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Registro Completo |
Biblioteca(s): |
Embrapa Amazônia Oriental; Embrapa Florestas. |
Data corrente: |
06/06/1995 |
Data da última atualização: |
22/05/2009 |
Autoria: |
BASTOS, T. X. |
Título: |
Effect of pine forest canopy removal on flatwood soil temperature and moisture regime. |
Ano de publicação: |
1978 |
Fonte/Imprenta: |
1978. |
Páginas: |
126 f. |
Idioma: |
Inglês |
Notas: |
Thesis (Master of Science) - University of Florida, Gainesville. |
Conteúdo: |
Soil temperature and moisture regimes in three site conditions control, (undisturbed) minimum preparation (harvested and burned) and maximum (harvest, sheared, chopped, and bedded) preparation were studied in a mixed slash (Pinus elliottii engelm. var. elleiottii) longleaf (Pinus palustris Mill.) pine flatwood forest in north Florida at 0,5, 10, 20 and 50-cm depths. Measurements were taken on the two dominant soil series in the area p electra and wauchula. Te area with the most intense site preparation had significantly higher maximum temperatures, follwed by minimum preparation and control areas. Overall mean and minimum temperatues were higher in the control areas followed by maximum and minimum preparation areas. Variations between maximum and minimum temperatures were higher in the maximum preparation floowed by minimum preparation and control areas. Temperatures at the various depths were significantly different for maximum and minimum temperatures and amplitudes. Higher temperature ocurred at surface follweed by 10, 20 and 50 cm depths. The opposite occurred in relation to minimum temperature. The amplitudes were greater at the surface than at 10, 20, and 50 cm depths. Temperature measurements were not significantly different between the two soils. Soil moisture regimes were also characterized on the two soil series three site conditions and soil depths. There were significant differences in soil moiture regime between the two soils, with soil moisture higher in the mauchula than the electra soil. The maximumsite preparation area possessed higher moisture contents followed by minimum site preparation and the control. The soil at 50 cm depths possessed significantly higher soil moisture, followed by soil at 5, 10 and 20 cm depths. Soil moisture was also compared in a control; minimum preparation unburned; minimum preparation, burned; and maximum preparation burned areas at 20 cm depth in the electra ann wauchula soils. There was a significant difference in water content between the two soils and site preparations. Wauchula possessed highter soil moiture contens than the electra. SOil moisture was in the order: maximum preparation, burned> minimum preparation, unburned>minimum preparation, burned>the control. The association between soil moisture, soil temperature and rainfall was evaluated for the 10, 20 and 50 cm depths in the electra soil in the undisturbed (control) forest. The regression evaluation fitted for the 20 cm depth indicated that rainfall made a greater contribution to the prediction of soil moisture than soil temperature. MenosSoil temperature and moisture regimes in three site conditions control, (undisturbed) minimum preparation (harvested and burned) and maximum (harvest, sheared, chopped, and bedded) preparation were studied in a mixed slash (Pinus elliottii engelm. var. elleiottii) longleaf (Pinus palustris Mill.) pine flatwood forest in north Florida at 0,5, 10, 20 and 50-cm depths. Measurements were taken on the two dominant soil series in the area p electra and wauchula. Te area with the most intense site preparation had significantly higher maximum temperatures, follwed by minimum preparation and control areas. Overall mean and minimum temperatues were higher in the control areas followed by maximum and minimum preparation areas. Variations between maximum and minimum temperatures were higher in the maximum preparation floowed by minimum preparation and control areas. Temperatures at the various depths were significantly different for maximum and minimum temperatures and amplitudes. Higher temperature ocurred at surface follweed by 10, 20 and 50 cm depths. The opposite occurred in relation to minimum temperature. The amplitudes were greater at the surface than at 10, 20, and 50 cm depths. Temperature measurements were not significantly different between the two soils. Soil moisture regimes were also characterized on the two soil series three site conditions and soil depths. There were significant differences in soil moiture regime between the two soils, with soil moisture higher in the ma... Mostrar Tudo |
Palavras-Chave: |
Cobertura florestal; Conteudo de agua no solo; Manejo florestal; Pinhal; Plant soil relations; Remoção de copa; Site factors; Sítio; Soils. |
Thesagro: |
Ecologia Florestal; Pinus Elliottii; Pinus Palustris; Relação Solo-Planta; Solo; Temperatura do Solo; Umidade do Solo. |
Thesaurus Nal: |
canopy; coniferous forests; forest ecology; forest management; Pinus; soil temperature; soil water content. |
Categoria do assunto: |
-- K Ciência Florestal e Produtos de Origem Vegetal |
Marc: |
LEADER 03714nam a2200409 a 4500 001 1304702 005 2009-05-22 008 1978 bl uuuu m 00u1 u #d 100 1 $aBASTOS, T. X. 245 $aEffect of pine forest canopy removal on flatwood soil temperature and moisture regime. 260 $a1978.$c1978 300 $a126 f. 500 $aThesis (Master of Science) - University of Florida, Gainesville. 520 $aSoil temperature and moisture regimes in three site conditions control, (undisturbed) minimum preparation (harvested and burned) and maximum (harvest, sheared, chopped, and bedded) preparation were studied in a mixed slash (Pinus elliottii engelm. var. elleiottii) longleaf (Pinus palustris Mill.) pine flatwood forest in north Florida at 0,5, 10, 20 and 50-cm depths. Measurements were taken on the two dominant soil series in the area p electra and wauchula. Te area with the most intense site preparation had significantly higher maximum temperatures, follwed by minimum preparation and control areas. Overall mean and minimum temperatues were higher in the control areas followed by maximum and minimum preparation areas. Variations between maximum and minimum temperatures were higher in the maximum preparation floowed by minimum preparation and control areas. Temperatures at the various depths were significantly different for maximum and minimum temperatures and amplitudes. Higher temperature ocurred at surface follweed by 10, 20 and 50 cm depths. The opposite occurred in relation to minimum temperature. The amplitudes were greater at the surface than at 10, 20, and 50 cm depths. Temperature measurements were not significantly different between the two soils. Soil moisture regimes were also characterized on the two soil series three site conditions and soil depths. There were significant differences in soil moiture regime between the two soils, with soil moisture higher in the mauchula than the electra soil. The maximumsite preparation area possessed higher moisture contents followed by minimum site preparation and the control. The soil at 50 cm depths possessed significantly higher soil moisture, followed by soil at 5, 10 and 20 cm depths. Soil moisture was also compared in a control; minimum preparation unburned; minimum preparation, burned; and maximum preparation burned areas at 20 cm depth in the electra ann wauchula soils. There was a significant difference in water content between the two soils and site preparations. Wauchula possessed highter soil moiture contens than the electra. SOil moisture was in the order: maximum preparation, burned> minimum preparation, unburned>minimum preparation, burned>the control. The association between soil moisture, soil temperature and rainfall was evaluated for the 10, 20 and 50 cm depths in the electra soil in the undisturbed (control) forest. The regression evaluation fitted for the 20 cm depth indicated that rainfall made a greater contribution to the prediction of soil moisture than soil temperature. 650 $acanopy 650 $aconiferous forests 650 $aforest ecology 650 $aforest management 650 $aPinus 650 $asoil temperature 650 $asoil water content 650 $aEcologia Florestal 650 $aPinus Elliottii 650 $aPinus Palustris 650 $aRelação Solo-Planta 650 $aSolo 650 $aTemperatura do Solo 650 $aUmidade do Solo 653 $aCobertura florestal 653 $aConteudo de agua no solo 653 $aManejo florestal 653 $aPinhal 653 $aPlant soil relations 653 $aRemoção de copa 653 $aSite factors 653 $aSítio 653 $aSoils
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Embrapa Florestas (CNPF) |
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Registro Completo
Biblioteca(s): |
Embrapa Cerrados. |
Data corrente: |
23/01/2023 |
Data da última atualização: |
23/01/2023 |
Tipo da produção científica: |
Resumo em Anais de Congresso |
Autoria: |
OLIVEIRA JÚNIOR, A. A. de; CARMONA, R.; GONCALVES, H. M.; CONCEIÇÃO, B. S.; COSTA, T. E. da; SOUZA, M. P. de. |
Afiliação: |
ANTÔNIO ALVES DE OLIVEIRA JÚNIOR; RICARDO CARMONA; HELENICE MOURA GONCALVES, CPAC; BRUNO SANTOS CONCEIÇÃO; THIAGO ESTÁCIO DA COSTA; MAIZA PEREIRA DE SOUZA. |
Título: |
Efeito do diâmetro do caule na alporquia em pequizeiro. |
Ano de publicação: |
2022 |
Fonte/Imprenta: |
In: CONGRESSO BRASILEIRO DE FRUTICULTURA, 27., 2022, Florianópolis. Valorização da ciência brasileira para a produção de frutas: anais. Florianópolis: SBF: Epagri: UDESC: UFSC: Embrapa, 2022. |
Páginas: |
p. 1874-1876 |
Idioma: |
Português |
Conteúdo: |
O potencial comercial do pequizeiro é ascendente, devido às características organolépticas marcantes do fruto que servem para uma infinidade de usos. A utilização do pequi vai muito além do uso humano, podendo ser utilizado na alimentação animal, sendo o farelo da casca do pequi uma alternativa viável para a alimentação de ruminantes. A propagação por sementes é comum em algumas espécies arbóreas devido à ausência de informações envolvendo outros métodos. Considerando as elevadas taxas de alogamia nas flores de pequizeiro, mudas produzidas de forma seminal apresentam grande variabilidade genética, o que acarreta enorme variabilidade fenotípica nos pomares. Para atenuar esses efeitos, a propagação via alporquia, que induz a formação de raízes adventícias em partes de caule ainda ligadas à planta mãe, apesar de mais trabalhosa, muitas vezes é mais eficiente na obtenção de mudas, a exemplo do que ocorre em pessegueiro (CASTRO e SILVEIRA, 2003). O objetivo do presente trabalho foi avaliar o efeito do diâmetro do caule e da planta matriz na sobrevivência, no calejamento e no enraizamento de alporques de pequizeiros nativos na região do Distrito Federal. |
Thesagro: |
Caule; Pequi. |
Categoria do assunto: |
-- |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/1151144/1/Helenice-EFEITO-DO-DIAMETRO-DO-CAULE-NA-ALPORQUIA-EM-PEQUIZEIRO.pdf
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Marc: |
LEADER 01929nam a2200205 a 4500 001 2151144 005 2023-01-23 008 2022 bl uuuu u00u1 u #d 100 1 $aOLIVEIRA JÚNIOR, A. A. de 245 $aEfeito do diâmetro do caule na alporquia em pequizeiro.$h[electronic resource] 260 $aIn: CONGRESSO BRASILEIRO DE FRUTICULTURA, 27., 2022, Florianópolis. Valorização da ciência brasileira para a produção de frutas: anais. Florianópolis: SBF: Epagri: UDESC: UFSC: Embrapa$c2022 300 $ap. 1874-1876 520 $aO potencial comercial do pequizeiro é ascendente, devido às características organolépticas marcantes do fruto que servem para uma infinidade de usos. A utilização do pequi vai muito além do uso humano, podendo ser utilizado na alimentação animal, sendo o farelo da casca do pequi uma alternativa viável para a alimentação de ruminantes. A propagação por sementes é comum em algumas espécies arbóreas devido à ausência de informações envolvendo outros métodos. Considerando as elevadas taxas de alogamia nas flores de pequizeiro, mudas produzidas de forma seminal apresentam grande variabilidade genética, o que acarreta enorme variabilidade fenotípica nos pomares. Para atenuar esses efeitos, a propagação via alporquia, que induz a formação de raízes adventícias em partes de caule ainda ligadas à planta mãe, apesar de mais trabalhosa, muitas vezes é mais eficiente na obtenção de mudas, a exemplo do que ocorre em pessegueiro (CASTRO e SILVEIRA, 2003). O objetivo do presente trabalho foi avaliar o efeito do diâmetro do caule e da planta matriz na sobrevivência, no calejamento e no enraizamento de alporques de pequizeiros nativos na região do Distrito Federal. 650 $aCaule 650 $aPequi 700 1 $aCARMONA, R. 700 1 $aGONCALVES, H. M. 700 1 $aCONCEIÇÃO, B. S. 700 1 $aCOSTA, T. E. da 700 1 $aSOUZA, M. P. de
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