Unit 3-Freshwater Systems Flashcards
Wetlands
• Systems that combine elements of fresh water and dry land
• Extremely rich and productive
• Slows runoff, reduces flooding, recharges aquifers and filters pollutants
Many have been drained and filled for agricultural purposes
Composed of freshwater marshes, swamps, bogs
Freshwater marshes
○ Shallow water allows plants to grow above water’s surface
Cattails and bulrushes common in North American marshes
Swamps
○ Also contain shallow water rich in vegetation, but occur in forested areas
Can be created when beaver build dams across streams, flooding wooded areas upstream
Bogs
Ponds thoroughly covered with thick floating mats of vegetation
Lakes and Ponds:
• Bodies of open standing water
Several different zones, since physical conditions and types of life within them vary depending on depth and distance from shore
Littoral Zone
§ Region ringing the edge of a water body
§ Water is shallow enough that aquatic plants grow from the mud and reach above the water’s surface
Nutrients and productive plant growth make region rich in invertebrates (larvae. sails, crayfish), provides food for fish, birds…etc
Benthic Zone
§ Extends along bottom of entire water body (from shore to deepest point)
§ Many invertebrates live in the mud on the bottom, feeding on detritus (organic matter fragments) or preying on each other
Can be photic or aphotic (can be shallow enough for light to penetrate)
Limnetic Zone
§ Open portion of lake or pond, away from the shore
§ Lots of light (in the photic zone), supports phytoplankton, which support zooplankton
□ Phytoplankton and zooplankton are then both eaten by fish
§ Sunlight intensity and water temperature decreases with depth
Clear water allows sunlight to penetrate deeply, turbid water does not
Profundal Zone
§ In the aphotic zone (sunlight does not reach here)
Lacks plant life, lower in dissolved oxygen and supports fewer animals
Oligotrophic lakes and ponds
• Oligotrophic lakes and ponds have low nutrient and high oxygen conditions, can slowly give way to high nutrient, low oxygen conditions of eutrophic lakes and ponds
Animals living under oligotrophic conditions adapt to eutrophic conditions
Ground Water and the Hydrologic Cycle:
• Any precipitation reaching Earth’s surface that does not evaporate, flows into waterways, or is taken up by organisms become groundwater
• Becomes surface water again through springs and wells
• Flows downhill and from areas of high press to low pressure, emerging to join surface water bodies at discharge zones
Groundwater makes up one fifth of the Earth’s freshwater supply
Aquifers:
Porous formations of rock, sand, or gravel that hold ground water
Zone of aeration
Zone of saturation
Water table
Recharge zone
Zone of aeration
§ Upper layer
Contains pore spaces partly willed with water
Zone of saturation
§ Lower layer
Pore spaces completely filled with water
Water table
○ Boundary between zone of aeration and zone of saturation known as the water table
Below the water table, all pore spaces are completely filled with water, above the water table, some pater is present in spaces, but the ground is not completely saturated