EFFECT OF PH ON PRECIPITATION OF HUMIC-ACID FROM PEAT AND MINERAL SOILS ON THE DISTRIBUTION OF PHOSPHORUS FORMS IN HUMIC AND FULVIC-ACID FRACTIONS

Humic and fulvic acid fractions were isolated from a mineral soil and a peat by adjusting the pH of the alkali extracts to a range of values from 0.2 to 2.5. Total inorganic and organic forms of phosphorus (P) in the acids were measured by chemical analysis and by P-31 NMR spectroscopy. As the pH of precipitation of the mineral soil humic acid increased, there was an increase in the total P of the humic acid which related to the inorganic P component. In contrast with the peat, the increases observed in the pH range 0.2 to 1.5 were the result of changes in organic P. Using P-31 nuclear magnetic resonance spectroscopy, the ratio of inorganic to organic P as mono- and di-esters in the peat humic acid was found to increase from 1:4.8 at pH 2 to 1:19 at pH 2.5. In contrast with mineral soil humic acid, the ratio decreased from 1:6.1 at pH 0.2 to 1:1.3 at pH 2.5. The mono-ester to di-ester ratio was about 3 in the peat and 10 in the mineral soil and varied little with pH of precipitation. Phosphonates were detected only in the peat humic acid precipitated in the pH range 1.0 to 2.0