Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/127305
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dc.contributor.authorMcLaren, T.I.-
dc.contributor.authorSmernik, R.J.-
dc.contributor.authorMcLaughlin, M.J.-
dc.contributor.authorMcBeath, T.M.-
dc.contributor.authorMcCaskill, M.R.-
dc.contributor.authorRobertson, F.A.-
dc.contributor.authorSimpson, R.J.-
dc.date.issued2020-
dc.identifier.citationNutrient Cycling in Agroecosystems, 2020; 116(2):151-164-
dc.identifier.issn1385-1314-
dc.identifier.issn1573-0867-
dc.identifier.urihttp://hdl.handle.net/2440/127305-
dc.descriptionPublished Online 8 November 2019-
dc.description.abstractGrasslands are a globally important use of land for food and fibre production, which often require the addition of phosphorus (P) fertiliser to maximise plant production. However, a large proportion of the added P can accumulate in pools of poorly available inorganic and organic P in the surface soil layer under grasslands. The aim of this study was to identify the chemical nature of the organic P in soils from a long-term fertiliser by grazing permanent pasture experiment that have received varying additions of phosphatic fertiliser (cumulative P input of 27, 169, 311, 513, 745 and 1035 kg P ha⁻¹) over a period of 37 years. The design of the experiment uniquely provides insight into the response of soil organic P to the addition of fertiliser P on the decadal scale. On average, 46% of the added fertiliser P was recovered as total P in the 0–100 mm soil layer after 37 years of phosphate addition. The content of both inorganic and organic forms of soil P increased with the addition of fertiliser P. The accumulation of organic P increased linearly up to a cumulative P input of 745 kg P ha⁻¹ and plateaued thereafter. The majority of organic P in all treatments was detected as a broad signal in the phosphomonoester region of solution ³¹P nuclear magnetic resonance (NMR) spectra; this also accounted for 79% of the accumulated organic P in fertilised soil. Our results indicate that accumulation of P in the organic portion as complex forms eventually reaches a new equilibrium where no net accumulation would be expected with further addition of phosphate.-
dc.description.statementofresponsibilityTimothy I. McLaren, Ronald J. Smernik, Michael J. McLaughlin, Therese M. McBeath, Malcolm R. McCaskill, Fiona A. Robertson, Richard J. Simpson-
dc.language.isoen-
dc.publisherSpringer Nature-
dc.rights© Springer Nature B.V. 2019-
dc.subjectFertilizer; HLTPE; grasslands; NSP; phosphorus cycling; speciation-
dc.titleSoil phosphorus pools with addition of fertiliser phosphorus in a long-term grazing experiment-
dc.typeJournal article-
dc.identifier.doi10.1007/s10705-019-10035-y-
pubs.publication-statusPublished-
dc.identifier.orcidSmernik, R.J. [0000-0001-6033-5855]-
dc.identifier.orcidMcLaughlin, M.J. [0000-0001-6796-4144]-
dc.identifier.orcidMcBeath, T.M. [0000-0001-6423-367X]-
Appears in Collections:Agriculture, Food and Wine publications
Aurora harvest 4

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