The percentage of total phosphorus in samples from Lake Memphremagog and five of its tributaries which was biologically available was measured on three dates, with criteria the distribution of radioactive P among exchanging fractions and the enzymatic release of soluble P from particulate P when stored with chloroform. In lake water, available P formed 83% of the total; in rivers much less (18–57%) was available. Large molecular weight phosphorus (>5,000 mol wt), separated by gel filtration, was usually the most refractory fraction, but substantial amounts of unavailable P were also associated with particles and small molecular weight P (<400 mol wt). Soluble P of intermediate molecular weight formed too small a fraction for determination of its availability. Variations in the percentage of available P in natural waters could substantially alter the biological effect of a given phosphorus load.
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Robert H. Peters (1981) studied this question.
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