Title: Ch 8: Nutrient Regeneration in Terrestrial and Aquatic Ecosystems
1Ch 8 Nutrient Regeneration in Terrestrial and
Aquatic Ecosystems
2Objectives
- 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
-
3Intrasystem (within 1) vs. intersystem (between 1
2) cycling in ecosystems
Ecosystem 2
Ecosystem 1
Ecosystem 1
2
Input ?
?
?
?
?
Output ?
Input ?
? output
?
?
4Generalized model nutrient cycle, including
regeneration, in terrestrial ecosystem.
Intra
Inter
5Intrasystem cycling
Figure 1
6Nutrient 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
7Life in the soil and litterinverts, bacteria,
fungi
8Nutrient 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
9Depolymerization of large organic molecules in
soil regulates nutrient cycling. Microbes
plants compete for small monomers (e.g. amino and
nucleic acids)
Figure 2
10Leaf quality (e.g. toughness/chemicals) affects
regeneration.Climate affects nutrient
regeneration
- Decomposition rate and what seasons
- Weathering rate and what seasons
- Soil properties
11Soil 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
12How 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
13Annual 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
14What 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
15Intersystem cycling Nutrients gained (input) and
lost (output) by an ecosystem
Ecosystem 2
Ecosystem 1
Ecosystem 1
2
Input ?
?
?
?
?
Output ?
Input ?
? output
?
?
16Contrast intra- vs. inter-system cycling in a
terrestrial ecosystem.
Atmosphere
17Intersystem cycling
--gtInput from waterflow
18Nutrient inputs on land from
- Lithosphere (weathering of bedrock and
- soil)
- Atmosphere
- Wetfall (in precipitation)
- Dryfall (particles)
- Hydrosphere
- Human Activities
19What are two generalizations about nutrient
input from the atmosphere?
Figure 5
20Nutrient losses (output) on land to
- Atmosphere
- Streams and groundwater
- Which cycle links terrestrial and aquatic
ecosystems?
21Nutrient Budgets
- Balanced (equilibrium) inputs outputs
- Unbalanced (non-equilibrium)
- inputs gt outputs ???
- outputs gt inputs ???
22Question 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
23Figure 6
24Hubbard Brook watershed and experimental sites
25Hubbard Brook Ecosystem Study How does
deforestation affect streamflow and nutrient loss
(output)?
26Weir (dam) method of gaining output data
27Method of gathering input data
28Results
What is the conclusion (as in discussion)?
Figure 7
29What are two patterns?(1 general and 1
qualifying) What stats to do?
Figure 8
30Watershed 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
32Summarize the pattern. What causes
variation in amount of input?
Figure 11
33Nutrients and Aquatic ProductivityWhat
accounts for the highest and lowest levels?
Fig. 12
34NPP 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
35Temperate 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
36Productivity varies in temperate lakes
nutrient-limited
well-nourished, productive
37What element controls the trophic structure and
productivity of lakes?
CNP
CN
Figure 16
38Estuaries 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.
39Intra- vs. inter-system energy flow in a salt
marsh. 10 of GPP exported.
Figure 17