Topic 33 Flashcards

1
Q

Internal cycling of nutrients

A

primarily concerned with the flow of nutrients through the ecosystem dominated by the biological processes of primary production and decomposition

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2
Q

Many transformations take place in the..

A

non living (abiotic) component- atmosphere, water, soil.

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3
Q

Weathering of rocks and minerals releases..

A

inorganic nutrients into soil and water thins available for plant uptake

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4
Q

Biogeochemical cycle

A

flow of all nutrients from the nonliving to the living and back to the nonliving components of the ecosystem in a more or less cyclic path

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5
Q

2 major types of cycles (based on primary source of nutrient input)

A

-gaseous cycles

sedimentary cycles

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6
Q

Gaseous cycles

A

main pool of nutrients: atmosphere and ocean. ex: nitrogen, oxygen, CO2, dominant components of atmosphere

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7
Q

Sedimentary

A

main pool of nutrients: soil, socks, minerals. nutrients required by organisms come initially from inorganic source via weathering

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8
Q

All cycles involve..

A

biological and non biological processes, both driven by flow of energy through the ecosystem

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9
Q

Water is the..

A

medium in which inorganic nutrient travel through the ecosystem

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10
Q

Without water..

A

biochemical cycles would stop

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11
Q

Inputs of nutrients into the ecosystem depend on

A

the type of ecosystem

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12
Q

Terrestrial input

A

nutrient inputs are supplemented by rain, snow, air currents and animals

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13
Q

Wetfall

A

precipitation inputs nutrients

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14
Q

Dryfall

A

airborne particles with associated nutrients fall from the atmosphere

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15
Q

Aquatic input

A

major source of nutrients are from the surround land in the form of drainage, water, detritus and sediment (also wet and dry fall)

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16
Q

Input of organic carbon from terrestrial ecosystems constitutes the..

A

majority of energy input into stream and river ecosystem

17
Q

Output step 1

A

release into atmosphere

18
Q

Output step 2

A

inorganic nutrients released via leaching (dissolved and washed) out of the soil in underground water –> streams

19
Q

Output step 3

A

organic matter exported from forest ecosystems by streams and rivers –> lakes

20
Q

Output step 4

A

organic matters transferred between ecosystems in form of faces and other rates via movement patterns of consumers

21
Q

Output step 5

A

harvesting- nutrients stored in organisms are directly lost during removal from the system but balanced by adding fertilizers because nutrients become limited

22
Q

Processes of inputs and outputs of nutrients during biochemical cycles link

A

different ecosystems

23
Q

The output from one ecosystem represents ..

A

inputs to another (terrestrial –> aquatic system)

24
Q

Processes of nutrient exchange among ecosystems requires..

A

examining biogeochemical cycles from much broader view than single ecosystem. (true of those nutrients w gaseous cycle)

25
Q

Main pools are the atmosphere and ocean which have..

A

local circulation patterns because carbon is the basic nutrient in all organic compounds

26
Q

Terrestrial carbon cycle

A

photosynthesis: CO2 – organic form – herbivores – carnivores – organic matter – decomposers – plant tissue. CO2 released back into atmosphere via respiration

27
Q

Swamps and Marshes

A

dead organic matter falls into water doesn’t completely decompose, carbon stored as humus or peat. buildup of partially decomposed organic mater forms fossil fuels – long terms.

28
Q

Freshwater and marine ecosystem

A

CO2 diffuses into the surface water form atmosphere –> carbonates. Phytoplankton uses carbonates – plant tissue – herbivores – carnivores –organic matter – decomposers – plant tissue. CO2 releases via respiration is either reused or released into atmosphere (diffusion)

29
Q

Diffusion

A

movement of substance from area of higher to lower concentration

30
Q

Earths C budget (100,000,000 Gt) most..

A

buried in sedimentary rocks (not involved in cycle) = 99%

31
Q

Global cycle is = 55,000 Gt and divided into..

A
  • oceans (major) 38,000 Gt
  • fossil fuels (decomposed matter) 10,00 Gt
  • atmosphere 750 Gt
  • terrestrial 2000 Gt
32
Q

Oceans Carbon

A

surface water to atmosphere is main exchange site. exchange rate governed by diffusion gradient between surface waters and atmosphere

33
Q

Terrestrial Carbon

A

includes soil and organisms, exchange rate governed by diffusion gradient between plant leaf and atmosphere (photosynthesis) historically exchanges of CO2 between terrestrial environments and the atmosphere were thought t be in equilibrium (has increased)

34
Q

Atmospheric Carbon

A

CO2 in atmosphere have increase 25% in last 100 years. industrial revolution CO2 increase steadily by mid 1900s increased exponentially

35
Q

Historically CO2 is ..

A

280-290 ppm.

36
Q

Burning fossil fuels in industrialized nations

A

adding 6.4 Gt/year in 1990s

37
Q

Deforestation

A

forested lands are typically clearly and burned for farming. adding 2.2 Gt / year in 1990s.

38
Q

Also issues with increased levels of…

A

methane which is 25x more effective as greenhouse gas

39
Q

Predictions of global warming

A
  • increases average global temps and precipitation (increase 2-6 C in 100 years)
  • changes will not be evenly disturbed over Earths surface (warming is expected to be greater during winter months)
  • increased variability in climate (more sever storms and hurricanes, great snowfall increasing variability in rainfall)