We used 16 soils to compare the Hedley method for soil phosphorus fractiona
tion to an alternative method recently developed by Ruttenberg to different
iate among P fractions in marine sediments. For forms of labile and Fe-boun
d P in soils, these methods were poorly correlated, with the Hedley fractio
nation showing a greater ability to discriminate among variations in plant-
available P. For Ca-bound P, total organic P, and total P, the methods were
well correlated (r(2) = 0.93, 0.48, 0.74, respectively), although the sum
of P measured in the Ruttenberg extractions is only 45% of the total P reco
vered by the Hedley fractionation. The Hedley fractionation seems superior
when an index of plant-available phosphorus and a separation of organic and
inorganic forms is needed, whereas the Ruttenberg method allows a separati
on of CaCO3-bound P from apatite-P, which is potentially useful in calcareo
us soils.