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Connecting Environmental
Aspects of Nutrient
Management and Conservation
Planning
Peter Tomlinson and Nathan Nelson
Department of Agronomy
• Tailored to the desired conservation planning outcome
• Production: Yield, Nutrient management, Profitability, Equipment
resources, etc.
• Conservation: Soil health & conservation, Water quality, Sustainability,
Climate resiliency, etc.
• Consider potential side-effects
• May necessitate the overlay of additional practices
• A management paradigm shift
• Shift away from simple implementation of single conservation
practices or even multiple “stacked practices”
• Holistic implementation of a
conservation management systems
Conservation Planning
• Challenge – producers inadvertently over-apply to avoid yield
reductions (Roberts et al., 2018)
• Blanco-Canqui et al. (2018) noted that cover crops effectively
decreased sediment and N losses but reduced soluble P losses in
fewer than 25% of studies
• Nitrogen
• Excess N beyond plant demand results in an exponential increase in
N2O (Kim et al., 2013)
• Venterea et al. (2012) found that using multiple components of 4R
Nutrient Stewardship lowered N2O emissions
• Phosphorus
• To date, claims that soil health practices alone can significantly
reduce P losses are not substantiated by peer-reviewed literature
(Duncan et al., 2019)
Nitrogen and Phosphorus Management
Method of Tillage
Conventional Conservation No Till Pasture
Sedimentloss(ton/ac)
0
2
4
6
8
523
195
94 478
Reduce erosion with
no-till Numbers indicate number of
watershed years included in
the dataset
Data from the MANAGE v3 database (Harmel et al., 2008)
Method of Tillage
Conventional Conservation No Till Pasture
TotalPloss(lb/ac)
0
2
4
6
8
10
427
207
107
528
Reduce Total P loss
with no-till Numbers indicate number of
watershed years included in
the dataset
Data from the MANAGE v3 database (Harmel et al., 2008)
No-till can increase dissolved P loss
Dissolved P entering Lake Erie
Method of Tillage
Conventional Conservation No Till Pasture
DissolvedPloss(lb/ac)
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
465
185
66
460
Effect of tillage on dissolved P loss
Data from the MANAGE v3 database (Harmel et al., 2008)
(Stow et al., 2015)
decreasing sediment
decreasing then plateau total P
decreasing then increasing dissolved P
No-till can increase dissolved P loss
Effect of no-till on form of P in runoff water
Source: Daryanto et al., 2017. J. Environ. Qual. 46:1028–1037
Potential Mechanisms
• Soil stratification due to less soil
mixing:
• Surface P loading due to
increased broadcast P fertilizer
application and accumulation of
plant residues
• Lysed plant and microbial cells
from freeze/dry, termination
methods, and wet/dry periods
No-till can increase dissolved P loss
• Increased SOM and microbial
activity could augment
mineralization efficiency
• Gonzalez-Chavez et al.
(2010) found no-till
increased proteins related to
arbuscular mycorrhizal fungi
by 43%, doubled microbial
biomass C and N and
increased microbial biomass
P by 250%
• Some organic P compounds
(30-65% of total P) can be
more labile than ortho-P
while other can compete for
sorption sites
• This could lead to increased
soluble ortho-P and
bioavailable organic P in
solution
No-till can increase dissolved P loss
Potential Mechanisms
Kansas Agricultural
Watershed Field Laboratory
Graduate Student:
David Abel, Elliott Carver, and Laura Starr
Faculty:
Nathan Nelson, Kraig Roozeboom, Gerard
Kluitenberg, Peter Tomlinson, DeAnn Presley
and Jeff Williams
decreased erosion
more than 65%
Cover crop effects on sediment
Cover crop effects on form of P loss
Increased dissolved P
65%
Cover crop effects on soil biological indicators
Fertilizer management effects on P loss
Fall 2017
Fertilizer management effects on soil test P
Phosphorus Cycle
Dissolved P
H2PO4
- / HPO4
2-
Adsorbed P
Root
Zone
Mineralization
Immobilization
Uptake
Leaching
H2PO4
- / HPO4
2-
Organic P
Secondary
Mineral P
Precipitation
Desorption
Adsorption
Primary
Mineral P DissolutionDissolution
P in grain,
forage, fruit, etc.
Residue P
Fertilizer and
Manure P
Dissolved P loss
(minimal loss)
Recycling
Exports
Erosion/RunoffAdditions
Particulate P loss
Dissolved P loss
Particulate P loss
Dissolved P loss
Particulate P loss
Alternate
Management Alternate
Management
Paradigm Shift
• Holistic implementation of
conservation management
systems
• Nutrient management factors
(rate, timing, placement, and
source) should be appropriate for
the conservation practices
• New nutrient management
paradigm:
• Managing on the margins of
deficiency required to meet crop
production goals.
For Example:
Guided by coalition of
agricultural and conservation
organizations to support
farmers’ efforts to implement
precise nutrient management
and conservation practices.
www.4rplus.org
Thank you
Peter Tomlinson - Environmental Quality
(ptomlin@ksu.edu)
Department of Agronomy, Kansas State University
Cover crop effects on runoff
Cumulative Emissions Yield Scaled Emissions
N Fertilizer Replacement Value
1Means with different letters within columns are significantly different (LSD=0.05)
• Regression
equation of
grain yield for
chemical
fallow as a
function of N
fertilizer rate
• Solved the
equation
substituting
the mean grain
yield at 0-N for
each cover
crop treatment
Cover crop
treatment
Mean grain yield
at 0 N rate
(bu ac-1)
Fertilizer N
equivalent
value
(lb N ac-1)
Chemical fallow 88 b -
Double-crop soybean 91 b 8 b
Summer legume 100 a 30 a
Summer non-legume 64 c -45 c
Winter legume 87 b -1 b
Winter non-legume 87 b -3 b
Preza Fontes, G., P. Tomlinson, K. Roozeboom, and D. Ruiz Diaz. 2017. Grain Sorghum Response to
Nitrogen Fertilizer Following Cover Crops. Agronomy Journal. DOI: 10.2134/agronj2017.03.0180. 109(6)
2723-2737. KAES# 17-286-J.
• Rainfall
• Duration and intensity of events
• Structural Conservation Practices
• Terraces and Terrace Maintenance
• Waterways
• Sediment basins
for tile outlet
terraces
• Residue
• No-till
• Cover crops
How Can we Keep Soil and Nutrients in Place

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July 29-130-Peter Tomlinson

  • 1. Connecting Environmental Aspects of Nutrient Management and Conservation Planning Peter Tomlinson and Nathan Nelson Department of Agronomy
  • 2. • Tailored to the desired conservation planning outcome • Production: Yield, Nutrient management, Profitability, Equipment resources, etc. • Conservation: Soil health & conservation, Water quality, Sustainability, Climate resiliency, etc. • Consider potential side-effects • May necessitate the overlay of additional practices • A management paradigm shift • Shift away from simple implementation of single conservation practices or even multiple “stacked practices” • Holistic implementation of a conservation management systems Conservation Planning
  • 3. • Challenge – producers inadvertently over-apply to avoid yield reductions (Roberts et al., 2018) • Blanco-Canqui et al. (2018) noted that cover crops effectively decreased sediment and N losses but reduced soluble P losses in fewer than 25% of studies • Nitrogen • Excess N beyond plant demand results in an exponential increase in N2O (Kim et al., 2013) • Venterea et al. (2012) found that using multiple components of 4R Nutrient Stewardship lowered N2O emissions • Phosphorus • To date, claims that soil health practices alone can significantly reduce P losses are not substantiated by peer-reviewed literature (Duncan et al., 2019) Nitrogen and Phosphorus Management
  • 4. Method of Tillage Conventional Conservation No Till Pasture Sedimentloss(ton/ac) 0 2 4 6 8 523 195 94 478 Reduce erosion with no-till Numbers indicate number of watershed years included in the dataset Data from the MANAGE v3 database (Harmel et al., 2008)
  • 5. Method of Tillage Conventional Conservation No Till Pasture TotalPloss(lb/ac) 0 2 4 6 8 10 427 207 107 528 Reduce Total P loss with no-till Numbers indicate number of watershed years included in the dataset Data from the MANAGE v3 database (Harmel et al., 2008)
  • 6. No-till can increase dissolved P loss Dissolved P entering Lake Erie Method of Tillage Conventional Conservation No Till Pasture DissolvedPloss(lb/ac) 0.0 0.2 0.4 0.6 0.8 1.0 1.2 1.4 1.6 465 185 66 460 Effect of tillage on dissolved P loss Data from the MANAGE v3 database (Harmel et al., 2008) (Stow et al., 2015) decreasing sediment decreasing then plateau total P decreasing then increasing dissolved P
  • 7. No-till can increase dissolved P loss Effect of no-till on form of P in runoff water Source: Daryanto et al., 2017. J. Environ. Qual. 46:1028–1037
  • 8. Potential Mechanisms • Soil stratification due to less soil mixing: • Surface P loading due to increased broadcast P fertilizer application and accumulation of plant residues • Lysed plant and microbial cells from freeze/dry, termination methods, and wet/dry periods No-till can increase dissolved P loss
  • 9. • Increased SOM and microbial activity could augment mineralization efficiency • Gonzalez-Chavez et al. (2010) found no-till increased proteins related to arbuscular mycorrhizal fungi by 43%, doubled microbial biomass C and N and increased microbial biomass P by 250% • Some organic P compounds (30-65% of total P) can be more labile than ortho-P while other can compete for sorption sites • This could lead to increased soluble ortho-P and bioavailable organic P in solution No-till can increase dissolved P loss Potential Mechanisms
  • 10. Kansas Agricultural Watershed Field Laboratory Graduate Student: David Abel, Elliott Carver, and Laura Starr Faculty: Nathan Nelson, Kraig Roozeboom, Gerard Kluitenberg, Peter Tomlinson, DeAnn Presley and Jeff Williams
  • 11. decreased erosion more than 65% Cover crop effects on sediment
  • 12. Cover crop effects on form of P loss Increased dissolved P 65%
  • 13. Cover crop effects on soil biological indicators
  • 15. Fall 2017 Fertilizer management effects on soil test P
  • 16. Phosphorus Cycle Dissolved P H2PO4 - / HPO4 2- Adsorbed P Root Zone Mineralization Immobilization Uptake Leaching H2PO4 - / HPO4 2- Organic P Secondary Mineral P Precipitation Desorption Adsorption Primary Mineral P DissolutionDissolution P in grain, forage, fruit, etc. Residue P Fertilizer and Manure P Dissolved P loss (minimal loss) Recycling Exports Erosion/RunoffAdditions Particulate P loss Dissolved P loss Particulate P loss Dissolved P loss Particulate P loss Alternate Management Alternate Management
  • 17. Paradigm Shift • Holistic implementation of conservation management systems • Nutrient management factors (rate, timing, placement, and source) should be appropriate for the conservation practices • New nutrient management paradigm: • Managing on the margins of deficiency required to meet crop production goals. For Example: Guided by coalition of agricultural and conservation organizations to support farmers’ efforts to implement precise nutrient management and conservation practices. www.4rplus.org
  • 18. Thank you Peter Tomlinson - Environmental Quality (ptomlin@ksu.edu) Department of Agronomy, Kansas State University
  • 19. Cover crop effects on runoff
  • 20. Cumulative Emissions Yield Scaled Emissions
  • 21. N Fertilizer Replacement Value 1Means with different letters within columns are significantly different (LSD=0.05) • Regression equation of grain yield for chemical fallow as a function of N fertilizer rate • Solved the equation substituting the mean grain yield at 0-N for each cover crop treatment Cover crop treatment Mean grain yield at 0 N rate (bu ac-1) Fertilizer N equivalent value (lb N ac-1) Chemical fallow 88 b - Double-crop soybean 91 b 8 b Summer legume 100 a 30 a Summer non-legume 64 c -45 c Winter legume 87 b -1 b Winter non-legume 87 b -3 b Preza Fontes, G., P. Tomlinson, K. Roozeboom, and D. Ruiz Diaz. 2017. Grain Sorghum Response to Nitrogen Fertilizer Following Cover Crops. Agronomy Journal. DOI: 10.2134/agronj2017.03.0180. 109(6) 2723-2737. KAES# 17-286-J.
  • 22. • Rainfall • Duration and intensity of events • Structural Conservation Practices • Terraces and Terrace Maintenance • Waterways • Sediment basins for tile outlet terraces • Residue • No-till • Cover crops How Can we Keep Soil and Nutrients in Place

Editor's Notes

  1. Successful and comprehensive conservation planning necessitates a holistic approach. Planning must consider all of the conservation and production goals such as yield, soil health, soil conservation, nutrient management, water quality, sustainability, and climate resilience.
  2. In areas at high risk for P loss, adjusting other management practices (e.g., nutrient placement, drainage management) may be necessary to achieve soil health objectives without further water quality degradation
  3. In areas at high risk for P loss, adjusting other management practices (e.g., nutrient placement, drainage management) may be necessary to achieve soil health objectives without further water quality degradation
  4. Environ. Sci. Technol. 46:10660–10666. doi:10.1021/es302315d Published in: Craig A. Stow; YoonKyung Cha; Laura T. Johnson; Remegio Confesor; R. Peter Richards; Environ. Sci. Technol.  2015, 49, 3392-3400. DOI: 10.1021/es5062648 Copyright © 2015 American Chemical Society
  5. Source: Daryanto et al., 2017. J. of Environ. Qual. 46:1028–1037; doi:10.2134/jeq2017.03.0121 There were 126, 60, and 45 data points from 20, 13, and 12 studies for soluble P, particulate P, and total P concentrations, respectively. For P loads, there were 83, 52, and 39 data points from 20, 10, and 10 studies for soluble P, particulate P, and total P, respectively.
  6. SI resulted in about 30% decrease in TP and about 45% decrease in dissolved P loss. (no effect on particulate P).
  7. Stats for 7/13/16 event Inches min inches/hr total precip 0.94 81 0.7 max 3 min rainfall 0.34 3 6.8 max 10 min rainfall 0.74 10 4.44 max 20 min rainfall 0.89 20 2.67 101 104 total runoff (ft3) 2100 2099 area (ac) 1.2 1.27 runoff (inches) 0.48 0.46 peak runoff (cfs) 1.06 1.6 time to peak (min) 28 17 time to ini. of runoff (min) 7 2 runoff duration (min) 141 102