Contrasting subsurface denitrification characteristics under temperate pasture lands and its implications for nutrient management in agricultural catchments

dc.contributor.authorRivas, A
dc.contributor.authorSingh, R
dc.contributor.authorHorne, DJ
dc.contributor.authorRoygard, J
dc.contributor.authorMatthews, A
dc.contributor.authorHedley, MJ
dc.coverage.spatialEngland
dc.date.accessioned2020-09-17T22:36:48Z
dc.date.available2020-07-28
dc.date.issued2020-10-15
dc.date.submitted2020-07-06
dc.description.abstractSubsurface denitrification plays a key role in the reduction or ‘attenuation’ of nitrate contamination of groundwater and surface waters. We investigated subsurface denitrification characteristics in the vadose zone and shallow groundwater at four sites under pastoral farming in the Manawatū River catchment, located in the lower part of North Island, New Zealand. The denitrification potential of the vadose zone was determined by the laboratory incubation assays measuring the denitrifying enzyme activity (DEA) in soil samples collected from different soil horizons (up to 2.1 m below ground surface), whereas denitrification rates in shallow groundwaters were measured in situ by single-well, push-pull tests conducted in piezometers installed at multiple depths at the study sites. Soils and underlying geology, defining hydrogeologic settings, appear to influence the spatial variability of subsurface denitrification characteristics at the study sites. Where the vadose zone is thin and composed of coarse-textured soils, percolation of nitrate was evident in observed high nitrate-nitrogen concentrations (>5 mg L⁻¹) in oxic and young shallow groundwaters, but low nitrate-nitrogen concentrations (<0.05 mg L⁻¹) were observed in the reduced shallow groundwater found underneath the fine textured soils and/or a thick vadose zone. This was confirmed by the push-pull tests measuring denitrification rates from 0.08 to 1.07 mg N L⁻¹ h⁻¹ in the reduced shallow groundwaters (dissolved oxygen or DO < 0.5 mg L⁻¹), while negligible in the oxic groundwaters (DO > 5 mg L⁻¹) found at the study sites. These contrasting subsurface denitrification characteristics determine the ultimate delivery of nitrate losses from agricultural soils to receiving waters, where the fine textured thick vadose zone and reducing groundwater conditions offer nitrate reduction in the subsurface environment.
dc.format.extentpp.111067-111067
dc.format.mediumPrint-Electronic
dc.identifierS0301-4797(20)30995-6
dc.identifierhttps://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=elements_prod&SrcAuth=WosAPI&KeyUT=WOS:000574828000003&DestLinkType=FullRecord&DestApp=WOS_CPL
dc.identifier.doi10.1016/j.jenvman.2020.111067
dc.identifier.eissn1095-8630
dc.identifier.issn0301-4797
dc.identifier.other32736232 (pubmed)
dc.identifier.urihttps://hdl.handle.net/10182/12701
dc.languageen
dc.language.isoen
dc.publisherElsevier
dc.relationThe original publication is available from Elsevier - https://doi.org/10.1016/j.jenvman.2020.111067 - http://dx.doi.org/10.1016/j.jenvman.2020.111067
dc.relation.isPartOfJournal of Environmental Management
dc.relation.urihttps://doi.org/10.1016/j.jenvman.2020.111067
dc.rights© 2020 Elsevier Ltd. All rights reserved.
dc.subjectagriculture
dc.subjectwater quality
dc.subjectnitrate attenuation
dc.subjectpush-pull test
dc.subjectshallow groundwater
dc.subjectNew Zealand
dc.subject.anzsrcANZSRC::050304 Soil Chemistry (excl. Carbon Sequestration Science)
dc.subject.anzsrcANZSRC::030503 Organic Chemical Synthesis
dc.subject.meshNitrates
dc.subject.meshWater Pollutants, Chemical
dc.subject.meshEnvironmental Monitoring
dc.subject.meshAgriculture
dc.subject.meshNew Zealand
dc.subject.meshDenitrification
dc.subject.meshGroundwater
dc.subject.meshNutrients
dc.titleContrasting subsurface denitrification characteristics under temperate pasture lands and its implications for nutrient management in agricultural catchments
dc.typeJournal Article
lu.contributor.unitLU
lu.contributor.unitLU|Lincoln Agritech
lu.contributor.unitLU|Research Management Office
lu.contributor.unitLU|Research Management Office|OLD QE18
lu.identifier.orcid0000-0002-2772-2711
pubs.article-number111067
pubs.publication-statusPublished online
pubs.publisher-urlhttp://dx.doi.org/10.1016/j.jenvman.2020.111067
pubs.volume272
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