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Josan
Manure-component Effects on P Release from Manure-amended
Sandy Soils
M. S. Josan
IntroductionIntroduction
Active and abandoned dairiesActive and abandoned dairies
Continuous release of P from these soils Continuous release of P from these soils even years after abandonment (Nair et al., even years after abandonment (Nair et al., 2003)2003)
Paucity of P retaining mineralsPaucity of P retaining minerals
Manure components are important in the Manure components are important in the fate of P in dairy manure-impacted soilsfate of P in dairy manure-impacted soils
Importance of Mg in P dynamics in these Importance of Mg in P dynamics in these soils has not been recognizedsoils has not been recognized
Properties of Manure Impacted Properties of Manure Impacted and Unimpacted Soilsand Unimpacted Soils
Impacted Unimpacted
pH 6.7-7.5
EC (dS m-1) 0.4-0.8
Total Ca (mg kg-1) 3200-8400
Total Mg (mg kg-1) 700-2100
Total P (mg kg-1) 1000-3200
Total Fe (mg kg-1) 190 – 1200
Total Al (mg kg-1) 300 - 4000
Impacted Unimpacted
pH 6.7-7.5 3.8 - 5.0
EC (dS m-1) 0.4-0.8 0.07 – 0.20
Total Ca (mg kg-1) 3200-8400 50 – 640
Total Mg (mg kg-1) 700-2100 10 – 50
Total P (mg kg-1) 1000-3200 58 – 190
Total Fe (mg kg-1) 190 – 1200 300 – 1800
Total Al (mg kg-1) 300 - 4000 120 - 1138
RationaleRationale
High Ca concentrations and pH should High Ca concentrations and pH should favor the formation of relatively stable favor the formation of relatively stable calcium phosphatescalcium phosphates
Stable Ca-P minerals (such as apatite) Stable Ca-P minerals (such as apatite) have not been found in heavy manure-have not been found in heavy manure-impacted soils (Wang et al. 1995)impacted soils (Wang et al. 1995)
Non-formation of Ca-P minerals could be Non-formation of Ca-P minerals could be due to inhibition by Mg, biogenic Si, and due to inhibition by Mg, biogenic Si, and DOCDOC
HypothesesHypotheses
The release of phosphorus (P) in dairy The release of phosphorus (P) in dairy
manure-impacted soils is controlled by manure-impacted soils is controlled by
sparingly soluble Ca and/or Mg-sparingly soluble Ca and/or Mg-
phosphate phasesphosphate phases
Magnesium phosphate is a manure Magnesium phosphate is a manure
component rather than a component component rather than a component
formed in soil after manure applicationformed in soil after manure application
ObjectivesObjectives
Assess the release of Ca, Mg and P in Assess the release of Ca, Mg and P in soil solution from dairy manure-soil solution from dairy manure-impacted soilsimpacted soils
Evaluate Ca and/or Mg-P association in Evaluate Ca and/or Mg-P association in dairy manure and manure-impacted dairy manure and manure-impacted soilssoils
Materials and MethodsMaterials and Methods
Soil and manure samplingSoil and manure sampling
Particle size fractionation and chemical Particle size fractionation and chemical characterization of soil and manure samplescharacterization of soil and manure samples
Repeated water Repeated water extractionsextractions
Column leachingColumn leaching
Materials and MethodsMaterials and Methods
Chemical equilibrium modeling (V-Chemical equilibrium modeling (V-MINTEQ)MINTEQ)
– Soil and dairy manure column Soil and dairy manure column effluentseffluents
– Saturation paste extractsSaturation paste extracts
Chemical fractionationChemical fractionation
Josan
Fractionation Scheme
Soil (2g)
NH4Cl-P
20 mL 1M NH4Cl
2-h shaking
Labile -P
Total P
Org. –P=
(Total P- In -P) Nair et al., 1995
NaOH-P
20 mL 0.1M NaOH
17-h shaking
Fe/Al -P
HCl-P
20 mL 0.5M HCl
24-h shaking
Ca/Mg -P
Residual-P
Ignition at 550o C
Acid solubilization
Mainly organic -P
Josan
Percentage of P Fractions in A-horizon of a Heavily Manure-impacted soil
(TP= 2900 mg kg-1) 1st NH4Cl Extraction10%
69%
3%
10%
8%
Ca/Mg -PN
H4C
l -P
Resid
ual -P
Al/Fe -POrg. -P
Hieltjes and Lijklema (1980)
Nair et al. (1995)
Josan
Percentage of P Fractions in A-horizon of a Heavily Manure-impacted soil
(TP= 2900 mg kg-1) 2nd NH4Cl Extraction
20%
59%
3%
10%
8%
Ca/Mg -P
Resid
ual -P
NH4Cl -PAl/Fe -POrg. -P
Josan
Percentage of P Fractions in A-horizon of a Heavily Manure-impacted soil
(TP= 2900 mg kg-1) 3rd NH4Cl Extraction
35%
44%
3%
10%
8%
Ca/Mg -P
Resid
ual -P
NH4Cl -PAl/Fe -POrg. -P
Josan
Percentage of P Fractions in A-horizon of a Heavily Manure-impacted soil
(TP= 2900 mg kg-1) ‘n’ Extractions
70%
9%
3%
10%
8%
Ca/Mg -P
Resid
ual -P
NH4Cl -P
Al/Fe -POrg. -P
Josan
Modified Fractionation Scheme
Soil (2g)
NH4Cl-P
20 mL 1M NH4Cl
2-h shaking
1st Extraction
NH4Cl-P
20 mL 1M NH4Cl
2-h shaking
10th Extraction or Greater
NH4Cl-P
20 mL 1M NH4Cl
2-h shaking
2nd Extraction
NH4Cl-P
20 mL 1M NH4Cl
2-h shaking
3rd Extraction
Residual-P
Ignition at 550o C
Acid solubilization
NaOH-P
20 mL 0.1M NaOH
17-h shaking
HCl-P
20 mL 0.5M HCl
24-h shaking
• Ca, Mg, and P concentrations will be determined in each extraction
Materials and MethodsMaterials and Methods
Solid state assessments: Solid state assessments:
– Density separationDensity separation
– X-ray diffraction (X-ray diffraction (XRD) XRD)
– Thermogravimetery (Thermogravimetery (TG) TG)
– Scanning electron microscopy (Scanning electron microscopy (SEM) SEM)
and Energy dispersive X-ray analysis and Energy dispersive X-ray analysis
(EDS)(EDS)
Josan
Solid State Assessment
XRD
TG
SEM
Air-dried soil Air-dried manure
Particle size fractionation and pre-concentration
? P with Mg or Ca
Density separation
<2.0 g cm-3
>2.0 g cm-3
Density separation
<2.0 g cm-3
>2.0 g cm-3
Silt Clay
Statistical Analysis Statistical Analysis
Analysis of variance (ANOVA)Analysis of variance (ANOVA)
– The Student-Newman-KeulsThe Student-Newman-Keuls
Non-parametric statistics (the Kruskal-Non-parametric statistics (the Kruskal-
Wallis test)Wallis test)
Josan
Preliminary Results
Josan
SRP, Mg and Ca Relationships for Active Dairy Manure Soils during Repeated Water Extractions
Josan et al. 2005 (in press)
y = 1.98x - 3.81
r 2 = 0.68 (Mg)
y = -0.19x + 79.4
r 2 = 0.01 (Ca)
0
20
40
60
80
100
120
140
160
0 20 40 60 80 100 120 140Mg or Ca (mg kg-1)
SR
P (
mg
kg-1
)
Mg Ca
Josan
SRP, Mg and Ca Relationships for Abandoned Dairy Manure Soils during Repeated Water Extractions
Josan et al. 2005 (in press)
y = 1.19x + 10.83
r 2 = 0.62 (Mg)
y = 0.45x + 21.0
r 2 = 0.20 (Ca)
0
20
40
60
80
100
120
140
0 20 40 60 80 100 120 140Mg or Ca (mg kg-1)
SRP
(mg
kg-1
)
Mg Ca
Josan
Speciation Data from Column Leachates
Mineral
PhaseFormula
Active Abandoned
(SI = log IAP - log Ksp)
Struvite (NH4MgPO4·6H2O) -0.28 -1.63
Farringtonite Mg3(PO4)2 -1.03 -1.68
Newberryite MgHPO4·3H2O -0.60 -0.86
Monetite CaHPO4 0.17 0.54
Brushite CaHPO4·2H2O -0.11 0.26
Hydroxyapatite [Ca5(PO4)3 (OH)] 12.84 12.16
Josan et al. 2005 (in press)
Dot Map Images of Dairy Manure Dot Map Images of Dairy Manure Clay Size FractionClay Size Fraction
Expected Results and Implications Expected Results and Implications
P stabilization via crystallization of calcium P stabilization via crystallization of calcium phosphates (even at near-neutral pH) may be phosphates (even at near-neutral pH) may be preempted by Mg-P associationpreempted by Mg-P association
Mg-P association is a key factor for high P Mg-P association is a key factor for high P activities in these soilsactivities in these soils
Approaches to minimize P releaseApproaches to minimize P release– P-retaining soil amendments P-retaining soil amendments – Management of animal diet to eliminate Mg-P Management of animal diet to eliminate Mg-P
formation. formation.
AcknowledgmentsAcknowledgmentsSupported in part by the USDA-NRI Supported in part by the USDA-NRI Committee MembersCommittee Members– Dr. Vimala Nair (Chair)Dr. Vimala Nair (Chair)– Dr. Willie HarrisDr. Willie Harris– Dr. George O’ConnorDr. George O’Connor– Dr. Dean RhueDr. Dean Rhue– Dr. Tom ObrezaDr. Tom Obreza– Dr. Amelia Dempere (Materials Science & Dr. Amelia Dempere (Materials Science &
Engineering Department)Engineering Department)
Thanks are also due to several people in SWSD Thanks are also due to several people in SWSD who have helped me since my joining the who have helped me since my joining the departmentdepartment
Comments and SuggestionsComments and Suggestions
ThanksThanks