After the Storm: Fate and Leaching of Particulate Nitrogen (PN) in the Fluvial Network and the Influence of Watershed Sources and Moisture Conditions

Large storms can erode, transport, and deposit substantial amounts of particulate nitrogen (PN) in the fluvial network. The fate of this input and its consequence for water quality is poorly understood. This study investigated the transformation and leaching of PN using a 56-day incubation experimen...

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Autores principales: Chelsea Krieg, Erin Johnson, Erin Peck, Jinjun Kan, Shreeram Inamdar
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Lenguaje:EN
Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/37d020011768476a9407ab69c9f8a6a3
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spelling oai:doaj.org-article:37d020011768476a9407ab69c9f8a6a32021-11-25T19:15:11ZAfter the Storm: Fate and Leaching of Particulate Nitrogen (PN) in the Fluvial Network and the Influence of Watershed Sources and Moisture Conditions10.3390/w132231822073-4441https://doaj.org/article/37d020011768476a9407ab69c9f8a6a32021-11-01T00:00:00Zhttps://www.mdpi.com/2073-4441/13/22/3182https://doaj.org/toc/2073-4441Large storms can erode, transport, and deposit substantial amounts of particulate nitrogen (PN) in the fluvial network. The fate of this input and its consequence for water quality is poorly understood. This study investigated the transformation and leaching of PN using a 56-day incubation experiment with five PN sources: forest floor humus, upland mineral A horizon, stream bank, storm deposits, and stream bed. Experiments were subjected to two moisture regimes: continuously moist and dry–wet cycles. Sediment and porewater samples were collected through the incubation and analyzed for N and C species, as well as the quantification of nitrifying and denitrifying genes <i>(amo</i>A, <i>nir</i>S, <i>nir</i>K). C- and N-rich watershed sources experienced decomposition, mineralization, and nitrification and released large amounts of dissolved N, but the amount of N released varied depending on the PN source and moisture regime. Drying and rewetting stimulated nitrification and suppressed denitrification in most PN sources. Storm deposits released large amounts of porewater N regardless of the moisture conditions, indicating that they could readily act as N sources under a variety of conditions. The inputs, processing, and leaching of large, storm-driven PN inputs become increasingly important as the frequency and intensity of large storms is predicted to increase with global climate change.Chelsea KriegErin JohnsonErin PeckJinjun KanShreeram InamdarMDPI AGarticlenitrogenparticulate organic matterfluvial depositionstormsmineralizationnitrificationHydraulic engineeringTC1-978Water supply for domestic and industrial purposesTD201-500ENWater, Vol 13, Iss 3182, p 3182 (2021)
institution DOAJ
collection DOAJ
language EN
topic nitrogen
particulate organic matter
fluvial deposition
storms
mineralization
nitrification
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
spellingShingle nitrogen
particulate organic matter
fluvial deposition
storms
mineralization
nitrification
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
Chelsea Krieg
Erin Johnson
Erin Peck
Jinjun Kan
Shreeram Inamdar
After the Storm: Fate and Leaching of Particulate Nitrogen (PN) in the Fluvial Network and the Influence of Watershed Sources and Moisture Conditions
description Large storms can erode, transport, and deposit substantial amounts of particulate nitrogen (PN) in the fluvial network. The fate of this input and its consequence for water quality is poorly understood. This study investigated the transformation and leaching of PN using a 56-day incubation experiment with five PN sources: forest floor humus, upland mineral A horizon, stream bank, storm deposits, and stream bed. Experiments were subjected to two moisture regimes: continuously moist and dry–wet cycles. Sediment and porewater samples were collected through the incubation and analyzed for N and C species, as well as the quantification of nitrifying and denitrifying genes <i>(amo</i>A, <i>nir</i>S, <i>nir</i>K). C- and N-rich watershed sources experienced decomposition, mineralization, and nitrification and released large amounts of dissolved N, but the amount of N released varied depending on the PN source and moisture regime. Drying and rewetting stimulated nitrification and suppressed denitrification in most PN sources. Storm deposits released large amounts of porewater N regardless of the moisture conditions, indicating that they could readily act as N sources under a variety of conditions. The inputs, processing, and leaching of large, storm-driven PN inputs become increasingly important as the frequency and intensity of large storms is predicted to increase with global climate change.
format article
author Chelsea Krieg
Erin Johnson
Erin Peck
Jinjun Kan
Shreeram Inamdar
author_facet Chelsea Krieg
Erin Johnson
Erin Peck
Jinjun Kan
Shreeram Inamdar
author_sort Chelsea Krieg
title After the Storm: Fate and Leaching of Particulate Nitrogen (PN) in the Fluvial Network and the Influence of Watershed Sources and Moisture Conditions
title_short After the Storm: Fate and Leaching of Particulate Nitrogen (PN) in the Fluvial Network and the Influence of Watershed Sources and Moisture Conditions
title_full After the Storm: Fate and Leaching of Particulate Nitrogen (PN) in the Fluvial Network and the Influence of Watershed Sources and Moisture Conditions
title_fullStr After the Storm: Fate and Leaching of Particulate Nitrogen (PN) in the Fluvial Network and the Influence of Watershed Sources and Moisture Conditions
title_full_unstemmed After the Storm: Fate and Leaching of Particulate Nitrogen (PN) in the Fluvial Network and the Influence of Watershed Sources and Moisture Conditions
title_sort after the storm: fate and leaching of particulate nitrogen (pn) in the fluvial network and the influence of watershed sources and moisture conditions
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/37d020011768476a9407ab69c9f8a6a3
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