GES175, Science of Soils Lecture 10 Phosphorus. Phosphorus Soil-Plant Relations * Energy and...

GES175, Science of Soils

Lecture 10

Phosphorus

Phosphorus Soil-Plant Relations

* Energy and reproduction

* Growth and developmentroot growth

maturity (seed set, flowering,...)

* Maintained by organic matter cycling

Slide 10.2

Water Quality

• accelerated eutrophication

• P (often) promotes algae growth

- may promote anoxia and lead to ‘dead’

zones

• P from point and nonpoint sources

Slide 10.3

Phosphorus Fixation

* Limited Biological Availability

• P reacts strongly with soil material - limits bioavailability - limits transport through soil - movement occurs via erosion

• Adsorbs and precipitates

Slide 10.4

Adsorption Reactions

* Strong adsorption on soil minerals

- adsorption on Fe- and Al-oxides

- adsorption on ‘edge’ sites of silicate clays

(dominantly kaolinite)

Slide 10.5

Volcanic Ash

Slide 10.6

Inorganic P Compounds(precipitates)

Acid soils

Fe and Al phosphates

FePO42H2O, AlPO4

2H2O

Alkaline soils

Ca and Mg phosphates

Slide 10.7

Ca(H2PO4)2 monocalcium phosphate

CaHPO4

dicalcium phosphate

Ca3(PO4)2

tricalcium phosphate

3Ca3(PO4)2Ca(OH)2

hydroxyapatite

3Ca3(PO4)2CaCO3

carbonate apatite

decreasing solubility

Inorganic P CompoundsSlide 10.8

pH

6

8

Nomenclature

H3PO4 = phosphoric acid

H2PO4- = monobasic

HPO4-2 = dibasic

PO4-3 = tribasic

Slide 10.9

acid soilsacid soils alkalinealkaline soilssoils

Phosphate Ion: ProtonationSlide 10.10

Most Available P between pH 6 - 7Slide 10.11

Organic Soil Phosphorus

* 20 - 80 % of total soil P is organic

* Mostly inositol phosphates,

C6H6(OH)6

- 10 - 50 % of organic-P

- some nucleic acid and phospholipids

Slide 10.12

Organic-P

Slide 10.13

(available P)

Cycling: A slow release mechanism

HxPO4x-3

mineralizationim

mob

iliza

tion

Solid Phase-PO4(unavailable)

Symbiotic Relation:Fungi and Plants

Mycorrhizae root infections, a key to phosphorus uptake

Fungal hyphae

mycorrihizae

Plant root

The End

Reactions at High pH Values

* P converts to less soluble Ca and Mg compounds

Ca(H2PO4)2 + CaCO3 + H2O 2 CaHPO42H2O + CO2 very less

soluble soluble

6 CaHPO42H2O + 3 CaCO3 3 Ca3(PO4)2 + 3 CO2 + 5 H2O

less soluble

3 Ca3(PO4)2 + CaCO3 3Ca3(PO4)2CaCO3

very insoluble

- most serious in calcareous soils of arid regions

Slide 10.11