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Publicação:
Lime and phosphogypsum impacts on soil organic matter pools in a tropical Oxisol under long-term no-till conditions

dc.contributor.authorCarmeis Filho, Antonio C.A. [UNESP]
dc.contributor.authorPenn, Chad J.
dc.contributor.authorCrusciol, Carlos A.C. [UNESP]
dc.contributor.authorCalonego, Juliano C. [UNESP]
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.contributor.institutionUnited States Department of Agriculture
dc.date.accessioned2018-12-11T16:46:12Z
dc.date.available2018-12-11T16:46:12Z
dc.date.issued2017-04-01
dc.description.abstractImproving soil organic matter (SOM) quality in tropical acid soils is important for increasing the sustainability of agricultural ecosystems. This research evaluated the effect of the surface application of lime and phosphogypsum on the quality and amount of SOM in a long-term crop rotation under no-till conditions. The research was performed in a kaolinitic, thermic Typic Haplorthox for 12 years with annual crops under no-till. The treatments included no soil amendments, and amendment with phosphogypsum, lime, and lime + phosphogypsum. After three applications of soil amendments (2002, 2004, and 2010), surface liming increased the SOM input through addition of aboveground and root biomass, varying amount according to crop species, growing season, and soil depth. Although phosphogypsum had no effect on plant biomass production, the application of phosphogypsum with lime increased nitrogen (N) by up to 50% in the uppermost soil depths. The application of lime alone significantly increased the total organic carbon (TOC) at all depths, although the greatest effects were observed at 0.10–0.20 and 0.20–0.40 m, with an increase of 44% and 41%, respectively. Moreover, lime + phosphogypsum also exhibited the highest potential for C mineralization, which was attributed to an increased proportion of TOC as particulate organic carbon (POC). The proportion of TOC as humin and fulvic acid increased with the application of lime + phosphogypsum at 0–0.05 m, with an increase from 55% to 92% and from 1.4% to 1.6%, respectively. Overall, the combination of lime and phosphogypsum increased both the labile and stable C pools.en
dc.description.affiliationSão Paulo State University (UNESP) College of Agricultural Sciences Department of Crop Science, P. O. Box 237
dc.description.affiliationNational Soil Erosion Research United States Department of Agriculture
dc.description.affiliationUnespSão Paulo State University (UNESP) College of Agricultural Sciences Department of Crop Science, P. O. Box 237
dc.format.extent11-23
dc.identifierhttp://dx.doi.org/10.1016/j.agee.2017.02.027
dc.identifier.citationAgriculture, Ecosystems and Environment, v. 241, p. 11-23.
dc.identifier.doi10.1016/j.agee.2017.02.027
dc.identifier.file2-s2.0-85014432379.pdf
dc.identifier.issn0167-8809
dc.identifier.scopus2-s2.0-85014432379
dc.identifier.urihttp://hdl.handle.net/11449/169511
dc.language.isoeng
dc.relation.ispartofAgriculture, Ecosystems and Environment
dc.relation.ispartofsjr1,747
dc.rights.accessRightsAcesso aberto
dc.sourceScopus
dc.subjectDolomitic lime
dc.subjectHumic substances
dc.subjectRoot growth
dc.subjectSoil acidity
dc.titleLime and phosphogypsum impacts on soil organic matter pools in a tropical Oxisol under long-term no-till conditionsen
dc.typeArtigo
dspace.entity.typePublication
unesp.author.lattes9281484833327774[3]
unesp.author.orcid0000-0003-4673-1071[3]

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