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Registro Completo |
Biblioteca(s): |
Embrapa Caprinos e Ovinos. |
Data corrente: |
17/05/2011 |
Data da última atualização: |
25/09/2019 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
CÂNDIDO, M, J. D.; SILVA, R. G. da; NEIVA, J. N. M.; FACO, O.; BENEVIDES, Y. I.; FARIAS, S. F. |
Afiliação: |
Magno José Duarte Cândido, Universidade Federal do Ceará-UFC, Fortaleza-CE.; Rodrigo Gregório da Silva, Faculdade Tecnológica CENTEC, Quixeramobim - CE.; José Neuman Miranda Neiva, Universidade Federal do Tocantins - UFT, Campus de Araguaína - TO.; OLIVARDO FACO, CNPC; Yuri Ida Benevides, Graduanda, UFC, Fortaleza, CE.; Sarah Feitosa Farias, Graduada, UFC, Fortaleza, CE. |
Título: |
Fluxo de biomassa em capim-tanzânia pastejado por ovinos sob três períodos de descanso. |
Ano de publicação: |
2006 |
Fonte/Imprenta: |
Revista Brasileira de Zootecnia, v. 35, n. 6, p. 2234-2242, 2006. |
DOI: |
http://dx.doi.org/10.1590/S1516-35982006000800006 |
Idioma: |
Português |
Conteúdo: |
Resumo: Avaliou-se o fluxo de biomassa em Panicum maximum cv. Tanzânia pastejado por ovinos com três períodos de descanso (PD), definidos pela expansão de 1,5; 2,5 e 3,5 novas folhas por perfilho, em um delineamento inteiramente casualizado, com duas repetições (piquetes). Estimaram-se as taxas de alongamento de lâmina foliar total (TAlF), de senescência de lâminas foliares remanescentes do pastejo anterior (TSFA), de senescência das novas folhas formadas no PD (TSFP) e de senescência total (TSFT=TSFA+TSFP), a taxa de alongamento das hastes (TAlH), a razão entre as TAlF das folhas 1 e 2 (razão TAlF1/TAlF2), a densidade populacional de perfilhos (DPP), o filocrono e as taxas de crescimento (TCC) e de acúmulo (TAC) da cultura. A razão TAlF1/2 não foi afetada pelos PD, mas reduziu ao longo dos ciclos na pastagem sob PD 3,5. A TAlF não foi afetada pelos PD. A TAlH, a TSFA e a TSFT na pastagem sob PD 1,5 foram menores que nas demais. Houve TSFP somente na pastagem sob PD 3,5. O filocrono da pastagem sob PD 1,5 foi superior ao observado nas demais. A densidade populacional de perfilhos (DPP) da pastagem sob o PD 2,5 foi similar à verificada na pastagem sob PD 1,5 e superior à verificada sob PD 3,5. Houve redução na DPP ao longo dos ciclos na pastagem sob PD 3,5. As taxas de crescimento (TCC) e de acúmulo (TAC) foram superiores na pastagem sob PD 2,5. O prolongamento do PD elevou as TAlH e TSFT e reduziu a DPP e a TAC. Portanto, o PD do capim-tanzânia pastejado por ovinos não deve exceder o tempo necessário à expansão de 2,5 novas folhas por perfilho. [Biomass flow in tanzaniagrass pasture under three resting periods grazed by sheep]. Abstract: The biomass flow in Panicum maximum cv. Tanzânia pasture grazed by sheep under three resting periods (PD), defined by the expansion of 1.5; 2.5 and 3.5 new leaves per tiller (1.5F; 2.5F and 3.5F, respectively) was evaluated in a randomized completely design with two replicates (paddocks). It was determined the leaf elongation rate (TAlF), the residual leaf senescence rate (TSFA), the post-grazing leaf senescence rate (TSFP) and the total leaf senescence rate (TSFT), the stem elongation rate (TAlH), the TAlF of leaves 1 and 2 ratio (TALF1/2), the tiller population density (DPP), the phylochron and the crop growth (TCC) and accumulation (TAC) rates. The TAlF1/2 ratio was not affected by the PD, however, it decreased over the cycles at the 3.5F PD pasture. The TAlF was not affected by the PD. The TAlH was inferior at the 1.5F PD pasture, as well as the TSFA and the TSFT. There was TSFP only at the 3.5F PD pasture. The phylochron of the 1.5F PD pasture was superior to the others. The DPP of the 2.5F PD pasture was similar to that of the 1.5F PD pasture, and it was superior to the 3.5F PD pasture. There was reduction of the DPP following the cycles at the 3.5F PD pasture. The TCC and the TAC of the 2.5F PD pasture were superior than the others. The extension of the PD raised the TAlH and the TSFT and reduced the DPP and the TAC. As a conclusion, the resting period should not exceed the time necessary to the expansion of 2.5 leaves on the tiller for tanzaniagrass pastures grazed by sheep. MenosResumo: Avaliou-se o fluxo de biomassa em Panicum maximum cv. Tanzânia pastejado por ovinos com três períodos de descanso (PD), definidos pela expansão de 1,5; 2,5 e 3,5 novas folhas por perfilho, em um delineamento inteiramente casualizado, com duas repetições (piquetes). Estimaram-se as taxas de alongamento de lâmina foliar total (TAlF), de senescência de lâminas foliares remanescentes do pastejo anterior (TSFA), de senescência das novas folhas formadas no PD (TSFP) e de senescência total (TSFT=TSFA+TSFP), a taxa de alongamento das hastes (TAlH), a razão entre as TAlF das folhas 1 e 2 (razão TAlF1/TAlF2), a densidade populacional de perfilhos (DPP), o filocrono e as taxas de crescimento (TCC) e de acúmulo (TAC) da cultura. A razão TAlF1/2 não foi afetada pelos PD, mas reduziu ao longo dos ciclos na pastagem sob PD 3,5. A TAlF não foi afetada pelos PD. A TAlH, a TSFA e a TSFT na pastagem sob PD 1,5 foram menores que nas demais. Houve TSFP somente na pastagem sob PD 3,5. O filocrono da pastagem sob PD 1,5 foi superior ao observado nas demais. A densidade populacional de perfilhos (DPP) da pastagem sob o PD 2,5 foi similar à verificada na pastagem sob PD 1,5 e superior à verificada sob PD 3,5. Houve redução na DPP ao longo dos ciclos na pastagem sob PD 3,5. As taxas de crescimento (TCC) e de acúmulo (TAC) foram superiores na pastagem sob PD 2,5. O prolongamento do PD elevou as TAlH e TSFT e reduziu a DPP e a TAC. Portanto, o PD do capim-tanzânia pastejado por ovinos não deve ... Mostrar Tudo |
Palavras-Chave: |
Herbage accumulation rate; Leaf elongation rate; Leaf senescence rate; Lotação rotativa; Rotational stocking; Stem elongation rate; Variedade Tanzânia. |
Thesagro: |
Biomassa; Caule; Ovino; Panicum Maximum; Pastagem; Pastejo. |
Thesaurus Nal: |
Sheep. |
Categoria do assunto: |
L Ciência Animal e Produtos de Origem Animal |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/34773/1/API-Fluxo-de-biomassa-em.pdf
|
Marc: |
LEADER 04263naa a2200361 a 4500 001 1888734 005 2019-09-25 008 2006 bl uuuu u00u1 u #d 024 7 $ahttp://dx.doi.org/10.1590/S1516-35982006000800006$2DOI 100 1 $aCÂNDIDO, M, J. D. 245 $aFluxo de biomassa em capim-tanzânia pastejado por ovinos sob três períodos de descanso.$h[electronic resource] 260 $c2006 520 $aResumo: Avaliou-se o fluxo de biomassa em Panicum maximum cv. Tanzânia pastejado por ovinos com três períodos de descanso (PD), definidos pela expansão de 1,5; 2,5 e 3,5 novas folhas por perfilho, em um delineamento inteiramente casualizado, com duas repetições (piquetes). Estimaram-se as taxas de alongamento de lâmina foliar total (TAlF), de senescência de lâminas foliares remanescentes do pastejo anterior (TSFA), de senescência das novas folhas formadas no PD (TSFP) e de senescência total (TSFT=TSFA+TSFP), a taxa de alongamento das hastes (TAlH), a razão entre as TAlF das folhas 1 e 2 (razão TAlF1/TAlF2), a densidade populacional de perfilhos (DPP), o filocrono e as taxas de crescimento (TCC) e de acúmulo (TAC) da cultura. A razão TAlF1/2 não foi afetada pelos PD, mas reduziu ao longo dos ciclos na pastagem sob PD 3,5. A TAlF não foi afetada pelos PD. A TAlH, a TSFA e a TSFT na pastagem sob PD 1,5 foram menores que nas demais. Houve TSFP somente na pastagem sob PD 3,5. O filocrono da pastagem sob PD 1,5 foi superior ao observado nas demais. A densidade populacional de perfilhos (DPP) da pastagem sob o PD 2,5 foi similar à verificada na pastagem sob PD 1,5 e superior à verificada sob PD 3,5. Houve redução na DPP ao longo dos ciclos na pastagem sob PD 3,5. As taxas de crescimento (TCC) e de acúmulo (TAC) foram superiores na pastagem sob PD 2,5. O prolongamento do PD elevou as TAlH e TSFT e reduziu a DPP e a TAC. Portanto, o PD do capim-tanzânia pastejado por ovinos não deve exceder o tempo necessário à expansão de 2,5 novas folhas por perfilho. [Biomass flow in tanzaniagrass pasture under three resting periods grazed by sheep]. Abstract: The biomass flow in Panicum maximum cv. Tanzânia pasture grazed by sheep under three resting periods (PD), defined by the expansion of 1.5; 2.5 and 3.5 new leaves per tiller (1.5F; 2.5F and 3.5F, respectively) was evaluated in a randomized completely design with two replicates (paddocks). It was determined the leaf elongation rate (TAlF), the residual leaf senescence rate (TSFA), the post-grazing leaf senescence rate (TSFP) and the total leaf senescence rate (TSFT), the stem elongation rate (TAlH), the TAlF of leaves 1 and 2 ratio (TALF1/2), the tiller population density (DPP), the phylochron and the crop growth (TCC) and accumulation (TAC) rates. The TAlF1/2 ratio was not affected by the PD, however, it decreased over the cycles at the 3.5F PD pasture. The TAlF was not affected by the PD. The TAlH was inferior at the 1.5F PD pasture, as well as the TSFA and the TSFT. There was TSFP only at the 3.5F PD pasture. The phylochron of the 1.5F PD pasture was superior to the others. The DPP of the 2.5F PD pasture was similar to that of the 1.5F PD pasture, and it was superior to the 3.5F PD pasture. There was reduction of the DPP following the cycles at the 3.5F PD pasture. The TCC and the TAC of the 2.5F PD pasture were superior than the others. The extension of the PD raised the TAlH and the TSFT and reduced the DPP and the TAC. As a conclusion, the resting period should not exceed the time necessary to the expansion of 2.5 leaves on the tiller for tanzaniagrass pastures grazed by sheep. 650 $aSheep 650 $aBiomassa 650 $aCaule 650 $aOvino 650 $aPanicum Maximum 650 $aPastagem 650 $aPastejo 653 $aHerbage accumulation rate 653 $aLeaf elongation rate 653 $aLeaf senescence rate 653 $aLotação rotativa 653 $aRotational stocking 653 $aStem elongation rate 653 $aVariedade Tanzânia 700 1 $aSILVA, R. G. da 700 1 $aNEIVA, J. N. M. 700 1 $aFACO, O. 700 1 $aBENEVIDES, Y. I. 700 1 $aFARIAS, S. F. 773 $tRevista Brasileira de Zootecnia$gv. 35, n. 6, p. 2234-2242, 2006.
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Registro original: |
Embrapa Caprinos e Ovinos (CNPC) |
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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
|
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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