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| Registros recuperados : 19 | |
| 12. |  | SENA, J. M. A. de; MIRANDA, R. DE q.; GALVÍNCIO, J. D.; ALBERTON, B. de C.; MORELLATO, L. P. C.; MOURA, M. S. B. de. Associação clima x monitoramento fenológico da Caatinga por meio de câmeras digitais: aspectos metodológicos. In: JORNADA DE INICIAÇÃO CIENTÍFICA DA EMBRAPA SEMIÁRIDO, 11., 2016, Petrolina. Anais... Petrolina: Embrapa Semiárido, 2016. p. 163-169. (Embrapa Semiárido. Documentos, 271).| Biblioteca(s): Embrapa Semiárido. |
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| 14. | | ALBERTON, B.; MARTIN, T. C. M.; ROCHA, H. R. da; RICHARDSON, A. D.; MOURA, M. S. B. de; TORRES, R. S.; MORELLATO, L. P. C. Relationship between tropical leaf phenology and ecosystem productivity using phenocameras. Frontiers in Environmental Science, v. 11, 1223219, Sept. 2023.| Biblioteca(s): Embrapa Semiárido. |
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| 15. | | RAMOS, D. M.; ANDRADE, J. M.; ALBERTON, B. C.; MOURA, M. S. B. de; DOMINGUES, T. F.; NEVES, N.; LIMA, J. R. S.; SOUZA, R.; SOUZA, E.; SILVA, J. R.; SANTO, M. M. E.; MORELLATO, L. P. C.; CUNHA, J. Multiscale phenology of seasonally dry tropical forests in an aridity gradient. Frontiers in Environmental Sciience, v. 11, 1275844, 2023.| Biblioteca(s): Embrapa Semiárido. |
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| 16. | | MOURA, M. S. B. de; MIRANDA, R. Q.; ALBERTON, B.; MORELLATO, L. P. C.; RODRIGUES, G. D. S.; SOUZA, L. S. B.; GALVINCIO, J. D.; KIILL, L. H. P. Uso de índices RGB para o Bioma Caatinga associados a dados meteorológicos e índices de vegetação: estudos iniciais. In: CONGRESSO BRASILEIRO DE METEOROLOGIA, 18., 2014, Recife. O papel da meteorologia na construção de uma sociedade sustentável. Recife: SBMET, 2014.| Biblioteca(s): Embrapa Semiárido. |
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| 17. | | JARDIM, A. M. da R. F.; MORAIS, J. E. F. de; SOUZA, L. S. B. de; MARIN, F. R.; MOURA, M. S. B. de; MORELLATO, L. P. C.; MONTENEGRO, A. A. de A.; OMETTO, J. P. H. B.; LIMA, J. L. M. P. de; DUBEUX JÚNIOR, J. C. B.; SILVA, T. G. F. da. Sink or carbon source? how the Opuntia cactus agroecosystem interacts in the use of carbon, nutrients and radiation in the Brazilian semi-arid region. Journal of Hydrology, v. 625, 130121, 2023.| Biblioteca(s): Embrapa Semiárido. |
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| 18. | | FERNANDES, G. W.; ARANTES-GARCIA, L.; BARBOS, M.; BARBOS, N. P. U.; BATISTA, E. K. L.; BEIROZ, W.; RESENDE, F. M.; ABRAHÃO, A.; ALMADA, E. D.; ALVES, E.; ALVES, N. J.; ANGRISANO, P.; ARISTA, M.; ARROYO, J.; ARRUDA, A. J.; BAHIA, T. de O.; BRAGA, L.; BRITO, L.; CALLISTO, M.; CAMINHA-PAIVA, D.; CARVALHO, M.; CONCEIÇÃO, A. A.; COSTA, L. N.; CRUZ, A.; CUNHA-BLUM, J.; DAGEVOS, J.; DIAS, B. F. S.; PINTO, V. D.; DIRZO, R.; DOMINGOS, D. Q.; ECHTERNACHT, L.; FERNANDES, S.; FIGUEIRA, J. E. C.; FIORINI, C. F.; GIULIETTI, A. M.; GOMES, A.; GOMES, V. M.; GONTIJO, B.; GOULART, F.; GUERRA, T. J.; JUNQUEIRA, P. A.; LIMA-SANTOS, D.; MARQUES, J.; MEIRA-NETO, J.; MIOLA, D. T. B.; MORELLATO, L. P. C.; NEGREIROS, D.; NEIRE, E.; NEVES, A. C.; NEVES, F. S.; NOVAIS, S.; OKI, Y.; OLIVEIRA, E.; OLIVEIRA, R. S.; PIVARI, M. O.; PONTES JUNIOR, E.; RANIERI, B. D.; RIBAS, R. P.; SCARIOT, A.; ECHAEFER, C. E.; SENA, L.; SILVA, P. G. da; SIQUEIRA, P. R.; SOARES, N. C.; SOARES-FILHO, B.; SOLAR, R.; TABARELLI, M.; VASCONCELLOS, R.; VILELA, E.; SILVEIRA, F. A. O. Biodiversity and ecosystem services in the Campo Rupestre: a road map for the sustainability of the hottest Brazilian biodiversity hotspot. Perspectives in Ecology and Conservation, v. 18, p. 213-222, 2020| Biblioteca(s): Embrapa Recursos Genéticos e Biotecnologia. |
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| 19. | | RAMOS, F. N.; MORTARA, S. R.; MONALISA-FRANCISCO, N.; ELIAS, J. P. C.; MENINI NETO, L.; FREITAS, L.; KERSTEN, R. de A.; AMORIM, A. M.; MATOS, F. B. de; NUNES-FREITAS, A. F.; ALCANTARA, S.; ALEXANDRE, M. H. N.; ALMEIDA-SCABBIA, R. J. de; ALMEIDA, O. J. G. de; ALVES, F. E.; ALVES, R. M. de O.; ALVIM, F. S.; ANDRADE, A. C. S. de; ANDRADE, S. de; AONA, L. Y. S.; ARAUJO. A. C.; ARAÚJO, K. C. T. de; ARIATI, V.; ASSIS, J. C.; AZEVEDO, C. O. de; BARBOSA, B. F.; BARBOSA, D. E. F.; BARBOSA, F. dos R.; BARROS, F. de; BASILIO, G. A.; BATAGHIN, F. A.; BERED, F.; BIANCHI, J. S.; BLUM, C. T.; BOETLER, C. R.; BONNET, A.; BRANCALION, P. H. S.; BREIER, T. B.; BRION, C. de T.; BUZATTO, C. R.; CABRAL, A.; CADORIN, T. J.; CAGLIONI, E.; CANÊZ, L.; CARDOSO, P. H.; CARVALHO, F. S. de; CARVALHO, R. G.; CATHARINO, E. L. M.; CEBALLOS, S. J.; CEREZINI, M. T.; CÉSAR, R. G.; CESTARI, C.; CHAVES, C. J. N.; CITADINE-ZANETTE, V.; COELHO, L. F. M.; COFFANI-NUNES, J. V.; COLARES, R.; COLLETTA, G. D.; CORRÊA, N. de M.; COSTA, A. F. da; COSTA, G. M. da; COSTA, L. M. S.; COSTA, N. G. S.; COUTO, D. R.; CRISTOFOLINI, C.; CRUZ, A. C. R. da; DEL NERI, L. A.; DI PASQUO, M.; DIAS, A. dos S.; DIAS, L. do C. D.; DISLICH, R.; DUARTE, M. C.; FABRICANTE, J. R.; FARACHE, F. H. A.; FARIA, A. P. G. de; FAXINA, C.; FERREIRA, M. T. M.; FISCHER, E.; FONSECA, C. R.; FONTOURA, T.; FRANCISCO, T. M.; FURTADO, S. G.; GALETTI, M.; GALETTI, M.; GARBIN, M. L.; GASPER, A. L. de; GOETZE, M.; GOMES-DA-SILVA, J.; GONÇALVES, M. F. A.; GONZAGA, D. R.; SILVA, A. C. G. e; GUARALDO, A. de C.; GUARINO, E. de S. G.; GUISLON, A. V.; HUDSON, L. B.; JARDIM, J. G.; JUNGBLUTH, P.; KAESER, S. dos S.; KESSOUS, I. M.; KOCH, N. M.; KUNIYOSHI, Y. S.; LABIAK, P. H.; LAPATE, M. E.; SANTOS, A. C. L.; LEAL, R. L. B.; LEITE, F. S.; LEITMAN, P.; LIBONI, A. P.; LIEBSCH, D.; LINGNER, D. V.; LOMBARDI, J. A.; LUCAS, E.; LUZZI, J. dos R.; MAI, P.; MANIA, L. F.; MANTOVANI, W.; MARAGNI, A. G.; MARQUES, M. C. M.; MARQUEZ, G.; MARTINS, C.; MARTINS, L. do N.; MARTINS, P. L. S. S.; MAZZIERO, F. F. F.; MELO, C. de A.; MELO, M. M. F. de; MENDES, A. F.; MESACASA, L.; MORELLATO, L. P. C.; MORENO, V. de S.; MULLER, A.; MURAKAMI, M. M. da S.; CECCONELLO, E.; NARDY, C.; NERVO, M. H.; NEVES, B.; NOGUEIRA, M. G. C.; NONATO, F. R.; OLIVEIRA-FILHO, A. T. de; OLIVEIRA, C. P. L. de; OVERBECK, G. E.; MARCUSSO, G. M.; PACIENCIA, M. L. B.; PADILHA, P.; PADILHA, P. T.; PEREIRA, A. C. A.; PEREIRA, L. C.; PEREIRA, R. A. S.; PINCHEIRA-ULBRICH, J.; PIRES, J. S. R.; PIZO, M. A.; PÔRTO, K. C.; RATTIS, L.; REIS, J. R. de M.; REIS, S. G. dos; ROCHA-PESSÔA, T. C.; ROCHA, C. F. D.; ROCHA, F. S.; RODRIGUES, A. R. P.; RODRIGUES, R. R.; ROGALSKI, J. M.; ROSANELLI, R. L.; ROSSADO, A.; ROSSATTO, D. R.; ROTHER, D. C.; RUIZ-MIRANDA, C. R.; SAITER, F. Z.; SAMPAIO, M. B.; SANTANA, L. D.; SANTOS, J. S. dos; SARTORELLO, R.; SAZIMA, M.; SCHMITT, J. L.; SCHNEIDER, G.; SCHROEDER, B. G.; SEVEGNANI, L.; SILVA JÚNIOR, V. O.; SILVA, F. R. da; SILVA, M. J. da; SILVA, M. P. P.; SILVA, R. G.; SILVA, S. M.; SINGER, R. B.; SIQUEIRA, G.; SOARES, L. E.; SOUSA, H. C. de; SPIELMANN, A.; TONETTI, V. R.; TONIATO, M. T. Z.; ULGUIM, P. S. B.; VAN DEN BERG, C.; VAN DEN BERG, E.; VARASSIN, I. G.; SILVA, I. B. V. da; VIBRANS, A. C.; WAECHTER, J. L.; WEISSENBERG, E. W.; WINDISCH, P. G.; WOLOWSKI, M.; YAÑEZ, A.; YOSHIKAWA, V. N.; ZANDONÁ, L. R.; ZANELLA, C. M.; ZANIN, E. M.; ZAPPI, D. C.; ZIPPARRO, V. B.; ZORZANELLI, J. P. F.; RIBEIRO, M. C. Atlantic epiphytes: a data set of vascular and non-vascular epiphyte plants and lichens from the Atlantic Forest. Ecology, v. 100, n. 2, e02541, 2019. 59 p.| Biblioteca(s): Embrapa Cerrados; Embrapa Clima Temperado; Embrapa Florestas. |
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| Registros recuperados : 19 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Semiárido. |
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Data corrente: |
18/01/2024 |
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Data da última atualização: |
23/01/2024 |
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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: |
JARDIM, A. M. da R. F.; MORAIS, J. E. F. de; SOUZA, L. S. B. de; MARIN, F. R.; MOURA, M. S. B. de; MORELLATO, L. P. C.; MONTENEGRO, A. A. de A.; OMETTO, J. P. H. B.; LIMA, J. L. M. P. de; DUBEUX JÚNIOR, J. C. B.; SILVA, T. G. F. da. |
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Afiliação: |
ALEXANDRE MANIÇOBA DA ROSA FERRAZ JARDIM, UFRPE; JOSÉ EDSON FLORENTINO DE MORAIS, UFRPE, Serra Talhada, PE; LUCIANA SANDRA BASTOS DE SOUZA, UFRPE, Serra Talhada, PE; FABIO RICARDO MARIN, USP; MAGNA SOELMA BESERRA DE MOURA, CPATSA; LEONOR PATRICIA CERDEIRA MORELLATO, UNESP, Rio Claro, SP; ABELARDO ANTÔNIO DE ASSUNÇÃO MONTENEGRO, UFRPE; JEAN PIERRE HENRY BALBAUD OMETTO, INPE; JOÃO L. M. P. DE LIMA, MARE—Marine and Environmental Sciences Centre, ARNET – Aquatic Research Network, Department of Civil Engineering, Faculty of Sciences and Technology; JOSÉ CARLOS BATISTA DUBEUX JÚNIOR, North Florida Research and Education Center, University of Florida; THIERES GEORGE FREIRE DA SILVA, Department of Agricultural Engineering, Federal Rural University of Pernambuco, Serra Talhada, PE. |
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Título: |
Sink or carbon source? how the Opuntia cactus agroecosystem interacts in the use of carbon, nutrients and radiation in the Brazilian semi-arid region. |
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Ano de publicação: |
2023 |
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Fonte/Imprenta: |
Journal of Hydrology, v. 625, 130121, 2023. |
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DOI: |
https://doi.org/10.1016/j.jhydrol.2023.130121 |
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Idioma: |
Inglês |
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Conteúdo: |
Anthropogenic disturbances directly influence environmental processes and increase the concentration of carbon (C) in the atmosphere. Here, we compare the differences in the seasonality of the balance of carbon, energy, and radiation, as well as seek to identify the interrelationships between these environmental variables and their impact on the growth of Opuntia cactus. Data were acquired from an eddy covariance flux tower over a cactus crop agroecosystem (2019–2021) in the Brazilian semi-arid region. In addition, we use plant growth rates, carbon and nutrient stocks, evapotranspiration (ET) and water use efficiency (WUE), and radiation (RUE). We show that the closure of the surface energy balance was 71%, although there are minimal fluxes of available energy lost (29%) by unquantified processes. At all seasons, the highest net ecosystem CO2 exchange (NEE) rate was between 11:00–13:00 (�� 5.75 μmol m�� 2 s�� 1). During the dry and wet-dry season, there was the lowest daily gross primary productivity (GPP) (2.5 μmol m�� 2 s�� 1) and net radiation—Rn (217.97 W m�� 2). Ecosystem respiration was more expressive during the wet season (2.41 μmol m�� 2 s�� 1), and maximum diurnal value of 2.65 μmol m�� 2 s�� 1. Furthermore, the latent heat flux was higher during the wet season (114.68 W m�� 2) and lowered in the dry season (9.39 W m�� 2). The net assimilation rate showed higher values during the dry-wet transition. The dry season presented higher nutrient use efficiency and WUE (14.77 g m�� 2 mm�� 1). The highest ET occurred during the wet season (227 mm), and RUE was 81.48% higher than in the dry season. Overall, the cactus was a potential C sink during the three years of assessment (NEE: �� 377 g C m�� 2 year�� 1; GPP: 881 g C m�� 2 year�� 1). The results help us to understand that most of the Rn energy is used in the sensible heat flux (58% ratio). MenosAnthropogenic disturbances directly influence environmental processes and increase the concentration of carbon (C) in the atmosphere. Here, we compare the differences in the seasonality of the balance of carbon, energy, and radiation, as well as seek to identify the interrelationships between these environmental variables and their impact on the growth of Opuntia cactus. Data were acquired from an eddy covariance flux tower over a cactus crop agroecosystem (2019–2021) in the Brazilian semi-arid region. In addition, we use plant growth rates, carbon and nutrient stocks, evapotranspiration (ET) and water use efficiency (WUE), and radiation (RUE). We show that the closure of the surface energy balance was 71%, although there are minimal fluxes of available energy lost (29%) by unquantified processes. At all seasons, the highest net ecosystem CO2 exchange (NEE) rate was between 11:00–13:00 (�� 5.75 μmol m�� 2 s�� 1). During the dry and wet-dry season, there was the lowest daily gross primary productivity (GPP) (2.5 μmol m�� 2 s�� 1) and net radiation—Rn (217.97 W m�� 2). Ecosystem respiration was more expressive during the wet season (2.41 μmol m�� 2 s�� 1), and maximum diurnal value of 2.65 μmol m�� 2 s�� 1. Furthermore, the latent heat flux was higher during the wet season (114.68 W m�� 2) and lowered in the dry season (9.39 W m�� 2). The net assimilation rate showed higher values during the dry-wet transition. The dry season presented higher nutrient use efficiency and WUE (1... Mostrar Tudo |
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Palavras-Chave: |
Agroecossistema; Cacto de sequeiro; Concentração de carbono; Covariância de redemoinho; Opuntia cactus; Planta CAM; Semiárido; Sumidouro ou fonte de carbono; Troca líquida de CO2. |
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Thesagro: |
Caatinga; Cacto; Carbono; Ecossistema; Evapotranspiração. |
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Thesaurus NAL: |
Evapotranspiration; Opuntia. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/1161040/1/Sink-or-carbon-source-how-the-Opuntia-cactus-agroecosystem-interacts-in-the-use-of-carbon-nutrients-and-radiation-in-the-Brazilian-semi-arid-region.pdf
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Marc: |
LEADER 03353naa a2200445 a 4500
001 2161040
005 2024-01-23
008 2023 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1016/j.jhydrol.2023.130121$2DOI
100 1 $aJARDIM, A. M. da R. F.
245 $aSink or carbon source? how the Opuntia cactus agroecosystem interacts in the use of carbon, nutrients and radiation in the Brazilian semi-arid region.$h[electronic resource]
260 $c2023
520 $aAnthropogenic disturbances directly influence environmental processes and increase the concentration of carbon (C) in the atmosphere. Here, we compare the differences in the seasonality of the balance of carbon, energy, and radiation, as well as seek to identify the interrelationships between these environmental variables and their impact on the growth of Opuntia cactus. Data were acquired from an eddy covariance flux tower over a cactus crop agroecosystem (2019–2021) in the Brazilian semi-arid region. In addition, we use plant growth rates, carbon and nutrient stocks, evapotranspiration (ET) and water use efficiency (WUE), and radiation (RUE). We show that the closure of the surface energy balance was 71%, although there are minimal fluxes of available energy lost (29%) by unquantified processes. At all seasons, the highest net ecosystem CO2 exchange (NEE) rate was between 11:00–13:00 (�� 5.75 μmol m�� 2 s�� 1). During the dry and wet-dry season, there was the lowest daily gross primary productivity (GPP) (2.5 μmol m�� 2 s�� 1) and net radiation—Rn (217.97 W m�� 2). Ecosystem respiration was more expressive during the wet season (2.41 μmol m�� 2 s�� 1), and maximum diurnal value of 2.65 μmol m�� 2 s�� 1. Furthermore, the latent heat flux was higher during the wet season (114.68 W m�� 2) and lowered in the dry season (9.39 W m�� 2). The net assimilation rate showed higher values during the dry-wet transition. The dry season presented higher nutrient use efficiency and WUE (14.77 g m�� 2 mm�� 1). The highest ET occurred during the wet season (227 mm), and RUE was 81.48% higher than in the dry season. Overall, the cactus was a potential C sink during the three years of assessment (NEE: �� 377 g C m�� 2 year�� 1; GPP: 881 g C m�� 2 year�� 1). The results help us to understand that most of the Rn energy is used in the sensible heat flux (58% ratio).
650 $aEvapotranspiration
650 $aOpuntia
650 $aCaatinga
650 $aCacto
650 $aCarbono
650 $aEcossistema
650 $aEvapotranspiração
653 $aAgroecossistema
653 $aCacto de sequeiro
653 $aConcentração de carbono
653 $aCovariância de redemoinho
653 $aOpuntia cactus
653 $aPlanta CAM
653 $aSemiárido
653 $aSumidouro ou fonte de carbono
653 $aTroca líquida de CO2
700 1 $aMORAIS, J. E. F. de
700 1 $aSOUZA, L. S. B. de
700 1 $aMARIN, F. R.
700 1 $aMOURA, M. S. B. de
700 1 $aMORELLATO, L. P. C.
700 1 $aMONTENEGRO, A. A. de A.
700 1 $aOMETTO, J. P. H. B.
700 1 $aLIMA, J. L. M. P. de
700 1 $aDUBEUX JÚNIOR, J. C. B.
700 1 $aSILVA, T. G. F. da
773 $tJournal of Hydrology$gv. 625, 130121, 2023.
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Embrapa Semiárido (CPATSA) |
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