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DAT Biology > limnology exam 3 > Flashcards

limnology exam 3 Flashcards

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1
Q

3 legal criteria used to define wetlands

A

1) water saturation: frequent or prolonged presence of water at or near the soil surface
2) Vegetation: adapted to wet/waterlogged soils
- is there vegetation present? have they adapted
ex: hydrophytes- there’s a federal list of species
3) presence of hydric soil
- soils presently soaked with water develop certain chemicals
- >waterlogged (saturated)
- >anoxic, high in organic matter content

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2
Q

wetland classificaitons based on vegitation

A
  • emergent wetlands
  • forested wetlands
  • scrub/shrub wetlands
  • shallow water/pond wetlands
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3
Q

emergent wetlands

A

plants have roots in water, but stems and leaves growing out of water-emerging out of water

  • dominated by grasses, sedges, rushes, forbs (non-woody)
  • marshes, wet meadows, fens
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4
Q

forested wetlands

A

trees present, saturated soils= swaps

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5
Q

scrub/shrub wetlands

A

oftern border a lake or stream
lots of shrubs, plants
have a little bit of everything

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6
Q

shallow water/pond wetlands

A

aquatic macrophytes present

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7
Q

hydrology based categorization of wetlands

A

fens
bogs
swamps/marshes

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8
Q

fens

A

mostly fed by groundwater

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9
Q

bogs

A

mostly precipitation fed

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10
Q

swamps/marshes

A

fed mostly by surface flow (streams, rivers, floodplains, beaver ponds)

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11
Q

Wetland functions

A
  1. Habitat-biodiversity hotspots
  2. flood attenuation
  3. Water quality
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12
Q

Wetland function: Biodiversity hotspots

A

Wetlands have lots of biodiversity
difficult to generalize
provide habitat for ducks- fish and wildlife habitat nursery
3/4 of WI wildlife species are dependent on wetlands
>1/3 of US threatened and endangered species live only on wetlands
so they are considered biodiversity hotspots

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13
Q

Wetland function: flood attenuation

A

wetlands are places to store water
act like a sponge
water enters quickly (during a flood) but leaves slowly

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14
Q

Wetlands function: water quality

A

1) reduce water velocity
2) Wetlands plants take up nutrients
3) waterlogged soil effects

4)Overall wetland effect on nutrients
5) Other consequences of waterlogged soils:
decomp slows
organic carbon

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15
Q

1) reduce water velocity

A

-> so sediments settle out
good for fish
good for P levels as P sticks to sediment particles, so P enters wetlands and may not leave

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16
Q

2) Wetlands plants take up nutrients

A

2) Wetlands plants take up nutrients- so no excess nutrients go into the environments

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17
Q

3)waterlogged soil effects:

A

in normal soils, soil particles + air pockets = lots of O2 all the way through the soil
but water logged soils are anoxic
waterlogging eliminates O2 form the soil, so therefore hydric soils are often anoxic
so usually in waterlogged soils, O2 is gone within millimeters
effects: No O2 -> Denitrification (NO3- -> N2 gas) eliminate nitrate from the soil
therefore wetlands prevent dead zones

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18
Q

Overall wetland effect on nutrients

A

wetlands can reduce (but not eliminate) sediments, excess nutrients

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19
Q

other waterlogged soils

A

water logging slows microbial respiration
Organic C + O2 -> CO2 + H2O
no O2 so different microbes present so less decomposition and so organic matter accumulates which is why these soils are so rich in organic matter
i.e they have a carbon storage function
Peat= partially decayed plant material
-about 40% of terrestrial C is stored in peat soils-
predominantlyy in N. America and Eurasia= arctic places
important for locking away carbon
-wetlands can have diverse plants Ex: sphagnum moss which stores for long periods of time, makes environment acidic, important for agriculture
-peat-> millions of years to coal
-arctic permafrost thaw: thaws so locked up C going back into Circulation
-Boreal peatland flow: burning organic C -> turns it into CO2

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20
Q

Channel form reflects a balance between?

A

channel form reflects a balance between
1, sediment inputs
2. channel slope-building dams changes this
3. the river’s hydrology

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21
Q

Stream and river habitat

A

water column:since there is a current= unidirctional fow
benthic zone: upper, well oxygenated sediment layer
hyporheic zone: mixing zone between stream water and groundwater. meet and miz below the benthic zone
riparian zone/floodplain: terrestrial-aquatic interface

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22
Q

Discharge

A

Q, units: m^3/s
volume of water passing through a channel cross-section per unit time
Q=V x A

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23
Q

Hydrograph

A

graph of discharge over time

Q vs time

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24
Q

Habitat

A

water column: since there is a current= directional flow
-benthic zone: upper well oxygenated sediment layer
hyporheic zone: mixing zone between stream water + groundwater meet and mix-below benthic zone
riparian zone/floodplain: terrestrial-aquatic interference

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25
Q

flow regime

A

-characteristic discharge pattern of a river over time: magnitude, frequency, duration, timing, rate of change
-reflects regional climate, geology, and human alterations to rivers
-can be used to identify determinants of stream community composition
-also used to access extent of human alteration
>change in flow regimes over time
ex: Illinios river- dam built, coal mining so they stabilized the river, and developed farm land around it

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26
Q

Temperature in stream and rivers

A

no thermal stratification- stream and rivers are well mixed
have greater thermal variation than in lakes
variation affected by
-stream order
-groundwater inputs
small streams are in forests so shaded, and as stream size increases, less thermal buffering/inputs from groundwater

27
Q

light in streams and rivers

A

2 controls:

  • surrounding conditions: trees, canyons, banks
  • water characteristics: depth, suspended and dissolved material
28
Q

Small streams (light)

A

can either recieve lots of light or very little light based on geography and season- streams in desert get lots of light, but strea0ms in forest recieve little light
for shallow stream, light can reach bottom

29
Q

Large rivers (light)

A

recieve lots of light due to open canopy
light rarely reaches bottom
water in large rivers usually turbid (cloudy, thick with suspended material)
not a lot of benthic communities present, present mostly near top

30
Q

chemical condtions

A

-vertical stratification is rare
DO- rivers are well mixed so DO generally very high
>due to big air/water interface
>mixing due to turbulent water flow
-some exceptions,O2 problems in streams below sewege outfalls
steams that are slow, warm also have DO problems
-Hyporheic zones often have low O2- so different chemical reactions happen here

31
Q

Biota in rivers

A

-major force of driving evolution of lotic organisms= adapting to flowing water
-such as: maintaining position, surviving flow extremes (flooding and drying), eating
-Some adaptations to flow:
>staying put: hooks, claws, suction cups, balast, body shape- to deal with oncoming flow
>taking advantage of flow: filter feeders- very common among benthic invertebrates ex: hawaiian gobi- crawl up waterfalls

32
Q

Biota in small-medium stream

A

shallow, physically variable, may have lots of light

  • no plankton! benthic organisms dominate, periphyton (FW organisms that cling to plants or other organisms)
  • lots of macroinvertebrates also present
  • small fish present
33
Q

large rivers biota

A

deep, turbid water, range of flow velocities
-plankton develop since eep
benthic invertebrates-restricted to lateral areas as in lakes, on sides in shallow areas
big fish present ex: paddle fish, lake sturgeon spawn in river

34
Q

reservoirs distribution and abundance

A

20% of global anual runoff is stored in revervoirs
everywhere and lots-3 years worth of rain/water can be stored in some reservoirs
between 1/3 to 1/2 watersystems are severely impacted by reservoir
over 3500 dams in WI
mostly built for farming and livestock

35
Q

reservoir types

A

1) flow modification
-run of river
-flood control
-hydropower
-water supply, recreation
most reservoirs are multi-purpose

2) outflow types
- epilimnetic release
- hypolimentic release
- adjustable release
- size

36
Q

Flow modification reservoir

run of the river

A

flow regime not different from when its coming in and going out

37
Q

Flow modification reservoir

flood control

A

capture high flows and hold them back, release water during low flows

38
Q

Flow modification reservoir

hydropower

A

most common reasons- vary in affecting river flow, release water when energy is needed- daily fluctuations

39
Q

Flow modification reservoir

recreation, irrigation

A

to make water available when and where it is needed- watering lawns etc

40
Q

Outflow type reservoir: epilimnetic release

A

pulling out water from the top

“run of the river”

41
Q

Outflow type reservoir:

hypolimnetic release

A

pull water out from the bottom

42
Q

Outflow type reservoir:

adjustable release

A

pull water from the top or bottomw or middle of river

43
Q

Outflow type reservoir: size

A

small->large->pharonic (huge)

44
Q

reservoir zones

A

-riverine zone
transitional zone
lacustrine zone

45
Q

riverine zone

A

water slowing down as depth increases, still has a current

46
Q

transitional zone

A

depth increases, velocity slows, loss of flow,
downstream
sediment begins to deposit, water begins to clear
most sediment drops ou or gets deposited in this zone

47
Q

lacustrine zone

A

looks more like a lake, stratification, anoxia develops, no flow, clear water

48
Q

primary productivity in rservoirs

A

age effects: howold the reservoir is
new ones have a trophic upsurge and high production, lots of algae grwoth
occurs since high nutruesnt from the decomposition of terrestrial material that has been flooded
then occurs the trophic depression: a later decline in productivity
-old reservoirs often are eutrophic, especially smaller reservoirs

49
Q

Light, N&P, NEP (net ecosystem production) for riverine, transitional, lacustrine zones

A

light:

  • riverine: low (lots of sediments)
  • transitional: ,oderate (dropping sediment)
  • lacustrine: high (all sediment sropped)

N&P

riverine: high (because new material beng brought in)
transitional: moderate
lacustrin: low

Net ecosystem production:

riverine: variable, moderate
transitional: high
lacustrin: low (often oligotrophic)

50
Q

Cumulative effects of having reservoirs

A

fragmentatin: breaks up habitat
biodiversity: declines in migratory fish, mussels, riparin plant diversity, point of establishment for invasives
geomorphology: delta, beach erosion, starving some places of sediment
hydrology: redistribution of surface water
chemistry: reservoir surfaces a major source of greenhouse gases- not really a very clean energy

51
Q

Lake Wingra flow

A

1/3 water comes from precipitation, 1/3 surface flow, 1/3 ground water
high surface outflow

52
Q

Lake mendota flow

A

big inputs from river, very little from groundwater, some precidpitation
low surface outflow

53
Q

Unsaturated zone

A

water is held tightly by cappilary force- water adheres to soil particles andiair pockets
lots of water=all air spaces filled = less o2

54
Q

saturated zone

A

ground water- completely filled up air spaces between soil particles

55
Q

water table

A

depth to saturated zone
small near permanent water bodies
depth fluctuations over time due to: changes in recharge, withdrawl, evapotranspiration

56
Q

aquifer

A

a geological formation through which groundwater can move/store and be extracted
some rocks types are better at storing water and easier to extract from ex: sand
harder: clay

57
Q

cone of depression

A

a local draw down of groundwater where lots of pumping occurs
occurs due to urbanization

58
Q

ogallala aquifer

great plains aquifer

A

feeds agriculture- removig water thats been out of circulation and utting it bac into circulation- will not retur so not sustainable

59
Q

highland lake
lowland lake
seepage lake
drainage lake

A

highland lake:hgh precipitation inputs
lowland lake: low precip, high groundwater inputs, conductivity increases, chlorophyl a increases=more productive lakes, number of species also increases
seepage lake: no streams coing in or out
drainage lake: has connections, streams in and out

60
Q

effects of groungwater inputs

A

seepage flux: groundater discharges into lake, seepage increases which causes algae to increase
nitrates are high in groundwater to gw can fertilize algae
algal mats indicate where groundwater emerges from

61
Q

groundwater and fish

A

spawning: dying salmon release fish eggs- fish eggs need enough o2 and cold water= allows to find location of groundwater discharge

desert ish: oxygen
build nests in areas of gw recharge
as groundwater does not have O2, and surface water provides O2 rich water to eggs

62
Q

land use/ land cover LULC

A

identified by plant cover and land use by people

63
Q

conditions favoring a strong effect of LULC on surface water body

A

1 Surface water: LULC will have strong effects if surface water inputs are big contributer

  1. water body size: and for small water basins- lots of land, not so much water

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