Phosphate solubilizing microorganisms; the modern philosopher’s stone

The search for the mediaeval philosopher’s stone and the search for effective phosphate solubilizing microorganisms are analogous. Both are based on an erroneous assumption about nature. Advocates for phosphate solubilizing microorganisms think that P is present in soils as discrete compounds of iro...

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Published inPlant and soil Vol. 508; no. 1; pp. 21 - 28
Main Author Barrow, N. J.
Format Journal Article
LanguageEnglish
Published Cham Springer International Publishing 01.03.2025
Springer Nature B.V
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Abstract The search for the mediaeval philosopher’s stone and the search for effective phosphate solubilizing microorganisms are analogous. Both are based on an erroneous assumption about nature. Advocates for phosphate solubilizing microorganisms think that P is present in soils as discrete compounds of iron, aluminium, and calcium. This is not consistent with many observations. Rather, P is adsorbed on, and penetrates, into variable-charge surfaces. Further, phosphate solubilizing microorganisms often do not compete with microorganisms already present or produce acid under soil conditions. When responses do occur, they are more likely to be caused by effects of decreased pH on uptake of P by plant roots rather than on release of P by soil We are more likely to conserve resources and to decrease water pollution by understanding that previous applications have changed soil conditions so that subsequent applications are more effective, and much less phosphate is required.
AbstractList The search for the mediaeval philosopher’s stone and the search for effective phosphate solubilizing microorganisms are analogous. Both are based on an erroneous assumption about nature. Advocates for phosphate solubilizing microorganisms think that P is present in soils as discrete compounds of iron, aluminium, and calcium. This is not consistent with many observations. Rather, P is adsorbed on, and penetrates, into variable-charge surfaces. Further, phosphate solubilizing microorganisms often do not compete with microorganisms already present or produce acid under soil conditions. When responses do occur, they are more likely to be caused by effects of decreased pH on uptake of P by plant roots rather than on release of P by soil We are more likely to conserve resources and to decrease water pollution by understanding that previous applications have changed soil conditions so that subsequent applications are more effective, and much less phosphate is required.
Author Barrow, N. J.
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Keywords Phosphate solubilising microorganisms
Effects of pH
Response curves
Phosphate uptake
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Snippet The search for the mediaeval philosopher’s stone and the search for effective phosphate solubilizing microorganisms are analogous. Both are based on an...
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SubjectTerms Acidification
Agriculture
Aluminum
Aluminum compounds
Biomedical and Life Sciences
calcium
Calcium compounds
Ecology
iron
Life Sciences
Medieval period
Microorganisms
Opinion Paper
Philosophers
Phosphate
phosphates
Plant Physiology
Plant roots
Plant Sciences
Pollution control
soil
Soil conditions
Soil pollution
Soil Science & Conservation
solubilization
Stone
variable charge
Water pollution
Title Phosphate solubilizing microorganisms; the modern philosopher’s stone
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