environmental p management and the iowa p index p water quality-soil fertility...mallarino, haq,...
TRANSCRIPT
![Page 1: Environmental P Management and the Iowa P Index P Water Quality-Soil Fertility...Mallarino, Haq, Klatt, Baker, Kanwar, Pedersen, & Pecinovsky. ISU Soil-Test P and Tile Drainage P Loss](https://reader033.vdocument.in/reader033/viewer/2022061004/60b2a684c09bba5aa435948f/html5/thumbnails/1.jpg)
Environmental P Management
and the Iowa P Index
Antonio P. Mallarino
Department of Agronomy
Iowa State University
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Very AbundantAbundantRareRareBacteria
Rough FishPoor QualityGood QualityHigh QualitySport Fish
Very PoorPoorExcellentGoodFish & Wildlife
Habitat
Very PoorPoorGoodHighBiodiversity
ConstantFrequentInfrequentImprobableNH3 Toxicity
Very RapidRapidSlowVery SlowSilt / Filling
ConstantFrequentAbsentAbsentToxic Algae
AnoxicHypoxicAdequateAbundantOxygen
Very PoorPoorGoodExcellentClarity
Hyper Eutrophic
200+ ppb
Eutrophic
70-200 ppb
Mesotrophic
20-70 ppb
Oligotrophic
0-20 ppb
Attribute
John Downing, ISU
Impact of P on Water Quality
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Pathways for P Loss
• Soil erosion:- gully- sheet and rill- stream bank
Precipitation
Precipitation
Infiltration
Saturated Soil
Drainage Tile Flow
Seepage
Receiving Water
Impermeable Layer
Perched Water Table
Tile Inlet
• Surface runoff:- infiltration excess- saturation excess- seepage
• Subsurface drainage:- tiles- coarse soil/subsoil
Precipitation
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Forms of Soil P Lost
• Dissolved P in water: immediate but
short-term impact on water quality of
streams and lakes:
- surface water runoff
- through the soil profile (tiles)
• P bound to sediment (particulate P):
slow but large long-term impacts
mainly on lake water
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The Need for a P Index
• Soil-test P interpretation classes and P
recommendations for crops do not
apply for environmental purposes
• Factors influencing P transport with
soil and water loss (erosion, runoff,
drainage) often are more important
• Soil P, P management, and soil & water
transport factors should be integrated
into a risk rating system
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Advantages of the P Index
• The P index seems a complicated tool,
but is the best one
• Use of a simple soil P threshold would
not be effective, will be too low in
some conditions and unnecessarily
restrictive in others
• The P index is field specific, and gives
producers needed flexibility
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P Index, Nutrient Reduction Strategy
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P Index Three Components
Soil Erosion(Particulate P)
Water Runoff
(Dissolved P)
Tile
Drainage(Dissolved P)
Source Factors- soil P
- application method,
timing, and rate
Soil and water
conservation
practices
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Soil Erosion Component
Loss of P Bound to Sediment
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Soil P Loss and Soil Erosion
• Estimates P in sediment that is
effectively transported to a stream
• Various factors:
- Total soil P
- Soil loss (RUSLE 2 estimate)
- Sediment traps and delivery, filter
strips, sediment enrichment in P
- Distance to channeled water flow
- Availability for algae growth
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Estimating Total Soil P
• Can be measured by testing but it is a
highly variable and expensive test
• Uses an equation based on data from
Iowa and neighboring states
- Average total P in the 6-inch layer of
low-testing soils
- A recent routing soil P test
- Total P = 500 + (3 x Bray-1 Soil P)
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Sediment Trap Factor
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Filter Strip Factor
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Estimate of Sediment Delivery
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Surface Runoff Component
Loss of Dissolved P
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Soil P Loss and Surface Runoff
• Estimate of surface runoff volume
(NRCS runoff curve numbers)
• Dissolved P concentration in runoff
increases with increasing soil-test P,
uses average relationships from
research in Iowa and other states
• Use agronomic soil-test P methods
and sampling depth recommended for
crop production in Iowa
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Runoff P Loss and Soil-Test P Level
Bray-1 Soil P (ppm)
0 200 400 600 800
Dis
so
lve
d R
ea
ctive
P (
mg/L
)
0.0
0.5
1.0
1.5
DRP = 0.05 + 0.0017 Bray P
r2 = 0.83
Marshall
Nicollet
Fayette
Tama
Harps
BP vs DPav all except Harps Regr
Olsen Soil P (ppm)
0 100 200 300 400 500 600 700D
isso
lve
d R
ea
ctive
P (
pp
m)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
All Soils
DRP = 0.08 + 0.004 Olsen P
r ² = 0.94
Marshall
Nicollet
Fayette
Tam a
Harps (calcareous)
Allen and Mallarino, 2006 Allen and Mallarino, 2009
Mallarino, Haq, Allen, Baker; ISU
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P in Surface Runoff and Soil P
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P in Surface Runoff and Soil P
Mallarino & Klatt; ISU
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P Rate and Application Factors
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P Rate and Application Factors
• The main way the Index accounts for P
rate is through long-term effects on
soil-test P
• This factor applies to recent fertilizer
or manure application, since the last
soil test
- Impacts of the P application rate,
method, and timing of application on
dissolved P loss
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Method and Time of P Application
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Deep P Placement
0
10
20
30
40
50
60
70Chisel-DiskBroadcast
Chisel-DiskDeep Band
Bra
y-1
So
il P
(p
pm
)
No-TillBroadcast
No-TillDeep Band
Depth (inches)
0-3 3-6
Borges and Mallarino, ISU
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Swine Manure Placement and Runoff P
Baker, Klatt, Mallarino, Pederson. ISU0.0
Runoff P
Concentr
ation (
mg/L
)
0.5
1.0
1.5
2.0
2.5
3.0
Fertilizer P
to maintain
optimum
soil Pinjected
low manurerate
Fallinjected
high manurerate
Winterbroadcast
low manurerate
Springinjected
low manurerate
Winter broadcasthigh manure rate
Springinjected
high manurerate
Total dissolved P
Total P
Fall
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Manure Incorporation and Runoff P Loss
Haq, Mallarino, Allen, Kanwar, & Pederson; ISU
Dissolved Reactive P
P in
Ru
no
ff (
mg
P/L
)
0
2
4
6
8
10
12
14
Incorporated
NotIncorporatedCheck
Low Manure
High Manure
Total Runoff P
0
5
10
15
20
25
30
35
40
Incorporated
NotIncorporatedCheck
Low Manure
High Manure
Poultry Manure at 0, 150, and 300 lb N/acre, Shortly After Application
Averages Across Six Years, One Site
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Subsurface Drainage Component
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Soil P Loss and Subsurface Drainage
• Assumes water flow as 10% of annual
precipitation
• Are tiles or sandy subsoil present?
• Assume no P loss if answer is no
• Soil-test P drainage factor:
- 0.1 if Bray P is less than 100 ppm
- 0.2 if Bray P is 100 ppm or higher
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Mallarino, Haq, Klatt, Baker, Kanwar, Pedersen, & Pecinovsky. ISU
Soil-Test P and Tile Drainage P Loss
Mehlich-3 Soil-Test P (ppm)
0 20 40 60 80 100 120 140
Tile D
rain
ag
e D
isso
lved
P (
mg
/L)
0.00
0.02
0.04
0.06
0.08
0.10
0.12
0.14
Nicollet-Webster soils, poultry manure
Kenyon-Clyde soils, swine manure and P fertilizer
Nicollet-Webster soils, swine manure
16 to 20 ppmoptimum levelfor corn andsoybean
EnvironmentalChange Point
< 0.5 lb P2O5
lost/acre/year
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Tile Drainage P and STP
Northeast Research Farm, Water Quality Project
Soil-Test P (Bray-1, ppm)
0 20 40 60 80 100 120
Dra
inage P
Concentr
ation (
mg L
-1)
0.00
0.02
0.04
0.06
0.08
0.10
0.12
0.14
Soil-Test P (Bray-1, ppm)
0 20 40 60 80 100 120
P L
oss w
ith D
rain
age (
kg h
a-1
)
0.00
0.05
0.10
0.15
0.20
0.25
0.30
P Concentration Amount of P Loss
Optimum for
Corn and Soybean
Optimum for
Corn and Soybean
Haq, Mallarino, Baker, Helmers, Pederson; 2011
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The P Index Calculator
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P Index Risk Ratings
Current P and soil conservation practices
result in:
• Very Low or Low impacts
- Excellent from an ecological water
quality perspective
• Medium impact
- Acceptable P loss, but future practices
should not increase the risk of P loss
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Site Vulnerability Ratings
• High impact
- Obvious problem, new soil conservation
and/or P management practices should
be implemented
• Very High impact
- Extreme problem, new soil conservation
and P management practices that may
require no P application are needed
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Combined Effects: Erosion and Soil P
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Combined Effects:Application Method and Soil P
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Study Individual Components
Index Component
Gross Erosion 10 RUSLE erosion: 10 ton
Sediment Trap/SDR 0.49 SIDP: 1,000 feet
Buffer Factor 1 Buffer: None
Enrichment Factor 1.1 Tillage without Buffer
STP Erosion Factor 1.54 Bray 1-P: 200 ppm
Erosion 8.30
Runoff Factor 0.21 RCN: 78
Precipitation Factor 7.9 Adams County
STP Runoff Factor 1.05 Bray 1-P: 200 ppm
P Application Factor 0.02 100 lb P2O5/acre; 24 hr. incorp.
Runoff 1.78Flow Factor 0.1 Tile/Coarse Subsurface: Yes
Precipitation Factor 7.9 Adams County
STP Drainage Factor 0.2 Bray 1-P: 200 ppm
Subsurface 0.16
P- Index 10.2 High Risk Rating
Very High Soil Test, High Erosion
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A. Mallarino, ISUP APPLIED (lb P
2O
5/acre)
50 100 150 200 250 300 350 400
P IN
DE
X V
AL
UE
4.4
4.8
5.2
5.6
IMPACT OF P RATE AND APPLICATION METHOD
100 ppm STP
5 ton erosionTo frozen
ground
Injected or
incorporatedM
H
RISK
A. Mallarino, ISU
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Meaning of Partial P Index Values
• The index provide partial ratings for
Erosion, Runoff and Subsurface
Drainage components
• The partial ratings are very useful:
- identify reasons of high loss risk
- suggests what P management or soil
conservation practices will be more
effective
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Index Component
Gross Erosion 10 RUSLE erosion: 10 ton
Sediment Trap/SDR 0.49 SIDP: 1,000 feet
Buffer Factor 1 Buffer: None
Enrichment Factor 1.1 Tillage without Buffer
STP Erosion Factor 1.54 Bray 1-P: 200 ppm
Erosion 8.30
Runoff Factor 0.21 RCN: 78
Precipitation Factor 7.9 Adams County
STP Runoff Factor 1.05 Bray 1-P: 200 ppm
P Application Factor 0.02 100 lb P2O5/acre; 24 hr. incorp.
Runoff 1.78
Flow Factor 0.1 Tile/Coarse Subsurface: Yes
Precipitation Factor 7.9 Adams County
STP Drainage Factor 0.2 Bray 1-P: 200 ppm
Subsurface 0.16
P- Index 10.2 High Risk Rating
Very High Soil Test, High Erosion
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Zoning fields for
P Index calculation
and P management
VL
L
L-MM
H
Soil-test P was
74 to 180 ppm
(Very High)
But the P Index
ratings were
Very Low to High
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Delineate Field Zones for P Index Calculation
5.57.0
10
642
2-59-14
14-18
138
485
5-93.4
6.7
6.7
1.5
4.614-18
180
118
150
106
74
2.8
1.0
2.0
5.0
1.3
Soil Series Erosion (ton/acre)
N-Based Manure?P Index RatingSoil-Test P (ppm)
Slopes (%)
Yes
Yes
No
?? ??
Mallarino, Wittry, & Stewart. ISU & NRCS
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P Index and P Management
• The index is a P assessment tool
• Identifies reasons for high P loss, but
has no built-in limits for soil-test P or
P application rates
• Suggests alternative field-specific
management and soil & and water
conservation practices to reduce risk
of P loss
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Northwest Iowa Runoff P Study
Natural Rainfall, 100 lb P2O5/acre to Corn for the C-S Rotation (6 Years Avgs.)
Tillage No-Till
Runoff
P L
oss
(lb
P/a
cre)
0
2
4
6
8
10
Tillage No-Till
Corn after Soybean Soybean after Corn
Dissolved PTotal P Dissolved PTotal P
21%
54%
24%
68%
Mallarino, Haq, et al., 2012
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Grass Filter Strips
>90%
Reduction
in P export
from
watersheds
with prairie
filter strips.
But recent
research
shows can
increase
dissolved P
loss
Zhou et al., 2014
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Differences between fertilizer and manure P sources
and of time to a runoff event on P loss with surface
runoff after applying P with or without incorporation
Field Rainfall Simulations
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P Source Effects: Immediate Runoff EventR
un
off P
Lo
ss (
kg
ha
-1)
0.0
0.5
1.0
1.5
2.0
2.5
No P
BeefCattle
Manure
PoultryManure
LiquidSwine
Manure
FertilizerDissolved P
Total P
18%29% 31%
49%
88%% Dissolved P of TP
Runoff within 24 hours, No Incorporation, Broadcast 100 lb P2O5/a
to Soybean Residue - Means of 21 Fields
Haq, Mallarino, & Allen. ISU
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P Rate, Incorporation, Time to Runoff
Allen and Mallarino. ISU
Dis
solv
ed P
(kg h
a-1
)
0.0
0.1
0.2
0.3
0.4
0.5
0 10 20 30 40 50
Runoff T
ota
l P
(kg h
a-1
)
0.0
0.2
0.4
0.6
0.8
Not Incorporated
Incorporated
Liquid Swine Manure P Rate (kg P ha-1
)0 10 20 30 40 50
24-hour Event15-day Event
24-hour Event 15-day Event
5
6 7
1632
56
62
1
Not Incorporated
Incorporated1
46
12
1 9 9
3
Not Incorporated
IncorporatedNot Incorporated
Incorporated
ns
6-mo Event
Not Incorporated
Incorporated
0 10 20 30 40 50
ns
15-day Event24-hour Event
6-mo Event
Not Incorporated
Incorporated
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P Sources Applied in Fall or Winter
Haq and Mallarino, 2012
Snowmelt Runoff Fall Application Snowmelt Runoff Winter Application
DAPFertilizer
No P
PoultryManure
Run
off
P C
once
ntr
ation
(m
g/L
)
0
5
10
15
20
25
DAPFertilizer
PoultryManure
No P
LSD DRP 2.7
LSD BAP 2.9
LSD TP 3.0
LSD DRP 7.6
LSD BAP 8.3
LSD TP 10.1
Dissolved P
Bioavailable P
Total P
Dissolved P
Bioavailable P
Total P
100 lb P2O5/acre to Soybean Residue, No Incorporation
Averages of 3 Fields
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Cover Crops and P Loss with Runoff
Averages of Four Years
NT NTCC Till TillCC
Runoff
P L
oss (
kg P
ha
-1)
0.0
0.2
0.4
0.6
0.8
DRPTP
NT NTCC Till TillCC
Runoff
P C
oncentr
ation (
mg P
L-1
)
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
DRPTP
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When do P losses occur?
• When there is soil erosion or water
runoff!
• Late February to late June:
- Snow melt and high-rainfall period
- Little or no crop canopy
- Saturated soils (moisture, floods)
- Reduced conditions (soluble Fe+2)
- Soils tilled and with little cover
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Sound Phosphorus Management
• Use conservation practices!
• Apply manure based on crop nutrient
needs and P index ratings.
• Reduce P of manure: feed phytase
enzyme, low phytate grain, reduce P
supplements as much as possible.
• Dedicate time to careful manure
application. Incorporate or inject it
without increasing soil erosion.
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This institution is an equal opportunity provider. For the full non-discrimination statement
or accommodation inquiries, go to www.extension.iastate.edu/diversity/ext
515-294-6200
Soil Fertility Web Site
http://www.agronext.iastate.edu/soilfertility/
This institution is an equal opportunity provider. For the full non-discrimination statement
or accommodation inquiries, go to www.extension.iastate.edu/diversity/ext