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Registro Completo |
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Biblioteca(s): |
Embrapa Florestas. |
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Data corrente: |
13/01/2009 |
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Data da última atualização: |
08/07/2010 |
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Autoria: |
NÓBREGA, R. S. A.; PAULA, A. M. de; VILAS BOAS, R. C.; NÓBREGA, J. C. A.; MOREIRA, F. M. de S. |
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Título: |
Parâmetros morfológicos de mudas de Sesbania virgata (Caz.) Pers e de Anadenanthera peregrina (L.) cultivadas em substrato fertilizado com composto de lixo urbano. |
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Ano de publicação: |
2008 |
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Fonte/Imprenta: |
Revista Árvore, Viçosa, v. 32, n. 3, p. 587-597, maio/jun. 2008. |
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Idioma: |
Português |
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Conteúdo: |
Objetivou-se avaliar o efeito do composto de lixo urbano nos parâmetros morfológicos de mudas de sesbânia e de angico. Os substratos de cultivo tiveram as seguintes proporções de composto e de amostras de subsolo de Neossolo Quartzarênico ou de Latossolo Vermelho-Amarelo (%): 0:100; 20:80; 40:60; 60:40 e 80:20, sem a utilização de fertilização mineral. As sementes de sesbânia foram inoculadas com a estirpe recomendada BR 5401. Os parâmetros morfológicos das mudas de sesbânia e angico, suas relações e índice de qualidade de Dickson (IQD) foram determinados aos 56 e 120 dias após a semeadura, respectivamente para cada espécie. Os efeitos dos substratos nos parâmetros morfológicos das mudas de sesbânia e angico variaram de acordo com as proporções do substrato. Para o angico, a adição do composto proporcionou aumento na altura da parte aérea, razão entre massa seca de parte aérea por massa seca de raiz e IQD. Para sesbânia, a adição do composto de lixo ao substrato proporcionou aumento na altura da parte aérea, diâmetro do coleto, massa seca de raiz, da parte aérea e total, razão entre massa seca da parte aérea por massa seca de raiz, IQD e número de nódulos. A obtenção de máxima produção de matéria seca total, diâmetro do coleto e IQD foi de 57:43, sendo, portanto, esta a proporção composta de lixo:solo recomendada para a produção de mudas de sesbânia. |
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Palavras-Chave: |
Leguminosas; Reciclagem de resíduos; Terra de subsolo. |
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Thesagro: |
Adubação; Tubete. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 02172naa a2200229 a 4500
001 1315306
005 2010-07-08
008 2008 bl uuuu u00u1 u #d
100 1 $aNÓBREGA, R. S. A.
245 $aParâmetros morfológicos de mudas de Sesbania virgata (Caz.) Pers e de Anadenanthera peregrina (L.) cultivadas em substrato fertilizado com composto de lixo urbano.
260 $c2008
520 $aObjetivou-se avaliar o efeito do composto de lixo urbano nos parâmetros morfológicos de mudas de sesbânia e de angico. Os substratos de cultivo tiveram as seguintes proporções de composto e de amostras de subsolo de Neossolo Quartzarênico ou de Latossolo Vermelho-Amarelo (%): 0:100; 20:80; 40:60; 60:40 e 80:20, sem a utilização de fertilização mineral. As sementes de sesbânia foram inoculadas com a estirpe recomendada BR 5401. Os parâmetros morfológicos das mudas de sesbânia e angico, suas relações e índice de qualidade de Dickson (IQD) foram determinados aos 56 e 120 dias após a semeadura, respectivamente para cada espécie. Os efeitos dos substratos nos parâmetros morfológicos das mudas de sesbânia e angico variaram de acordo com as proporções do substrato. Para o angico, a adição do composto proporcionou aumento na altura da parte aérea, razão entre massa seca de parte aérea por massa seca de raiz e IQD. Para sesbânia, a adição do composto de lixo ao substrato proporcionou aumento na altura da parte aérea, diâmetro do coleto, massa seca de raiz, da parte aérea e total, razão entre massa seca da parte aérea por massa seca de raiz, IQD e número de nódulos. A obtenção de máxima produção de matéria seca total, diâmetro do coleto e IQD foi de 57:43, sendo, portanto, esta a proporção composta de lixo:solo recomendada para a produção de mudas de sesbânia.
650 $aAdubação
650 $aTubete
653 $aLeguminosas
653 $aReciclagem de resíduos
653 $aTerra de subsolo
700 1 $aPAULA, A. M. de
700 1 $aVILAS BOAS, R. C.
700 1 $aNÓBREGA, J. C. A.
700 1 $aMOREIRA, F. M. de S.
773 $tRevista Árvore, Viçosa$gv. 32, n. 3, p. 587-597, maio/jun. 2008.
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Registro original: |
Embrapa Florestas (CNPF) |
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Registro Completo
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Biblioteca(s): |
Embrapa Amazônia Oriental. |
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Data corrente: |
09/12/2016 |
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Data da última atualização: |
19/05/2022 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
WENDISCH, M.; PÖSCHL, U.; ANDREAE, M. O.; MACHADO, L. A. T.; ALBRECHT, R.; SCHLAGER, H.; ROSENFELD, D.; MARTIN, S. T.; ABDELMONEM, A.; AFCHINE, A.; ARAUJO, A. C.; ARTAXO, P.; AUFMHOFF, H.; BARBOSA, H. M. J.; BORRMANN, S.; BRAGA, R.; BUCHHOLZ, B.; CECCHINI, M. A.; COSTA, A.; CURTIUS, J.; DOLLNER, M.; DORF, M.; DREILING, V.; EBERT, V.; EHRLICH, A.; EWALD, F.; FISCH, G.; FIX, A.; FRANK, F.; FÜTTERER, D.; HECKL, C.; HEIDELBERG, F.; HÜNEKE, T.; JÄKEL, E.; JÄRVINEN, E.; JURKAT, T.; KANTER, S.; KÄSTNER, U.; KENNTNER, M.; KESSEKMEIER, J.; KLIMACH, T.; KNECHT, M.; KOHL, R.; KÖLLING, T.; KRÄMER, M.; KRÜGER, M.; KRISNA, T. C.; LAVRIC, J. V.; LONGO, K.; MAHNKE, C.; MANZI, A. O.; MAYER, B.; MERTES, S.; MINIKIN, A.; MOLLEKER, S.; MÜNCH, S.; NILIUS, B.; PFEILSTICKER, K.; PÖHLKER, C.; ROIGER, A.; ROSE, D.; ROSENOW, D.; SAUER, D.; SCHNAITER, M.; SCHNEIDER, J.; SCHULZ, C.; SOUZA, R. A. F. de; SPANU, A.; STOCK, P.; VILA, D.; VOIGT, C.; WALSER, A.; WALTER, D.; WEIGEL, R.; WEINZIERL, B.; WERNER, F.; YAMASOE, M. A.; ZIEREIS, H.; ZINNER, T.; ZÖGER, M. |
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Afiliação: |
Manfred Wendisch, Universität Leipzig; Ulrich Pöschl, Max Planck Institute for Chemistry; Meinrat O. Andreae, Max Planck Institute for Chemistry; Luiz A. T. Machado, INPE; Rachel Albrecht, USP; Hans Schlager, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Daniel Rosenfeld, The Hebrew University of Jerusalem; Scot T. Martin, Harvard University; Ahmed Abdelmonem, Karlsruhe Institute of Technology; Armin Afchine, Forschungszentrum Jülich (FZJ); ALESSANDRO CARIOCA DE ARAUJO, CPATU; Paulo Artaxo, USP; Heinfried Aufmhoff, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Henrique M. J. Barbosa, USP; Stephan Borrmann, Johannes Gutenberg-Universität Mainz; Ramon Braga, INPE; Bernhard Buchholz, Physikalisch-Technische Bundesanstalt; Micael Amore Cecchini, INPE; ANJA COSTA, Forschungszentrum Jülich (FZJ); Joachim Curtius, Universität Frankfurt; Maximilian Dollner, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Marcel Dorf, Max Planck Institute for Chemistry; Volker Dreiling, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Volker Ebert, Physikalisch-Technische Bundesanstalt; André Ehrlich, Universität Leipzig; Florian Ewald, Ludwig-Maximilians-Universität; Gilberto Fisch, Instituto de Aeronaútica e Espaço; Andreas Fix, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Fabian Frank, Universität Frankfurt; Daniel Fütterer, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Christopher Heckl, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Fabian Heidelberg, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Tilman Hüneke, Universität Heidelberg; Evelyn Jäkel, Universität Leipzig; Emma Järvinen, Karlsruhe Institute of Technology; Tina Jurkat, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Sandra Kanter, Universität Leipzig; Udo Kästner, Leibniz-Institut für Troposphärenforschung (TROPOS); Mareike Kenntner, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Jürgen Kesselmeier, Max Planck Institute for Chemistry; Thomas Klimach, Max Planck Institute for Chemistry; Matthias Knecht, Universität Heidelberg; Rebecca Kohl, Universität Frankfurt; Tobias Kölling, Ludwig-Maximilians-Universität; Martina Krämer, Forschungszentrum Jülich (FZJ); Mira Krüger, Max Planck Institute for Chemistry; Trismono Candra Krisna, Universität Leipzig; Jost V. Lavric, Max Planck Institute for Biogeochemistry; Karla Longo, INPE; Christoph Mahnke, Institut für Physik der Atmosphäre; Antonio O. Manzi, INPA; Bernhard Mayer, Ludwig-Maximilians-Universität; Stephan Mertes, Leibniz-Institut für Troposphärenforschung (TROPOS); Andreas Minikin, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Sergej Molleker, Johannes Gutenberg-Universität Mainz; Steffen Münch, Universität Frankfurt; Björn Nillius, Max Planck Institute for Chemistry; Klaus Pfeilsticker, Universität Heidelberg; Christopher Pöhlker, Max Planck Institute for Chemistry; Anke Roiger, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Diana Rose, Universität Frankfurt; Dagmar Rosenow, Universität Leipzig; Daniel Sauer, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Martin Schnaiter, Karlsruhe Institute of Technology; Johannes Schneider, Max Planck Institute for Chemistry; Christiane Schulz, Max Planck Institute for Chemistry; Rodrigo A. F. de Souza, UEAM; Antonio Spanu, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Paul Stock, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Daniel Vila, INPE; Christiane Voigt, Johannes Gutenberg-Universität Mainz; Adrian Walser, Deutsches Zentrum für Luft- und Raumfahrt (DLR); David Walter, Max Planck Institute for Chemistry; Ralf Weigel, Johannes Gutenberg-Universität Mainz; Bernadett Weinzierl, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Frank Werner, Universität Leipzig; Marcia A. Yamasoe, USP; Helmut Ziereis, Deutsches Zentrum für Luft- und Raumfahrt (DLR); Tobias Zinner, Ludwig-Maximilians-Universität; Martin Zöger, Deutsches Zentrum für Luft- und Raumfahrt (DLR). |
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Título: |
Acridicon-Chuva campaign: studying tropical deep convective clouds and precipitation over Amazonia using the New German research aircraft HALO. |
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Ano de publicação: |
2016 |
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Fonte/Imprenta: |
Bulletin of the American Meteorological Society, v. 97, n. 10, p. 1885-1908, Oct. 2016. |
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DOI: |
http://dx.doi.org/10.1175/BAMS-D-14-00255.1 |
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Idioma: |
Inglês |
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Conteúdo: |
Between 1 September and 4 October 2014, a combined airborne and ground-based measurement campaign was conducted to study tropical deep convective clouds over the Brazilian Amazon rain forest. The new German research aircraft, High Altitude and Long Range Research Aircraft (HALO), a modified Gulfstream G550, and extensive ground-based instrumentation were deployed in and near Manaus (State of Amazonas). The campaign was part of the German?Brazilian Aerosol, Cloud, Precipitation, and Radiation Interactions and Dynamics of Convective Cloud Systems?Cloud Processes of the Main Precipitation Systems in Brazil: A Contribution to Cloud Resolving Modeling and to the GPM (Global Precipitation Measurement) (ACRIDICON? CHUVA) venture to quantify aerosol?cloud?precipitation interactions and their thermodynamic, dynamic, and radiative effects by in situ and remote sensing measurements over Amazonia. The ACRIDICON?CHUVA field observations were carried out in cooperation with the second intensive operating period of Green Ocean Amazon 2014/15 (GoAmazon2014/5). In this paper we focus on the airborne data measured on HALO, which was equipped with about 30 in situ and remote sensing instruments for meteorological, trace gas, aerosol, cloud, precipitation, and spectral solar radiation measurements. Fourteen research flights with a total duration of 96 flight hours were performed. Five scientific topics were pursued: 1) cloud vertical evolution and life cycle (cloud profiling), 2) cloud processing of aerosol particles and trace gases (inflow and outflow), 3) satellite and radar validation (cloud products), 4) vertical transport and mixing (tracer experiment), and 5) cloud formation over forested/deforested areas. Data were collected in near-pristine atmospheric conditions and in environments polluted by biomass burning and urban emissions. The paper presents a general introduction of the ACRIDICON? CHUVA campaign (motivation and addressed research topics) and of HALO with its extensive instrument package, as well as a presentation of a few selected measurement results acquired during the flights for some selected scientific topics. MenosBetween 1 September and 4 October 2014, a combined airborne and ground-based measurement campaign was conducted to study tropical deep convective clouds over the Brazilian Amazon rain forest. The new German research aircraft, High Altitude and Long Range Research Aircraft (HALO), a modified Gulfstream G550, and extensive ground-based instrumentation were deployed in and near Manaus (State of Amazonas). The campaign was part of the German?Brazilian Aerosol, Cloud, Precipitation, and Radiation Interactions and Dynamics of Convective Cloud Systems?Cloud Processes of the Main Precipitation Systems in Brazil: A Contribution to Cloud Resolving Modeling and to the GPM (Global Precipitation Measurement) (ACRIDICON? CHUVA) venture to quantify aerosol?cloud?precipitation interactions and their thermodynamic, dynamic, and radiative effects by in situ and remote sensing measurements over Amazonia. The ACRIDICON?CHUVA field observations were carried out in cooperation with the second intensive operating period of Green Ocean Amazon 2014/15 (GoAmazon2014/5). In this paper we focus on the airborne data measured on HALO, which was equipped with about 30 in situ and remote sensing instruments for meteorological, trace gas, aerosol, cloud, precipitation, and spectral solar radiation measurements. Fourteen research flights with a total duration of 96 flight hours were performed. Five scientific topics were pursued: 1) cloud vertical evolution and life cycle (cloud profiling), 2) cloud processi... Mostrar Tudo |
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Palavras-Chave: |
Precipitação. |
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Thesagro: |
Chuva; Medição; Nuvem. |
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Thesaurus NAL: |
Amazonia. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 05044naa a2201141 a 4500
001 2058326
005 2022-05-19
008 2016 bl uuuu u00u1 u #d
024 7 $ahttp://dx.doi.org/10.1175/BAMS-D-14-00255.1$2DOI
100 1 $aWENDISCH, M.
245 $aAcridicon-Chuva campaign$bstudying tropical deep convective clouds and precipitation over Amazonia using the New German research aircraft HALO.$h[electronic resource]
260 $c2016
520 $aBetween 1 September and 4 October 2014, a combined airborne and ground-based measurement campaign was conducted to study tropical deep convective clouds over the Brazilian Amazon rain forest. The new German research aircraft, High Altitude and Long Range Research Aircraft (HALO), a modified Gulfstream G550, and extensive ground-based instrumentation were deployed in and near Manaus (State of Amazonas). The campaign was part of the German?Brazilian Aerosol, Cloud, Precipitation, and Radiation Interactions and Dynamics of Convective Cloud Systems?Cloud Processes of the Main Precipitation Systems in Brazil: A Contribution to Cloud Resolving Modeling and to the GPM (Global Precipitation Measurement) (ACRIDICON? CHUVA) venture to quantify aerosol?cloud?precipitation interactions and their thermodynamic, dynamic, and radiative effects by in situ and remote sensing measurements over Amazonia. The ACRIDICON?CHUVA field observations were carried out in cooperation with the second intensive operating period of Green Ocean Amazon 2014/15 (GoAmazon2014/5). In this paper we focus on the airborne data measured on HALO, which was equipped with about 30 in situ and remote sensing instruments for meteorological, trace gas, aerosol, cloud, precipitation, and spectral solar radiation measurements. Fourteen research flights with a total duration of 96 flight hours were performed. Five scientific topics were pursued: 1) cloud vertical evolution and life cycle (cloud profiling), 2) cloud processing of aerosol particles and trace gases (inflow and outflow), 3) satellite and radar validation (cloud products), 4) vertical transport and mixing (tracer experiment), and 5) cloud formation over forested/deforested areas. Data were collected in near-pristine atmospheric conditions and in environments polluted by biomass burning and urban emissions. The paper presents a general introduction of the ACRIDICON? CHUVA campaign (motivation and addressed research topics) and of HALO with its extensive instrument package, as well as a presentation of a few selected measurement results acquired during the flights for some selected scientific topics.
650 $aAmazonia
650 $aChuva
650 $aMedição
650 $aNuvem
653 $aPrecipitação
700 1 $aPÖSCHL, U.
700 1 $aANDREAE, M. O.
700 1 $aMACHADO, L. A. T.
700 1 $aALBRECHT, R.
700 1 $aSCHLAGER, H.
700 1 $aROSENFELD, D.
700 1 $aMARTIN, S. T.
700 1 $aABDELMONEM, A.
700 1 $aAFCHINE, A.
700 1 $aARAUJO, A. C.
700 1 $aARTAXO, P.
700 1 $aAUFMHOFF, H.
700 1 $aBARBOSA, H. M. J.
700 1 $aBORRMANN, S.
700 1 $aBRAGA, R.
700 1 $aBUCHHOLZ, B.
700 1 $aCECCHINI, M. A.
700 1 $aCOSTA, A.
700 1 $aCURTIUS, J.
700 1 $aDOLLNER, M.
700 1 $aDORF, M.
700 1 $aDREILING, V.
700 1 $aEBERT, V.
700 1 $aEHRLICH, A.
700 1 $aEWALD, F.
700 1 $aFISCH, G.
700 1 $aFIX, A.
700 1 $aFRANK, F.
700 1 $aFÜTTERER, D.
700 1 $aHECKL, C.
700 1 $aHEIDELBERG, F.
700 1 $aHÜNEKE, T.
700 1 $aJÄKEL, E.
700 1 $aJÄRVINEN, E.
700 1 $aJURKAT, T.
700 1 $aKANTER, S.
700 1 $aKÄSTNER, U.
700 1 $aKENNTNER, M.
700 1 $aKESSEKMEIER, J.
700 1 $aKLIMACH, T.
700 1 $aKNECHT, M.
700 1 $aKOHL, R.
700 1 $aKÖLLING, T.
700 1 $aKRÄMER, M.
700 1 $aKRÜGER, M.
700 1 $aKRISNA, T. C.
700 1 $aLAVRIC, J. V.
700 1 $aLONGO, K.
700 1 $aMAHNKE, C.
700 1 $aMANZI, A. O.
700 1 $aMAYER, B.
700 1 $aMERTES, S.
700 1 $aMINIKIN, A.
700 1 $aMOLLEKER, S.
700 1 $aMÜNCH, S.
700 1 $aNILIUS, B.
700 1 $aPFEILSTICKER, K.
700 1 $aPÖHLKER, C.
700 1 $aROIGER, A.
700 1 $aROSE, D.
700 1 $aROSENOW, D.
700 1 $aSAUER, D.
700 1 $aSCHNAITER, M.
700 1 $aSCHNEIDER, J.
700 1 $aSCHULZ, C.
700 1 $aSOUZA, R. A. F. de
700 1 $aSPANU, A.
700 1 $aSTOCK, P.
700 1 $aVILA, D.
700 1 $aVOIGT, C.
700 1 $aWALSER, A.
700 1 $aWALTER, D.
700 1 $aWEIGEL, R.
700 1 $aWEINZIERL, B.
700 1 $aWERNER, F.
700 1 $aYAMASOE, M. A.
700 1 $aZIEREIS, H.
700 1 $aZINNER, T.
700 1 $aZÖGER, M.
773 $tBulletin of the American Meteorological Society$gv. 97, n. 10, p. 1885-1908, Oct. 2016.
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