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dc.contributor.authorFalk, Nicholas-
dc.contributor.authorDropp, Ian G.-
dc.contributor.authorDrouillard, Ken G.-
dc.date.accessioned2023-08-14T06:54:42Z-
dc.date.available2023-08-14T06:54:42Z-
dc.date.issued2023-
dc.identifier.urihttps://link.springer.com/article/10.1007/s00267-023-01859-0-
dc.identifier.urihttps://dlib.phenikaa-uni.edu.vn/handle/PNK/8803-
dc.descriptionCc-BYvi
dc.description.abstractThe ability of headwater bed and suspended sediments to mitigate non-point agricultural phosphorus (P) loads to the lower Great Lakes is recognized, but the specific biogeochemical processes promoting sediment P retention or internal P release remain poorly understood. To elucidate these mechanisms, three headwater segments located within priority watersheds of Southern Ontario, Canada, were sampled through the growing season of 2018–2020. The study employed equilibrium P assays along with novel assessments of legacy watershed nutrients, nitrogen (N) concentrations, sediment redox, and microbial community composition. 20-year data revealed elevated total P (TP) and total Nitrogen (TN) at an inorganic fertilizer and manure fertilizer-impacted site, respectively.vi
dc.language.isoenvi
dc.publisherSpringervi
dc.subjectTPvi
dc.subjectTNvi
dc.titleBiogeochemical Processes and Microbial Dynamics Governing Phosphorus Retention and Release in Sediments: A Case Study in Lower Great Lakes Headwatersvi
dc.typeBookvi
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