacial lakes in the world.

  6. The Seven Rila Lakes in Rila, Bulgaria Lake Jokulsarlon, in Iceland.

  7. Oxbow Lakes • Formed by meandering rivers • Loops of river gets cut off • Lakes are long and narrow, and usually U-shaped • Common in low valleys and flat coastal areas

  8. Oxbow Lake • An oxbow in the making: meanders and sandbank deposition on the Nowitna River, Alaska

  9. How Does an Oxbow Lake Form? (1) On the inside of the loop, the river travels more slowly leading to deposition of silt.

  10. (2) Meanwhile water on the outside edges tends to flow faster, which erodes the banks making the meander even wider. (3) Over time the loop of the meander widens until the neck vanishes altogether.

  11. (4) Then the meander is removed from the river's current and the horseshoe shaped oxbow lake is formed. -- Without a current to move the water along, sediment builds up along the banks and fills in the lake.

  12. Oxbow Lake • Oxbow lake and the Chippewa River in Eau Claire, Wisconsin.

  13. Playas • Formed from multiple things that leave a depression • Soil erosion, wind, animal herds • Small, shallow, and circular • Common in dry plains areas • These lakes are ephemeral, and only form at certain times of the year

  14. Playas are important habitat for migratory birds and waterfowl. • The Red-winged Blackbird, Blue-winged Teal, and the Mallard can all be found in playa lakes at some time of the year. 

  15. Sandhill cranes winter in playa lakes

  16. Playa lakes in Kansas agricultural area

  17. Man-Made Lakes • Water reservoirs formed from • Damming rivers • Old rock quarries or mines • Stock ponds on farms and ranches Lake Mead is formed as a result of damming the Colorado River by the Hoover Dam in Nevada

  18. Zipingpu Dam on the Min River in China

  19. Lentic Habitats • Characterized by • The shoreline • The sides of the basin • The surface of the water • The bottom sediments

  20. Zones of Lentic Habitats • Littoral zone • Limnetic zone • Profundal zone

  21. Littoral Zone • Along shore where light can penetrate to the bottom • Rooted plants can grow • Shores have coarse sediments from action of waves • Sheltered areas have finer sediments (silt and clay) – plant growth in this zone • Animal life includes • Invertebrates common to lotic habitats • Small fish

  22. Limnetic Zone • Upper open water area of a pond or lake • Lack of rooted plants because light can’t penetrate the bottom • Plankton and fish are common

  23. Profundal Zone • Deep, bottom-water area • No light penetration • No photosynthetic organisms or rooted plants • Sediments are silt and clay mixed with organic matter that settles to the bottom • Organisms living here are tolerant of little or no light or oxygen.

  24. Biological Productivity • The amount of plankton, algae, aquatic macroinvertebrates and fish that a body of water can produce and sustain • Usually limited to the depth of light penetration • Light penetration is limited by color of the water and amount of suspended solids

  25. Ponds vs. Lakes • Pond = body of water where light penetrates all the way to the bottom • Lake = depth of light penetration varies from several inches to several feet

  26. Determining the Trophic State • Total Plant Nutrients • Phosphorous and nitrogen are needed for plant growth and maintenance • Certain level is needed (too much or too little is not a good thing) • If nutrients are too high, algae blooms occur • Increase the turbidity of the water • Decrease the oxygen levels

  27. Chlorophyll A • Measure of the algae population • Influenced by the amount of nutrients • Water Clarity (turbidity) • Water clarity determines how far light can penetrate • Phytoplankton and plants need light to grow, so they won’t grow if light is limited • Algae blooms cause lower water clarity

  28. Characteristics of Biological Productivity • 4 categories of lake classification based on biological productivity • Oligotrophic • Mesotrophic • Eutrophic • hypereutrophic

  29. Oligotrophic Lakes • Nutrient level and productivity is low • Water is clear • Low aquatic plants and plankton • Few fish • Sandy bottoms with little organic material

  30. Mesotrophic Lakes • Nutrients and productivity is moderate • Some aquatic plants • Water clarity is becoming somewhat cloudy

  31. Littoral habitat in a mesotrophic lake

  32. Eutrophic Lakes • Nutrient level and productivity is high • Large populations of algae, plankton, fish, plants, and macroinvertebrates • Frequent plankton blooms • Sediments with high organic matter • Water is commonly colored

  33. Hypereutrophic • Nutrient levels and productivity are very high • Large populations of aquatic plants and animals • Frequent plankton blooms • Sediments with most organic matter

  34. Ponds and Shallow Lakes • Temperature and dissolved oxygen remains about the same from top to bottom • Water is easily mixed by the wind • Photosynthesis and plant growth can occur from top to bottom (since light can penetrate all the way down)

  35. Deep Lakes • Water temperature and dissolved oxygen levels can remain same from top to bottom layers in the winter • During warm summer months, layers form • The surface if warmed up by the sun • Denser, colder water remains below it • Doesn’t get mixed by the wind

  36. Fall Turnover

  37. Effects of Turnovers • Mixing of once layered water returns oxygen levels to the deep areas. • Areas in the south have one turnover per year in the fall. • In the north, lakes become stratified in the summer and the winter (because ice forms on the surface, causing inverse stratification). Thus, there are two turnovers (fall and spring).

  38. Zones of Stratification • Three distinct layers form in deep lakes during the summer months: • Epilimnion • Metalimnion • Hypolimnion

  39. Epilimnion • Warmest zone near the surface • Circulates freely with varying temperatures according to location on the globe • Wind and currents mix surface water • Most organisms found in this layer • Area of greatest productivity • Greatest light penetration • Greatest oxygen content

  40. Metalimnion • Middle layer • Steep declines in temperature (area of the thermocline) • Temp. decreases 1oC per meter of depth

  41. Hypolimnion • Third layer • Deep and cold with little to no temperature change • Low oxygen due to few or no plants • Little to no mixing by wind • Bottom-dwelling organisms and bacteria feed on organic matter and further deplete the oxygen • Little or no light penetration

  42. Ecological Succession • Lakes and ponds evolve differently then flowing water ecosystems. • Over time, sediments become higher on the floor of ponds and lakes, and build up. The shallower the lake becomes, the further light can penetrate, so more plants grow on the bottom. • Water tolerant plants and shrubs move in. • Marshes, swamps, and bogs are usually the mature stage of a lake.

  43. A lake gradually fills with organic and inorganic sediments, shrinking the area of the pond • A bog forms, then a marshy area • Finally, a meadow completes the succession stages

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