Lecture 7a Flashcards

(48 cards)

1
Q

Standing Waters: Concepts (Lake)

A

Is a large or considerable body of standing water either salt of fresh water surrounded by land

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2
Q

Standing Waters: Concepts (Shallow Lake)

A

Is a large body of water easily mixed to the bottom by casual winds

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3
Q

Standing Waters: Concepts (Pond)

A

Is a small and shallow body of water where light penetrates to the bottom

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4
Q

Standing Waters: Concepts (wetland (mire))

A

Is a body of water where vegetation protrudes from water surface (water table at/near land surface)

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5
Q

Standing Waters: Concepts (What encompasses a Wetland (4))

A
  1. Bog
  2. Fen
  3. Marsh
  4. Swamp
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6
Q

What is a Bog:

A

A peatland with acidic peat (un-decomposed organic matter) and nutrient poor (ombrotrophic: rainwater)

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7
Q

What is a Fen?

A

Is a peatland that is neutral/alkaline fed by nutrient poor mineral-rich surface or ground water +/- tall plants (trees)

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8
Q

What is a Marsh?

A

Is a nutrient rich wetland with emergents (no trees)

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9
Q

What is a Swamp?

A

Is a waterlogged wetland with conifers/deciduous

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10
Q

11 Categories of Lakes:

A
  1. Tectonic activities
  2. Volcanic activities
  3. Landslides
  4. Glacial, nival activities, permafrost and ice
  5. Karstic events and solution
  6. Fluvial lakes, lakes in floodplains and deltaic areas
  7. Costal Lakes
  8. Deflation Lakes
  9. Plant accumulations and animale (raised peat bogs, beavers)
  10. Artifical lakes
  11. Meteoric impacts
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11
Q
  1. Tectonic Activity Lakes
A
  • Graben Lake
  • Rift Lake
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12
Q
  1. Volcanic Activity Lakes:
A

Flooded crater Lakes

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13
Q
  1. Landslide Lakes:
A

In between mountain ranges

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14
Q
  1. Glacial, Nival (snow), Ice, and Permafrost Lakes:
A
  • Alpine Lake Basins
  • Morains as Dams
  • Proglacial Lake
  • Fluvioglacial Plain Lakes
  • Plonge Pool Lake
  • Glacier Scour Lake
  • Patterned Ground Lake
  • Great Lake Formation
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15
Q
  1. Karstic events and solution
A

Sinkhole Lakes (temperate and tropical)

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16
Q
  1. Fluvial lakes, lakes in floodplains and deltaic areas
A

Fluvial Lakes

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17
Q
  1. Coastal Lakes
A

Lakes near the shoreline of the ocean

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18
Q
  1. Deflation Lakes
A
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19
Q
  1. Plant Accumulation and Animal Lakes
A

Lakes made by animals like beavers after putting in dams in rivers/creeks
Leads to a large accumulation of biodiversity in the lake

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20
Q
  1. Artificial Lakes and Reservoirs
A
  • Drinking water
  • Irrigation
  • Retention
  • Mills
  • Fish ponds
  • Strip Mining
  • Defense and war
  • Fire/Ice/Farm ponds
  • Hydroelectiric Power Reservoirs
  • Recreation
  • Purification
21
Q
  1. Meteoric Impact Lakes
A

Formed where large meteors hit the Earth’s surface and formed a basin

22
Q

Lake Have Vertical Structure due to:

A
  • Stratification
  • Thermal Stratification
  • Lake Mixing
23
Q

What is Stratification?

A

Structuring of water body into layers due to physical, chemical, biological inputs and processes

24
Q

What is Thermal Stratification?

A

Varies by latitude and climate due to different thermal inputs including wind feilds

25
What is Lake Mixing?
Is caused by energy inputs in a balance between buoyancy and inertia. There are seasonal mixing patterns caused by a variety of energy inputs
26
Lake Structure (1. Morphometry)
Basin shape (irregular, dendritic, rounded to DL)
27
Lake Structure (2. Hydrology)
Retention time goes to chemical properties
28
Lake Structure (3. Light)
Compensation depth 1. Littoral 2. Limnetic zones 3. Profoundal zones
29
Lake Structure (4. Heat)
Stratification vs. mixing leads to biology/chemistry 1. Epilimnion 2. Metalimnion 3. Hypolimnion
30
Lake Structure (5. Turbulence)
Lake mixing, sediment stability/mobility in littoral
31
What can Lead to Stratification?
Thermal inputs and lack of mixing
32
What Does Stratification Indicate?
The presence of layer of different density conditions. The less dense water has higher buoyancy and floats on more dense water
33
What Determines if Different Densities Arise? (stratification)
This is due to temperature and also chemistry
34
When does Mixing Occur During Stratification
When mixing overwhelms the buoyancy
35
7 Mixing Patterns in Lakes:
1. Diel/episodic 2. Dimictic 3. Monomictic 4. Amictic 5. Polymictic 6. Holomictic 7. Meromictic
36
Stratification/Mixing Patterns (1. Diel/episodic)
Diurnal mixing
37
Stratification/Mixing Patterns (2. Dimictic)
(2/yr) Spring and fall mixing
38
Stratification/Mixing Patterns (3. Monomictic)
(1/yr) Fall mixing
39
Stratification/Mixing Patterns (4. Amictic)
(0/yr) No Mixing
40
Stratification/Mixing Patterns (5. Polymictic)
(>2/yr) Small, shallow lakes
41
Stratification/Mixing Patterns (6. Holomictic)
Entire lake mixes
42
Stratification/Mixing Patterns (7. Meromictic)
Deep layer of non-mixing water
43
Lake Structure - Mixing (Energy Inputs)
- Solar - Wind stress - Density Gradients
44
Littoral/Limnetic Zones Receives/Responds Considerable Energy (3)
1. Thermal 2. Wind 3. Density Interactions
45
Littoral/Limnetic Zones Receives/Responds Considerable Energy (1. Thermal)
Heating, convection, precipitation, evaporation, rivers, groundwater
46
Littoral/Limnetic Zones Receives/Responds Considerable Energy (2. Wind)
Creates water, stokes drift, seiches, horizontal mixing, Langmuir cells
47
Littoral/Limnetic Zones Receives/Responds Considerable Energy (3. Density Interactions)
- Stratification, instabilities, pumping, cooling, rivers - Morphometry is also important
48