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Organic Phosphorus Solid phase interactions Courtney Giles, PhD Candidate School of Engineering, Environmental Engineering Geochemistry of Natural Waters (GEOL235) Tuesday 25 October 2011, 2:30-3:45pm Delehanty 219

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Organic Phosphorus Solid phase interactions

Courtney Giles, PhD Candidate School of Engineering, Environmental Engineering Geochemistry of Natural Waters (GEOL235) Tuesday 25 October 2011, 2:30-3:45pm Delehanty 219

What I Study:

Organic P: PHYTATE

What I Study:

Organic P: PHYTATE

How can soil bacteria do this?

What I Study:

Organic P: PHYTATE

Siderophores/Organic Anions

What I Study:

Organic P: PHYTATE

Result: Plant availability INCREASES

How does Organic P get there in the first place?

Organic P: PHYTATE

How is it removed?

How is it removed? DESORPTION

Today Soil Organic P Forms/Sources Behavior in Soils Measurement DESORPTION (e.g. phytate) Mechanisms Kinetics

Soil Phosphorus

Total Soil P

Soil Phosphorus

Inorganic Organic

Total Soil P

Inorganic Phosphorus

Inorganic

Total Soil P

Inorganic Phosphorus

Inorganic Mono-Phosphate

Pyro-Phosphate

Poly-Phosphate

= P O

O-

O-

-O

= P O

O-

O-

O = P O

O-

O-

= P O

O-

O-

O = P O

O-

O-

n

FORMS

Total Soil P

Inorganic Phosphorus

Inorganic

= P O

O-

O-

-O

= P O

O-

O-

O = P O

O-

O-

= P O

O-

O-

O = P O

O-

O-

n

Fertilization Mineral P

Organic breakdown

Microbial storage

SOURCES

Total Soil P

Organic Inorganic

Organic Phosphorus

Total Soil P

Organic Inorganic

Organic Phosphorus Orthophosphate

Diesters

1

2

Total Soil P

Organic Inorganic

Organic Phosphorus

Nucleic Acids (0.2 – 2.4% Organic P) DNA, RNA Phospholipids (0.5 – 7% Organic P) phosphatidylcholine (lecithin) Phosphatidylethanolamine (cephalin) Fatty Acids Teichoic acids

Orthophosphate

Diesters

FORMS

Total Soil P

Organic Inorganic

Organic Phosphorus

Nucleic Acids (0.2 – 2.4% Organic P) Biological Phospholipids (0.5 – 7% Organic P) Cell membrane Cell membrane Fatty Acids Microbial cell wall/membrane

Orthophosphate

Diesters

SOURCES

Organic Phosphorus

Nucleic Acids (0.2 – 2.4% Organic P) DNA, RNA Phospholipids (0.5 – 7% Organic P) phosphatidylcholine (lecithin) Phosphatidylethanolamine (cephalin) Fatty Acids Teichoic acids (Microbial cell wall/membrane)

Orthophosphate

Diesters Find the phospho-di-ester bonds…..

Organic Phosphorus

Nucleic Acids (0.2 – 2.4% Organic P) DNA, RNA Phospholipids (0.5 – 7% Organic P) phosphatidylcholine (lecithin) Phosphatidylethanolamine (cephalin) Fatty Acids Teichoic acids (Microbial cell wall/membrane)

Find the phospho-di-ester bonds…..

Total Soil P

Organic Inorganic

Organic Phosphorus

Orthophosphate Monoesters

Organic Phosphorus

Inositol phosphates

glycerophosphates

AMP

FORMS Orthophosphate Monoesters

Organic Phosphorus

Seed/grain, eukaryotes

Biological

Phospholipid break-down

Biological

SOURCES Orthophosphate Monoesters

Total Soil P

Organic Inorganic

Organic Phosphorus

Orthophosphate

Monoesters

Orthophosphate

Diesters

Inorganic

= P O

O-

O-

-O

= P O

O-

O-

O = P O

O-

O-

Organic Phosphorus ORIGINS in SOIL

The Phytate Story

Manures

Feed Digestion

Animal Feed

Plant Seeds

Today Soil Organic P Forms/Sources

Behavior in Soils Measurement DESORPTION (e.g. phytate) Mechanisms Kinetics

Today Soil Organic P Forms/Sources

Behavior in Soils Measurement DESORPTION (e.g. phytate) Mechanisms Kinetics

PHYTATE

GOETHITE

Today Soil Organic P Forms/Sources

Behavior in Soils Measurement DESORPTION (e.g. phytate) Mechanisms Kinetics

PHYTATE

GOETHITE

Abiotic Biotic

PROCESSES

PHYTATE

GOETHITE Celi et al. 2001a

Abiotic

Sorption and Desorption influenced by: P Concentration Mineral surface characteristics pH Ionic strength Temperature

PHYTATE

GOETHITE Celi et al. 2001a

Abiotic

Sorption and Desorption influenced by: P Concentration Mineral surface characteristics pH Ionic strength Temperature

PHYTATE

GOETHITE

1. Depends on aqueous CHARGE SPECIES

Celi et al. 2001a

Abiotic

PHYTATE

GOETHITE

2. Depends on mineral surface CHARGE

Celi et al. 2001a

Abiotic

3. Depends on electrostatic INTERACTIONS

Celi et al. 2001a

Abiotic

GOETHITE

3. Depends on electrostatic INTERACTIONS

Celi et al. 2001a

Abiotic

Celi et al. 2001a CALCITE

Abiotic

Celi et al. 2000

Phytate and Phosphate on Calcite Abiotic

Biotic

InsP6

Biotic DEGRADATION

InsP5

InsP6

Biotic DEGRADATION

= P O

O-

O-

-O

InsP5

InsP6

InsP4

Biotic DEGRADATION

= P O

O-

O-

-O

= P O

O-

O-

-O

InsP5

InsP6

InsP4

InsP3

Biotic DEGRADATION

= P O

O-

O-

-O

= P O

O-

O-

-O

= P O

O-

O-

-O

InsP6

Biotic DEGRADATION

= P O

O-

O-

-O = P O

O-

O-

-O

= P O

O-

O-

-O

= P O

O-

O-

-O = P O

O-

O-

-O

= P O

O-

O-

-O

InsP0

Enzyme Hydrolysis

InsP6

Biotic DEGRADATION

InsP0

Enzyme Hydrolysis

PHYTASES Fungus Bacteria Plants

ABIOTIC PROCESSES

RECAP: Behavior in Soils

GOETHITE – phytate

ABIOTIC PROCESSES

RECAP: Behavior in Soils

GOETHITE – InsP6

BIOTIC PROCESSES

ABIOTIC PROCESSES

RECAP: Behavior in Soils

ABIOTIC PROCESSES

GOETHITE – InsP6

BIOTIC PROCESSES

RECAP: Behavior in Soils

ABIOTIC PROCESSES

BIOTIC PROCESSES

PHYSICAL PROCESSES

RECAP: Behavior in Soils

Section 1

The Inositol Phosphates in

Soils and Manures ABIOTIC PROCESSES

BIOTIC PROCESSES

PHYSICAL PROCESSES

Today Soil Organic P Forms/Sources Behavior in Soils

Measurement

DESORPTION (e.g. phytate) Mechanisms Kinetics

Today Soil Organic P Forms/Sources Behavior in Soils

Measurement

DESORPTION (e.g. phytate) Mechanisms Kinetics

Aqueous Extraction

31P-NMR Enzymatic Hydrolysis

METHODS

Extraction Soil

WATER

SODIUM

BICARBONATE

NaOH EDTA

‘The Inositol Phosphates in Soils and Manures: Abundance, Cycling, and Measurement’. Giles, CD, BJ Cade-Menun, JE Hill, 2011, Can. J. Soil Sci., in press.

Aqueous Extraction

Extraction Soil

WATER

SODIUM

BICARBONATE

NaOH EDTA

‘The Inositol Phosphates in Soils and Manures: Abundance, Cycling, and Measurement’. Giles, CD, BJ Cade-Menun, JE Hill, 2011, Can. J. Soil Sci., in press.

Aqueous Extraction

Total Soil P

Inorganic Organic

Extraction Soil

WATER

SODIUM

BICARBONATE

NaOH EDTA

Aqueous Extraction

Total Soil P

Inorganic Organic

‘The Inositol Phosphates in Soils and Manures: Abundance, Cycling, and Measurement’. Giles, CD, BJ Cade-Menun, JE Hill, 2011, Can. J. Soil Sci., in press.

Aqueous Extraction

Spectroscopy

Enzyme

Hydrolysis

Extraction Soil

‘The Inositol Phosphates in Soils and Manures: Abundance, Cycling, and Measurement’. Giles, CD, BJ Cade-Menun, JE Hill, 2011, Can. J. Soil Sci., in press.

Solution 31P

NMR

NaOH-EDTA Soil

Solution 31P Nuclear Magnetic Resonance Spectroscopy

Aqueous Extraction

Solution 31P

NMR

NaOH-EDTA Soil

Barbara J. Cade-Menun 2007

Solution 31P Nuclear Magnetic Resonance Spectroscopy

‘The Inositol Phosphates in Soils and Manures: Abundance, Cycling, and Measurement’. Giles, CD, BJ Cade-Menun, JE Hill, 2011, Can. J. Soil Sci., in press.

5 0 -5 PPM

Pyrophosphate

Orthophosphate

Other Diesters

Phosphate Diester

Orthophosphate Monoesters

Solution 31P Nuclear Magnetic Resonance Spectroscopy

Enzyme

Hydrolysis

NaOH-EDTA Soil

‘The Inositol Phosphates in Soils and Manures: Abundance, Cycling, and Measurement’. Giles, CD, BJ Cade-Menun, JE Hill, 2011, Can. J. Soil Sci., in press.

Total Soil P

Organic Inorganic

Enzymatic Hydrolysis

Enzyme

Hydrolysis

NaOH-EDTA Soil

‘The Inositol Phosphates in Soils and Manures: Abundance, Cycling, and Measurement’. Giles, CD, BJ Cade-Menun, JE Hill, 2011, Can. J. Soil Sci., in press.

Total Soil P

Organic Inorganic

Enzymatic Hydrolysis

PHOSPHATASES

Enzyme

Hydrolysis

NaOH-EDTA Soil

‘The Inositol Phosphates in Soils and Manures: Abundance, Cycling, and Measurement’. Giles, CD, BJ Cade-Menun, JE Hill, 2011, Can. J. Soil Sci., in press.

Enzymatic Hydrolysis

PHOSPHATASES Diesterases

Total Soil P

Organic Inorganic

Enzyme

Hydrolysis

NaOH-EDTA Soil

‘The Inositol Phosphates in Soils and Manures: Abundance, Cycling, and Measurement’. Giles, CD, BJ Cade-Menun, JE Hill, 2011, Can. J. Soil Sci., in press.

Enzymatic Hydrolysis

PHOSPHATASES

Monoesterases

Total Soil P

Organic Inorganic

Enzyme

Hydrolysis

NaOH-EDTA Soil

‘The Inositol Phosphates in Soils and Manures: Abundance, Cycling, and Measurement’. Giles, CD, BJ Cade-Menun, JE Hill, 2011, Can. J. Soil Sci., in press.

Enzymatic Hydrolysis

PHOSPHATASES

Monoesterases

Total Soil P

Organic Inorganic

Phytases

Enzyme

Hydrolysis

NaOH-EDTA Soil

‘The Inositol Phosphates in Soils and Manures: Abundance, Cycling, and Measurement’. Giles, CD, BJ Cade-Menun, JE Hill, 2011, Can. J. Soil Sci., in press.

Enzymatic Hydrolysis

PHOSPHATASES

Total Soil P

Organic Inorganic

Phytases

Monoesterases

Diesterases P

P

P

Enzymatic Hydrolysis

P Concentration

Ab

sorb

ence

Beer-Lambert A = e l c

Enzyme

Hydrolysis

NaOH-EDTA Soil

Enzymatic Hydrolysis

Total Soil P

Organic Inorganic

ESTIMATES Enzyme-Labile P

MEASURES Specific P classes

Today Soil Organic P Forms/Sources Behavior in Soils Measurement

DESORPTION (e.g. phytate) Mechanisms Kinetics

Today Soil Organic P Forms/Sources Behavior in Soils Measurement

DESORPTION (e.g. phytate) Mechanisms Kinetics

Negligible under environmental conditions…

Today Soil Organic P Forms/Sources Behavior in Soils Measurement

DESORPTION (e.g. phytate) Mechanisms Kinetics

Possible with Organic Anions/Siderophores…

Mechanisms….

Mechanisms….

Chelation

P Fe (III)

Mechanisms….

Chelation

P Fe (III)

- Bacterial Siderophores

- Citrate - Oxalate

Mechanisms….

Competitive Displacement

P

Mechanisms….

Competitive Displacement

P

Depends on the DISSOCIATION CONSTANTS (K) metal-organic anion metal-siderophore

Mechanisms….

Competitive Displacement

P

Citrate

Mechanisms….

Reductive Dissolution

P Fe (III) Fe (II)

Electron Donor

Mechanisms….

Reductive Dissolution

P Fe (III) Fe (II)

Ascorbate

Electron Donor

Mechanisms….

Chelation

Competitive Displacement

Reductive Dissolution

P Fe (III)

P

P Fe (III) Fe (II)

Fe

Organic Anions/ Siderophores Incubate

phytate

goethite

Measure P, Fe in supernatant

t = 0 t = 1 t = 2

.

.

. t = n

Desorption Kinetics

Methods….

Desorption Kinetics

Average Rate of Desorption in 0-4 h

(mmol L-1 h-1 )

InsP6 0.01

Fe 0.49

Average Rate of Desorption in 6-37 h

(mmol L-1 h-1 )

InsP6 0.004

Fe 0.74

Ascorbate Example….

Desorption Kinetics

Ascorbate Example….

Influence of pH and Oxalate Concentration

Oxalate Example….

0

2

4

6

8

10

0 10 20 30

InsP

6 (

uM

)

hour

100 mM pH 3.5

10 mM pH 3.5

1 mM pH 3.5

0

1

2

3

4

5

6

7

8

9

10

0 10 20 30

InsP

6 (

uM

)

hour

100 mM pH 5.5

10 mM pH 5.5

1 mM pH 5.5

Influence of pH and Oxalate Concentration

Oxalate Example….

-1

1

3

5

7

9

11

100 10 1

InsP

6 (

uM

)

mM Oxalic Acid

pH 5.5

pH 3.5

0

2

4

6

8

10

0 10 20 30

InsP

6 (

uM

)

hour

100 mM pH 3.5

10 mM pH 3.5

1 mM pH 3.5

0

1

2

3

4

5

6

7

8

9

10

0 10 20 30

InsP

6 (

uM

)

hour

100 mM pH 5.5

10 mM pH 5.5

1 mM pH 5.5

Questions? Comments? Concerns?

[email protected] Perkins 203