Please use this identifier to cite or link to this item: http://www.alice.cnptia.embrapa.br/alice/handle/doc/1115017
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dc.contributor.authorLEMAINSKI, J.eng
dc.contributor.authorDENARDIN, J. E.eng
dc.contributor.authorDONAGEMMA, G. K.eng
dc.date.accessioned2019-12-11T18:10:34Z-
dc.date.available2019-12-11T18:10:34Z-
dc.date.created2019-11-25
dc.date.issued2019
dc.identifier.citationIn: WORLD CONGRESS OF SOIL SCIENCE, 21., 2018, Rio de Janeiro. Soil science: beyond food and fuel: proceedings... Viçosa, MG: SBCS, 2019. v. 2, p. 396. WCSS 2018.eng
dc.identifier.urihttp://www.alice.cnptia.embrapa.br/alice/handle/doc/1115017-
dc.descriptionSoil structure depends on physical, chemical, and biological factors. The interaction of these factors is a result of quantity and quality of residues and other inputs added to the soil, as well as their physicochemical conditions. Liming is an essential management practice in acid soils. When in excess, liming alters the electrolytic solution of the soil with impacts on its structure. In this sense, negative charges increase with pH, reducing the attraction between clay particles and resulting in increased clay dispersion and soil aggregate destabilization.eng
dc.language.isoengeng
dc.rightsopenAccesseng
dc.titleSoil structural properties under addition of crop residues and limestone.eng
dc.typeResumo em anais e proceedingseng
dc.date.updated2019-12-11T18:10:34Z
dc.subject.thesagroOxisoleng
dc.subject.thesagroArgilaeng
dc.subject.thesagroPheng
dc.subject.thesagroPlantio Diretoeng
dc.subject.nalthesaurusOxisolseng
dc.subject.nalthesaurusClayeng
dc.subject.nalthesaurusSoil pHeng
dc.subject.nalthesaurusNo-tillageeng
riaa.ainfo.id1115017eng
riaa.ainfo.lastupdate2019-12-11
dc.contributor.institutionJORGE LEMAINSKI, CNPT; JOSE ELOIR DENARDIN, CNPT; GUILHERME KANGUSSU DONAGEMMA, CNPS.eng
Appears in Collections:Resumo em anais de congresso (CNPS)

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