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dc.contributor.authorSONG, G. X.eng
dc.contributor.authorNOVOTNY, E. H.eng
dc.contributor.authorHAYES, M. H. B.eng
dc.date.accessioned2019-11-11T18:13:32Z-
dc.date.available2019-11-11T18:13:32Z-
dc.date.created2019-11-11
dc.date.issued2018
dc.identifier.citationIn: INTERNATIONAL CONFERENCE OF HUMIC SUBSTANCES AND THEIR CONTRIBUTION TO THE CLIMATE CHANGE MITIGATION, 19., 2018, Albena Resort. Book of abstracts. Sofia: Bulgarian Humic Substances Society, 2018. p. 321-322.eng
dc.identifier.urihttp://www.alice.cnptia.embrapa.br/alice/handle/doc/1114115-
dc.descriptionMaize (Zea mays, a C4 plant) stover was incubated in a long-term cultivated soil for 24 months in order to better understand the transformation of crop residues into soil organic matter. Humic fractions, including humin, were isolated using an exhaustive sequential extraction procedure based on the charge density and polarity differences of the humic substances: Repetitive aqueous NaOH extraction was carried out at pH 7, 10.6, 12.6, and with 0.5 M NaOH. Then, an exhaustive 0.1 M NaOH + 6 M urea solution was applied to the soil residue to isolate the soluble 'urea humin' fraction. All isolates were further fractionated by the XAD-8 and XAD-4 resin-in-tandem procedure. Finally a concentrated suphuric acid plus DMSO solvent was employed to the fine clay to isolate the most recalcitrant humin material. The samples were characterized by elemental and delta13C analyses, FTIR and solid-state 13C NMR spectroscopy with CSA-filter and DD spectral editing. The data indicated that ca 47%~60% and 28%~40% of tranformed organic carbon was in the HAs and FAs fractions. The urea FA fractions and DMSO/acid FA fractions showed less 13C enrichment compared to the fulvic fractions isolated in alkaline only solutions. The refractory humin was predominantly aliphatic and with low aromaticity.eng
dc.language.isoengeng
dc.rightsopenAccesseng
dc.titleEvolution of maize residues into SOM in a study of two years incubation.eng
dc.typeArtigo em anais e proceedingseng
dc.date.updated2019-11-11T18:13:32Z
dc.subject.thesagroSoloeng
dc.subject.thesagroMatéria Orgânicaeng
dc.subject.thesagroResíduo Agrícolaeng
dc.subject.nalthesaurusSoil organic mattereng
dc.subject.nalthesaurusCrop residueseng
dc.subject.nalthesaurusHumificationeng
dc.subject.nalthesaurusHumic substanceseng
dc.subject.nalthesaurusHumineng
riaa.ainfo.id1114115eng
riaa.ainfo.lastupdate2019-11-11
dc.contributor.institutionG. X. SONG, SHANDONG UNIVERSITY, QINGDAO, CHINA; ETELVINO HENRIQUE NOVOTNY, CNPS; MICHAEL H. B. HAYES, UNIVERSITY OF LIMERICK, IRELAND.eng
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