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Balancing of soil nutrients
to aid soil fertility programs, and
improves soil resilience to extreme weather conditions
Zouheir Massri, Ph.D
Soil Physics & Fertility Research Manager.
AgroLiquid, Michigan
Jerry Wilhm, Ph.D
Senior Research Manager
AgroLiquid, Michigan
74th
SOIL
AND WATER
CONSERVATION
SOCIETY
Soil fertility shows considerable variability in Ag. and research fields:
Variabilities are high when droughts are more severe, rainfall events
intensity, and varies with:
1. Soil type, soil texture, and soil structure.
2. Physical and chemical measurements (pH, organic matter, N, P, K, CEC, and etc.).
Gilford sandy loam
Dominant Soil Order: Mollisols
Percent Mollisols: 90%
Dominant Soil
Suborder:
Aquolls
Percent Aquolls 90%
Farmland Class: Prime farmland if drained
Parkhill loam
Dominant Soil Order: Inceptisols
Percent Inceptisols: 95%
Dominant Soil Suborder: Aquepts
Percent Aquepts 95%
Farmland Class: Prime farmland if drained
Capac loam, 0 to 4 percent slopes
Dominant Soil Order: Alfisols
Percent Alfisols: 90%
Dominant Soil Suborder: Aqualfs
Percent Aqualfs 90%
Farmland Class: Prime farmland if drained
Boyer complex, 0 to 6 percent slopes
Dominant Soil Order: Alfisols
Percent Alfisols: 100%
Dominant Soil Suborder: Udalfs
Percent Udalfs 100%
Farmland Class:
Farmland of local
importance
Marlette loam, 2 to 6 percent slopes
Dominant Soil Order: Alfisols
Percent Alfisols: 90%
Dominant Soil Suborder: Udalfs
Percent Udalfs 90%
Farmland Class:
All areas are prime
farmland
Corunna sandy loam
Dominant Soil Order: Mollisols
Percent Mollisols: 90%
Dominant Soil Suborder: Aquolls
Percent Aquolls 90%
Farmland Class: Prime farmland if drained
Adrian muck
Dominant Soil
Order:
Histosols
Percent Histosols: 100%
Dominant Soil
Suborder:
Saprists
Percent Saprists 100%
Farmland Class: Farmland of local importance
Boyer complex, 6 to 12 percent slopes
Dominant Soil Order: Alfisols
Percent Alfisols: 100%
Dominant Soil Suborder: Udalfs
Percent Udalfs 100%
Farmland Class: Farmland of local importance
Corn yield- 2018, NCRS farm7, AgroLiquid, Michigan
Soil fertility shows considerable variability in Ag. and research fields:
Variabilities are high when droughts are more severe, rainfall events
intensity, and varies with:
1. Soil type, soil texture, and soil structure.
2. Physical and chemical measurements (pH, organic matter, N, P, K, CEC, and etc.).
3. Soil available nutrients can vary widely as we move across Ag. field vs.
3.1. Variable application rates.
3.1. Variable application mix.
3.2. Variability of treatments spatial design.
D
D
D
D D
D
Liebig's Law of the Minimum
Nutrients Balance and Soil Resilience:
 Liebig's Law of the Minimum
- any deficiency of one plant nutrient will severely limit the
efficiency of other nutrients.
 In view of the widespread occurrence of nutrients
deficiencies, the scope and content of balanced fertilization
itself has changed.
 Likely, to includes now the deliberate application of all
nutrients that the soil cannot supply in adequate amounts for
optimal crop yield.
Soil Resilience vs. the 4- R principle
1. Right source
2. Right rate
3. Right time
4. Right place, and
5. and the Right ratio or (Variable Rate Technology- VRT, or the 5th –R)
The right ratio:
 The N/K ratio during plant vegetative growth.
 P/micro-elements (Fe, Mn, Zn and Cu), negative interaction.
 Ca/Mg ratio and potential adhesion of soil particles (Mg). This is a site specific.
 K/ Mg ratio (0.25- 0.35), Soil Health index by A&L Lab.
 NH4
+/ Ca2+, Mg2+, and K+
 % of Ca (65-72), Soil Health index by A&L Lab.
VRT, a practice was thought to enable growers to overcome challenges and to
adjust soil nutrients inputs based upon the soil properties and variabilities,
increase their yield, and to benefit the environment.
Therefore the main focus is:
1. To evaluate the long-term spatial and temporal nutrients variability associated
with fertilization programs.
2. Equalize soil nutrient dynamics using soil test information conducted to
determine affordable fertilizer application rates.
3. improve crops economic revenue, and improves soil conditions resilience.
4. Establishing soil fertility programs to improve soil resilience to extreme
weather conditions.
Soil Health indicators/ resilience:
1. Soil organic carbon.
2. Sort term carbon mineralization
3. Total N
4. Nitrogen mineralization rate.
5. Bulk density
6. Texture
7. Aggregate stability
8. Water infiltration rate
9. Water holding capacity
10. pH
11. EC
11. Erosion rating
12. Soil penetration resistance
13. Crop yield
14. CEC
15. Base saturation
16. Extractable K, P, Ca, Mg, Na
18. Extractable micronutrients: Fe, Zn, Cu, Mn
K+ (ppm)
3D of soil spatial distribution of potassium soil content (ppm)
sampled at 0-6” on April 12, 2018
Average 147.3 ppm
STDEV 34.61
0
50
100
150
200
250
300
350
0 5 10 15 20 25 30 35
ExchangeablePotassium(ppm)
Soil Cation-Exchange Capacity, CEC (meq/ 100g soil)
Changes of Available Potassium as related to Soil CEC
(Data of Midwest labs.)
Very low
Very high
Applied K (ppm) = ((
𝑺𝒐𝒊𝒍 𝒕𝒆𝒔𝒕 𝑲 𝒑𝒑𝒎 𝑿 𝟒% 𝑲 𝒃𝒂𝒔𝒆 𝒔𝒂𝒕𝒖𝒓𝒂𝒕𝒊𝒐𝒏
%𝑲 𝒔𝒐𝒊𝒍 𝒕𝒆𝒔𝒕 𝒃𝒂𝒔𝒆 𝒔𝒂𝒕𝒖𝒓𝒂𝒕𝒊𝒐𝒏
)- (𝑺𝒐𝒊𝒍 𝒕𝒆𝒔𝒕 𝑲 𝒑𝒑𝒎)
 An equalization of potassium was decided to apply to apply muriate of potash (0-0-62) as source of
potassium at rates to achieve 4% base saturation, as accepted level of potassium sufficiency.
 % K in the soil test base saturation) of soil testing was used for this in order to compensate for
variations in soil CEC (Cation Exchange Capacity) which influences sufficiency interpretation levels for
cations (positive charged soil nutrients).
What we did:
 The phosphorus was applied to the maintenance level based upon the amount of P2O5 phosphate needed
for a corn yield goal of 170 bu./ acre according to the Tri-State Fertilizer Guide (Vitosh et al., 1995).
Neal Kinsey et al., 1993
Pre-planting soil testing data of soil CEC (meq/100g soil), available potassium and phosphorus (ppm),
and amounts of applied K and P (ppm) following Tri-State Fertility Guide for Corn, and corn yield
(Bu/acre) of 18-701.
Reps Treatments CEC Pre-Planting soil
testing (ppm)
Soil content after
application
Applied K and P
(pound acre-1) in form
of
Corn yield
meq/100g K P1 Bray
K
(ppm)*
P
(ppm) Potash
(0-0—62)
DAP
(18-46-0)
Bu/ acre
Rep-1
Plot-1
(control) 10.1 126 10 126 10 0.0 0.0 148.9
Plot-2 9.7 139 11 150 29.1 43.6 180.0 153.4
Plot-3 9.7 123 10 149 29.2 101.0 191.0 164.4
Plot-4 10.9 124 13 171 28.9 182.1 158.0 167.5
Plot-5 11.0 125 13 172 28.9 183.5 158.0 157.8
Plot-6 11.2 147 19 173 28.3 100.4 93.0 157.8
Plot-7 11.9 153 22 185 28.1 125.6 61.0 165.3
Plot-8 13.4 186 19 207 28.3 80.0 93.0 174.7
Plot-9 13.2 210 24 210 27.9 0.0 39.0 172.0
Plot-10 13.0 181 22 201 28.1 77.8 61.0 184.1
Average
11.8
147.3 13.2 182.1 28.9 142.8 156.0 170*
STDEV**
1.5
34.6 6.4 28.0 0.5 65.7 102.2 11.7
Correlation of CEC vs K (ppm) of soil testing, R= 0.6
Correlation of CEC vs K (ppm) of soil testing + applied K (ppm), R= 0.9
What we did:
 Dry fertilizers were broadcast-applied over the corresponding
plots using a calibrated Gandy spreader supplemented with a
customized PTO-driven turbine to evenly blow the granules over
the 15-foot wide plots.
 The Potash was applied on May 9 and the DAP on May 10.
Fertilizers were incorporated into the ground with tillage following
application Gandy spreader:
Dry fertilizer applicator.
 Corn planted May 10, 2018
 A planter fertilizer application of 3 gal of Pro-Germinator® (9-24-3 + 0.1 Fe) + 3 gal of Kalibrate® (2-0-
10 +6S) + 1 quart of Micro 500® (micronutrients) per acre was applied in the seed furrow at planting
to promote uniformity for early growth.
 45 gal/ acre of High NRG-N® (27- 0-0- +7S) side-dressed by 360 Y-DROP® on June 15, 2018.
y = 124.13e0.0017x
R= 0.71
130
140
150
160
170
180
190
200
100 120 140 160 180 200 220 240
CornyieldBushel/Acre
Bushel/Acre
Values of K+ (ppm) of soil testing and preplanting applied K+
Correlation of corn yield vs recommended application rates
of (K + soil testing of K)
Average yield of applied K (B./acre) = 170
Average yield of control (B./acre) = 154
75
100
125
150
175
200
225
250
0 5 10 15 20 25 30 35 40
2018 K
2019 K
Soil testing-2019
STDEV = 23
Soil testing-2018
STDEV = 35
Sampled plots
K+(ppm)
Values of soil testing of potassium in 2018 and 2019
200
150
100
3D spatial distribution
Values of soil testing K (ppm)
19- 701
3D of soil spatial distribution of potassium soil content (ppm)
sampled at 0-6” on April 24, 2019
Average 138.4 ppm
STDEV 23.20
Conclusion for K:
2018 (corn) 2019 (Soybeans)
STDEV: 34.61 23.20
Lower value (of K soil testing, ppm) 104 105
Higher value (of K soil testing, ppm) 243 194
Average values (of K soil testing, ppm) 147.3 138.4
Applied Potash (Lb./acre) 5140 6710
Average of carry over (ppm): Control = 14
Treated = 45.3
Conclusion:
 Soil nutrients are dynamic in ag. fields conditions and in research plots.
 Soil nutrients variability and availability, likely occur, due to non-continuity of nutrient
levels of application and can vary widely as we move across agriculture growers’ field
and research plots.
 VRT, a practice, likely, will enable growers to overcome challenges and to adjust soil nutrients
inputs based upon the soil properties and variabilities, increase their yield, and to benefit the
environment.
 Hence, VRT a manageable tool of soil fertility for Soil Resilience and to benefit the
environment.
 Rationale management of soil fertility programs improves soil resilience to extreme
weather conditions, by providing healthy chemo-biophysical environment for plants.
Thank you
Questions
74th
SOIL
AND WATER
CONSERVATION
SOCIETY
Zouheir Massri, Ph.D
Soil Physics & Fertility Research Manager.
AgroLiquid, Michigan
Zouheir.Massri@agroliquid.com
Selecting Indicators for Soil Health/ Soil Resilience:
1. Ease of sampling.
2. Ease of measurement.
3. Accuracy.
4. Reliability.
5. Sensitive to management.
6. Cost sensitive to management, and Interpretability.

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July 29-1110-Zouheir Massri

  • 1. Balancing of soil nutrients to aid soil fertility programs, and improves soil resilience to extreme weather conditions Zouheir Massri, Ph.D Soil Physics & Fertility Research Manager. AgroLiquid, Michigan Jerry Wilhm, Ph.D Senior Research Manager AgroLiquid, Michigan 74th SOIL AND WATER CONSERVATION SOCIETY
  • 2. Soil fertility shows considerable variability in Ag. and research fields: Variabilities are high when droughts are more severe, rainfall events intensity, and varies with: 1. Soil type, soil texture, and soil structure. 2. Physical and chemical measurements (pH, organic matter, N, P, K, CEC, and etc.).
  • 3. Gilford sandy loam Dominant Soil Order: Mollisols Percent Mollisols: 90% Dominant Soil Suborder: Aquolls Percent Aquolls 90% Farmland Class: Prime farmland if drained Parkhill loam Dominant Soil Order: Inceptisols Percent Inceptisols: 95% Dominant Soil Suborder: Aquepts Percent Aquepts 95% Farmland Class: Prime farmland if drained Capac loam, 0 to 4 percent slopes Dominant Soil Order: Alfisols Percent Alfisols: 90% Dominant Soil Suborder: Aqualfs Percent Aqualfs 90% Farmland Class: Prime farmland if drained Boyer complex, 0 to 6 percent slopes Dominant Soil Order: Alfisols Percent Alfisols: 100% Dominant Soil Suborder: Udalfs Percent Udalfs 100% Farmland Class: Farmland of local importance Marlette loam, 2 to 6 percent slopes Dominant Soil Order: Alfisols Percent Alfisols: 90% Dominant Soil Suborder: Udalfs Percent Udalfs 90% Farmland Class: All areas are prime farmland Corunna sandy loam Dominant Soil Order: Mollisols Percent Mollisols: 90% Dominant Soil Suborder: Aquolls Percent Aquolls 90% Farmland Class: Prime farmland if drained Adrian muck Dominant Soil Order: Histosols Percent Histosols: 100% Dominant Soil Suborder: Saprists Percent Saprists 100% Farmland Class: Farmland of local importance Boyer complex, 6 to 12 percent slopes Dominant Soil Order: Alfisols Percent Alfisols: 100% Dominant Soil Suborder: Udalfs Percent Udalfs 100% Farmland Class: Farmland of local importance
  • 4. Corn yield- 2018, NCRS farm7, AgroLiquid, Michigan
  • 5. Soil fertility shows considerable variability in Ag. and research fields: Variabilities are high when droughts are more severe, rainfall events intensity, and varies with: 1. Soil type, soil texture, and soil structure. 2. Physical and chemical measurements (pH, organic matter, N, P, K, CEC, and etc.). 3. Soil available nutrients can vary widely as we move across Ag. field vs. 3.1. Variable application rates. 3.1. Variable application mix. 3.2. Variability of treatments spatial design. D D D D D D
  • 6. Liebig's Law of the Minimum Nutrients Balance and Soil Resilience:  Liebig's Law of the Minimum - any deficiency of one plant nutrient will severely limit the efficiency of other nutrients.  In view of the widespread occurrence of nutrients deficiencies, the scope and content of balanced fertilization itself has changed.  Likely, to includes now the deliberate application of all nutrients that the soil cannot supply in adequate amounts for optimal crop yield.
  • 7. Soil Resilience vs. the 4- R principle 1. Right source 2. Right rate 3. Right time 4. Right place, and 5. and the Right ratio or (Variable Rate Technology- VRT, or the 5th –R) The right ratio:  The N/K ratio during plant vegetative growth.  P/micro-elements (Fe, Mn, Zn and Cu), negative interaction.  Ca/Mg ratio and potential adhesion of soil particles (Mg). This is a site specific.  K/ Mg ratio (0.25- 0.35), Soil Health index by A&L Lab.  NH4 +/ Ca2+, Mg2+, and K+  % of Ca (65-72), Soil Health index by A&L Lab.
  • 8. VRT, a practice was thought to enable growers to overcome challenges and to adjust soil nutrients inputs based upon the soil properties and variabilities, increase their yield, and to benefit the environment. Therefore the main focus is: 1. To evaluate the long-term spatial and temporal nutrients variability associated with fertilization programs. 2. Equalize soil nutrient dynamics using soil test information conducted to determine affordable fertilizer application rates. 3. improve crops economic revenue, and improves soil conditions resilience. 4. Establishing soil fertility programs to improve soil resilience to extreme weather conditions.
  • 9. Soil Health indicators/ resilience: 1. Soil organic carbon. 2. Sort term carbon mineralization 3. Total N 4. Nitrogen mineralization rate. 5. Bulk density 6. Texture 7. Aggregate stability 8. Water infiltration rate 9. Water holding capacity 10. pH 11. EC 11. Erosion rating 12. Soil penetration resistance 13. Crop yield 14. CEC 15. Base saturation 16. Extractable K, P, Ca, Mg, Na 18. Extractable micronutrients: Fe, Zn, Cu, Mn
  • 10.
  • 11. K+ (ppm) 3D of soil spatial distribution of potassium soil content (ppm) sampled at 0-6” on April 12, 2018 Average 147.3 ppm STDEV 34.61
  • 12. 0 50 100 150 200 250 300 350 0 5 10 15 20 25 30 35 ExchangeablePotassium(ppm) Soil Cation-Exchange Capacity, CEC (meq/ 100g soil) Changes of Available Potassium as related to Soil CEC (Data of Midwest labs.) Very low Very high
  • 13. Applied K (ppm) = (( 𝑺𝒐𝒊𝒍 𝒕𝒆𝒔𝒕 𝑲 𝒑𝒑𝒎 𝑿 𝟒% 𝑲 𝒃𝒂𝒔𝒆 𝒔𝒂𝒕𝒖𝒓𝒂𝒕𝒊𝒐𝒏 %𝑲 𝒔𝒐𝒊𝒍 𝒕𝒆𝒔𝒕 𝒃𝒂𝒔𝒆 𝒔𝒂𝒕𝒖𝒓𝒂𝒕𝒊𝒐𝒏 )- (𝑺𝒐𝒊𝒍 𝒕𝒆𝒔𝒕 𝑲 𝒑𝒑𝒎)  An equalization of potassium was decided to apply to apply muriate of potash (0-0-62) as source of potassium at rates to achieve 4% base saturation, as accepted level of potassium sufficiency.  % K in the soil test base saturation) of soil testing was used for this in order to compensate for variations in soil CEC (Cation Exchange Capacity) which influences sufficiency interpretation levels for cations (positive charged soil nutrients). What we did:  The phosphorus was applied to the maintenance level based upon the amount of P2O5 phosphate needed for a corn yield goal of 170 bu./ acre according to the Tri-State Fertilizer Guide (Vitosh et al., 1995). Neal Kinsey et al., 1993
  • 14. Pre-planting soil testing data of soil CEC (meq/100g soil), available potassium and phosphorus (ppm), and amounts of applied K and P (ppm) following Tri-State Fertility Guide for Corn, and corn yield (Bu/acre) of 18-701. Reps Treatments CEC Pre-Planting soil testing (ppm) Soil content after application Applied K and P (pound acre-1) in form of Corn yield meq/100g K P1 Bray K (ppm)* P (ppm) Potash (0-0—62) DAP (18-46-0) Bu/ acre Rep-1 Plot-1 (control) 10.1 126 10 126 10 0.0 0.0 148.9 Plot-2 9.7 139 11 150 29.1 43.6 180.0 153.4 Plot-3 9.7 123 10 149 29.2 101.0 191.0 164.4 Plot-4 10.9 124 13 171 28.9 182.1 158.0 167.5 Plot-5 11.0 125 13 172 28.9 183.5 158.0 157.8 Plot-6 11.2 147 19 173 28.3 100.4 93.0 157.8 Plot-7 11.9 153 22 185 28.1 125.6 61.0 165.3 Plot-8 13.4 186 19 207 28.3 80.0 93.0 174.7 Plot-9 13.2 210 24 210 27.9 0.0 39.0 172.0 Plot-10 13.0 181 22 201 28.1 77.8 61.0 184.1 Average 11.8 147.3 13.2 182.1 28.9 142.8 156.0 170* STDEV** 1.5 34.6 6.4 28.0 0.5 65.7 102.2 11.7 Correlation of CEC vs K (ppm) of soil testing, R= 0.6 Correlation of CEC vs K (ppm) of soil testing + applied K (ppm), R= 0.9
  • 15. What we did:  Dry fertilizers were broadcast-applied over the corresponding plots using a calibrated Gandy spreader supplemented with a customized PTO-driven turbine to evenly blow the granules over the 15-foot wide plots.  The Potash was applied on May 9 and the DAP on May 10. Fertilizers were incorporated into the ground with tillage following application Gandy spreader: Dry fertilizer applicator.  Corn planted May 10, 2018  A planter fertilizer application of 3 gal of Pro-Germinator® (9-24-3 + 0.1 Fe) + 3 gal of Kalibrate® (2-0- 10 +6S) + 1 quart of Micro 500® (micronutrients) per acre was applied in the seed furrow at planting to promote uniformity for early growth.  45 gal/ acre of High NRG-N® (27- 0-0- +7S) side-dressed by 360 Y-DROP® on June 15, 2018.
  • 16. y = 124.13e0.0017x R= 0.71 130 140 150 160 170 180 190 200 100 120 140 160 180 200 220 240 CornyieldBushel/Acre Bushel/Acre Values of K+ (ppm) of soil testing and preplanting applied K+ Correlation of corn yield vs recommended application rates of (K + soil testing of K) Average yield of applied K (B./acre) = 170 Average yield of control (B./acre) = 154
  • 17. 75 100 125 150 175 200 225 250 0 5 10 15 20 25 30 35 40 2018 K 2019 K Soil testing-2019 STDEV = 23 Soil testing-2018 STDEV = 35 Sampled plots K+(ppm) Values of soil testing of potassium in 2018 and 2019
  • 18. 200 150 100 3D spatial distribution Values of soil testing K (ppm) 19- 701 3D of soil spatial distribution of potassium soil content (ppm) sampled at 0-6” on April 24, 2019 Average 138.4 ppm STDEV 23.20
  • 19. Conclusion for K: 2018 (corn) 2019 (Soybeans) STDEV: 34.61 23.20 Lower value (of K soil testing, ppm) 104 105 Higher value (of K soil testing, ppm) 243 194 Average values (of K soil testing, ppm) 147.3 138.4 Applied Potash (Lb./acre) 5140 6710 Average of carry over (ppm): Control = 14 Treated = 45.3
  • 20. Conclusion:  Soil nutrients are dynamic in ag. fields conditions and in research plots.  Soil nutrients variability and availability, likely occur, due to non-continuity of nutrient levels of application and can vary widely as we move across agriculture growers’ field and research plots.  VRT, a practice, likely, will enable growers to overcome challenges and to adjust soil nutrients inputs based upon the soil properties and variabilities, increase their yield, and to benefit the environment.  Hence, VRT a manageable tool of soil fertility for Soil Resilience and to benefit the environment.  Rationale management of soil fertility programs improves soil resilience to extreme weather conditions, by providing healthy chemo-biophysical environment for plants.
  • 21. Thank you Questions 74th SOIL AND WATER CONSERVATION SOCIETY Zouheir Massri, Ph.D Soil Physics & Fertility Research Manager. AgroLiquid, Michigan Zouheir.Massri@agroliquid.com
  • 22. Selecting Indicators for Soil Health/ Soil Resilience: 1. Ease of sampling. 2. Ease of measurement. 3. Accuracy. 4. Reliability. 5. Sensitive to management. 6. Cost sensitive to management, and Interpretability.

Hinweis der Redaktion

  1. The development of agriculture has lead to a disturbance in the nutrient balance (integrated farming vs. mechanized).
  2. Soils show considerable variability in fields. Soil texture, soil type, physical measurements (pH, organic matter, etc.) as well as nutrient levels can vary widely as you move across a field.
  3. The development of agriculture has lead to a disturbance in the nutrient balance (integrated farming vs. mechanized).
  4. Imbalanced nutrient supply results in mining of the soil nutrient reserves. Imbalanced availability of nutrients also encourages luxury consumption of nutrients supplied in excess. The nutrients balance depends on the supply from the soil and the demand by the plant. Nutrient imbalance impacts fertilizer use efficiency. The phenomenon of cation /anion balance. Balanced soil fertility has direct impact on soil resilience.
  5. This is common knowledge that has led to Variable Rate Technology (VRT).
  6. In view of the widespread occurrence of other nutrient deficiencies, the scope and content of balanced fertilization itself has changed. It now includes the deliberate application of all such nutrients that the soil cannot supply in adequate amounts for optimal crop yield.