Title: Phosphorus Chemistry in Soil and Water Systems
1Phosphorus Chemistry in Soil and Water Systems
- Neil Hansen
- WCROC, Morris
- Department of Soil, Water, and Climate
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4Phosphorus Essential For Plants
- Element Relative Amount
- Molybdenum 1
- Copper 100
- Zinc 300
- Manganese 1000
- Iron 2000
- Boron 2000
- Chlorine 3000
- Sulfur 30000
- Phosphorus 60000
- Magnesium 80000
- Calcium 125000
- Potassium 250000
- Nitrogen 1000000
- 0.1 - 0.4 of dry matter
- ATP (energy)
- DNA, RNA
- phospholipids
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5Phosphorus Deficiency
- Stunting
- Limited root growth and branching
- Thin stemmed
- Delayed maturity
- Poor seed quality
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6Eutrophication
- Nutrients stimulate algal productivity
- Decay of algae depletes oxygen
- Light penetration limited
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8- Most of the Earths P is in the form of very
slowly soluble minerals for example - Tricalcium phosphate Ca3(PO4)2
- Fluorapatite 3 Ca3(PO4)2CaF 2
- Variscite AlPO42H2O
- Phosphate PO43-
- Phosphoric acid H3 PO4
- In soil solution HPO42- and
H2PO4- - In agriculture, P is most often expressed as P2O5
- P x 2.29 P2O5
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10Soil Phosphorus
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11Soil Phosphorus
- Total P concentration for MN soils averages 1200
lbs P/ac - Soluble P concentration averages 6 lbs P/ac
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12Soil Test P
- Extractants used to estimate the amount of P that
will be available to a crop. - Soil Test P includes soil solution P and a
portion of the labile P.
Labile P
(1)
P in the Soil Solution
Slowly available P
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13STP Extractants
- Bray (HCl and NH4F)
- Olson (NaHCO3)
- Mehlich (HCl and H2SO4)
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15Contrasting P Issues
- Phosphorus losses of environmental importance are
very small relative to phosphorus inputs. - Cost of excess P are downstream and cross many
boundaries
16- Lake water concentrations between 0.01 and 0.02
ppm generally accelerate eutrophication - Soil solution concentrations 0.2 to 0.3 ppm
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17Phosphorus In Water
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18Phosphorus Chemistry in Water
- Bio-availability
- Particulate P Variable (5-10)
- Dissolved P Completely
Total P Soluble (Y x Particulate)
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19Crop and Environmental responses to applied P are
management dependent
- Application Rate and frequency
- Tillage Practice
- Placement
- Source
20P Management For A Corn-Soybean Rotation
Sam Evans, George Rehm, Neil Hansen, George
Nelson WCROC Morris
- Variables
- Tillage system
- Fertilizer Rate
- Annual vs. biennial application
- Fertilizer Placement
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232000 Rain Simulations on 36 Plots
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24- Only tillage had a significant effect on Total P
loss in runoff - Neither fertilizer rate nor placement affected
total P in runoff, despite large differences in
STP - Soluble P losses were the same for all treatments
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26- Eroded Particles are a major source of P in
runoff - P concentration of eroded particles is enriched
relative to STP - Particulate P is not all bio-available
- Can settle out
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27- Soluble P in runoff can originate from soil,
plant tissue, or applied P - All soluble P is bio-available
- Not settled out
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28Estimating Risk of P moving to surface waters
-The P Index-
- Source characteristics
- Soil test P
- P application rate and source
- P application method
- Transport characteristics
- Soil Erosion
- Runoff class
- Connectivity to surface water
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29Phosphorus Index - Transport Factor Table
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30Source Factor Table
31Risk Level
- Risk Level Source X Transport
- The site is then classified for risk
- Management Practice Recommendations based on
outcome
32Development of MN P Index
- If not developed properly for MN conditions
- Fail to meet water quality goals
- Farmers may incur undue regulatory pressures
- Validation is critical
- Soil types and landscapes
- Management practices
- Climatic conditions
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33Process Overview
- Identify soil P categories
- Develop a field scale risk assessment index
- Evaluate the P index on a field scale
- Evaluate the P Index for water quality risk
assessment at the watershed scale
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