The oxygen isotopic composition of phosphate in river water and its potential sources in the Upper River Taw catchment, UK
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Can sources of aquatic PO4 be traced using its stable oxygen isotope ratio?

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Various PO4 sources within a catchment were analysed for their δ18OPO4.

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River δ18OPO4 indicated that rapid microbial cycling of PO4 was occurring.

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This method appears inappropriate in systems where PO4 cycling is rapid.

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