Biological P cycling is influenced by the form of P fertilizer in an Oxisol

cg.contributor.affiliationUniversity of Illinoisen
cg.contributor.affiliationUniversity of Californiaen
cg.contributor.affiliationInternational Center for Tropical Agricultureen
cg.contributor.crpWater, Land and Ecosystemsen
cg.coverage.countryKenyaen
cg.coverage.iso3166-alpha2KEen
cg.coverage.regionAfricaen
cg.coverage.regionEastern Africaen
cg.creator.identifierRolf Sommer: 0000-0001-7599-9056en
cg.howPublishedFormally Publisheden
cg.identifier.doihttps://doi.org/10.1007/s00374-017-1226-9en
cg.isijournalISI Journalen
cg.issn0178-2762en
cg.issue8en
cg.journalBiology and Fertility of Soilsen
cg.reviewStatusPeer Reviewen
cg.subject.ciatSOIL INFORMATIONen
cg.volume53en
dc.contributor.authorMargenot, Andrew J.en
dc.contributor.authorSommer, Rolfen
dc.contributor.authorMukalama, Johnen
dc.contributor.authorParikh, Sanjai J.en
dc.date.accessioned2017-08-16T16:03:35Zen
dc.date.available2017-08-16T16:03:35Zen
dc.identifier.urihttps://hdl.handle.net/10568/83158
dc.titleBiological P cycling is influenced by the form of P fertilizer in an Oxisolen
dcterms.abstractPhosphate rock (PR) is an alternative fertilizer to increase the P content of P-deficient weathered soils. We evaluated the effects of fertilizer form on indicators of biological cycling of P using an on-farm trial on a Rhodic Kandiudox in western Kenya. Treatment plots were sampled after 13 cropping seasons of P applications as Minjingu phosphate rock (PR) or as triple super phosphate (TSP) (50 kg P ha−1 season−1), as well as a P-unfertilized control (0 kg P ha−1 season−1). Soils (0–15 and 15–30 cm) were analyzed for microbial biomass P (Pmic), activities of acid phosphomonoesterase, alkaline phosphomonoesterase, and phosphodiesterase, and sequentially extractable P fractions. P additions as Minjingu PR yielded 299% greater Pmic than TSP at 0–15-cm depth despite similar labile P concentrations in the two P fertilization treatments and stimulated activities of acid phosphomonoesterase (+39%). When added in the soluble form of TSP, a greater percentage of total soil P was present in mineral-bound forms (+33% Fe- and Al-associated P). Higher soil pH under Minjingu PR (pH 5.35) versus TSP (pH 5.02) and the P-unfertilized treatment (pH 4.69) at 0–15-cm depth reflected a liming effect of Minjingu PR. The form of P fertilizer can influence biological P cycling in weathered soils, potentially improving P availability under Minjingu PR relative to TSP via enhanced microbial biomass P and enzymatic drivers of P cycling.en
dcterms.accessRightsOpen Accessen
dcterms.available2017-08-11en
dcterms.bibliographicCitationMargenot, Andrew J.; Sommer, Rolf; Mukalama, John; Parikh, Sanjai J.. 2017. Biological P cycling is influenced by the form of P fertilizer in an Oxisol . Biology and Fertility of Soils 53(8): 899-909.en
dcterms.extentp. 899-909en
dcterms.issued2017-11en
dcterms.languageenen
dcterms.licenseCC-BY-4.0en
dcterms.publisherSpringeren
dcterms.subjectphosphorusen
dcterms.subjectphosphataseen
dcterms.subjectoxisolen
dcterms.subjectsoilen
dcterms.subjectsoil propertiesen
dcterms.subjectsoil fertilityen
dcterms.subjectfósforoen
dcterms.subjectferralsolesen
dcterms.subjectmicrobiologyen
dcterms.typeJournal Articleen

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