Week 3: Hydro cycle, and the physiology of ground water and wetland Flashcards

1
Q

Describe the Hydro cycle

A

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
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2
Q

Describe precipitation trends

A

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)
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3
Q

Water infiltration layers

A
  • 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
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4
Q

What is percolation

A

describes flow of water through particles

  • > Texture and composition play a part
  • > the rate of pertulation into saturated zone (regarge of aquafir)
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5
Q

Hydraulic conductivity

A

rate of water flow through soil, dependent of permeability, measures in meters per day

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6
Q

porosity

A

amount of water held in empty spaces between particles (must be connected spaces

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7
Q

Groundwater types

A

Homo or hetero (how predictable the flow is and variation of soil)
- Karst landforms (escarpment) underlakes, on surface and then goes underneath

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8
Q

Hyporthic zone

A

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
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9
Q

How to define a wetland

A

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
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10
Q

What are wetland functions

A
  • > Natural filters of containments
  • > HUGE carbon sinks
  • > drainage for agriculture systems and flooding (often filled in to use more for agi or land use)
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11
Q

Where are wetlands located

A

-> near large bodies of water or at high altitudes ( since cool, less evap, more water stays)

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12
Q

Coastal wetland types

A
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)
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13
Q

Inland wetlands

A

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)
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14
Q
  • Peatlands
A

(acuumilate organic matter, w little decom (cold temp)
Bog: acidic, low water flow, not diverse
Fen: run off or grounwater, alkaline high diversity

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15
Q

Smaller wetlands

A

are e[hermal, caused by snow or percip

ex// verinal pools in forests, alligators making their own for catch food

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16
Q

Key characteristics

A

permanence, predictability and seasonality } influences tha amount of diversity
-> more perm , more diversity, more complex food web
Variability opens it to more colonizing of wetlands

17
Q

Sources of wetland

A

Ephermal wetlands } source is rainwater, could only exist during wet season
Surface water from runoffs common
If groundwater, most constant/permenent

18
Q

How is CC affecting it

A

Warming temperatures are (1) inc evaporation (2) changing precip patterns (3) Increased the decom rate, makes it less of a carbon sink, releases carbon int the atmosphere