Movement of energy and matter in ecosystems Flashcards

1
Q

first law of thermodynamics

A

energy can be converted from one form to another but cannot be created or destroyed

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2
Q

second law

A

Transformations of energy always result in some loss or dissipation of energy

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3
Q

Amount of energy at higher levels

A

smaller than in producers

also a number of ecological constraints that make the transfer even less efficient

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4
Q

as energy from one trophic level to next is must be transferred via

A

consumption assimilation and production

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5
Q

What does the energy between trophic levels depends on

A

efficiency of each step

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6
Q

consumption efficiency

A

Proportion of the net production of the lower trophic level that is consumed

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7
Q

consumption efficiency =

A

consumed energy/ net production of the lower trophic level

Not all plant material consumed

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8
Q

assimilation

A

percent of the consumed energy that becomes available for work or growth
Don’t assimilate all of what you consume- excrete/regurgitate

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9
Q

assimilation efficiency =

A

assimilated energy/consumed energy

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10
Q

net production efficiency

A

percentage of assimilated energy that is incorporated into new biomass
Lower in highly active animals

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11
Q

net production efficiency

A

net production energy/assimilated energy

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12
Q

ecological effiency

A

percentage of net production from one level compared to the next lower level

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13
Q

ecological efficiency

A

net production of energy of a trophic level/ net production energy of a lower trophic level
Equivalent to product of 3 steps previously

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14
Q

ecological efficiency explain number of trophic levels

A

plants avoid being consumed by defences
Less energy moving up trophic levels because of low consumption efficiency
Less transferred supports lower trophic levels

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15
Q

aquatic ecoystems

A

algae consumed more efficiently leading to support for more trophic levels

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16
Q

standing crop

A

amount of biomass present at a particular at a particular time in a system

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17
Q

low consumption efficiency by higher trophic level means

A

biomass residence high
Means energy and standing crop may differ
consumers not eating all the plants

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18
Q

movement of matter through the ecosystem

A

matter moves between abiotic and biotic

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19
Q

exchange from ocean to atmosphere

A

relatively fast

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20
Q

exchange from mantle to lithosphere

A

relatively slow

21
Q

Rate of exchange between pools

A

depends on types of biota

22
Q

flow of matter

A

no new matter, all recycled

23
Q

water cycle

A

water availability affects rates of primary productivity and decomp

24
Q

human impact on the water cycle

A
over-abstraction from lakes and rivers
vegetation loss 
soil erosion
pollution of surface water and ground aquifers
drainage of wetlands
climate impacts
25
Q

What do man made impervious surfaces do

A

incr runoff and affect groundwater supply- less infiltration of water so decr evapotranspiration

26
Q

take carbon out of the atmosphere

A

assimilation by plants and animals
assimilation into soil
organic decomp (animal waste/dead animals and plants)
assimilation by phytoplankton

27
Q

releasing carbon

A

fossil fuel

respiration

28
Q

human impacts on carbon cycle

A

by burning fossil fuels intoducing carbon back into the cycle that has been out of it for many years eg carbon in form of oil and peat

29
Q

solutions to high CO2

A

plant trees
incr phytoplankton
reduce fossil fuel output, renewable energy

30
Q

nitrogen cycle

A

most nitrogen is in the atmosphere

31
Q

How is nitrogen fixed

A

bacterial fixation, lightning fixation

Burning material releases some material that precipitates into nitrates

32
Q

Industrial fixation

A

revolutionised agriculture but incr eutrophication

33
Q

Increased nitrogen

A

dominant species get more dominant

decr diversity due to loss of other species

34
Q

eutrophication

A

results in incr primary productivity but -ve effects incl species loss, changes in community structure and toxicity

35
Q

What is the main environmental form of phosphorous

A

PO4

36
Q

Phos cycle

A

v little in the atmosphere

37
Q

main source of phosphorous

A

rocks of maritime origin

38
Q

Human impacts on Phos cycle

A

livestock waste and P used in inorganic fertilisers both contribute to eutrophication

Over harvesting crops

39
Q

3 steps of decomp

A

leaching, partitioning and micropartitioning

40
Q

key players in decomp

A

invertebrates and microbes

41
Q

decomp rates depend on

A

temp- colder = litter accumulating (because warmer= faster decomp= less accumulation) and more variation in types of soil affects composition of forest

Precip, and groups of organisms

42
Q

deforestation

A

incr volume of water runoffs

Incr loss of nutrients

43
Q

Mining

A

causes deforestation, physical damage, contamination
Deep disturbance of soil
Heavy machinery compacts soil
Bringing toxic substances to the surface- contamination

44
Q

fire

A

important in many ecosystems eg savanas, grasslands:

  • germination of seeds
  • regeneration of nutrients locked in biomass
  • control of pests

Incr temp,water usage, precip and drought due to climate change incr incedence of fire
Habitat fragmentation makes habitats vulnerable to fire

45
Q

Fire affects nutrient cycling

A

loss of N and C
Transfer of nutrients to ash
Warmer soil profiles which alter microbial growth and decomp rates
Devastating for ecosystems not adapted to fires

46
Q

restoration ecology

A

speed up recovery of degraded ecosystems using knowledge of nutrient cycles
2 strategies: bioremediation and augmentation of ecosystem processes

47
Q

bioremediation

A

use organisms to detoxify ecosystems
use plants, bacteria and fungi
These organisms can: absorb and conc toxic compounds facilitating removal from environment
Metabolise toxic molecules into inorganic or non toxic

48
Q

augmentation

A

use organisms to add essential materials to a degraded ecosystem
eg nitrogen fixing bacteria to incr available nitrogen in the soil