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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: |
LEADER 04427naa a2200829 a 4500
001 2031648
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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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Registro original: |
Embrapa Amazônia Oriental (CPATU) |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Cerrados. Para informações adicionais entre em contato com cpac.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Cerrados. |
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Data corrente: |
16/10/1996 |
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Data da última atualização: |
16/10/1996 |
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Autoria: |
RESCK, D. V. S. |
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Título: |
Effect of crop residues and liming on soil physical and chemical properties of tropical and temperate soils. |
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Ano de publicação: |
1986 |
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Fonte/Imprenta: |
[s.l.]: Purdue University, 1986. |
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Páginas: |
264p. |
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Idioma: |
Inglês |
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Notas: |
Ph.D. Thesis. |
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Conteúdo: |
Fertilization and liming, as well as the return of crop residues to the soil, are essential to prevent a rapid loss of organic carbon content from cultivated soils. Tropical and Temperate soils will likely respond differently to these amendments. An incubation study was designed to test the effects of corn, soybean, or no residue additons, with or without the addition of lime, on soil physical and chemical properties of two Oxisols (virgin and cultivated) from the Cerrados region of Brazili and a Mollisol and Inceptisol from Indiana. The soil properties measured at 0, 10, 20, 30, 60 and 90 days of incubation included organic carbon, pH, cation exchange capacity (CEC), water-stable aggregation, and water retention at -10, -33, and -100 kPa water potential. Carbon dioxide evolution was measured at short time intervals throughout the 90 days of incubation. The decrease in organic carbon content with time was in the order Inceptisol > Mollisol > Cultivated Oxisol > Virgin oxisol. Microbial activity, as measured by CO2 evolution rates, was almost twice as great in the Temperate soils as in the Tropical soils. The addition of lime and crop residues tended to decrease water retention capacity of the Virgin Oxisol, whereas the no residue treatment was not affected by lime. Lime did not affect water retention for any crops in the Cultivated Oxisol or in the Mollisol. Time of incubation had a positive effect on soil water-stable aggregation. Lime decreased water-stable aggregation in the Virgin Oxisol when to residue... MenosFertilization and liming, as well as the return of crop residues to the soil, are essential to prevent a rapid loss of organic carbon content from cultivated soils. Tropical and Temperate soils will likely respond differently to these amendments. An incubation study was designed to test the effects of corn, soybean, or no residue additons, with or without the addition of lime, on soil physical and chemical properties of two Oxisols (virgin and cultivated) from the Cerrados region of Brazili and a Mollisol and Inceptisol from Indiana. The soil properties measured at 0, 10, 20, 30, 60 and 90 days of incubation included organic carbon, pH, cation exchange capacity (CEC), water-stable aggregation, and water retention at -10, -33, and -100 kPa water potential. Carbon dioxide evolution was measured at short time intervals throughout the 90 days of incubation. The decrease in organic carbon content with time was in the order Inceptisol > Mollisol > Cultivated Oxisol > Virgin oxisol. Microbial activity, as measured by CO2 evolution rates, was almost twice as great in the Temperate soils as in the Tropical soils. The addition of lime and crop residues tended to decrease water retention capacity of the Virgin Oxisol, whereas the no residue treatment was not affected by lime. Lime did not affect water retention for any crops in the Cultivated Oxisol or in the Mollisol. Time of incubation had a positive effect on soil water-stable aggregation. Lime decreased water-stable aggregation in ... Mostrar Tudo |
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Palavras-Chave: |
Cultura agricola; Maize; Regiao Tropical; Soil chemicophysical properties; Tropical zones. |
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Thesagro: |
Calagem; Cambissolo; Cerrado; Glycine Max; Milho; Oxisol; Planossolo; Propriedade Físico-Química; Região Temperada; Resíduo Orgânico; Soja; Solo; Zea Mays. |
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Thesaurus NAL: |
Cambisols; crop residues; Ferralsols; Inceptisols; liming; Mollisols; Planosols; soybeans; temperate zones. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 02702nam a2200457 a 4500
001 1551943
005 1996-10-16
008 1986 bl uuuu m 00u1 u #d
100 1 $aRESCK, D. V. S.
245 $aEffect of crop residues and liming on soil physical and chemical properties of tropical and temperate soils.
260 $a[s.l.]: Purdue University$c1986
300 $a264p.
500 $aPh.D. Thesis.
520 $aFertilization and liming, as well as the return of crop residues to the soil, are essential to prevent a rapid loss of organic carbon content from cultivated soils. Tropical and Temperate soils will likely respond differently to these amendments. An incubation study was designed to test the effects of corn, soybean, or no residue additons, with or without the addition of lime, on soil physical and chemical properties of two Oxisols (virgin and cultivated) from the Cerrados region of Brazili and a Mollisol and Inceptisol from Indiana. The soil properties measured at 0, 10, 20, 30, 60 and 90 days of incubation included organic carbon, pH, cation exchange capacity (CEC), water-stable aggregation, and water retention at -10, -33, and -100 kPa water potential. Carbon dioxide evolution was measured at short time intervals throughout the 90 days of incubation. The decrease in organic carbon content with time was in the order Inceptisol > Mollisol > Cultivated Oxisol > Virgin oxisol. Microbial activity, as measured by CO2 evolution rates, was almost twice as great in the Temperate soils as in the Tropical soils. The addition of lime and crop residues tended to decrease water retention capacity of the Virgin Oxisol, whereas the no residue treatment was not affected by lime. Lime did not affect water retention for any crops in the Cultivated Oxisol or in the Mollisol. Time of incubation had a positive effect on soil water-stable aggregation. Lime decreased water-stable aggregation in the Virgin Oxisol when to residue...
650 $aCambisols
650 $acrop residues
650 $aFerralsols
650 $aInceptisols
650 $aliming
650 $aMollisols
650 $aPlanosols
650 $asoybeans
650 $atemperate zones
650 $aCalagem
650 $aCambissolo
650 $aCerrado
650 $aGlycine Max
650 $aMilho
650 $aOxisol
650 $aPlanossolo
650 $aPropriedade Físico-Química
650 $aRegião Temperada
650 $aResíduo Orgânico
650 $aSoja
650 $aSolo
650 $aZea Mays
653 $aCultura agricola
653 $aMaize
653 $aRegiao Tropical
653 $aSoil chemicophysical properties
653 $aTropical zones
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