Riparian Lowlands in Clay Till Landscapes Part II: Nitrogen Reduction and Release Along Variable Flow Paths
Riparian lowlands are known to control catchment nitrogen (N) balances. This study examined the role of agricultural tile drainage systems, often present in clay till landscapes, on the transport, transformation, and mass balance of N species in four riparian peat lowland transects receiving agricul...
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description | Riparian lowlands are known to control catchment nitrogen (N) balances. This study examined the role of agricultural tile drainage systems, often present in clay till landscapes, on the transport, transformation, and mass balance of N species in four riparian peat lowland transects receiving agricultural tile drainage water. Monitoring of N speciation of drain, stream, and groundwater, combined with a previously established water balance, enabled the determination of N mass balances for different flow paths including groundwater, subsurface drain water, and overland flow for each piezometer transect. The type of overland flow largely affected nitrate‐N (NO3‐N) removal efficiency, as determined by the total N output from a transect relative to the NO3‐N loading (%). Infiltration and subsurface flow followed by exfiltration (short return flow) allowed an efficient removal of NO3‐N (71–94%), while direct overland flow strongly lowered NO3‐N removal (25%) in one transect. The hydraulic loading rate versus the lowland infiltration capacity determined the transport pathways and thus the resulting NO3‐N removal efficiency. For all transects there was a net export of organic N and/or ammonium, associated with in situ N release from peat decomposition, through overland flow and groundwater discharge. These exports partly counterbalanced NO3‐N removal and significantly reduced the overall total N removal for the riparian lowlands. However, the N removal efficiencies remained positive (1–56%). The study indicates that N budgets for riparian lowlands need to account for overland flow as a transport pathway for N.
Key Points
Nitrate (NO3−) removal in riparian lowlands (RLs) depends on the infiltration of NO3− into organic riparian lowland sediments.
Direct overland flow, bypassing the RL soil and sediment, decreases nitrate removal.
RLs may be sinks or sources of nitrogen (N) depending on the balance between removal of nitrate and release of ammonium and organic N. |
doi_str_mv | 10.1029/2019WR025810 |
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Key Points
Nitrate (NO3−) removal in riparian lowlands (RLs) depends on the infiltration of NO3− into organic riparian lowland sediments.
Direct overland flow, bypassing the RL soil and sediment, decreases nitrate removal.
RLs may be sinks or sources of nitrogen (N) depending on the balance between removal of nitrate and release of ammonium and organic N.</description><identifier>ISSN: 0043-1397</identifier><identifier>EISSN: 1944-7973</identifier><identifier>DOI: 10.1029/2019WR025810</identifier><language>eng</language><publisher>Washington: John Wiley & Sons, Inc</publisher><subject>Ammonium ; Ammonium compounds ; Catchment area ; Clay ; Denitrification ; Drainage systems ; Drainage water ; Flow paths ; Groundwater ; Groundwater discharge ; Hydraulic loading ; Infiltration ; Infiltration capacity ; Load distribution ; Loading rate ; Lowlands ; Mass balance ; Nitrate ; Nitrates ; Nitrogen ; Overland flow ; Peat ; Receiving waters ; Removal ; Return flow ; Riparian lowlands ; Speciation ; Subsurface drains ; Subsurface flow ; Surface runoff ; Tile drainage ; Transport ; Water balance ; Wetlands</subject><ispartof>Water resources research, 2020-04, Vol.56 (4), p.n/a</ispartof><rights>2020. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3680-e4342514bbd568b267554fce8f7c8d0d32288946eb6aade1a366ba3b3bb74c9e3</citedby><cites>FETCH-LOGICAL-a3680-e4342514bbd568b267554fce8f7c8d0d32288946eb6aade1a366ba3b3bb74c9e3</cites><orcidid>0000-0001-9930-620X ; 0000-0002-8207-6820 ; 0000-0003-2631-7228 ; 0000-0002-9134-8293 ; 0000-0002-2276-0233</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2019WR025810$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2019WR025810$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,11493,27901,27902,45550,45551,46443,46867</link.rule.ids></links><search><creatorcontrib>Petersen, R. J.</creatorcontrib><creatorcontrib>Prinds, C.</creatorcontrib><creatorcontrib>Jessen, S.</creatorcontrib><creatorcontrib>Iversen, B. V.</creatorcontrib><creatorcontrib>Kjaergaard, C.</creatorcontrib><title>Riparian Lowlands in Clay Till Landscapes Part II: Nitrogen Reduction and Release Along Variable Flow Paths</title><title>Water resources research</title><description>Riparian lowlands are known to control catchment nitrogen (N) balances. This study examined the role of agricultural tile drainage systems, often present in clay till landscapes, on the transport, transformation, and mass balance of N species in four riparian peat lowland transects receiving agricultural tile drainage water. Monitoring of N speciation of drain, stream, and groundwater, combined with a previously established water balance, enabled the determination of N mass balances for different flow paths including groundwater, subsurface drain water, and overland flow for each piezometer transect. The type of overland flow largely affected nitrate‐N (NO3‐N) removal efficiency, as determined by the total N output from a transect relative to the NO3‐N loading (%). Infiltration and subsurface flow followed by exfiltration (short return flow) allowed an efficient removal of NO3‐N (71–94%), while direct overland flow strongly lowered NO3‐N removal (25%) in one transect. The hydraulic loading rate versus the lowland infiltration capacity determined the transport pathways and thus the resulting NO3‐N removal efficiency. For all transects there was a net export of organic N and/or ammonium, associated with in situ N release from peat decomposition, through overland flow and groundwater discharge. These exports partly counterbalanced NO3‐N removal and significantly reduced the overall total N removal for the riparian lowlands. However, the N removal efficiencies remained positive (1–56%). The study indicates that N budgets for riparian lowlands need to account for overland flow as a transport pathway for N.
Key Points
Nitrate (NO3−) removal in riparian lowlands (RLs) depends on the infiltration of NO3− into organic riparian lowland sediments.
Direct overland flow, bypassing the RL soil and sediment, decreases nitrate removal.
RLs may be sinks or sources of nitrogen (N) depending on the balance between removal of nitrate and release of ammonium and organic N.</description><subject>Ammonium</subject><subject>Ammonium compounds</subject><subject>Catchment area</subject><subject>Clay</subject><subject>Denitrification</subject><subject>Drainage systems</subject><subject>Drainage water</subject><subject>Flow paths</subject><subject>Groundwater</subject><subject>Groundwater discharge</subject><subject>Hydraulic loading</subject><subject>Infiltration</subject><subject>Infiltration capacity</subject><subject>Load distribution</subject><subject>Loading rate</subject><subject>Lowlands</subject><subject>Mass balance</subject><subject>Nitrate</subject><subject>Nitrates</subject><subject>Nitrogen</subject><subject>Overland flow</subject><subject>Peat</subject><subject>Receiving waters</subject><subject>Removal</subject><subject>Return flow</subject><subject>Riparian lowlands</subject><subject>Speciation</subject><subject>Subsurface drains</subject><subject>Subsurface flow</subject><subject>Surface runoff</subject><subject>Tile drainage</subject><subject>Transport</subject><subject>Water balance</subject><subject>Wetlands</subject><issn>0043-1397</issn><issn>1944-7973</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp9kM9LwzAcxYMoOKc3_4CAV6v51SbxJsXpoKiU6Y4ladOZGZuadIz993bMgydPj-_j894XHgCXGN1gROQtQVguS0RSgdERmGDJWMIlp8dgghCjCaaSn4KzGNcIYZZmfAI-S9urYFUHC791qmsitB3MndrBhXUOFnurVr2J8FWFAc7nd_DZDsGvTAdL02zqwfoOjtR4OaOigffOdyv4vm_VzsCZ89sxO3zEc3DSKhfNxa9OwdvsYZE_JcXL4zy_LxJFM4ESwygjKWZaN2kmNMl4mrK2NqLltWhQQwkRQrLM6EypxuAxlWlFNdWas1oaOgVXh94--O-NiUO19pvQjS8rQiUTEgtBRur6QNXBxxhMW_XBfqmwqzCq9nNWf-cccXrAt9aZ3b9stSzzkrCUI_oDMWl17g</recordid><startdate>202004</startdate><enddate>202004</enddate><creator>Petersen, R. 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J. ; Prinds, C. ; Jessen, S. ; Iversen, B. V. ; Kjaergaard, C.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3680-e4342514bbd568b267554fce8f7c8d0d32288946eb6aade1a366ba3b3bb74c9e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Ammonium</topic><topic>Ammonium compounds</topic><topic>Catchment area</topic><topic>Clay</topic><topic>Denitrification</topic><topic>Drainage systems</topic><topic>Drainage water</topic><topic>Flow paths</topic><topic>Groundwater</topic><topic>Groundwater discharge</topic><topic>Hydraulic loading</topic><topic>Infiltration</topic><topic>Infiltration capacity</topic><topic>Load distribution</topic><topic>Loading rate</topic><topic>Lowlands</topic><topic>Mass balance</topic><topic>Nitrate</topic><topic>Nitrates</topic><topic>Nitrogen</topic><topic>Overland flow</topic><topic>Peat</topic><topic>Receiving waters</topic><topic>Removal</topic><topic>Return flow</topic><topic>Riparian lowlands</topic><topic>Speciation</topic><topic>Subsurface drains</topic><topic>Subsurface flow</topic><topic>Surface runoff</topic><topic>Tile drainage</topic><topic>Transport</topic><topic>Water balance</topic><topic>Wetlands</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Petersen, R. J.</creatorcontrib><creatorcontrib>Prinds, C.</creatorcontrib><creatorcontrib>Jessen, S.</creatorcontrib><creatorcontrib>Iversen, B. 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J.</au><au>Prinds, C.</au><au>Jessen, S.</au><au>Iversen, B. V.</au><au>Kjaergaard, C.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Riparian Lowlands in Clay Till Landscapes Part II: Nitrogen Reduction and Release Along Variable Flow Paths</atitle><jtitle>Water resources research</jtitle><date>2020-04</date><risdate>2020</risdate><volume>56</volume><issue>4</issue><epage>n/a</epage><issn>0043-1397</issn><eissn>1944-7973</eissn><abstract>Riparian lowlands are known to control catchment nitrogen (N) balances. This study examined the role of agricultural tile drainage systems, often present in clay till landscapes, on the transport, transformation, and mass balance of N species in four riparian peat lowland transects receiving agricultural tile drainage water. Monitoring of N speciation of drain, stream, and groundwater, combined with a previously established water balance, enabled the determination of N mass balances for different flow paths including groundwater, subsurface drain water, and overland flow for each piezometer transect. The type of overland flow largely affected nitrate‐N (NO3‐N) removal efficiency, as determined by the total N output from a transect relative to the NO3‐N loading (%). Infiltration and subsurface flow followed by exfiltration (short return flow) allowed an efficient removal of NO3‐N (71–94%), while direct overland flow strongly lowered NO3‐N removal (25%) in one transect. The hydraulic loading rate versus the lowland infiltration capacity determined the transport pathways and thus the resulting NO3‐N removal efficiency. For all transects there was a net export of organic N and/or ammonium, associated with in situ N release from peat decomposition, through overland flow and groundwater discharge. These exports partly counterbalanced NO3‐N removal and significantly reduced the overall total N removal for the riparian lowlands. However, the N removal efficiencies remained positive (1–56%). The study indicates that N budgets for riparian lowlands need to account for overland flow as a transport pathway for N.
Key Points
Nitrate (NO3−) removal in riparian lowlands (RLs) depends on the infiltration of NO3− into organic riparian lowland sediments.
Direct overland flow, bypassing the RL soil and sediment, decreases nitrate removal.
RLs may be sinks or sources of nitrogen (N) depending on the balance between removal of nitrate and release of ammonium and organic N.</abstract><cop>Washington</cop><pub>John Wiley & Sons, Inc</pub><doi>10.1029/2019WR025810</doi><tpages>24</tpages><orcidid>https://orcid.org/0000-0001-9930-620X</orcidid><orcidid>https://orcid.org/0000-0002-8207-6820</orcidid><orcidid>https://orcid.org/0000-0003-2631-7228</orcidid><orcidid>https://orcid.org/0000-0002-9134-8293</orcidid><orcidid>https://orcid.org/0000-0002-2276-0233</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Ammonium Ammonium compounds Catchment area Clay Denitrification Drainage systems Drainage water Flow paths Groundwater Groundwater discharge Hydraulic loading Infiltration Infiltration capacity Load distribution Loading rate Lowlands Mass balance Nitrate Nitrates Nitrogen Overland flow Peat Receiving waters Removal Return flow Riparian lowlands Speciation Subsurface drains Subsurface flow Surface runoff Tile drainage Transport Water balance Wetlands |
title | Riparian Lowlands in Clay Till Landscapes Part II: Nitrogen Reduction and Release Along Variable Flow Paths |
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