2015
DOI: 10.5935/1806-6690.20150029
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Carbon dynamics in no-till soil due to the use of industrial organic waste and mineral fertilizer

Abstract: -The use of organic waste from industrial processes in agriculture is a strategy not only for improving soil properties but also for promoting the utilization of recycled nutrients by market crops and for reducing environmental impact. The aim of this study was to evaluate the effects of using organic waste from pork and poultry slaughterhouses (OWS) applied alone or in combination with mineral fertilizer (MF) on the dynamics of soil organic matter (SOM) compartments. The experimental design adopted was that o… Show more

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Cited by 7 publications
(3 citation statements)
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“…Entre os indicadores de qualidade edáfica, a matéria orgânica do solo (MOS) é capaz de detectar alterações no ambiente decorrentes do uso e ocupação (ROMANIW et al, 2015), pois o estoque, as formas de carbono (C) orgânico e os atributos químicos, físicos e biológicos do solo estão estreitamente relacionados (BALDOTTO et al, 2010). Em solos com cobertura vegetal natural, o C orgânico encontra-se em equilíbrio dinâmico, com teores praticamente constantes com o tempo (ASSUNÇÃO et al, 2019).…”
Section: Introductionunclassified
“…Entre os indicadores de qualidade edáfica, a matéria orgânica do solo (MOS) é capaz de detectar alterações no ambiente decorrentes do uso e ocupação (ROMANIW et al, 2015), pois o estoque, as formas de carbono (C) orgânico e os atributos químicos, físicos e biológicos do solo estão estreitamente relacionados (BALDOTTO et al, 2010). Em solos com cobertura vegetal natural, o C orgânico encontra-se em equilíbrio dinâmico, com teores praticamente constantes com o tempo (ASSUNÇÃO et al, 2019).…”
Section: Introductionunclassified
“…Regarding the contribution of different fractions of organic matter to the total soil carbon, in general, the silt + clay fraction (<53 mm) was the predominant fraction (Table 2). This fraction corresponded to more than 50% of the fractions of soil organic matter (Figure 2) and is considered the most stable fraction, as it is in a more advanced stage of decomposition and has a longer residence time in the soil (Lisboa, Conant, Haddix, Cerri, & Cerri, 2009;Signor et al, 2014;Romaniw et al, 2015;Sousa et al, 2018).…”
Section: Resultsmentioning
confidence: 99%
“…Contribution of fractions of soil organic matter to total organic carbon from soil samples collected from different depths of sugarcane systems. (Conceição, Bayerll, Dieckowll, & Santos, 2014;Romaniw et al, 2015).…”
Section: Resultsmentioning
confidence: 99%