Week 3: Hydro cycle, and the physiology of ground water and wetland Flashcards
Describe the Hydro cycle
this describes how water moves around the planet (large scale)
- > Most FW comes from ocean evaporation powered by solar energy
- > condenses, comes down as precipitation
Describe precipitation trends
Due to air/ocean, the western part of NA most rainy, also along the equator
- > Most all rain = fw, some enters plants through transpiration
- > infiltrates soil or runs off as surface water (water yield, water that doesn’t become infiltrated)
Water infiltration layers
- 4 zones, unsat zone, capillary fringe (adhesion, water travel) water table (where the boundary of unsat and sat meet)
- > saturated zone is where the aquifers are
- > unconfined (changes in size, connected to the water table
- > COnfined, deepest, impenitrable
What is percolation
describes flow of water through particles
- > Texture and composition play a part
- > the rate of pertulation into saturated zone (regarge of aquafir)
Hydraulic conductivity
rate of water flow through soil, dependent of permeability, measures in meters per day
porosity
amount of water held in empty spaces between particles (must be connected spaces
Groundwater types
Homo or hetero (how predictable the flow is and variation of soil)
- Karst landforms (escarpment) underlakes, on surface and then goes underneath
Hyporthic zone
The hyporheic zone is the region of sediment and porous space beneath and alongside a stream bed, where there is a mixing of shallow groundwater and surface water.
- > extange of nutrence
- > this varries
How to define a wetland
as there is a ton of variability, leading to many sub habitats in a single ecosystem
- > has hydrophyte plants (love water)
- > hydraulic-soil }lots of water, top anaerobic, ton of organic soil on top
What are wetland functions
- > Natural filters of containments
- > HUGE carbon sinks
- > drainage for agriculture systems and flooding (often filled in to use more for agi or land use)
Where are wetlands located
-> near large bodies of water or at high altitudes ( since cool, less evap, more water stays)
Coastal wetland types
Tidal salt march (brackish, fresh further inland, filled in by tides, lots of variation) Mangrove swamp (SE asia, tsunamic control, salty with low o2 in water need special roots) Floating marsh ( Floating mass of plants, common in deltas w low floods)
Inland wetlands
some depressional formed other near bodies of water
- swamps (dominated by trees) Marches (by hurbacious shrubs)
- Riparian wetlands (adjacent to rivers and lakes, often flooded, the advantage to some plants
- pothole wetlands (in plains to missispi) Depression, saline due to evaporation leaving sediments
- Peatlands (acuumilate organic matter, w little decom (cold temp)
- Peatlands
(acuumilate organic matter, w little decom (cold temp)
Bog: acidic, low water flow, not diverse
Fen: run off or grounwater, alkaline high diversity
Smaller wetlands
are e[hermal, caused by snow or percip
ex// verinal pools in forests, alligators making their own for catch food