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dc.contributor.authorRusso, Tess A.  Concept link
dc.contributor.authorTully, Katherine L.  Concept link
dc.contributor.authorPalm, Cheryl  Concept link
dc.contributor.authorNeill, Christopher  Concept link
dc.date.accessioned2017-07-05T18:38:27Z
dc.date.available2017-07-05T18:38:27Z
dc.date.issued2017-05-16
dc.identifier.citationNutrient Cycling in Agroecosystems 108 (2017): 195–209en_US
dc.identifier.urihttps://hdl.handle.net/1912/9067
dc.description© The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Nutrient Cycling in Agroecosystems 108 (2017): 195–209, doi:10.1007/s10705-017-9852-z.en_US
dc.description.abstractMeeting food security requirements in sub-Saharan Africa (SSA) will require increasing fertilizer use to improve crop yields, however excess fertilization can cause environmental and public health problems in surface and groundwater. Determining the threshold of reasonable fertilizer application in SSA requires an understanding of flow dynamics and nutrient transport in under-studied, tropical soils experiencing seasonal rainfall. We estimated leaching flux in Yala, Kenya on a maize field that received from 0 to 200 kg ha−1 of nitrogen (N) fertilizer. Soil pore water concentration measurements during two growing seasons were coupled with results from a numerical fluid flow model to calculate the daily flux of nitrate-nitrogen (NO3−-N). Modeled NO3−-N losses to below 200 cm for 1 year ranged from 40 kg N ha−1 year−1 in the 75 kg N ha−1 year−1 treatment to 81 kg N ha−1 year−1 in the 200 kg N ha−1 treatment. The highest soil pore water NO3−-N concentrations and NO3−-N leaching fluxes occurred on the highest N application plots, however there was a poor correlation between N application rate and NO3−-N leaching for the remaining N application rates. The drought in the second study year resulted in higher pore water NO3−-N concentrations, while NO3−-N leaching was disproportionately smaller than the decrease in precipitation. The lack of a strong correlation between NO3−-N leaching and N application rate, and a large decrease in flux between 120 and 200 cm suggest processes that influence NO3−-N retention in soils below 200 cm will ultimately control NO3−-N leaching at the watershed scale.en_US
dc.description.sponsorshipEarth Institute, Columbia University; National Science Foundation IIA-0968211; Bill and Melinda Gates Foundationen_US
dc.language.isoen_USen_US
dc.publisherSpringeren_US
dc.relation.urihttps://doi.org/10.1007/s10705-017-9852-z
dc.rightsAttribution 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.subjectLeachingen_US
dc.subjectNitrogen fertilizeren_US
dc.subjectNitrateen_US
dc.subjectNumerical modelingen_US
dc.subjectSub-Saharan Africaen_US
dc.titleLeaching losses from Kenyan maize cropland receiving different rates of nitrogen fertilizeren_US
dc.typeArticleen_US
dc.identifier.doi10.1007/s10705-017-9852-z


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Attribution 4.0 International
Except where otherwise noted, this item's license is described as Attribution 4.0 International