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Registro Completo |
Biblioteca(s): |
Embrapa Solos. |
Data corrente: |
28/04/2022 |
Data da última atualização: |
28/04/2022 |
Autoria: |
RITA, J. C. de O.; GAMA-RODRIGUES, E. F. da; GAMA-RODRIGUES, A. C. da; POLIDORO, J. C. |
Afiliação: |
JOICE CLEIDE DE OLIVEIRA RITA, UENF; EMANUELA FORESTIERI DA GAMA-RODRIGUES, UENF; ANTONIO CARLOS DA GAMA-RODRIGUES, UENF; JOSE CARLOS POLIDORO, CNPS. |
Título: |
Fracionamento físico da matéria orgânica nas classes de agregado do solo sob sistemas agroflorestais de cacau no Sul da Bahia. |
Ano de publicação: |
2009 |
Fonte/Imprenta: |
In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 32., 2009, Fortaleza. O solo e a produção de bioenergia: perspectivas e desafios. [Viçosa, MG]: SBCS; Fortaleza: UFC, 2009. 1 CD-ROM. |
Idioma: |
Português |
Conteúdo: |
O presente estudo teve o objetivo de avaliar a distribuição do carbono e nitrogênio das frações da matéria orgânica nas classes de agregados de solos sob sistemas agroflorestais de cacau. Este estudo foi realizado em agrossistemas de cacau: cacauca-bruca; cacau com sombreamento definitivo de eritrina e floresta natural. |
Thesagro: |
Cacau; Carbono; Erythrina Glauca; Nitrogênio. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/1142467/1/Fracionamento-fisico-da-materia-organica-2009.pdf
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Marc: |
LEADER 01096nam a2200193 a 4500 001 2142467 005 2022-04-28 008 2009 bl uuuu u00u1 u #d 100 1 $aRITA, J. C. de O. 245 $aFracionamento físico da matéria orgânica nas classes de agregado do solo sob sistemas agroflorestais de cacau no Sul da Bahia.$h[electronic resource] 260 $aIn: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 32., 2009, Fortaleza. O solo e a produção de bioenergia: perspectivas e desafios. [Viçosa, MG]: SBCS; Fortaleza: UFC, 2009. 1 CD-ROM.$c2009 520 $aO presente estudo teve o objetivo de avaliar a distribuição do carbono e nitrogênio das frações da matéria orgânica nas classes de agregados de solos sob sistemas agroflorestais de cacau. Este estudo foi realizado em agrossistemas de cacau: cacauca-bruca; cacau com sombreamento definitivo de eritrina e floresta natural. 650 $aCacau 650 $aCarbono 650 $aErythrina Glauca 650 $aNitrogênio 700 1 $aGAMA-RODRIGUES, E. F. da 700 1 $aGAMA-RODRIGUES, A. C. da 700 1 $aPOLIDORO, J. C.
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Embrapa Solos (CNPS) |
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Biblioteca(s): |
Embrapa Amazônia Oriental. |
Data corrente: |
14/12/2015 |
Data da última atualização: |
26/05/2022 |
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. |
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. |
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. |
Ano de publicação: |
2015 |
Fonte/Imprenta: |
Atmospheric Chemistry and Physics Discuss, v. 15, n. 18, p. 11599-11726, 2015. |
DOI: |
10.5194/acpd-15-11599-2015 |
Idioma: |
Português |
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 |
Palavras-Chave: |
Monitoramento. |
Thesagro: |
Clima. |
Thesaurus NAL: |
Amazonia. |
Categoria do assunto: |
-- |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/135576/1/acpdDiscuss.pdf
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Marc: |
LEADER 04427naa a2200829 a 4500 001 2031648 005 2022-05-26 008 2015 bl uuuu u00u1 u #d 024 7 $a10.5194/acpd-15-11599-2015$2DOI 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. 700 1 $aARAUJO, A. 700 1 $aARTAXO, P. 700 1 $aBARBOSA, C. G. G. 700 1 $aBARBOSA, H. M. J. 700 1 $aBRITO, J. 700 1 $aCARBONE, S. 700 1 $aCHI, X. 700 1 $aCINTRA, B. B. L. 700 1 $aSILVA, N. F. da 700 1 $aDIAS, N. L. 700 1 $aDIAS-JÚNIOR, C. Q. 700 1 $aDITAS, F. 700 1 $aDITZ, R. 700 1 $aGODOI, A. F. L. 700 1 $aGODOI, R. H. M. 700 1 $aHEIMANN, M. 700 1 $aHOFFMANN, T. 700 1 $aKESSELMEIER, J. 700 1 $aKÖNEMANN, T. 700 1 $aKRÜGER, M. L. 700 1 $aLAVRIC, J. V. 700 1 $aMANZI, A. O. 700 1 $aMORAN-ZULOAGA, D. 700 1 $aNÖLSCHER, A. C. 700 1 $aNOGUEIRA, D. S. 700 1 $aPIEDADE, M. T. F. 700 1 $aPÖHLKER, C. 700 1 $aPÖSCHL, U. 700 1 $aRIZZO, L. V. 700 1 $aRO, C.-U. 700 1 $aRUCKTESCHLER, N. 700 1 $aSÁ, L. D. A. 700 1 $aSÁ, M. D. O. 700 1 $aSALES, C. B. 700 1 $aSANTOS, R. M. N. dos 700 1 $aSATURNO, J. 700 1 $aSCHÖNGART, J. 700 1 $aSÖRGEL, M. 700 1 $aSOUZA, C. M. de 700 1 $aSOUZA, R. A. F. de 700 1 $aSU, H. 700 1 $aTARGHETTA, N. 700 1 $aTÓTA, J. 700 1 $aTREBS, I. 700 1 $aTRUMBORE, S. 700 1 $aEIJCK, A. van 700 1 $aWALTER, D. 700 1 $aWANG, Z. 700 1 $aWEBER, B. 700 1 $aWILLIAMS, J. 700 1 $aWINDERLICH, J. 700 1 $aWITTMANN, F. 700 1 $aWOLFF, S. 700 1 $aYÁÑEZ-SERRANO, A. M. 773 $tAtmospheric Chemistry and Physics Discuss$gv. 15, n. 18, p. 11599-11726, 2015.
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