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dc.contributor.authorNziguheba, Generose
dc.contributor.authorSmolders, E.
dc.contributor.authorMerckx, R.
dc.date.accessioned2019-12-04T11:19:00Z
dc.date.available2019-12-04T11:19:00Z
dc.date.issued2005
dc.identifier.citationNziguheba, G., Smolders, E. & Merckx, R. (2005). Sulphur immobilization and availability in soils assessed using isotope dilution. Soil Biology and Biochemistry, 37(4), 635-644.
dc.identifier.issn0038-0717
dc.identifier.urihttps://hdl.handle.net/20.500.12478/3373
dc.description.abstractIncreasing recognition of S deficiency in soils has raised the need for understanding processes governing S cycling and availability in soils. However, the quantification of the two main processes of S cycling, i.e. mineralization and immobilization, remains difficult as these processes occur simultaneously. A modified isotope 35SO4 dilution technique was developed and used to measure the effect of sulphate (SO4) fertilization on S mineralization and immobilization in planted (pot experiment with ryegrass (Lolium multiflorum L.)) and unplanted soils (incubation). The immobilization and mineralization of S was calculated from the dynamics of stable and labelled S in soil KH2PO4 extracts containing an anion exchange membrane that concentrates SO4 and mainly excludes other S species. The mathematical analysis of the isotope dilution data differs from methods proposed earlier. The radiolabile S in unplanted soil (E value) and in ryegrass (L value) were used as a measure of total available S in soils. Sulphate immobilization rate significantly declined during incubation. Sulphate application reduced gross mineralization but surprisingly reduced SO4 immobilization. The E value significantly increased during the incubation in all soils as a result of gross mineralization, e.g. from 3.8 mg S kg−1 at day 0 to 11.5 mg S kg−1 at day 43 in the sandy soil with no sulphate addition. A full recovery in the E value of S added in (+S) treatments was achieved. Similarly, radiolabile S in the above-ground ryegrass biomass (L value) increased with S addition, with a full recovery of added S. The E and L values nearly fit a 1:1 line suggesting identical S dynamics in a planted and unplanted soil. The method proposed has operational advantages compared to methods used earlier.
dc.language.isoen
dc.subjectE Value
dc.subjectImmobilization
dc.subjectL Value
dc.subjectMineralization
dc.subjectRadioactive S
dc.subjectRyegrass
dc.subjectSulphate Fertilization
dc.subjectIncubation
dc.titleSulphur immobilization and availability in soils assessed using isotope dillution
dc.typeJournal Article
dc.description.versionPeer Review
cg.contributor.affiliationKatholieke Universiteit Leuven
cg.contributor.affiliationInternational Institute of Tropical Agriculture
cg.contributor.affiliationColumbia University
cg.coverage.regionAcp
cg.coverage.regionAfrica
cg.coverage.regionEurope
cg.coverage.regionEast Africa
cg.coverage.regionSouth America
cg.coverage.countryBelgium
cg.coverage.countryKenya
cg.coverage.countryColombia
cg.isijournalISI Journal
cg.authorship.typesCGIAR and advanced research institute
cg.iitasubjectPlant Breeding
cg.iitasubjectLivelihoods
cg.iitasubjectBioscience
cg.iitasubjectCrop Systems
cg.iitasubjectIntegrated Soil Fertility Management
cg.iitasubjectGenetic Improvement
cg.iitasubjectHandling, Transport, Storage And Protection Of Agricultural Products
cg.iitasubjectPests Of Plants
cg.iitasubjectPlant Genetic Resources
cg.accessibilitystatusLimited Access
local.dspaceid95047
cg.identifier.doihttps://dx.doi.org/10.1016/j.soilbio.2004.09.007


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