In order to estimate the role of phosphatases in maintaining the potential
bioavailable P pool in soils, water and 0.4M NaOH soil extracts were incuba
ted with immobilized acid phosphatase, alkaline phosphatase, phospholipase
and nuclease, separately, and in combinations. Immobilized nuclease at an o
ptimum pH of 7.0 hydrolyzed the most soluble unreactive P (SUP) both in wat
er and 0.4M NaOH extracts. The combination of immobilized alkaline phosphat
ase and nuclease increased the hydrolysis of SUP at pH 7.0 by up to 61% in
0.4M NaOH extracts relative to that due to immobilized nuclease alone. The
combination of immobilized acid phosphatase and nuclease, however, did not
increase the hydrolysis of SUP in either extract relative to that due to im
mobilized nuclease alone. Immobilized alkaline phosphatase and phospholipas
e increased the hydrolysis of SUP at pH 7.0 by up to 49% in 0.4M NaOH extra
cts relative to that due to immobilized phospholipase alone. Similarly, imm
obilized acid phosphatase and phospholipase increased the hydrolysis of SUP
at pH 7.0 by up to 49% in 0.4M NaOH extracts relative to that: due to immo
bilized phospholipase alone. The similarities in the optimum pH of indigeno
us phosphatases in soils and the immobilized phosphatases used in this stud
y, immobilized on positively charged supports, suggests that indigenous pho
sphatases could be immobilized on positively charged surfaces in soils.