Abstract
Abstract We examined the fractions of particulate phosphorus (PP) in the lower reaches of the Grand River, Canada, to test the hypothesis that the river is a source of both particulate-bound orthophosphate and labile species of PP. At the mouth of the Grand River, the proportion of particulate organic P (POP) was, on average, 57.7% of total PP, which was significantly higher than the proportion of particulate inorganic P (PIP) in PP. Analysis with 31P nuclear magnetic resonance (NMR) spectroscopy showed that the proportion of P species other than orthophosphate in the NaOH- EDTA extract was 1.75 times greater than that of orthophosphate. Labile P species (e.g. nucleotides and pyrophosphate) were present in the NMR spectrum; whereas, refractory organic P (myo-inositol hexakisphosphate) was absent. These results suggest that during winter and spring, the Grand River supplies primarily bioavailable phosphorus species in organic forms to Lake Erie, rather than inorganic orthophosphate. These results suggest that labile organic P is contained in PP rather than alkaline extractable inorganic P. Future studies should examine POP species in other rivers of the Lake Erie watershed.
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