As increasing amounts of arable land are being set aside, it is of imp
ortance to study the effect of vegetation on soil fertility. The fract
ionation of soil P under grassland, beech and spruce vegetation was in
vestigated in sites previously fertilized with P by extracting sequent
ially with Resin, NaHCO3, NaOH, HCI and finally NaOH after ultrasonic
pretreatment. Under beech a large part of extractable P was found in i
norganic fractions which are considered to be available for plants (Re
sin P(i) and Bicarbonate P(i)). Under grass, a large part of the extra
ctable P was found in potentially labile organic forms (Bicarbonate P(
o) and Fulvic acid P(o)). After 25 years of permanent grass vegetation
, the extractability of soil P was comparable to that from an adjacent
arable plot. On spruce covered soils most of the added fertilizer P w
as rendered unextractable 20-30 years after application. However the a
vailable data does not allow a clear interpretation of this phenomena,
as effects of soil parent material as well as vegetation may be taken
into consideration. No decrease in P-extractability was found between
beech and grass covered soils which had been fertilized for more than
200 years, when compared to less rich soils from the same area. On th
e basis of the current data it may be concluded that the vegetation af
fects the distribution of soil phosphorus fractions, and thus soil fer
tility. In the soils under investigation, grassland and beech vegetati
on conserved the phosphate availability to a high extent.