2021
DOI: 10.1038/s41598-021-87479-2
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Soil CO2 emission and soil attributes associated with the microbiota of a sugarcane area in southern Brazil

Abstract: The spatial structure of soil CO2 emission (FCO2) and soil attributes are affected by different factors in a highly complex way. In this context, this study aimed to characterize the spatial variability patterns of FCO2 and soil physical, chemical, and microbiological attributes in a sugarcane field area after reform activities. The study was conducted in an Oxisol with the measurement of FCO2, soil temperature (Ts), and soil moisture (Ms) in a regular 90 × 90-m grid with 100 sampling points. Soil samples were… Show more

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Cited by 8 publications
(2 citation statements)
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References 84 publications
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“…The production chain of this biofuel contributes significantly to minimizing environmental impacts, especially concerning global warming. Brazilian ethanol is a good example, as it is mainly produced from sugarcane, a grass with a high capacity to sequester carbon dioxide -CO₂ dispersed in the atmosphere during its development (Moitinho et al, 2021). The main ethanol producers in the world are the United States and Brazil; together, they produce about 82%, using corn as the main source in the US, sugarcane in Brazil, and more recently, corn (Silva and Castañeda-Ayarza, 2021).…”
Section: Resultsmentioning
confidence: 99%
“…The production chain of this biofuel contributes significantly to minimizing environmental impacts, especially concerning global warming. Brazilian ethanol is a good example, as it is mainly produced from sugarcane, a grass with a high capacity to sequester carbon dioxide -CO₂ dispersed in the atmosphere during its development (Moitinho et al, 2021). The main ethanol producers in the world are the United States and Brazil; together, they produce about 82%, using corn as the main source in the US, sugarcane in Brazil, and more recently, corn (Silva and Castañeda-Ayarza, 2021).…”
Section: Resultsmentioning
confidence: 99%
“…Soil microbial biomass C represents the active and biodegradable fraction of soil organic matter and is partially composed of several species of microorganisms that act as agents in the mineralization of organic matter. The dynamics of microbial activity are regulated, among other factors, by the C:N ratio of the soil, as the relationship between these two elements in the soil interferes with the degree of humification and stability of soil organic matter [34]. The fact that this relationship is a smaller agricultural system in the surface layer indicates that the decomposition process of organic matter is accelerated in this region, resulting in emissions and reduced mineralization of soil organic matter in the aforementioned system.…”
Section: Light Organic Matter and C:n Ratiomentioning
confidence: 99%