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Biblioteca(s): |
Embrapa Semiárido. |
Data corrente: |
09/02/2012 |
Data da última atualização: |
23/03/2023 |
Tipo da produção científica: |
Resumo em Anais de Congresso |
Autoria: |
COSTA, V. S. O.; BATISTA, D. da C.; MARIANO, R. L. R; BARBOSA, M. A. G. |
Afiliação: |
V. S. O. COSTA; DIOGENES DA CRUZ BATISTA, CPATSA; R. L. R. MARIANO, UFRPE; MARIA ANGELICA GUIMARAES BARBOSA, CPATSA. |
Título: |
Sobrevivência de Xanthomonas campestris pv. viticola em restos de poda de videira fragmentados e tratados com aceleradores de decomposição. |
Ano de publicação: |
2011 |
Fonte/Imprenta: |
Tropical Plant Pathology, v. 36, 2011. |
Páginas: |
p. 1215. |
Descrição Física: |
1 CD-ROM. |
Idioma: |
Português |
Notas: |
Suplemento. Edição dos Resumos do 44 Congresso Brasileiro de Fitopatologia, Bento Gonçalves, ago. 2011. |
Conteúdo: |
Este trabalho objetivou verificar a sobrevivência de Xcv em restos de poda fragmentados e tratados com aceleradores de decomposição. |
Palavras-Chave: |
Vitis spp; Xanthomonas campestris pv viticola. |
Thesagro: |
Cancro Bacteriano; Doença; Resistência; Uva. |
Thesaurus Nal: |
Grapes. |
Categoria do assunto: |
A Sistemas de Cultivo |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/53692/1/DIOGENES-2011.pdf
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Marc: |
LEADER 00986nam a2200253 a 4500 001 1914796 005 2023-03-23 008 2011 bl uuuu u00u1 u #d 100 1 $aCOSTA, V. S. O. 245 $aSobrevivência de Xanthomonas campestris pv. viticola em restos de poda de videira fragmentados e tratados com aceleradores de decomposição. 260 $aTropical Plant Pathology, v. 36$c2011 300 $ap. 1215.$c1 CD-ROM. 500 $aSuplemento. Edição dos Resumos do 44 Congresso Brasileiro de Fitopatologia, Bento Gonçalves, ago. 2011. 520 $aEste trabalho objetivou verificar a sobrevivência de Xcv em restos de poda fragmentados e tratados com aceleradores de decomposição. 650 $aGrapes 650 $aCancro Bacteriano 650 $aDoença 650 $aResistência 650 $aUva 653 $aVitis spp 653 $aXanthomonas campestris pv viticola 700 1 $aBATISTA, D. da C. 700 1 $aMARIANO, R. L. R 700 1 $aBARBOSA, M. A. G.
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Embrapa Semiárido (CPATSA) |
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Biblioteca(s): |
Embrapa Amazônia Oriental. |
Data corrente: |
04/11/2016 |
Data da última atualização: |
20/05/2022 |
Autoria: |
ZAHN, E.; DIAS, N. L.; ARAUJO, A.; SÁ, L.; SÖRGEL, M.; TREBS, I.; WOLFF, S.; MANZI, A. |
Afiliação: |
EINARA ZAHN, UFPR; NELSON L. DIAS, UFPR; ALESSANDRO CARIOCA DE ARAUJO, CPATU; LEONARDO SÁ, INPE; MATTHIAS SÖERGE, Max Planck Institute for Chemistry; IVONNE TREBS, ERIN; STEFAN WOLFF, Max Planck Institute for Chemistry; ANTÔNIO MANZI, INPA. |
Título: |
Scalar turbulent behavior in the roughness sublayer of an Amazonian forest. |
Ano de publicação: |
2016 |
Fonte/Imprenta: |
Atmospheric Chemistry and Physics Discussions, 18 Jan. 2016. |
DOI: |
10.5194/acp-2015-1043 |
Idioma: |
Português |
Conteúdo: |
An important current problem in micrometeorology is the characterization of turbulence in the roughness sublayer (RSL), where most of the measurements above tall forests are made. There, scalar turbulent fluctuations display significant departures from the predictions of Monin?Obukhov similarity theory (MOST). In this work, we analyze turbulence data of virtual temperature, carbon dioxide, and water vapor in the RSL above an Amazonian forest (with a canopy height of 40?m), measured at 39.4 and 81.6?m above the ground under unstable conditions. We found that dimensionless statistics related to the rate of dissipation of turbulence kinetic energy (TKE) and the scalar variance display significant departures from MOST as expected, whereas the vertical velocity variance follows MOST much more closely. Much better agreement between the dimensionless statistics with the Obukhov similarity variable, however, was found for the subset of measurements made at a low zenith angle Z, in the range 0°???|Z|???20°. We conjecture that this improvement is due to the relationship between sunlight incidence and the ?activation?deactivation? of scalar sinks and sources vertically distributed in the forest. Finally, we evaluated the relaxation coefficient of relaxed eddy accumulation: it is also affected by zenith angle, with considerable improvement in the range 0°???|Z|???20°, and its values fall within the range reported in the literature for the unstable surface layer. In general, our results indicate the possibility of better stability-derived flux estimates for low zenith angle ranges. MenosAn important current problem in micrometeorology is the characterization of turbulence in the roughness sublayer (RSL), where most of the measurements above tall forests are made. There, scalar turbulent fluctuations display significant departures from the predictions of Monin?Obukhov similarity theory (MOST). In this work, we analyze turbulence data of virtual temperature, carbon dioxide, and water vapor in the RSL above an Amazonian forest (with a canopy height of 40?m), measured at 39.4 and 81.6?m above the ground under unstable conditions. We found that dimensionless statistics related to the rate of dissipation of turbulence kinetic energy (TKE) and the scalar variance display significant departures from MOST as expected, whereas the vertical velocity variance follows MOST much more closely. Much better agreement between the dimensionless statistics with the Obukhov similarity variable, however, was found for the subset of measurements made at a low zenith angle Z, in the range 0°???|Z|???20°. We conjecture that this improvement is due to the relationship between sunlight incidence and the ?activation?deactivation? of scalar sinks and sources vertically distributed in the forest. Finally, we evaluated the relaxation coefficient of relaxed eddy accumulation: it is also affected by zenith angle, with considerable improvement in the range 0°???|Z|???20°, and its values fall within the range reported in the literature for the unstable surface layer. In general, our ... Mostrar Tudo |
Thesagro: |
Climatologia; Floresta Tropical. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/149608/1/acp-2015-1043.pdf
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Marc: |
LEADER 02283naa a2200241 a 4500 001 2055916 005 2022-05-20 008 2016 bl uuuu u00u1 u #d 024 7 $a10.5194/acp-2015-1043$2DOI 100 1 $aZAHN, E. 245 $aScalar turbulent behavior in the roughness sublayer of an Amazonian forest.$h[electronic resource] 260 $c2016 520 $aAn important current problem in micrometeorology is the characterization of turbulence in the roughness sublayer (RSL), where most of the measurements above tall forests are made. There, scalar turbulent fluctuations display significant departures from the predictions of Monin?Obukhov similarity theory (MOST). In this work, we analyze turbulence data of virtual temperature, carbon dioxide, and water vapor in the RSL above an Amazonian forest (with a canopy height of 40?m), measured at 39.4 and 81.6?m above the ground under unstable conditions. We found that dimensionless statistics related to the rate of dissipation of turbulence kinetic energy (TKE) and the scalar variance display significant departures from MOST as expected, whereas the vertical velocity variance follows MOST much more closely. Much better agreement between the dimensionless statistics with the Obukhov similarity variable, however, was found for the subset of measurements made at a low zenith angle Z, in the range 0°??<??|Z|??<??20°. We conjecture that this improvement is due to the relationship between sunlight incidence and the ?activation?deactivation? of scalar sinks and sources vertically distributed in the forest. Finally, we evaluated the relaxation coefficient of relaxed eddy accumulation: it is also affected by zenith angle, with considerable improvement in the range 0°??<??|Z|??<??20°, and its values fall within the range reported in the literature for the unstable surface layer. In general, our results indicate the possibility of better stability-derived flux estimates for low zenith angle ranges. 650 $aClimatologia 650 $aFloresta Tropical 700 1 $aDIAS, N. L. 700 1 $aARAUJO, A. 700 1 $aSÁ, L. 700 1 $aSÖRGEL, M. 700 1 $aTREBS, I. 700 1 $aWOLFF, S. 700 1 $aMANZI, A. 773 $tAtmospheric Chemistry and Physics Discussions, 18 Jan. 2016.
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