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Registro Completo |
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Biblioteca(s): |
Embrapa Agrobiologia; Embrapa Pantanal. |
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Data corrente: |
27/06/1995 |
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Data da última atualização: |
27/06/1995 |
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Autoria: |
SPARLING, G. P. |
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Título: |
Ratio of microbial biomass carbon to soil organic carbon as a sensitive indicator of changes in soil organic matter. |
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Ano de publicação: |
1992 |
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Fonte/Imprenta: |
Aust. J. Soil Res., v.30, p.195-207, 1992. |
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Idioma: |
Inglês
Português |
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Conteúdo: |
The sensitivity of soil organic carbon (Corg) and microbial carbon (Cmic) measurements, and the Cmic/Corg ratio, to reflect climatic, vegetation, cropping and management history was investigated using a range of topsoils in New Zealand. The Cmic generally comprised 1-4% of Corg, with the proportion being consistently greather under pastures, than the equivalent soil under native forest, exotic forest or arable cropping. However, absolute values differed markedly between soils and were greatly influenced by texture, mineralogy and the Corg content. The Cmic recovered more rapidly than Corg on returning to pasture following cropping. There was a generally greater Corg content in those soils from the areas with higher precipitation, but the precipitation-evaporation quotient proposed by Insam et al. (Soil Biol. Biochem. 1989, 21, 211-21) to predict the relationship between Cmic and Corg, greatly underestimated the Cmic content of New Zealand soils and there was too great a scatter in the data to derive a revised regression formula. The Cmic and the Cmic/Corg ratio are useful measures to monitor soil organic matter and both provide a more sensitive index than Corg measured alone. However, under typical climatic and land use conditions in New Zeland, the values do not appear readily transferrable between soils. To ascertain whether a soil has achieved equilibrium in organic matter status, it will be necessary to establish reference values to which a tested soil can be compared. |
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Palavras-Chave: |
BIOMASSA MICROBIANA. |
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Thesagro: |
Biomassa; Carbono; Clima; Matéria Orgânica; Método; Solo; Vegetação. |
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Thesaurus Nal: |
biomass; carbon; climate; organic matter; soil; vegetation. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 02246naa a2200289 a 4500
001 1616171
005 1995-06-27
008 1992 bl --- 0-- u #d
100 1 $aSPARLING, G. P.
245 $aRatio of microbial biomass carbon to soil organic carbon as a sensitive indicator of changes in soil organic matter.
260 $c1992
520 $aThe sensitivity of soil organic carbon (Corg) and microbial carbon (Cmic) measurements, and the Cmic/Corg ratio, to reflect climatic, vegetation, cropping and management history was investigated using a range of topsoils in New Zealand. The Cmic generally comprised 1-4% of Corg, with the proportion being consistently greather under pastures, than the equivalent soil under native forest, exotic forest or arable cropping. However, absolute values differed markedly between soils and were greatly influenced by texture, mineralogy and the Corg content. The Cmic recovered more rapidly than Corg on returning to pasture following cropping. There was a generally greater Corg content in those soils from the areas with higher precipitation, but the precipitation-evaporation quotient proposed by Insam et al. (Soil Biol. Biochem. 1989, 21, 211-21) to predict the relationship between Cmic and Corg, greatly underestimated the Cmic content of New Zealand soils and there was too great a scatter in the data to derive a revised regression formula. The Cmic and the Cmic/Corg ratio are useful measures to monitor soil organic matter and both provide a more sensitive index than Corg measured alone. However, under typical climatic and land use conditions in New Zeland, the values do not appear readily transferrable between soils. To ascertain whether a soil has achieved equilibrium in organic matter status, it will be necessary to establish reference values to which a tested soil can be compared.
650 $abiomass
650 $acarbon
650 $aclimate
650 $aorganic matter
650 $asoil
650 $avegetation
650 $aBiomassa
650 $aCarbono
650 $aClima
650 $aMatéria Orgânica
650 $aMétodo
650 $aSolo
650 $aVegetação
653 $aBIOMASSA MICROBIANA
773 $tAust. J. Soil Res.$gv.30, p.195-207, 1992.
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Registro original: |
Embrapa Agrobiologia (CNPAB) |
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| Registros recuperados : 84 | |
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| 10. | | TIBOLA, C. S.; NICOLLI, C. P.; SPOLTI, P.; DEL PONTE, E. M.; FERNANDES, J. M. C. Avaliação do teste imunológico Quicktox®na quantificação de deoxinivalenol em trigo para segregação de lotes. In: REUNIÃO DA COMISSÃO BRASILEIRA DE PESQUISA DE TRIGO E TRITICALE, 8.; SEMINÁRIO TÉCNICO DO TRIGO, 9., 2014, Canela; REUNIÃO DA COMISSÃO BRASILEIRA DE PESQUISA DE TRIGO E TRITICALE, 9.; SEMINÁRIO TÉCNICO DO TRIGO, 10., 2015, Passo Fundo. Anais... Passo Fundo: Biotrigo Genética: Embrapa Trigo, 2015. 2014-Fitopatologia-Trabalho 68. 1 CD-ROM.| Tipo: Artigo em Anais de Congresso |
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| 19. | | TIBOLA, C. S.; FERNANDES, J. M. C.; DEL PONTE, E. M.; SPOLTI, P.; PAVAN, W. Micotoxinas em trigo no Brasil: causas, panorama atual e perspectivas para o manejo. Revista Plantio Direto, Passo Fundo, v. 20, n. 124, p. 47-51, jul./ago. 2011.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: B - 5 |
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| 20. | | DEL PONTE, E. M.; GODOY, C. V.; CANTERI, M. G.; REIS, E. M.; YANG, X. B. Models and applications for risk assessment and prediction of Asian soybean rust epidemics. Fitopatologia Brasileira, Brasília, DF, v.31, n. 6, p. 533-544, Nov./Dec. 2006.| Biblioteca(s): Embrapa Soja. |
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| Registros recuperados : 84 | |
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