Nutrient Cycling - Cornell University
Transcript of Nutrient Cycling - Cornell University
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Nutrient Cycling
Essential for all life& its availability (or lack thereof) controls
the distribution of flora and fauna
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Its availability is controlled by 3 things
1.Sources
2.Sinks (pools)
3.Fluxes
For use by organisms, nutrients must be in a specific form –
each to its own…
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The largest sinks of nutrients are generally unavailable to organism,
But there is a large group of specialized organisms that can
transform this “unavailable” pool to usable form – and thus make it
available for all organism.Much of this transformation of nutrients
is controlled by soil characteristics!
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The Nitrogen CycleThree questions to think about
• What are the pools
• What are the sources and losses
• What are the fluxesThen think about what controls these…
NB ~ flux rates and pools are controlled by edaphic environmental conditions, while N
sources are often global in nature!
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In the soil environment, what controls N?
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1. Sources
a. humans – atmospheric deposition, inorganic fertilizer, waste, etc…
b. microorganisms – N fixation (symbiotic and non-symbiotic)
c. stochastic events – lightning and fire
2. Sinksa. atmosphere – 386 x 1016 kg
b. biomass – 0.045 x 1016 kg
c. soil – 0.02416 x 10 kg
3. Fluxes
a. immobilization ↔ mineralization (ammonification and nitrification)
b. denitrification
c. fixation – N fixation (biological and abiotic) and NH4+ fixation (colloids)
d. plant uptake
e. leaching and volatilization
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Sinks
a. atmosphere – 386 x 1016 kgb. biomass – 0.045 x 1016 kgc. soil – 0.02416 x 10 kg
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TemperatureMoistureOxygenNitrogen
Fluxesa. immobilization ↔ mineralization (ammonification and nitrification)b. denitrificationc. fixation – N fixation (biological and abiotic) and NH4+ fixation (colloids)d. plant uptakee. leaching and volatilization
What controls these fluxes in the soil?
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Temperature
Bioactivity
CO
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Moisture & Oxygen
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Nitrogen
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What are the consequences of N in the environment?1. Plant Growth
2. Leaching – Eutrophication
3. Acidification
4. Toxicity
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S Cycling and its behavior in Soil
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Sulfur Cycle
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S Sources
1. Soil Organic Matter@ 95 percent of the total amount of S in soils is found in SOM S is mineralized to SO4. - the only form of S that is absorbed by plant.
2. Soil Minerals S is weathered and transformed to available SO4
3. The AtmosphereFossil fuel combustion
4. Pesticides and FertilizersSome pesticides contain S - contribution of S in the soil is quite low. Fertilizers once supplied considerable S as impurity - Today, as the fertilizer products become more concentrated and the analysis increases, S contents are less.
5. Irrigation Water Where soils are sandy, the S content of the water is expected to be low.
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S Losses
1. Crop Removal or UptakeRemoval of S from the soil varies with crop and the yield of that crop
2. LeachingSO4 is soluble in water (like NO3
-) in soils and can be moved out of the root zone by leaching. The SO4 does not leach as rapidly as NO3
-. But, excessive rainfall or irrigation water can move SO4-S below the root zone where soils are sandy.
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S Pools
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Fluxes
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Plant Uptake
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What controls these fluxes in the soil?
TemperatureMoistureOxygenSulfur
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What are the consequences of S in the environment?1. Plant Growth
2. Leaching – Eutrophication
3. Acidification
4. Toxicity
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