The fate of particulate nitrogen in fluvial systems

dc.contributor.authorKrieg, Chelsea S.
dc.date.accessioned2018-11-20T13:26:43Z
dc.date.available2018-11-20T13:26:43Z
dc.date.issued2018
dc.date.updated2018-10-18T16:02:08Z
dc.description.abstractLarge storms can erode, transport, and deposit large amounts of allochthonous particulate organic matter (POM) and particulate nitrogen (PN) to the fluvial network. The role of storm-driven POM in the processing of fluvial C and N and its impact on water quality is still poorly understood. This study investigates the fate of C and N from storm-driven POM deposition using a 56-day incubation experiment of five known POM sources from a 79-ha forested watershed. Incubation columns were treated with one of two moisture treatments; Moisture Regime 1: sediment subjected to frequent rewetting treatments, Moisture Regime 2: sediments subjected to dry-wet cycles. Sediment and porewater samples were collected throughout the incubation and analyzed to characterize and compare the solid and solution pool chemistries and the abundances of nitrifying and denitrifying microbial populations. Key findings from this study are: (1) C and N rich sources experienced decomposition, mineralization, and nitrification and released large amounts of dissolved N, but the amount of N released varied by POM source and moisture regime. Drying and rewetting stimulated nitrification and suppressed denitrification in most POM sources. (2) Fluvial Storm Deposits released large amounts of porewater N regardless of the moisture conditions, indicating that they can readily act as N sources under a variety of conditions. (3) Forest Floor Humus was the only POM source to exhibit mineralization and denitrification when frequently rewetted. Under these conditions, this POM source acted as the strongest source of dissolved organic nitrogen. Under the drying and rewetting moisture conditions, Forest Floor Humus became a N source, specifically exhibiting intense decomposition, mineralization, and nitrification, resulting the release of large amounts porewater nitrate. The inputs and processing of large storm-driven PN inputs becomes increasingly more important as the frequency and intensity of these large storms are predicted to increase due to global climate change. Gaining a better understanding of the fate of the N derived from particulate materials is critical to the development and implementation of effective management practices for controlling water pollution and maintaining healthy waterways.en_US
dc.description.advisorInamdar, Shreeram P.
dc.description.degreeM.S.
dc.description.programUniversity of Delaware, Water Science and Policy Program
dc.identifier.doihttps://doi.org/10.58088/pafy-7p15
dc.identifier.unique1066343988
dc.identifier.urihttp://udspace.udel.edu/handle/19716/23921
dc.language.rfc3066en
dc.publisherUniversity of Delawareen_US
dc.relation.urihttps://search.proquest.com/docview/2130992204?accountid=10457
dc.subjectHealth and environmental sciencesen_US
dc.subjectEarth sciencesen_US
dc.subjectDrying and rewettingen_US
dc.subjectNitrogen leachingen_US
dc.subjectParticulate nitrogenen_US
dc.subjectParticulate organic matteren_US
dc.subjectStorm transporten_US
dc.titleThe fate of particulate nitrogen in fluvial systemsen_US
dc.typeThesisen_US

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