FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2898852303> ?p ?o ?g. }

• W2898852303 endingPage "63" @default.
• W2898852303 startingPage "55" @default.
• W2898852303 abstract "Abstract Using earthen liners at the base of an integrated constructed wetland (ICW) maintains a hydraulic continuum between the ICW and the underlying groundwater body. This may enable migration of reactive carbon (dissolved organic and inorganic carbon (DOC, DIC)) and reactive nitrogen (Nr) across this liner to groundwater along this continuum to groundwater. Therefore, in terms of a holistic assessment of ICWs, quantification of these losses is important and indeed from an environmental perspective comparing such losses to other ICW dis-connected areas within the same groundwater body is critical. The main objective of the present study on an ICW site in SE Ireland was to compare reactive forms of C and N in groundwater (three piezometer nests) representing the continuum end point of ICW Cell 2 and 3 with that of groundwater dis-connected to the ICW system. For this purpose two control planes consisting of shallow and deep groundwater piezometer nests were installed and monitored at 1 and 4 m depths, respectively underneath the earthen liners at 0.2 m adjacent to the ICW cells. Fieldwork was conducted between Nov 2013 and Nov 2014 and results showed that groundwater beneath the ICW liner had a highly reduced signal with C and N concentrations being significantly higher to those of the disconnected up-gradient groundwater. The DOC, DIC and dissolved CO2 and CH4 concentrations in groundwater beneath the ICW cells were significantly higher than the up-gradient groundwater. All the reactive forms of C were higher in Cell 2 than in Cell 3. With respect to depth, all forms of reactive C were higher in deeper groundwater than the shallow equivalents except for DOC. Equally, Nr concentrations (NH4+, DON, NO3−-N and N2O) were higher in groundwater beneath the ICW cells than the up-gradient groundwater. They were higher in Cell 2 than in Cell 3 and higher in shallow rather than deep groundwater. The fate of the reactive C and N is unknown. Typically DOC delivery from groundwater to surface water drives many biogeochemical processes as an electron donor to microbes or can be converted to CO2 and CH4 emissions and the dissolved CO2 and CH4 can be indirectly exchanged to the atmosphere. The results suggest that nutrient delivery from the ICW cells to the underlying groundwater needs to be evaluated and the design of earthen-lined ICWs should consider this nutrient loss continuum across the liner." @default.
• W2898852303 created "2018-11-09" @default.
• W2898852303 creator A5026847769 @default.
• W2898852303 creator A5027265116 @default.
• W2898852303 creator A5034067680 @default.
• W2898852303 creator A5050056399 @default.
• W2898852303 creator A5069030931 @default.
• W2898852303 creator A5075143157 @default.
• W2898852303 creator A5076189228 @default.
• W2898852303 date "2019-01-01" @default.
• W2898852303 modified "2023-10-16" @default.
• W2898852303 title "Reactive carbon and nitrogen concentrations and dynamics in groundwater beneath an earthen-lined integrated constructed wetland" @default.
• W2898852303 cites W1185477724 @default.
• W2898852303 cites W1595413178 @default.
• W2898852303 cites W1966975534 @default.
• W2898852303 cites W1971832606 @default.
• W2898852303 cites W1981403714 @default.
• W2898852303 cites W1982049978 @default.
• W2898852303 cites W1984257790 @default.
• W2898852303 cites W1987997312 @default.
• W2898852303 cites W1989871851 @default.
• W2898852303 cites W2004848850 @default.
• W2898852303 cites W2009588613 @default.
• W2898852303 cites W2012974465 @default.
• W2898852303 cites W2034604465 @default.
• W2898852303 cites W2040876503 @default.
• W2898852303 cites W2054008903 @default.
• W2898852303 cites W2056058687 @default.
• W2898852303 cites W2065554682 @default.
• W2898852303 cites W2068983676 @default.
• W2898852303 cites W2071903041 @default.
• W2898852303 cites W2072348341 @default.
• W2898852303 cites W2074139372 @default.
• W2898852303 cites W2076188975 @default.
• W2898852303 cites W2077085814 @default.
• W2898852303 cites W2084736516 @default.
• W2898852303 cites W2090411409 @default.
• W2898852303 cites W2097004990 @default.
• W2898852303 cites W2100956447 @default.
• W2898852303 cites W2103027657 @default.
• W2898852303 cites W2131958762 @default.
• W2898852303 cites W2139849977 @default.
• W2898852303 cites W2140197771 @default.
• W2898852303 cites W21454757 @default.
• W2898852303 cites W2165894939 @default.
• W2898852303 cites W2167395251 @default.
• W2898852303 cites W2170385664 @default.
• W2898852303 cites W2287376826 @default.
• W2898852303 cites W2569959290 @default.
• W2898852303 cites W2737454466 @default.
• W2898852303 doi "https://doi.org/10.1016/j.ecoleng.2018.10.021" @default.
• W2898852303 hasPublicationYear "2019" @default.
• W2898852303 type Work @default.
• W2898852303 sameAs 2898852303 @default.
• W2898852303 citedByCount "7" @default.
• W2898852303 countsByYear W28988523032019 @default.
• W2898852303 countsByYear W28988523032020 @default.
• W2898852303 countsByYear W28988523032021 @default.
• W2898852303 countsByYear W28988523032023 @default.
• W2898852303 crossrefType "journal-article" @default.
• W2898852303 hasAuthorship W2898852303A5026847769 @default.
• W2898852303 hasAuthorship W2898852303A5027265116 @default.
• W2898852303 hasAuthorship W2898852303A5034067680 @default.
• W2898852303 hasAuthorship W2898852303A5050056399 @default.
• W2898852303 hasAuthorship W2898852303A5069030931 @default.
• W2898852303 hasAuthorship W2898852303A5075143157 @default.
• W2898852303 hasAuthorship W2898852303A5076189228 @default.
• W2898852303 hasConcept C104779481 @default.
• W2898852303 hasConcept C127313418 @default.
• W2898852303 hasConcept C140205800 @default.
• W2898852303 hasConcept C159985019 @default.
• W2898852303 hasConcept C178790620 @default.
• W2898852303 hasConcept C185592680 @default.
• W2898852303 hasConcept C187320778 @default.
• W2898852303 hasConcept C18903297 @default.
• W2898852303 hasConcept C192562407 @default.
• W2898852303 hasConcept C2780367215 @default.
• W2898852303 hasConcept C39432304 @default.
• W2898852303 hasConcept C537208039 @default.
• W2898852303 hasConcept C67715294 @default.
• W2898852303 hasConcept C76177295 @default.
• W2898852303 hasConcept C76886044 @default.
• W2898852303 hasConcept C86803240 @default.
• W2898852303 hasConcept C87717796 @default.
• W2898852303 hasConcept C94061648 @default.
• W2898852303 hasConceptScore W2898852303C104779481 @default.
• W2898852303 hasConceptScore W2898852303C127313418 @default.
• W2898852303 hasConceptScore W2898852303C140205800 @default.
• W2898852303 hasConceptScore W2898852303C159985019 @default.
• W2898852303 hasConceptScore W2898852303C178790620 @default.
• W2898852303 hasConceptScore W2898852303C185592680 @default.
• W2898852303 hasConceptScore W2898852303C187320778 @default.
• W2898852303 hasConceptScore W2898852303C18903297 @default.
• W2898852303 hasConceptScore W2898852303C192562407 @default.
• W2898852303 hasConceptScore W2898852303C2780367215 @default.
• W2898852303 hasConceptScore W2898852303C39432304 @default.
• W2898852303 hasConceptScore W2898852303C537208039 @default.
• W2898852303 hasConceptScore W2898852303C67715294 @default.

• next