Nutrient cycling

 

1. Nutrient Cycling in Ecosystems

Following elements of an Ecosystem understand processes, function

Important for agricultural systems increased production + elements

Organic matter production (C) important and nutrients (N,P, etc.)

Create linkages between Biotic and Abiotic components Ecosystems

Biological communities processors of nutrients

Cycles called: Biogeochemical Cycles

Global Biogeochemical Cycles-Very Important climate etc. Closed system

2. Global Cycles – Summation all ecosystem cycles scale = Biosphere

Important to understand biogeochemical cycles various scales

At the Global scale everything averaged – linked to climate models

Local scale determine effect of cycling in one system having global effects

Example: Lake P Model (3-Compartment Model with 7 flux rates)

Each Compartment has a Pool of nutrients in standing stock

Flux rate is rate of movement of pool between compartments

3. Ecosystems are not isolated:

Fluxes between biogeochemical cycles different ecosystems

           Transfer elements between ecosystems: Meteorological, Geological, Biological transport systems

4. How do we determine rates of flux materials construct biogeochemical cycles?

Radioactive Tracers- Example Phosphorus Lake

Stable Isotope Tracers (signatures where material came from)

Measure fluxes directly or through concentration gradients

5. Terrestrial Nutrient Cycles – Forests

Important for Forestry Management (Economic and ecological issues)

How does harvesting trees influence long-term productivity forest?

6. Forests accumulate nutrients differently over time

Take up nutrients quickly then more slowly

Accumulate leaves & wood

Example Pineland Canada

7. Age stand effects where nutrients going

Very mature forest >open canopy & understory vegetation

Example: Spruce forest Russia

8. Turnover times for nutrients cycled soils & forest Temperature-dependent

Important in terms nutrient limitation of forest production

9. Internal recycling within forest part of nutrient cycle

Also, fluxes out of forest

Nutrient losses forests several mechanisms

Stream transport

Gases released soils/plants (ammonia, sulfide gas, etc.)

Fires (gases & particulates)

Forest harvesting (nutrients wood)

Sometime interaction 2 effects harvesting-stream transport

            Replacement nutrients after harvest > 50 years many forest-types


 

10. Globally Age soil define status nutrient “rich” or  “poor”

Northern Hemisphere glaciated soils tend rich nutrients

Alluvial soils of Mississippi delta rich

Australia, India, South America old world soils poor

Plants adapted by being able to use nutrients efficiently

Nutrient Use Efficiency (NUE)

11. Important Global Biogeochemical Cycles

Significant Effect on Humans & vice versa

Sulfur Cycle

Nitrogen Cycle

Carbon Cycle

12. Sulfur Cycle

160% > Natural Levels- Emissions Burning Fossil Fuels (SO2)

Consequence:Acid Precipitation <5.6

13. Effects acid rain not new phenomenon: Tasmania Australia

1896-1922 copper smelter Ore mine

48% Sulfur

40% Iron

<3% Copper

Vegetation mortality 24hrs

Erosion topsoil lost

Nutrient pore soils

80 yrs later same

14. Some optimism on reduction of emissions oxides associated fossil fuels

           1970 Passage Clean Air Act

15. Will forest & aquatic ecosystems recover effects acid rain? If yes, at what rate?

16. Nitrogen Cycle

Very important because Nitrogen major element limiting production biosphere

N2 abundant atmosphere (78%) only N2 fixers convert this N bioavailable N

Humans have doubled amount of bioavailable N in the Biosphere

Not evenly distributed N loading

Inputs of several forms of nitrogen depending on source-different effects

Nitrous Oxide: unreactive & persistent, Greenhouse gas, 0.25% increase/yr

Nitric Oxide, highly reactive, converted nitric acid, acid rain > W in US

Light reacts O2 & HC Ozone (smog) - Burning fossil fuels

Ammonia released from organic fertilizer waste

17. Major additions of nitrogen significant effects aquatic systems

18. Summary:

Nutrient cycle & recycle in ecosystems

Tracing nutrient cycles investigate important ecosystem processes

Logging or harvesting of biota storing elements can effect ecosystem function

NUE has allowed some species to adapt to low nutrient availability

Human activities are changing global biogeochemical cycles

Several cycles are being altered on a drastic scale with global consequences

These include sulfur cycle, nitrogen cycle, carbon cycle

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