Show simple item record

dc.contributor.authorGonzález Jiménez, J.L.
dc.contributor.authorHealy, Mark G.
dc.contributor.authorDaly, Karen
dc.date.accessioned2018-12-18T12:16:51Z
dc.date.issued2018-12-05
dc.identifier.citationGonzález Jiménez, J. L., Healy, M. G., & Daly, K. (2019). Effects of fertiliser on phosphorus pools in soils with contrasting organic matter content: A fractionation and path analysis study. Geoderma, 338, 128-135. doi: https://doi.org/10.1016/j.geoderma.2018.11.049en_IE
dc.identifier.issn1872-6259
dc.identifier.urihttp://hdl.handle.net/10379/14738
dc.description.abstractWith the intensification of agricultural production in many European countries, more marginal soils with elevated organic matter (OM) content are being brought into cultivation. However, little is known about the transformations in the constituent phosphorus (P) pools of organic soils receiving applications of P fertiliser. Soil P fractions were measured before and after receiving fertiliser in a controlled experiment to determine the change in the soil pools and path analysis was used to evaluate the relationships between P pools. In this study, P deficient soils ranging in OM content from 8 to 76 %, were placed in large pots, planted with ryegrass and subjected to P fertiliser applications ranging from 10 to 145 kg ha-1, and monitored over an eight-month study period. High OM soils had a diminished ability to build-up the labile pool from freshly applied P, with relatively low increases up to 200 % of the initial value, compared to mineral soils in which the labile pool increased to more than 2500 % of the initial concentration. Additionally, organic soils had higher P uptakes in the grass yield than mineral soils, indicating a higher availability of added P in the soil solution than mineral soils due to their limited sorption ability. In general, there was a reduction in the organic P pool over applications from 0 to 55 kg ha-1, which was indicative of partial mineralisation, but was followed by an accumulation of added P over applications from 55 to 145 kg P ha-1. The residual P pools did not build-up with P additions, but data indicated the occurrence of mineralisation in most of the soils with decreases of around 40 % of the initial concentrations. Organic and residual pools therefore displayed potential to supply P to more labile P pools across all soils of this study. Path analysis indicated that applied P was the only source of labile P in the soil with the highest OM content, leaving it dependant on continuous P applications to supply P for productivity, whereas in the rest of the soils there were interrelations between the non-labile and labile pools. Low pH strongly immobilised the applied P and should be corrected before the initiation of any fertilisation program, even in soils deficient in plant available P. The results demonstrated that P added as fertiliser to organic soils does not accumulate as in mineral soils, which may leave them susceptible to P losses in surface runoff. Therefore, organic soils under agricultural production located in high status catchments should receive low P applications and only during periods with low probability of precipitation to minimise the possibility of P exports to receiving waters.en_IE
dc.description.sponsorshipThis work was funded by the Irish Department of Agriculture, Forestry and the Marine (project reference 13/S488) as part of the Research Stimulus Fund 2013. José L. González Jiménez was funded by the Teagasc Walsh Fellowship Scheme. The authors would like to thank the landowners for generously providing the soils used in this study, and the support and assistance of D. Brennan, L Moloney Finn and I. Marongiu for their support and advice in the use of Teagasc Johnstown Castle laboratories. We would also like to thank the editor and two anonymous reviewers for their critical and helpful comments and suggestions.en_IE
dc.formatapplication/pdfen_IE
dc.language.isoenen_IE
dc.publisherElsevieren_IE
dc.relation.ispartofGeodermaen
dc.subjectP fractions; Build-up; Histosols; Hedley fractionation; Soil P cycling; Pathwaysen_IE
dc.subjectP fractionsen_IE
dc.subjectBuild-upen_IE
dc.subjectHistosolsen_IE
dc.subjectHedley fractionationen_IE
dc.subjectSoil P cyclingen_IE
dc.subjectPathwaysen_IE
dc.titleEffects of fertiliser on phosphorus pools in soils with contrasting organic matter content: A fractionation and path analysis studyen_IE
dc.typeArticleen_IE
dc.date.updated2018-12-14T16:13:02Z
dc.identifier.doi10.1016/j.geoderma.2018.11.049
dc.local.publishedsourcehttps://doi.org/10.1016/j.geoderma.2018.11.049en_IE
dc.description.peer-reviewedpeer-reviewed
dc.contributor.funderDepartment of Agriculture, Forestry and the Marine, Irelanden_IE
dc.contributor.funderTeagasc Walsh Fellowship Schemeen_IE
dc.description.embargo2020-12-05
dc.internal.rssid15526919
dc.local.contactMark Healy, Room Eng-1038, Civil Engineering, Col Of Engineering & Informatics, Nui Galway. 5364 Email: mark.healy@nuigalway.ie
dc.local.copyrightcheckedYes
dc.local.versionACCEPTED
nui.item.downloads1


Files in this item

Attribution-NonCommercial-NoDerivs 3.0 Ireland
This item is available under the Attribution-NonCommercial-NoDerivs 3.0 Ireland. No item may be reproduced for commercial purposes. Please refer to the publisher's URL where this is made available, or to notes contained in the item itself. Other terms may apply.

The following license files are associated with this item:

Thumbnail

This item appears in the following Collection(s)

Show simple item record