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dc.contributor.authorCade-Menun, B.J.
dc.contributor.authorJames, D.C.
dc.date.accessioned2018-07-26T15:02:19Z
dc.date.available2018-07-26T15:02:19Z
dc.date.issued2009-02-25
dc.identifier.urihttp://hdl.handle.net/10388/9173
dc.description.abstractIn soils and other environmental samples, phosphorus (P) may be found in a range of inorganic and organic forms. Inorganic P forms include orthophosphate, which is readily available to plants, and complex inorganic P forms such as pyrophosphate and polyphosphate. Organic P forms can be divided into groups such as orthophosphate monoesters (e.g. sugar phosphates, phytic acid) and orthophosphate diesters (e.g. phospholipids, DNA) and phosphonates. Identifying P forms is important to enhance crop growth, with and without fertilization, and to minimize P loss to water, where it can cause harmful algal blooms. This presentation describes some of our recent research using solution 31P NMR spectroscopy to characterize P forms in a range of Saskatchewan soils, as well as swine manure.en_US
dc.language.isoenen_US
dc.relation.ispartofSoils and Crops Workshop
dc.rightsAttribution-NonCommercial-NoDerivs 2.5 Canada*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/2.5/ca/*
dc.subjectmanureen_US
dc.titleCharacterizing phosphorus forms in Saskatchewan soils using solution 31P NMR spectroscopyen_US
dc.typePoster Presentationen_US
dc.description.versionNon-Peer Reviewed


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Attribution-NonCommercial-NoDerivs 2.5 Canada
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 2.5 Canada