21 resultados para Cherry Valley duck


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'Profusion Cherry' is a dwarf zinnia with prospect for pot use in Brazil. The success of flowering potted plants depends on its performance during transport and on the period of time that it performs well indoors. Benzyladenine application may retard leaf and flower senescence, increasing postproduction longevity and quality. Senescent flowers removal by consumers, to give a fresh appearance to home flowering potted plant, could influence source-sink relationship and postproduction. This study evaluated the effect of benzyladenine and senescent flowers removal on postproduction performance of 'Profusion Cherry', and observed the senescence symptoms. When plants, produced in greenhouse at São Paulo State, Brazil, had 4 to 5 open flowers, they were sprayed to runoff a single time (20ml/pot) with benzyladenine (0.4, 0.6, 0.8 or 1.0 mmol) and placed into plastic trays, without sleeve. The experimental design was a randomized blocks with 6 treatments (control, four benzyladenine concentrations and senescent flowers removal), 4 replications (2 pots per experimental unit), totalising 12 potted plants in each plastic tray (block). To simulate highway transport, plants remained for 4 days in a dark chamber, at 20.0 °C without irrigation. To include vibration, each plastic tray, was placed in an incubator shaker for 3hr a day, at 60 rpm, 25°C and darkness. After simulated transport, plants remained indoors (10h.day-1 with 18 μmol.m-2.s-1 PPF, 21.5 to 27.0°C and, 14 h.day-1 at darkness, 18.5 to 24.0°C) during 21 days. Plants performed well during simulated transport, and also indoors for two weeks. For most of evaluated parameters there was not significant effect of benzyladenine concentrations by Tukey's test. Senescent flowers removal did not delayed senescence or improved plants quality. The symptoms associated with the loss of decorative life were ray florets color fading and wilting, without abscission of flowers or petals.

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The aim of the study was to evaluate production and determine the level of total soluble solids for cherry tomatoes, under protected cultivation carried out with different types of spacing and pruning. The experiment was performed according to a randomized block design in a 2×2 factorial scheme, with two types of spacing between plants and two types of pruning, and with five repetitions. The cultivar 'Sindy' (De Ruiter) was utilized. Each experimental parcel contained seven plants, and fruits were collected from the five central plants. The seedlings were produced in Styrofoam trays of 128 cells and transplanted at 33 days after planting using two types of spacing between plants (0.3 and 0.5 m) and 1 m spacing between rows. The plants were grown as single-or double-stem form and staked individually. The parameters evaluated were the number of fruit per plant, fresh weight of fruit and the level of total soluble solids expressed in °Brix. There was no evidence of significant interaction between the treatments. For fresh weight of fruit per plant, there was a significant effect when the plants were grown with a spacing of 1 × 0.5 m, with 4.12 kg per plant, compared to a production of 3.00 kg per plant with a spacing of 1 × 0.3 m. With regard to the number of fruit per plant, a significant difference was seen between the two types of spacing, where a spacing of 1 × 0.3 m yielded a lower number of fruit per plant (188.8), compared to that observed with a spacing of 1 × 0.5 m (238.1). With regard to the two types of pruning, there was a significant effect for only the number of fruit per plant, where the mean number of fruit was 188.4 with one stem and 238.4 with two stems. No significant difference was observed between the treatments for the level of total soluble solids. It is concluded that for the cultivar 'Sindy', under protected cultivation, production is better with a spacing of 0.5 m between plants and the use of two stems per plant.

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Alguns exemplos de formação de minério supérgeno e sua interação com a morfogênese (paleosuperfícies) e resistência mineralógica são discutidas aqui. Registros geomorfológicos e mineralógicos na caracterização paleosuperfícies associam o intemperismo de minerais primários e sua relação com as concentrações de cobre e minério de ferro no sudeste do estado de São Paulo, Brasil. Distinguiram-se duas paleosuperfícies geradas por várias fases de intemperismo e controladas pela estrutura geológica. A primeira, mais antiga, é a paleosuperfície superior (900 - 1000 m de altitude), situado em Ribeirão Branco (Alto do Brancal), foram desenvolvidas em rochas silico-calcários. É formada por lateritas de ferro enriquecido por produtos secundários de cobre. O segundo nível de paleosuperfície é mais novo está localizado na região de Itapeva (Santa Blandina e Bairro do Sambra). Esta paleosuperfície é formada por percolação de cobre através da rocha alterada (saprolito). Outras características podem ser observadas como produtos neoformados em lateritas. Eles são classificados em dois tipos: a argila como produtos silico-cuprífero (com quantidades significativas de ferro) e de cobre minerais (crisocola, fixas nas vertentes). Essas feições reconheceram a presença de minérios de cobre e seu controle morfogénetico ajudando na exploração e prospecção de minérios supérgenos.

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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

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This manuscript aims proposing a methodology for correlating soil porosity to the respective geological units using geostatistical analysis techniques, including interpolation data by kriging. The site studied was in Lorena municipality, Paraíba do Sul Valley, southeastern Brazil. Specifically all studies were carried out within an area of 12 km2 located at Santa Edwirges farm. The database comprehended 41 soil samples taken at different geological and geomorphologic units at three different depths: surface, 50 cm and 100 cm depth. The geostatistical analyses results were correlated to a geological mapping specifically elaborated for the site. This mapping accounts for two different geological formations and a geological contact characterized by a shearing zone. The results indicate the existence of a significant relationship between the soil porosity and the respective geological units. The studies revealed that the residual soils from weathered granitic rocks tend to have higher porosities than the residual soils from weathered biotite gneiss rocks, while the soil porosity within the shearing zone is relatively un-sensitive to the respective geological formation. The spatial patterns observed were efficient to evaluate the relationship between the soil porosity, geology unit and the and geomorphology showing a good potential for correlating with others soil properties such as hydraulic conductivity, soil water retention curves and erosion potentials.