Using Oxygen Isotopes of Phosphate To Trace Phosphorus Sources and Cycling in Lake Erie
详细信息    查看全文
文摘
Water samples collected during three sampling trips to Lake Erie displayed oxygen isotopic values of dissolved phosphate (δ18Op) that were largely out of equilibrium with ambient conditions, indicating that source signatures may be discerned. δ18Op values in the Lake ranged from +10‰ to +17‰, whereas the equilibrium value was expected to be around +14‰. The riverine weighted average δ18Op value was +11‰ and may represent one source of phosphate to the Lake. The lake δ18Op values indicated that there must be one or more as yet uncharacterized source(s) of phosphate with a high δ18Op value. Potential sources other than rivers are not yet well-characterized with respect to δ18O 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.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700