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dc.contributor.authorNziguheba, Generose
dc.contributor.authorMerckx, R.
dc.contributor.authorPalm, C.
dc.date.accessioned2019-12-04T11:18:54Z
dc.date.available2019-12-04T11:18:54Z
dc.date.issued2005
dc.identifier.citationNziguheba, G., Merckx, R. & Palm, C. (2005). Carbon and nitrogen dynamics in a phosphorus-deficient soil amended with organic residues and fertilizers in western Kenya. Biology and Fertility of Soils, 41(4), 240-248.
dc.identifier.issn0178-2762
dc.identifier.urihttps://hdl.handle.net/20.500.12478/3350
dc.description.abstractThe contribution of organic resources to the restoration of soil fertility in smallholder farming systems in East Africa is being tested as an alternative to costly fertilizers. Organic inputs are expected to have advantages over fertilizers by affecting many biochemical properties controlling nutrient cycling. Our study examined changes in soil C and N, C and N mineralization, microbial biomass C (MBC) and N (MBN), and particulate organic matter (POM) in a P-limiting soil in western Kenya after applications of organic residues and fertilizers to overcome P limitation to crops. Leaf biomass from six different tree (shrub) species was incorporated into the soil at 5 Mg ha−1 for five consecutive maize growing seasons, over 2.5 years. Triple superphosphate was applied separately at 0, 10, 25, 50, and 150 kg P ha−1 in combination with 120 kg N ha−1 as urea. Soil inorganic N, soil organic C, mineralizable N, and total C in all POM fractions and total N in the 53- to 250-μm POM fraction increased following addition of all organic residues compared to the control. Whether there was an advantage of organic residue incorporation over inorganic fertilizer use depended on the soil parameter studied, the organic residue and the rate of fertilization. Most differences were found in N mineralization where 14.4–21.6 mg N kg−1 was mineralized in fertilizer treatments compared to 25.2–30.5 mg N kg−1 in organic residue treatments. C and N mineralization and the 53- to 250-μm POM fractions were the most sensitive parameters, correlating with most of the studied parameters. Organic residues can contribute to improved soil nutrient cycling while the magnitude of their contribution depends on the biochemical properties of the residues.
dc.description.sponsorshipInternational Development Research Centre
dc.language.isoen
dc.subjectLeaf Biomass
dc.subjectMicrobial Biomass Carbon
dc.subjectMineralization
dc.subjectParticulate Organic Matter
dc.subjectPhosphorus Fertilizer
dc.titleCarbon and nitrogen dynamics in a phosphorus deficient soil amended with organic residues and fertilizers in western Kenya
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.regionNorth America
cg.coverage.countryBelgium
cg.coverage.countryKenya
cg.coverage.countryUnited States
cg.authorship.typesCGIAR and advanced research institute
cg.iitasubjectSoil Health
cg.iitasubjectSoil Fertility
cg.iitasubjectDisease Control
cg.iitasubjectSoil Information
cg.iitasubjectPlant Diseases
cg.iitasubjectPlant Breeding
cg.iitasubjectPests Of Plants
cg.iitasubjectFarm Management
cg.iitasubjectFarming Systems
cg.iitasubjectPlant Production
cg.iitasubjectIntegrated Soil Fertility Management
cg.accessibilitystatusLimited Access
local.dspaceid95024


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