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| Registros recuperados : 7 | |
| 6. |  | MARTHA JUNIOR, G. B.; PENA JUNIOR, M. A. G.; MARCIAL, E. C.; CASTANHEIRA NETO, F.; TORRES, L. A.; NOGUEIRA, V. G. de C.; CHERVENSKI, V. M. B.; SILVA, G. T. S. da; WOSGRAU, A. C. Cenários exploratórios para o desenvolvimento tecnológico da agricultura brasileira : síntese. Brasília, DF : Embrapa, 2016. 26 p.| Biblioteca(s): Embrapa Unidades Centrais. |
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| 7. | | BUAINAIN, A. M.; FAVARETO, A.; CONTINI, E.; CHAVES, F. T.; HENZ, G. P.; GARCIA, J. R.; DAMIANI, O.; VIEIRA JUNIOR, P. A.; GRUNDLING, R. D. P.; NOGUEIRA, V. G. de C. Desafios para agricultura nos biomas brasileiros. Brasília, DF: Embrapa, 2020. 69 p. PDF: il. color.| Biblioteca(s): Embrapa Unidades Centrais. |
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| Registros recuperados : 7 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Amapá; Embrapa Pantanal; Embrapa Solos. |
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Data corrente: |
15/10/2015 |
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Data da última atualização: |
25/07/2017 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
B - 1 |
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Autoria: |
BERGIER, I.; MAIA, C. M. B. F.; GUIOTOKU, M.; PAIVA, P.; SILVA. A. P.; NOVOTNY, E. H. |
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Afiliação: |
IVAN BERGIER TAVARES DE LIMA, CPAP; CLAUDIA MARIA BRANCO DE F MAIA, CNPF; MARCELA GUIOTOKU, CNPF; PAULO MARCELO VERAS DE PAIVA, CPAF-AP; ANA PAULA SILVA, BOLSISTA EMBRAPA PANTANAL; ETELVINO HENRIQUE NOVOTNY, CNPS. |
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Título: |
Pyrolysis dynamics of biomass residues in hot-stage. |
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Ano de publicação: |
2015 |
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Fonte/Imprenta: |
BioResources, Raleigh, v. 10, n. 4, p. 7604-7617, Nov. 2015. |
|
Idioma: |
Inglês |
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Conteúdo: |
Original data for mass, element, and methane dynamics under controlled pyrolysis are presented for several biomass feedstocks. The experimental system consisted of an environmental (low-vacuum) scanning electron microscopy (ESEM) with a hot-stage and energy-dispersive X-ray spectroscopy (EDS) detector. A tunable diode laser (TDL) was coupled to the ESEM vacuum pump to measure the methane partial pressure in the exhaust gases. Thermogravimetric analysis and differential thermal analysis (TG/DTA) in a N2 atmosphere was also carried out to assess the thermal properties of each biomass. It was found that biochars were depleted or enriched in specific elements, with distinct methane formation change. Results depended on the nature of the biomass, in particular the relative proportion of lignocellulosic materials, complex organic compounds, and ash. As final temperature was increased, N generally decreased by 30 to 100%, C increased by 20 to 50% for biomass rich in lignocellulose, and P, Mg, and Ca increased for ash-rich biomass. Methane formation also allows discriminating structural composition, providing fingerprints of each biomass. Biomass with low ashes and high lignin contents peaks CH4 production at 330 and 460 °C, whereas those biomasses with high ashes and low lignin peaks CH4 production at 330 and/or 400 °C. |
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Palavras-Chave: |
Estrume; Fertilizer; Resíduos; Soil fertilizer. |
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Thesagro: |
Agricultura; Biomassa; Fertilizante. |
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Thesaurus NAL: |
agriculture; biochar; biomass. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/131245/1/Pyrolysis-Dynamics-of-biomass.pdf
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Marc: |
LEADER 02109naa a2200301 a 4500
001 2026460
005 2017-07-25
008 2015 bl uuuu u00u1 u #d
100 1 $aBERGIER, I.
245 $aPyrolysis dynamics of biomass residues in hot-stage.$h[electronic resource]
260 $c2015
520 $aOriginal data for mass, element, and methane dynamics under controlled pyrolysis are presented for several biomass feedstocks. The experimental system consisted of an environmental (low-vacuum) scanning electron microscopy (ESEM) with a hot-stage and energy-dispersive X-ray spectroscopy (EDS) detector. A tunable diode laser (TDL) was coupled to the ESEM vacuum pump to measure the methane partial pressure in the exhaust gases. Thermogravimetric analysis and differential thermal analysis (TG/DTA) in a N2 atmosphere was also carried out to assess the thermal properties of each biomass. It was found that biochars were depleted or enriched in specific elements, with distinct methane formation change. Results depended on the nature of the biomass, in particular the relative proportion of lignocellulosic materials, complex organic compounds, and ash. As final temperature was increased, N generally decreased by 30 to 100%, C increased by 20 to 50% for biomass rich in lignocellulose, and P, Mg, and Ca increased for ash-rich biomass. Methane formation also allows discriminating structural composition, providing fingerprints of each biomass. Biomass with low ashes and high lignin contents peaks CH4 production at 330 and 460 °C, whereas those biomasses with high ashes and low lignin peaks CH4 production at 330 and/or 400 °C.
650 $aagriculture
650 $abiochar
650 $abiomass
650 $aAgricultura
650 $aBiomassa
650 $aFertilizante
653 $aEstrume
653 $aFertilizer
653 $aResíduos
653 $aSoil fertilizer
700 1 $aMAIA, C. M. B. F.
700 1 $aGUIOTOKU, M.
700 1 $aPAIVA, P.
700 1 $aSILVA. A. P.
700 1 $aNOVOTNY, E. H.
773 $tBioResources, Raleigh$gv. 10, n. 4, p. 7604-7617, Nov. 2015.
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Registro original: |
Embrapa Pantanal (CPAP) |
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