995 resultados para tipo de céu
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A cultivar BRSMG Pioneiro, além de possuir grãos tipo carioca, apresenta como principal vantagem a resistência a vários patótipos de antracnose e ferrugem, sendo uma excelente opção para os produtores de feijão carioca da região Sul do país, nos plantios da safra e safrinha.
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ABSTRACT: During the years 2003 and 2004, four experiments were conducted in the winter season, under irrigation and in the raining season in the experimental area of the Embrapa Cerrados Research Center at Planaltina, Federal District. The objective was to identify cultivars that presented the following characteristics: resistance to diseases, high yield, resistance to lodging, desirable plant height and good market acceptance, to be indicated for cultivation in the Federal District. It was concluded that the cultivar BRS Cometa is indicated for this region, due to its high yield characteristics, resistance to diseases and lodging, excellent cooking qualities and erect type.
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2013
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2013
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1996
Avaliação de linhagens de feijão-de-corda tipo ramador em áreas dos tabuleiros costeiros de Sergipe.
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1997
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2014
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Este trabalho teve como objetivo calcular a uniformidade de irrigação para sistema de irrigação por aspersão do tipo canhão hidráulico submetido a vários espaçamentos em campo. Foi conduzido na propriedade hidroagrícola Lagoa do Ouro, no Município de Jequié, Bahia. O aspersor utilizado é do tipo canhão hidráulico, Plona-PLN 25. Foram utilizados 80 coletores no campo espaçados de 6 (m) para coleta das lâminas de água (mm). A evapotranspiração potencial da cultura foi medida a partir do tanque classe "A" instalado na propriedade. Os maiores valores apresentados de coeficientes de uniformidade CUC e CUD foram de 78% e 71% respectivamente para o espaçamento de 36x36 m; e os menores, 67% e 30% para o espaçamento 42x42 m.
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This article presents the physical structure of the land, organic substances content and the chemical composition of soil comprising subsoil of 21 urban greenery locations in the city of Poznań. As they tend to be commonly underestimated, they have also been presented with view to their vital functions in plants’ life processes. The analysed microelements are referred to their levels, the so-called geo-chemical background of Polish soils and the limit values for field soils with medium levels of nutrients.
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A diabetes mellitus do tipo 2 é caracterizada pela resistência à insulina e pela disfunção das células β do pâncreas. Os péptidos gastrintestinais, “gastric inhibitory polypeptide” (GIP) e “glucagon-like peptide-1” (GLP-1), são hormonas incretinas que estimulam, maioritariamente, a produção de insulina pós-prandial. Formulações contendo GLP-1 possuem um grande potencial no tratamento desta doença. Porém, o GLP-1 é eficaz apenas quando administrado por via parentérica. Para o tratamento da diabetes mellitus tipo 2 são usados análogos do GLP‑ 1 ou miméticos da incretina os quais são eficazes por via subcutânea. The pathogenesis of diabetes mellitus type 2 includes insulin resistance and progressive β-cell dysfunction. The gastrointestinal peptides, gastric inhibitory polypeptide (GIP) and glucagon‑like peptide-1 (GLP-1), are incretin hormones which are responsible for the major part of postprandial insulin secretion. Formulations containing GLP-1 have a great potential in the treatment of diabetes mellitus type 2. Nonetheless, GLP-1 is only efficient by continuous parenteral administration. GLP-1 analogues or incretin mimetics, exendine-4, are active after subcutaneous injection and can be used in the treatment of diabetes mellitus of type 2.
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Projeto de Pós-Graduação/Dissertação apresentado à Universidade Fernando Pessoa como parte dos requisitos para obtenção do grau de Mestre em Ciências Farmacêuticas
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Trabalho de Projeto apresentado à Universidade Fernando Pessoa como parte dos requisitos para obtenção do grau de Mestre em Análises Laboratoriais Especializadas, área de especialização em Análise Biomédica
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115 hojas : ilustraciones.
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22 hojas : ilustraciones, fotografías a color
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In the ancient and acidic Ultisol soils of the Southern Piedmont, USA, we studied changes in trace element biogeochemistry over four decades, a period during which formerly cultivated cotton fields were planted with pine seedlings that grew into mature forest stands. In 16 permanent plots, we estimated 40-year accumulations of trace elements in forest biomass and O horizons (between 1957 and 1997), and changes in bioavailable soil fractions indexed by extractions of 0.05 mol/L HCl and 0.2 mol/L acid ammonium oxalate (AAO). Element accumulations in 40-year tree biomass plus O horizons totaled 0.9, 2.9, 4.8, 49.6, and 501.3 kg/ha for Cu, B, Zn, Mn, and Fe, respectively. In response to this forest development, samples of the upper 0.6-m of mineral soil archived in 1962 and 1997 followed one of three patterns. (1) Extractable B and Mn were significantly depleted, by -4.1 and -57.7 kg/ha with AAO, depletions comparable to accumulations in biomass plus O horizons, 2.9 and 49.6 kg/ha, respectively. Tree uptake of B and Mn from mineral soil greatly outpaced resupplies from atmospheric deposition, mineral weathering, and deep-root uptake. (2) Extractable Zn and Cu changed little during forest growth, indicating that nutrient resupplies kept pace with accumulations by the aggrading forest. (3) Oxalate-extractable Fe increased substantially during forest growth, by 275.8 kg/ha, about 10-fold more than accumulations in tree biomass (28.7 kg/ha). The large increases in AAO-extractable Fe in surficial 0.35-m mineral soils were accompanied by substantial accretions of Fe in the forest's O horizon, by 473 kg/ha, amounts that dwarfed inputs via litterfall and canopy throughfall, indicating that forest Fe cycling is qualitatively different from that of other macro- and micronutrients. Bioturbation of surficial forest soil layers cannot account for these fractions and transformations of Fe, and we hypothesize that the secondary forest's large inputs of organic additions over four decades has fundamentally altered soil Fe oxides, potentially altering the bioavailability and retention of macro- and micronutrients, contaminants, and organic matter itself. The wide range of responses among the ecosystem's trace elements illustrates the great dynamics of the soil system over time scales of decades.