Sewage sludges have been used for many years as sources of P for agric
ultural crops, but there is a lack of information regarding the propor
tion of sludge P that can be used by crops. The aim of this work was t
o assess the importance of soil available P and sludge origin on the u
tilization of sludge P by plants. First, the changes in soil P isotopi
cally exchangeable within 1 min (E1min) were measured in incubated soi
l-sludge mixtures using two soils and four sludges. Then, the uptake o
f sludge P by ryegrass (Lolium perenne L.) was measured on the same sl
udge-amended soils. The application of sludges increased E1min to valu
es lower or equal to those obtained following the application monocalc
ium phosphate. Similarly the utilization of sludge P by ryegrass was s
ystematically lower than the utilization of P derived from a water-sol
uble fertilizer. In both soils, the lowest utilization of sludge P was
observed for the two FeSO4 flocculated and anaerobically digested slu
dges, while the primary sludge and the aerobically digested sludge rel
eased somewhat higher quantities of P to ryegrass. In the clayey soil,
the amount of sludge P taken up by the crop was significantly related
both to the sludge and soil available P content, whereas no such rela
tion was observed in the loamy soil because of its high available P co
ntent. The origin of the sludge and the soil available P content must
therefore be taken into account when advising sludge application to cr
ops to adjust P inputs to plant needs.