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Ch 8: Nutrient Regeneration in Terrestrial and Aquatic Ecosystems

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Title: Ch 8: Nutrient Regeneration in Terrestrial and Aquatic Ecosystems


1
Ch 8 Nutrient Regeneration in Terrestrial and
Aquatic Ecosystems
2
Objectives
  • Terrestrial regeneration
  • Intrasystem cycling
  • nutrient regeneration in soil
  • annual dynamics/balance the books
  • Intersystem cycling
  • inputs vs. outputs
  • Aquatic regeneration
  • nutrients productivity
  • timing of regeneration
  • sources of regeneration

3
Intrasystem (within 1) vs. intersystem (between 1
2) cycling in ecosystems

Ecosystem 2
Ecosystem 1
Ecosystem 1
2
Input ?
?
?
?
?
Output ?
Input ?

? output
?
?
4
Generalized model nutrient cycle, including
regeneration, in terrestrial ecosystem.
Intra
Inter
5
Intrasystem cycling
Figure 1
  • Figure 1

6
Nutrient regeneration occurs in the soil.
  • Rate depends on rate of ecosystem processes (e.g.
    decomposition mineralization).
  • Productivity depends on regeneration of nutrients
    from litter
  • decomposition
  • mineralization (organic --gt inorganic)
  • uptake
  • Nutrients added by weathering of rock slow
  • Nutrient uptake from soil by plants fast

7
Life in the soil and litterinverts, bacteria,
fungi
8
Nutrient regeneration from litter by
  • leaching of soluble substances
  • maceration by large detritus feeders
  • fungi breakdown cellulose/lignin--gt C,H,O
  • mineralization (organic---gtinorganic) of P, N,
    and S by bacteria

9
Depolymerization of large organic molecules in
soil regulates nutrient cycling. Microbes
plants compete for small monomers (e.g. amino and
nucleic acids)
Figure 2
10
Leaf quality (e.g. toughness/chemicals) affects
regeneration.Climate affects nutrient
regeneration
  • Decomposition rate and what seasons
  • Weathering rate and what seasons
  • Soil properties

11
Soil properties
  • Eutrophic (rich) soils
  • in geologically active areas young soils
  • rapid weathering of bedrock - adds
  • fresh nutrients
  • Oligotrophic (poor) soils
  • in old, geologically stable areas old
    soils
  • intense weathering if high temperatures
  • and abundant water ---gt
  • 1) high respiration ---gtacid pH
  • 2) removes clay and cations (e.g.
    Ca)
  • 3) reduces storage capacity for
    nutrients
  • 4) high leaching of cations
  • 5) nutrient-pool soils

12
How does vegetation aid nutrient
retention?(lower movement from intrasystem to
intersystem cycling)
  • 1 retain leaves for long time
  • 2 withdraw nutrients from leaves before drop
    (reabsorption)
  • 3 develop dense root mats near soil surface
  • 4 grab nutrients quickly before leached away
  • 5 store more nutrients in biomass, not soil

13
Annual dynamics/budget of intrasystem cycle
  • Storage
  • Annual requirement
  • make foliage
  • woody growth
  • leaching (throughfall and stemflow)
  • Annual uptake by roots
  • woody growth
  • returns from
  • leaching
  • litterfall
  • Reabsorption (before leaf fall)
  • Balanced if
  • annual requirement uptake reabsorption

14
What 3 components of the annual requirement
account for the total requirement (114.3)?
What 2 processes provide resources to meet the
total requirement (114.3)?What 3 components of
annual uptake account for total uptake
(92.1)?Is the forest in equilibrium?Explain
15
Intersystem cycling Nutrients gained (input) and
lost (output) by an ecosystem

Ecosystem 2
Ecosystem 1
Ecosystem 1
2
Input ?
?
?
?
?
Output ?
Input ?

? output
?
?
16
Contrast intra- vs. inter-system cycling in a
terrestrial ecosystem.
Atmosphere
17
Intersystem cycling
--gtInput from waterflow
18
Nutrient inputs on land from
  • Lithosphere (weathering of bedrock and
  • soil)
  • Atmosphere
  • Wetfall (in precipitation)
  • Dryfall (particles)
  • Hydrosphere
  • Human Activities

19
What are two generalizations about nutrient
input from the atmosphere?
Figure 5
20
Nutrient losses (output) on land to
  • Atmosphere
  • Streams and groundwater
  • Which cycle links terrestrial and aquatic
    ecosystems?

21
Nutrient Budgets
  • Balanced (equilibrium) inputs outputs
  • Unbalanced (non-equilibrium)
  • inputs gt outputs ???
  • outputs gt inputs ???

22
Question Does the presence of vegetation affect
the rate of nutrient output (loss) from an
ecosystem?Hypothesis IF vegetation increases
soil stability and intrasystem recycling of
nutrients,Experimental design
23
  • What is the prediction?

Figure 6
24
Hubbard Brook watershed and experimental sites
25
Hubbard Brook Ecosystem Study How does
deforestation affect streamflow and nutrient loss
(output)?

26
Weir (dam) method of gaining output data
27
Method of gathering input data
28
Results
What is the conclusion (as in discussion)?
Figure 7
29
What are two patterns?(1 general and 1
qualifying) What stats to do?
Figure 8
30
Watershed studies of precipitation and stream
chemistry
  • How important is intrasystem cycling relative to
    intersystem cycling of nutrients?
  • Is amount of nutrients in intrasystem cycle per
    year small or large compared to external inputs
    and outputs?

31
What contributes to input? output?What are
two main conclusions?
Figure 9
32
Summarize the pattern. What causes
variation in amount of input?
Figure 11
33
Nutrients and Aquatic ProductivityWhat
accounts for the highest and lowest levels?
Fig. 12
34
NPP of aquatic systems maintained by
  • Transport of nutrients from bottom sediments to
    surface (in shallow water or upwelling)
  • Recycling of nutrients within photic zone
  • Import of nutrients from other systems

35
Temperate lakes have annual cycles of nutrient
availability and productivity
  • Summer stratified- nutrients depleted by
    sedimentation of organic material --gt lowers NPP
  • Spring and Fall vertical mixing brings up
    nutrients to photic zone --gt
  • increases NPP

36
Productivity varies in temperate lakes
nutrient-limited
well-nourished, productive
37
What element controls the trophic structure and
productivity of lakes?
CNP
CN
Figure 16
38
Estuaries and salt marshes
  • Extremely productive due to
  • rapid local regeneration of nutrients
  • external input of added nutrients
  • Major exporters of C and nutrients to
  • marine systems.

39
Intra- vs. inter-system energy flow in a salt
marsh. 10 of GPP exported.
Figure 17
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