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Using oxygen isotopes of phosphate to trace phosphorus sources and cycling in lake Erie

Environmental Science and Technology

By:
, , , , , , ,
DOI: 10.1021/es8034126

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Abstract

Water samples collected during three sampling trips to Lake Erie displayed oxygen isotopic values of dissolved phosphate (??18O p) that were largely out of equilibrium with ambient conditions, indicating that source signatures may be discerned. ??18O p values in the Lake ranged from +10??? to +17???, whereas the equilibrium value was expected to be around +14???. The riverine weighted average ??18Op value was +11??? and may represent one source of phosphate to the Lake. The lake ?? 18Op values indicated that there must be one or more as yet uncharacterized source(s) of phosphate with a high ?? 18Op value. Potential sources other than rivers are not yet well-characterized with respect to ??18O of phosphate, but we speculate that a likely source may be the release of phosphate from sediments under reducing conditions created during anoxic events in the hypolimnion of the central basin of Lake Erie. Identifying potential phosphorus sources to the Lake is vital for designing effective management plans for reducing nutrient inputs and associated eutrophication. ?? 2009 American Chemical Society.

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Using oxygen isotopes of phosphate to trace phosphorus sources and cycling in lake Erie
Series title:
Environmental Science and Technology
DOI:
10.1021/es8034126
Volume
43
Issue:
9
Year Published:
2009
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
First page:
3108
Last page:
3114
Number of Pages:
7