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Registro Completo |
Biblioteca(s): |
Embrapa Pantanal. |
Data corrente: |
01/10/2004 |
Data da última atualização: |
06/04/2017 |
Autoria: |
HAMILTON, S. K.; SIPPEL, S. J.; MELACK, J. M. |
Afiliação: |
Department of Biological Sciences, University of California, Santa Barbara. |
Título: |
Dissolved oxygen, carbon dioxide, and methane in waters of the Pantanal wetland of Brazil. |
Ano de publicação: |
1993 |
Fonte/Imprenta: |
American Geoghysical Union Fall Meeting, Dec.1993, San Francisco. Abstract... San Francisco: [s.n], 1993. não paginado. |
Idioma: |
Inglês |
Conteúdo: |
The Pantnal is a 140,000-km2 complex of riverine floodplains and marshes in the upper Paraguay River basin. Most surface waters are shallow and slowly flowing, often with luxuriant growths of emergent and floating vascular plants. The water column is typically well-mixed or stratified only diurnally. We have sampled representative aquatic environments. throughout the region during 16 months for analysis of dissolved O2 (polarographic sensor), dissolved CO2 (calculated from pH, Gran alkalinity, temperature, and major ions), and dissolved CH4 (gas chromatography). Despite contact with the atmosphere, the waters are characteristically strongly oxygen-depleted: the median of 453 samples was 26% of atmospheric equilibrium (saturation), and 118 of those samples were <10% saturation. CO2 was nearly always supersaturated with a median partial pressure of 7560 ppmv (N=194). Ch4 was highly supersaturated (median 692 ppmv, N=447). This consistent pattern of O2 depletion and CO2 and CH4 accumulation reveals that overall, biological metabolism beneath the water surface is strongly heterotrophic; most net photosynthesis occurs above the water surface or during the dry season. Most anaerobic decomposition of organic matter probably culminates in methanogenesis due to the relative scarcity of alternate electron acceptors to support anaerobic respiration: the median concentration of sulface was only 0.55 uM (N=186; ion chromatography), dissolved H2S was <0.5 uM (methylene blue method), and the sum of nitrate plus nitrite was <7 uM. We are continuing to investigate the roles of iron and manganese in supporting anaerobic respiration, which may be significant but are difficult to estimate due to the participation of particulate forms of these elements. MenosThe Pantnal is a 140,000-km2 complex of riverine floodplains and marshes in the upper Paraguay River basin. Most surface waters are shallow and slowly flowing, often with luxuriant growths of emergent and floating vascular plants. The water column is typically well-mixed or stratified only diurnally. We have sampled representative aquatic environments. throughout the region during 16 months for analysis of dissolved O2 (polarographic sensor), dissolved CO2 (calculated from pH, Gran alkalinity, temperature, and major ions), and dissolved CH4 (gas chromatography). Despite contact with the atmosphere, the waters are characteristically strongly oxygen-depleted: the median of 453 samples was 26% of atmospheric equilibrium (saturation), and 118 of those samples were <10% saturation. CO2 was nearly always supersaturated with a median partial pressure of 7560 ppmv (N=194). Ch4 was highly supersaturated (median 692 ppmv, N=447). This consistent pattern of O2 depletion and CO2 and CH4 accumulation reveals that overall, biological metabolism beneath the water surface is strongly heterotrophic; most net photosynthesis occurs above the water surface or during the dry season. Most anaerobic decomposition of organic matter probably culminates in methanogenesis due to the relative scarcity of alternate electron acceptors to support anaerobic respiration: the median concentration of sulface was only 0.55 uM (N=186; ion chromatography), dissolved H2S was <0.5 uM (methylene blue method), and t... Mostrar Tudo |
Thesagro: |
Água; Dióxido de Carbono; Metano; Oxigênio. |
Thesaurus Nal: |
carbon dioxide; methane; oxygen; Pantanal; water. |
Categoria do assunto: |
-- |
Marc: |
LEADER 02496naa a2200253 a 4500 001 1811184 005 2017-04-06 008 1993 bl --- 0-- u #d 100 1 $aHAMILTON, S. K. 245 $aDissolved oxygen, carbon dioxide, and methane in waters of the Pantanal wetland of Brazil. 260 $c1993 520 $aThe Pantnal is a 140,000-km2 complex of riverine floodplains and marshes in the upper Paraguay River basin. Most surface waters are shallow and slowly flowing, often with luxuriant growths of emergent and floating vascular plants. The water column is typically well-mixed or stratified only diurnally. We have sampled representative aquatic environments. throughout the region during 16 months for analysis of dissolved O2 (polarographic sensor), dissolved CO2 (calculated from pH, Gran alkalinity, temperature, and major ions), and dissolved CH4 (gas chromatography). Despite contact with the atmosphere, the waters are characteristically strongly oxygen-depleted: the median of 453 samples was 26% of atmospheric equilibrium (saturation), and 118 of those samples were <10% saturation. CO2 was nearly always supersaturated with a median partial pressure of 7560 ppmv (N=194). Ch4 was highly supersaturated (median 692 ppmv, N=447). This consistent pattern of O2 depletion and CO2 and CH4 accumulation reveals that overall, biological metabolism beneath the water surface is strongly heterotrophic; most net photosynthesis occurs above the water surface or during the dry season. Most anaerobic decomposition of organic matter probably culminates in methanogenesis due to the relative scarcity of alternate electron acceptors to support anaerobic respiration: the median concentration of sulface was only 0.55 uM (N=186; ion chromatography), dissolved H2S was <0.5 uM (methylene blue method), and the sum of nitrate plus nitrite was <7 uM. We are continuing to investigate the roles of iron and manganese in supporting anaerobic respiration, which may be significant but are difficult to estimate due to the participation of particulate forms of these elements. 650 $acarbon dioxide 650 $amethane 650 $aoxygen 650 $aPantanal 650 $awater 650 $aÁgua 650 $aDióxido de Carbono 650 $aMetano 650 $aOxigênio 700 1 $aSIPPEL, S. J. 700 1 $aMELACK, J. M. 773 $tAmerican Geoghysical Union Fall Meeting, Dec.1993, San Francisco. Abstract... San Francisco: [s.n], 1993. não paginado.
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Registro original: |
Embrapa Pantanal (CPAP) |
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Biblioteca(s): |
Embrapa Semiárido. |
Data corrente: |
14/12/2020 |
Data da última atualização: |
14/12/2020 |
Tipo da produção científica: |
Documentos |
Autoria: |
CASTRO, J. M. da C. e; RIBEIRO, J. M. |
Afiliação: |
JOSE MAURO DA CUNHA E CASTRO, CPATSA; JULIANA MARTINS RIBEIRO, CPATSA. |
Título: |
Pesquisa e desenvolvimento para a cultura da goiabeira: a contribuição da Embrapa Semiárido. |
Ano de publicação: |
2020 |
Fonte/Imprenta: |
Petrolina, PE: Embrapa Semiárido, 2020. |
Páginas: |
82p |
Descrição Física: |
il. |
Série: |
(Embrapa Semiárido. Documentos, 297). |
ISSN: |
1808-9992. |
Idioma: |
Português |
Conteúdo: |
A goiabeira (Psidium guajava L.) é de fundamental importância econômica para o Semiárido brasileiro, principalmente, para os pequenos produtores. Por este motivo, a Embrapa Semiárido sempre dispensou muitos esforços de pesquisa com a cultura. Poucos anos depois da instalação da Embrapa Semiárido em Petrolina, PE, a goiabeira já foi avaliada e considerada promissora para cultivo em diversos locais do Nordeste do Brasil (Nunes et al., 1978). Com os primeiros plantios em condição de sequeiro, as pesquisas conduzidas levaram a cultura a uma posição de destaque na fruticultura irrigada dos dias atuais, conforme será apresentado ao longo deste documento. Numa revisão sobre os trabalhos desenvolvidos há cerca de 30 anos, o leitor poderá encontrar, de forma fácil e rápida, todos os esforços de pesquisa conduzidos pela Embrapa Semiárido, muitas vezes, com o envolvimento de instituições parceiras, que revelaram a importância socioeconômica da cultura da goiabeira observada nos dias atuais. |
Palavras-Chave: |
Cultivar; Goiabeira. |
Thesagro: |
Comportamento de Variedade; Goiaba; Propagação Vegetativa; Psidium Guajava. |
Thesaurus NAL: |
Cultivar identification; Cultivars; Guavas. |
Categoria do assunto: |
G Melhoramento Genético |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/219138/1/Doc-297-Goiabeira.pdf
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Marc: |
LEADER 01804nam a2200265 a 4500 001 2128050 005 2020-12-14 008 2020 bl uuuu 00u1 u #d 022 $a1808-9992. 100 1 $aCASTRO, J. M. da C. e 245 $aPesquisa e desenvolvimento para a cultura da goiabeira$ba contribuição da Embrapa Semiárido.$h[electronic resource] 260 $aPetrolina, PE: Embrapa Semiárido$c2020 300 $a82p$cil. 490 $a(Embrapa Semiárido. Documentos, 297). 520 $aA goiabeira (Psidium guajava L.) é de fundamental importância econômica para o Semiárido brasileiro, principalmente, para os pequenos produtores. Por este motivo, a Embrapa Semiárido sempre dispensou muitos esforços de pesquisa com a cultura. Poucos anos depois da instalação da Embrapa Semiárido em Petrolina, PE, a goiabeira já foi avaliada e considerada promissora para cultivo em diversos locais do Nordeste do Brasil (Nunes et al., 1978). Com os primeiros plantios em condição de sequeiro, as pesquisas conduzidas levaram a cultura a uma posição de destaque na fruticultura irrigada dos dias atuais, conforme será apresentado ao longo deste documento. Numa revisão sobre os trabalhos desenvolvidos há cerca de 30 anos, o leitor poderá encontrar, de forma fácil e rápida, todos os esforços de pesquisa conduzidos pela Embrapa Semiárido, muitas vezes, com o envolvimento de instituições parceiras, que revelaram a importância socioeconômica da cultura da goiabeira observada nos dias atuais. 650 $aCultivar identification 650 $aCultivars 650 $aGuavas 650 $aComportamento de Variedade 650 $aGoiaba 650 $aPropagação Vegetativa 650 $aPsidium Guajava 653 $aCultivar 653 $aGoiabeira 700 1 $aRIBEIRO, J. M.
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