The P-supplying power of the fine-textured soils from Abitibi-Temiscaming (
Quebec, Canada) has never been investigated. Anion exchange membranes (AEM)
, the electro-ultrafiltration (EUF) technique and chemical extractions were
used to describe their P status. Phosphorus was desorbed from four soils t
hat had received 52.4 kg P ha(-1) yr(-1) from 1994 to 1996 and from unferti
lized soils. The cumulative amount of P desorbed in 75 min by EUF from unfe
rtilized soils varied from 10 to 69 mg P kg(-1). Averaged over all sites an
d treatments, the amount of soil P extracted by different methods ranged fr
om 1.0 to 18.9 mg P kg(-1). The cumulative grass P uptake was significantly
related to P desorbed by all methods (0.39 < r < 0.84). A close relationsh
ip between grass P uptake and P-AEMs indicated the adequacy of the AEMs to
determine plant-available P in Abitibi-Temiscaming soils. A high degree of
linearity (0.97 < R-2 < 0.99) Of the EUF-P desorption curves at 200 V and 2
0 degreesC with time was obtained. This indicates that soils have a high ca
pacity to buffer removal of P from soil solution with reserve P. The EUF te
chnique has shown that these soils hold very large inorganic P reserves and
this may explain the lack of grass response to P fertilizers.