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| Registros recuperados : 119 | |
| 81. |  | CABRAL, O. M. R.; GASH, J. H. C.; ROCHA, H. R. da; MARSDEN, C.; LIGO, M. A. V.; FREITAS, H. C. de; TATSCH, J. D.; GOMES, E. Fluxes of CO2 above a plantation of Eucalyptus in southeast Brazil. Agricultural and Forest Meteorology, v. 151, p. 49?59, 2011.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 82. | | CABRAL, O. M. R.; ROCHA, H. R. da; GASH, J. H.; LIGO, M. A. V.; RAMOS, N. P.; PACKER, A. P.; BATISTA, E. R. Fluxes of CO2 above a sugarcane plantation in Brazil. Agricultural and Forest Meteorology, Amsterdam, v. 182-183, p. 54-66, 2013.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 83. | | PATRICIO, F. R. A.; ALMEIDA, I. M. G. de; SANTOS, A. S.; CABRAL, O. M. R.; TESSARIOLI NETO, J.; SINIGAGLIA, C.; BERIAM, L. O. S.; RODRIGUES NETO, J. Avaliação da solarização do solo para o controle de Ralstonia solanacearum. Fitopatologia Brasileira, Brasília, DF, v. 30, n. 5, p. 475-481, set./out. 2005.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 84. | | TATSCH, J. D.; ROCHA, H. R.; CABRAL, O. M. R.; FREITAS, H. C.; LLOPART, M.; ACOSTA, R.; LIGO, M. A. V. Avaliação do método de Multiple Imputation no preenchimento de falhas de fluxos de energia sobre uma área de cana-de-açúcar. In: BRAZILIAN MICROMETEOROLOGY WORKSHOP, 5., 2007, Santa Maria. Abstracts... Santa Maria: Universidade Federal de Santa Maria, 2007. CD-ROM.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 85. | | CABRAL, O. M. R.; ROCHA, H. R. da; GASH, J. H.; LIGO, M. A. V.; TATSCH, J. D.; FREITAS, H. C. de; BRASILIO, E. Water use in a sugarcane plantation. Global Change Biology. Bioenergy, Oxford, v. 4, p. 555-565, 2012.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 86. | | ROCHA, H. R. da; FREITAS, H. C. de; ROSOLEM, R.; TANNUS, R. N.; NEGRÓN-JUÁREZ, R. I.; LIGO, M. A. V.; CABRAL, O. M. R.; MESQUITA JÚNIOR, H. N. DE; BITENCOURT, M. D. Ciclo do carbono. In: PIVELLO, V. R.; VARANDA, E. M. (Org.) O Cerrado do pé-de-gigante - Parque Estadual de Vassununga: ecologia e conservação. São Paulo, SMA, 2005. p. 133-140. Parte III - As relações entre a vegetação e o meio físico no Cerrado pé-de-gigante.
Capítulo 14.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 87. | | ROCHA, H. R. da; FREITAS, H. C. de; ROSOLEM, R.; TANNUS, R. N.; NEGRÓN-JUÁREZ, R. I.; LIGO, M. A. V.; CABRAL, O. M. R.; MESQUITA JUNIOR, H. N. DE; BITENCOURT, M. D. Ciclo hidrológico e microclima. In: PIVELLO, V. R.; VARANDA, E. M. (Org.) O Cerrado do pé-de-gigante - Parque Estadual de Vassununga: ecologia e conservação. São Paulo, SMA, 2005. p. 37-46. Parte I - Caracterização física do Cerrado pé-de-gigante e uso das terras na região.
Capítulo 4.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 88. | | LIMA, M. A. de; PESSOA, M. C. P. Y.; NEVES, M. C.; CABRAL, O. M. R.; LUCHIARI JUNIOR, A.; HERMES, L. C.; DYNIA, J. F.; TOLEDO, L. G.; SOUZA, M. D. de. Emissão de metano proveniente da cultura de arroz irrigado no Brasil. In: REUNIÃO DA CULTURA DO ARROZ IRRIGADO, 22., 1997, Camboriú-SC. Resumo expandido. Itajaí: EPAGRI / IRGA/ EMBRAPA-CPACT, 1997. p.542-545| Biblioteca(s): Embrapa Meio Ambiente. |
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| 89. | | MCWILLIAM, A. L. C.; ROBERTS, J. M.; CABRAL, O. M. R.; LEITAO, M. V. B. R.; COSTA, A. C. L. de; MAITELLI, G. T.; ZAMPARONI, C. A. G. P. Leaf area index and above-ground biomass of terra firme rain forest and adjacent clearings in Amazonia. Functional Ecology, v. 7, n. 3, p. 310-317, 1993.| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 90. | | ALVALÁ, R. C. S.; GIELOW, R.; ROCHA, H. R. da; FREITAS, H. C.; LOPES, J. M.; MANZI, A. O.; RANDOW, C. von; DIAS, M. A. F. S.; CABRAL, O. M. R.; WATERLOO, M. J. Intradiurnal and seasonal variability of soil temperature, heat flux, soil moisture content, and thermal properties under forest and pasture in Rondônia. Journal of Geophysical Research, Washington, v. 107, n. D20, p. LBA10-1 - LBA 10-20, 2002.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 91. | | PACKER, A. P.; RAMOS, N. P.; CABRAL, O. M. R.; SILVA, L. R. da; MOLTOCARO, R. C. R.; BETTANIN, V. C.; MORASI, I. M.; AMARO, A. R. F. V. B. de L.; TEIXEIRA, W. G. Management of nitrogen fertilizer to reduce nitrous oxide (N2O) emission and ammonia (NH3) volatilization from coffee plantation. In: INTERNATIONAL PLANT NUTRITION COLLOQUIUM, 18., 2017, Copenhagen. Proceedings book... Copenhagen: International Plant Nutrition Council, 2017. Editors: Andreas Carstensen, Kristian Holst Laursen, Jan Kofod Schjorring. p. 769-770| Biblioteca(s): Embrapa Meio Ambiente. |
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| 92. | | COLMANETTI, M. A. A.; CUADRA, S. V.; ATTIA, A.; NOUVELLON, Y.; GUILLEMOT, J.; CAMPOE, O. C.; CABRAL, O. M. R.; LACLAU, J.; GALDOS, M.; LAMPARELLI, R.; BORTOLUCCI, J.; PEREIRA, B.; MAIRE, G. Le. Adaptation of Agro-IBIS model for Eucalyptus carbon budget estimation at regional level: a case study in São Paulo State, Brazil. Pesquisa Florestal Brasileira, v. 39, e201902043, p. 255-256, 2019. Special issue. Abstracts of the XXV IUFRO World Congress, 2019. 255| Biblioteca(s): Embrapa Meio Ambiente. |
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| 93. | | COLMANETTI, M. A. A.; CUADRA, S. V.; ATTIA, A.; NOUVELLON, Y.; GUILLEMOT, J.; CAMPOE, O. C.; CABRAL, O. M. R.; LACLAU, J.; GALDOS, M.; LAMPARELLI, R. A. C.; BORTOLUCCI, J.; PEREIRA, B.; LE MARIE, G. Adaptation of Agro-IBIS model for Eucalyptus carbon budget estimation at regional level - a case study in São Paulo State, Brazil. Pesquisa Florestal Brasileira, v. 39, e201902043, p. 255-256, 2019. Na publicação: Osvaldo Cabral. Special issue. Abstracts of the XXV IUFRO World Congress, 2019, Curitiba.| Biblioteca(s): Embrapa Agricultura Digital. |
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| 94. | | CUADRA, S. V.; COSTA, M. H.; KUCHARIK, C. J.; ROCHA, H. R. da; TATSCH, J. D.; INMAN-BAMBER, G.; ROCHA, R. P. da; LEITE, C. C.; CABRAL, O. M. R. A biophysical model of Sugarcane growth. Global Change Biology. Bioenergy, v. 4, n. 1, p. 36-48, 2012.| Biblioteca(s): Embrapa Clima Temperado; Embrapa Meio Ambiente. |
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| 95. | | ROCHA, H. R. da; GOULDEN, M.; MILLER, S.; MANZI, A. O.; CABRAL, O. M. R.; FREITAS, H. C. de; NOBRE, A.; SALESKA, S.; WOFSY, S.; KRUIJT, B.; RANDOW, C. VON. Patterns of CO2 and water fluxes measured by flux towers across tropical forest, ecotone and savanna ecosystems in Brazil. In: INTEGRATED LAND ECOSYSTEM - ATMOSPHERE PROCESSES STUDY, 1., 2006, Colorado, USA. Proceedings... Colorado, USA: Finnish Association for Aerosol Research, 2006. p. 215. (Report Series in Aerosol Science, n. 76). Editors: Anni Reissell, Asbjorn Aarflot.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 96. | | ROCHA, H. R. da; FREITAS, H. C.; ROSOLEM, R.; JUÁREZ, R. I. N.; TANNUS, R. N.; LIGO, M. A. V.; CABRAL, O. M. R.; DIAS, M. A. F. S. Measurements of CO2 exchange over a woodland savanna (Cerrado Sensu stricto) in southeast Brasil. Biota Neotropica, Campinas, v. 2, n. 1, p. 1-11, 2002.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 97. | | PACKER, A. P.; DEGASPARI, I. A. M.; RAMOS, N. P.; PINO JR. A. F.; CARMO, J. B.; ROSETTO, R.; PITOMBO, L.; CABRAL, O. M. R.; LIMA, M. A. de; ANDRADE, C. A. de. Site-specific N2O emission from soil related to the addition of sugarcane residues. In: INTERNATIONAL PLANT NUTRITION COLLOQUIUM, 17.; BORON SATELLITE MEETING, 2013, Istambul. Plant nutrition for nutrient and food security: proceedings book. Istambul: Sabanci University, 2013. p. 926-927.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 98. | | PACKER, A. P.; DEGASPARI, I. A. M.; MORASI, I. M.; VILELA, V. A. A.; MAXIMILIANO, V. C. B.; SANTOS, J. de O.; RAMOS, N. P.; CABRAL, O. M. R.; ROSETTO, R. Site-specific N2O emission from soil related to fertilization and sugarcane trash addition. In: WORLD FERTILIZER CONGRESS OF CIEC, 16., 2014, Rio de Janeiro. Technological innovation for a sustainable tropical agriculture: proceedings. Rio de Janeiro: International Scientific Centre of Fertilizers, 2014. p. 305-307.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 99. | | EPRON, D.; CABRAL, O. M. R.; LACLAU, J.-P.; DANNOURA, M.; PACKER, A. P.; PLAIN, C.; BATTIE-LACLAU, P.; MOREIRA, M. Z.; TRIVELIN, P. C. O.; BOUILLET, J-P.; GÉRANT, D.; NOUVELLON, Y. In situ 13CO2 pulse labelling of field-grown eucalypt trees revealed the effects of potassium nutrition and throughfall exclusion on phloem transport of photosynthetic carbon. Tree Physiology, Oxford, v. 36, n. 1, p. 6-21, 2016.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 100. | | VALDÉS, R. H.; TATSCH, J. D.; CABRAL, O. M. R.; ROCHA, H. R. da; BRASILIO, E. M. S.; GOERGEN, G.; MENDOZA, F. R. T.; PARCIANELLO, A. F.; KANNENBERG, C. Sensibilidade do modelo distribuído hidrológico da biosfera às propriedades hídricas do solo em uma pequena bacia de cerrado. Ciência e Natura, Santa Maria, v. 38, p. 277-283, 2016. Edição Especial dos Anais do IX Workshop Brasileiro de Micrometeorologia, Santa Maria, 2016.| Biblioteca(s): Embrapa Meio Ambiente. |
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| Registros recuperados : 119 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Meio Ambiente. |
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Data corrente: |
04/07/2007 |
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Data da última atualização: |
17/03/2021 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
Internacional - A |
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Autoria: |
ALVALÁ, R. C. S.; GIELOW, R.; ROCHA, H. R. da; FREITAS, H. C.; LOPES, J. M.; MANZI, A. O.; RANDOW, C. von; DIAS, M. A. F. S.; CABRAL, O. M. R.; WATERLOO, M. J. |
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Afiliação: |
R. C. S. ALVALA, Instituto Nacional de Pesquisas Espaciais/SP; R. GIELOW, Instituto Nacional de Pesquisas Espaciais/SP; H. R. DA ROCHA,, USP/SP; H. C. FREITAS, USP/SP; J. M. LOPES, USP; A. O. MANZI,, Instituto Nacional de Pesquisas Espaciais/SP; C. VON RANDOW, Instituto Nacional de Pesquisas Espaciais; M. A. F. S. DIAS, USP; OSVALDO MACHADO RODRIGUES CABRAL, CNPMA; M. J. WATERLOO, Vrije Universiteit Amsterdam, Amsterdam, Netherlands. |
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Título: |
Intradiurnal and seasonal variability of soil temperature, heat flux, soil moisture content, and thermal properties under forest and pasture in Rondônia. |
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Ano de publicação: |
2002 |
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Fonte/Imprenta: |
Journal of Geophysical Research, Washington, v. 107, n. D20, p. LBA10-1 - LBA 10-20, 2002. |
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Idioma: |
Inglês |
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Conteúdo: |
Soil temperatures depend on the soil heat flux, an important parameter in meteorological and plant growth-energy balance models. Thus, they were measured, together with soil moisture contents, within the LBA program at forest (Reserva Jaru) and pasture (Fazenda Nossa Senhora) sites in Rondônia, Brazilian Amazonia during wet (February) and dry (August) periods of 1999. The wet period showed maxima of the heat flux into the soil around five to six times smaller at the forest than at the pasture, except for some spikes that are related to stronger solar forcing, such as those due to sunspecks in the forest. This pattern remained during the dry period, but with doubled maximum values. Also, the soil heat flux and the soil temperatures responded very significantly to the passage of cold fronts in both periods at both sites. Temperature profiles measured in the 0.10-0.40 m soil layer showed daily averages and ranges smaller at the forest than at the pasture. The daily average of the soil moisture content in the same layer, during the wet season, increased with depth at both sites, with consistently lower values at the forest. However, their ranges were smaller at the pasture, except for the 0.40 m depth. During the dry period, these ranges were much higher at the pasture, but with nearer average values. Finally, the computed daily apparent soil thermal diffusivities, volumetric heat contents, and thermal conductivities are presented, with the first ones crossed with the measured soil moisture content. MenosSoil temperatures depend on the soil heat flux, an important parameter in meteorological and plant growth-energy balance models. Thus, they were measured, together with soil moisture contents, within the LBA program at forest (Reserva Jaru) and pasture (Fazenda Nossa Senhora) sites in Rondônia, Brazilian Amazonia during wet (February) and dry (August) periods of 1999. The wet period showed maxima of the heat flux into the soil around five to six times smaller at the forest than at the pasture, except for some spikes that are related to stronger solar forcing, such as those due to sunspecks in the forest. This pattern remained during the dry period, but with doubled maximum values. Also, the soil heat flux and the soil temperatures responded very significantly to the passage of cold fronts in both periods at both sites. Temperature profiles measured in the 0.10-0.40 m soil layer showed daily averages and ranges smaller at the forest than at the pasture. The daily average of the soil moisture content in the same layer, during the wet season, increased with depth at both sites, with consistently lower values at the forest. However, their ranges were smaller at the pasture, except for the 0.40 m depth. During the dry period, these ranges were much higher at the pasture, but with nearer average values. Finally, the computed daily apparent soil thermal diffusivities, volumetric heat contents, and thermal conductivities are presented, with the first ones crossed with the measured s... Mostrar Tudo |
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Palavras-Chave: |
Fluxo de calor; Variabilidade. |
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Thesagro: |
Balanço de Energia; Floresta; Pastagem; Temperatura do Solo; Umidade do Solo. |
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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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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/163809/1/Alvala-Intradiurnal-6959.pdf
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Marc: |
LEADER 02534naa a2200325 a 4500
001 1015531
005 2021-03-17
008 2002 bl uuuu u00u1 u #d
100 1 $aALVALÁ, R. C. S.
245 $aIntradiurnal and seasonal variability of soil temperature, heat flux, soil moisture content, and thermal properties under forest and pasture in Rondônia.$h[electronic resource]
260 $c2002
520 $aSoil temperatures depend on the soil heat flux, an important parameter in meteorological and plant growth-energy balance models. Thus, they were measured, together with soil moisture contents, within the LBA program at forest (Reserva Jaru) and pasture (Fazenda Nossa Senhora) sites in Rondônia, Brazilian Amazonia during wet (February) and dry (August) periods of 1999. The wet period showed maxima of the heat flux into the soil around five to six times smaller at the forest than at the pasture, except for some spikes that are related to stronger solar forcing, such as those due to sunspecks in the forest. This pattern remained during the dry period, but with doubled maximum values. Also, the soil heat flux and the soil temperatures responded very significantly to the passage of cold fronts in both periods at both sites. Temperature profiles measured in the 0.10-0.40 m soil layer showed daily averages and ranges smaller at the forest than at the pasture. The daily average of the soil moisture content in the same layer, during the wet season, increased with depth at both sites, with consistently lower values at the forest. However, their ranges were smaller at the pasture, except for the 0.40 m depth. During the dry period, these ranges were much higher at the pasture, but with nearer average values. Finally, the computed daily apparent soil thermal diffusivities, volumetric heat contents, and thermal conductivities are presented, with the first ones crossed with the measured soil moisture content.
650 $aAmazonia
650 $aBalanço de Energia
650 $aFloresta
650 $aPastagem
650 $aTemperatura do Solo
650 $aUmidade do Solo
653 $aFluxo de calor
653 $aVariabilidade
700 1 $aGIELOW, R.
700 1 $aROCHA, H. R. da
700 1 $aFREITAS, H. C.
700 1 $aLOPES, J. M.
700 1 $aMANZI, A. O.
700 1 $aRANDOW, C. von
700 1 $aDIAS, M. A. F. S.
700 1 $aCABRAL, O. M. R.
700 1 $aWATERLOO, M. J.
773 $tJournal of Geophysical Research, Washington$gv. 107, n. D20, p. LBA10-1 - LBA 10-20, 2002.
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Embrapa Meio Ambiente (CNPMA) |
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