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| Registros recuperados : 8 | |
| 2. |  | CAMPOS-FILHO, P. J.; LOPES, V. S.; KUWAHARA, M. K.; LOPES, I. O. N.; ARIAS, C. A.; MARCELINO, F. C. Validação de um método para detecção e quantificação de eventos de soja gm tolerante a herbicidas imidazolinonas por PCR convencional e quantitativo. In: JORNADA ACADÊMICA DA EMBRAPA SOJA, 4., 2009, Londrina. Resumos... Londrina: Embrapa Soja, 2009. p. 97-102. (Embrapa Soja. Documentos, 312). Editado por Odilon Ferreira Saraiva, Paula Geron Saiz Melo.| Biblioteca(s): Embrapa Soja. |
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| 3. | | CAMPOS-FILHO, P. J.; OLIVEIRA, G. B. A.; OLIVEIRA, E. F.; SILVA, S. O.; SILVA, J. B.; MANDARINO, J. M. G.; CARRÃO-PANIZZI, M. C.; OLIVEIRA, M. A. Avaliação das características físicas das sementes de cultivares de soja especiais para alimentação humana no processamento de extrato solúvel de soja. In: JORNADA ACADÊMICA DA EMBRAPA SOJA, 2008, Londrina. Resumos expandidos. .. Londrina: Embrapa Soja, 2008. p. 107-110 (Embrapa Soja. Documentos, 297).| Biblioteca(s): Embrapa Soja. |
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| 4. | | OLIVEIRA, E. F.; SILVA, S. O.; SILVA, J. B.; OLIVEIRA, G. B. A.; CAMPOS FILHO, P. J.; MANDARINO, J. M. G.; CARRÃO-PANIZZI, M. C. Determinação de isoflavonas e inibidor de tripsina de kunitz em grãos e extratos solúveis de soja, obtidos de cultivares especiais para alimentação humana. In: JORNADA ACADÊMICA DA EMBRAPA SOJA, 2008, Londrina. Resumos expandidos... Londrina: Embrapa Soja, 2008. p. 129-134 (Embrapa Soja. Documentos, 297).| Biblioteca(s): Embrapa Soja. |
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| 5. | | OLIVEIRA, M. A. de; CARRÃO-PANIZZI, M. C.; LEITE, R. S.; CAMPOS FILHO, P. J. de; VICENTINI, M. B. Quantificação dos teores de açúcares, oligossacarídeos e amido em genótipos/ cultivares de soja (Glycine Max (L) Merril) especiais utilizados para alimentação humana. Brazilian Journal of Food Technology, Campinas, v. 13, n. 1, p. 23-29, jan./mar. 2010.| Biblioteca(s): Embrapa Soja. |
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| 6. | | OLIVEIRA, M. A. de; CARRÃO-PANIZZI, M. C.; LEITE, R. S.; CAMPOS FILHO, P. J. de; VICENTINI, M. B. Quantificação dos teores de açúcares, oligossacarídeos e amido em genótipos/cultivares de soja (Glycine Max (L) Merril) especiais utilizados para alimentação humana. Brazilian Journal of Food Technology, Campinas, v. 13, n. 1, p. 23-29, jan./mar. 2010.| Biblioteca(s): Embrapa Soja. |
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| 7. | | SILVA, J. B. da; OLIVEIRA, G. B. A. de; SILVA, S. O.; OLIVEIRA, E. F. de; CAMPOS FILHO, P. J. de; CARRÃO-PANIZZI, M. C.; MANDARINO, J. M. G. Avaliação da preferência sensorial de extratos solúveis de soja, obtidos de cultivares especiais para a alimentação humana. In: JORNADA ACADÊMICA DA EMBRAPA SOJA, 3., 2008, Londrina. Resumos expandidos...Londrina: Embrapa Soja, 2008. p. 31-37 (Embrapa Soja. Documentos, 297).| Biblioteca(s): Embrapa Soja. |
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| 8. | | SILVA, S. O.; OLIVEIRA, E. F.; OLIVEIRA, G. B. A.; SILVA, J. B.; CAMPOS FILHO, P. J.; MANDARINO, J. M. G.; CARRÃO-PANIZZI, M. C. Composição centesimal e solubilidade da proteína de cultivares de soja especiais para alimentação humana no processamento de extrato solúvel de soja. In: JORNADA ACADÊMICA DA EMBRAPA SOJA, 2008, Londrina. Resumos expandidos... Londrina: Embrapa Soja, 2008. p. 135-140 (Embrapa Soja. Documentos, 297).| Biblioteca(s): Embrapa Soja. |
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| Registros recuperados : 8 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Amazônia Oriental. |
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Data corrente: |
14/12/2015 |
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Data da última atualização: |
26/05/2022 |
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Autoria: |
ANDREAE, M. O.; ACEVEDO, O. C.; ARAUJO, A.; ARTAXO, P.; BARBOSA, C. G. G.; BARBOSA, H. M. J.; BRITO, J.; CARBONE, S.; CHI, X.; CINTRA, B. B. L.; SILVA, N. F. da; DIAS, N. L.; DIAS-JÚNIOR, C. Q.; DITAS, F.; DITZ, R.; GODOI, A. F. L.; GODOI, R. H. M.; HEIMANN, M.; HOFFMANN, T.; KESSELMEIER, J.; KÖNEMANN, T.; KRÜGER, M. L.; LAVRIC, J. V.; MANZI, A. O.; MORAN-ZULOAGA, D.; NÖLSCHER, A. C.; NOGUEIRA, D. S.; PIEDADE, M. T. F.; PÖHLKER, C.; PÖSCHL, U.; RIZZO, L. V.; RO, C.-U.; RUCKTESCHLER, N.; SÁ, L. D. A.; SÁ, M. D. O.; SALES, C. B.; SANTOS, R. M. N. dos; SATURNO, J.; SCHÖNGART, J.; SÖRGEL, M.; SOUZA, C. M. de; SOUZA, R. A. F. de; SU, H.; TARGHETTA, N.; TÓTA, J.; TREBS, I.; TRUMBORE, S.; EIJCK, A. van; WALTER, D.; WANG, Z.; WEBER, B.; WILLIAMS, J.; WINDERLICH, J.; WITTMANN, F.; WOLFF, S.; YÁÑEZ-SERRANO, A. M. |
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Afiliação: |
M. O. ANDREAE, Max Planck Institute for Chemistry / University of California San Diego; O. C. ACEVEDO, Universidade Federal Santa Maria; ALESSANDRO CARIOCA DE ARAUJO, CPATU; P. ARTAXO, USP; C. G. G. BARBOSA, UFPR; H. M. J. BARBOSA, USP; J. BRITO, USP; S. CARBONE, USP; X. CHI, Max Planck Institute for Chemistry; B. B. L. CINTRA, INPA; N. F. DA SILVA, INPA; N. L. DIAS, UFPR; C. Q. DIAS-JÚNIOR, IFPA / INPA; F. DITAS, Max Planck Institute for Chemistry; R. DITZ, Max Planck Institute for Chemistry; A. F. L. GODOI, UFPR; R. H. M. GODOI, UFPR; M. HEIMANN, Max Planck Institute for Biogeochemistry; T. HOFFMANN, Johannes Gutenberg University; J. KESSELMEIER, Max Planck Institute for Chemistry; T. KÖNEMANN, Max Planck Institute for Chemistry; M. L. KRÜGER, Max Planck Institute for Chemistry; J. V. LAVRIC, Max Planck Institute for Biogeochemistry; A. O. MANZI, INPA; D. MORAN-ZULOAGA, Max Planck Institute for Chemistry; A. C. NÖLSCHER, Max Planck Institute for Chemistry; D. SANTOS NOGUEIRA, CENSIPAM; M. T. F. PIEDADE, INPA; C. PÖHLKER, Max Planck Institute for Chemistry; U. PÖSCHL, Max Planck Institute for Chemistry; L. V. RIZZO, USP; C.-U. RO, Inha University; N. RUCKTESCHLER, Max Planck Institute for Chemistry; L. D. A. SÁ, INPE; M. D. O. SÁ, INPA; C. B. SALES, INPA / CESP/UEA; R. M. N. D. SANTOS, UEA; J. SATURNO, Max Planck Institute for Chemistry; J. SCHÖNGART, Max Planck Institute for Chemistry / INPA; M. SÖRGEL, Max Planck Institute for Chemistry; C. M. DE SOUZA, INPA / UFAM/ICSEZ-Parintins; R. A. F. DE SOUZA, UEA; H. SU, Max Planck Institute for Chemistry; N. TARGHETTA, INPA; J. TÓTA, UEA / UFOPA; I. TREBS, Max Planck Institute for Chemistry; S. TRUMBORE, Max Planck Institute for Biogeochemistry; A. VAN EIJCK, Johannes Gutenberg University; D. WALTER, Max Planck Institute for Chemistry; Z. WANG, Max Planck Institute for Chemistry; B. WEBER, Max Planck Institute for Chemistry; J. WILLIAMS, Max Planck Institute for Chemistry; J. WINDERLICH, Max Planck Institute for Chemistry / Max Planck Institute for Biogeochemistry; F. WITTMANN, Max Planck Institute for Chemistry; S. WOLFF, Max Planck Institute for Chemistry / INPA; A. M. YÁÑEZ-SERRANO, Max Planck Institute for Chemistry / INPA. |
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Título: |
The Amazon Tall Tower Observatory (ATTO) in the remote Amazon basin: overview of first results from ecosystem ecology, meteorology, trace gas, and aerosol measurements. |
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Ano de publicação: |
2015 |
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Fonte/Imprenta: |
Atmospheric Chemistry and Physics Discuss, v. 15, n. 18, p. 11599-11726, 2015. |
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DOI: |
10.5194/acpd-15-11599-2015 |
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Idioma: |
Português |
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Conteúdo: |
The Amazon Basin plays key roles in the carbon and water cycles, climate change, atmospheric chemistry, and biodiversity. It already has been changed significantly by human activities, and more pervasive change is expected to occur in the next decades. It is therefore essential to establish long-term measurement sites that provide a baseline record of present-day climatic, biogeochemical, and atmospheric conditions and that will be operated over coming decades to monitor change in the Amazon region as human perturbations increase in the future. The Amazon Tall Tower Observatory (ATTO) has been set up in a pristine rain forest region in the central Amazon Basin, about 150 km northeast of the city of Manaus. An ecological survey including a biodiversity assessment has been conducted in the forest region surrounding the site. Two 80 m towers have been operated at the site since 2012, and a 325 m tower is nearing completion in mid-2015. Measurements of micrometeorological and atmospheric chemical variables were initiated in 2012, and their range has continued to broaden over the last few years. The meteorological and micrometeorological measurements include temperature and wind profiles, precipitation, water and energy fluxes, turbulence components, soil temperature profiles and soil heat fluxes, radiation fluxes, and visibility. A tree has been instrumented to measure stem profiles of temperature, light intensity, and water content in cryptogamic covers. The trace gas measurements comprise continuous monitoring of carbon dioxide, carbon monoxide, methane, and ozone at 5 to 8 different heights, complemented by a variety of additional species measured during intensive campaigns (e.g., VOC, NO, NO2, and OH reactivity). Aerosol optical, microphysical, and chemical measurements are made above the canopy as well as in the canopy space. They include light scattering and absorption, aerosol fluorescence, number and volume size distributions, chemical composition, cloud condensation nuclei (CCN) concentrations, and hygroscopicity. Initial results from ecological, meteorological, and chemical studies at the ATTO site are presented in this paper. MenosThe Amazon Basin plays key roles in the carbon and water cycles, climate change, atmospheric chemistry, and biodiversity. It already has been changed significantly by human activities, and more pervasive change is expected to occur in the next decades. It is therefore essential to establish long-term measurement sites that provide a baseline record of present-day climatic, biogeochemical, and atmospheric conditions and that will be operated over coming decades to monitor change in the Amazon region as human perturbations increase in the future. The Amazon Tall Tower Observatory (ATTO) has been set up in a pristine rain forest region in the central Amazon Basin, about 150 km northeast of the city of Manaus. An ecological survey including a biodiversity assessment has been conducted in the forest region surrounding the site. Two 80 m towers have been operated at the site since 2012, and a 325 m tower is nearing completion in mid-2015. Measurements of micrometeorological and atmospheric chemical variables were initiated in 2012, and their range has continued to broaden over the last few years. The meteorological and micrometeorological measurements include temperature and wind profiles, precipitation, water and energy fluxes, turbulence components, soil temperature profiles and soil heat fluxes, radiation fluxes, and visibility. A tree has been instrumented to measure stem profiles of temperature, light intensity, and water content in cryptogamic covers. The trace gas measureme... Mostrar Tudo |
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Palavras-Chave: |
Monitoramento. |
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Thesagro: |
Clima. |
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Thesaurus NAL: |
Amazonia. |
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Categoria do assunto: |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/135576/1/acpdDiscuss.pdf
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Marc: |
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100 1 $aANDREAE, M. O.
245 $aThe Amazon Tall Tower Observatory (ATTO) in the remote Amazon basin$boverview of first results from ecosystem ecology, meteorology, trace gas, and aerosol measurements.$h[electronic resource]
260 $c2015
520 $aThe Amazon Basin plays key roles in the carbon and water cycles, climate change, atmospheric chemistry, and biodiversity. It already has been changed significantly by human activities, and more pervasive change is expected to occur in the next decades. It is therefore essential to establish long-term measurement sites that provide a baseline record of present-day climatic, biogeochemical, and atmospheric conditions and that will be operated over coming decades to monitor change in the Amazon region as human perturbations increase in the future. The Amazon Tall Tower Observatory (ATTO) has been set up in a pristine rain forest region in the central Amazon Basin, about 150 km northeast of the city of Manaus. An ecological survey including a biodiversity assessment has been conducted in the forest region surrounding the site. Two 80 m towers have been operated at the site since 2012, and a 325 m tower is nearing completion in mid-2015. Measurements of micrometeorological and atmospheric chemical variables were initiated in 2012, and their range has continued to broaden over the last few years. The meteorological and micrometeorological measurements include temperature and wind profiles, precipitation, water and energy fluxes, turbulence components, soil temperature profiles and soil heat fluxes, radiation fluxes, and visibility. A tree has been instrumented to measure stem profiles of temperature, light intensity, and water content in cryptogamic covers. The trace gas measurements comprise continuous monitoring of carbon dioxide, carbon monoxide, methane, and ozone at 5 to 8 different heights, complemented by a variety of additional species measured during intensive campaigns (e.g., VOC, NO, NO2, and OH reactivity). Aerosol optical, microphysical, and chemical measurements are made above the canopy as well as in the canopy space. They include light scattering and absorption, aerosol fluorescence, number and volume size distributions, chemical composition, cloud condensation nuclei (CCN) concentrations, and hygroscopicity. Initial results from ecological, meteorological, and chemical studies at the ATTO site are presented in this paper.
650 $aAmazonia
650 $aClima
653 $aMonitoramento
700 1 $aACEVEDO, O. C.
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700 1 $aYÁÑEZ-SERRANO, A. M.
773 $tAtmospheric Chemistry and Physics Discuss$gv. 15, n. 18, p. 11599-11726, 2015.
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Embrapa Amazônia Oriental (CPATU) |
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