999 resultados para Gremios-Valencia-1849


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Diagnosis and Recommendation Integrated System (DRIS) applies nutrient ratios instead of the isolated concentration values of each nutrient in interpretation of tissue analysis. The objectives of this research were to establish adequate DRIS norms for 'Valencia' sweet orange irrigated commercial groves budded on three rootstocks and correlate indexes of nutrition balance with yield. Experiments were conducted in São Paulo State, Brazil. Rootstocks Rangpur lime, Caipira sweet orange, and Poncirus trifoliata, with more than six years old and yield above 40 ton ha-1 were utilized. Data referred to yield, tree spacing, rootstock and foliar concentrations of N, P, K, Ca, Mg, S, Fe, Mn, Cu, Zn, and B in non fruiting terminals for each grove were processed for the years 1994 through 1998. DRIS indexes were calculated by Nick criterion for choosing the ratio order of the nutrients and Jones calculation method of the ratio functions. Indexes of nutritional balance calculated from DRIS norms presented high correlation with yield for the three scion/rootstock combinations. DRIS norms defined in this research are valid, since leaf sampling is done on non fruiting terminals and the grove is irrigated.

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The objective of this work was the transformation of tobacco and 'Valencia' sweet orange with the GUS gene driven by the citrus phenylalanine ammonia-lyase (PAL) gene promoter (CsPP). Transformation was accomplished by co-cultivation of tobacco and 'Valência' sweet orange explants with Agrobacterium tumefaciens containing the binary vector CsPP-GUS/2201. After plant transformation and regeneration, histochemical analyses using GUS staining revealed that CsPP promoter preferentially, but not exclusively, conferred gene expression in xylem tissues of tobacco. Weaker GUS staining was also detected throughout the petiole region in tobacco and citrus CsPP transgenic plants.

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In orange commercial farms, Zn deficiencies symptoms and small fruits were observed in Corrientes, Argentine. During four years (1995 to 1998), Valencia orange (Citrus sinensis Osb.) on Rough lemon (C. jambhiri Lush.) rootstock, implanted in 1974 in sandy soil, where six treatments were tested. Treatments varied from 1 to 3 Kg KCl.tree-1.year-1 (applied in April and December) with and without Zineb 80, 0,35%. year-1, 20 L. tree-1 (13,3 g Zn.tree-1 applied in December). The experimental design was a randomized complete block with four replications, with a single tree and borders in the experimental plot. Foliar sample were taken every year in Autumn and Summer, foliar concentrations of Zn and K were determined by atomic spectrum absorption. Harvested fruits were classified into small, medium and big. Analysis of Variance, Tukey test and Pearson correlations between production and foliar concentrations were performed. Higher fertilization levels of K with Zn increased medium and big fruits production (Kg and percentage). Foliar concentrations of K and Zn were positively correlated with big and medium fruit production and negatively correlated with small one. Chemical names used: Ethilenbis-ditiocarbamate of Zn (Zineb).

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Después de las discusiones en Suiza sobre dinámica glaciar, algunos países europeos fueron explorados durante el siglo XIX para comprobar las hipótesis generadas en los Alpes. España fue el campo de trabajo de muchos científicos (J. Macpherson, A. Penck, II. Obermaier) que se interesaron por el límite sur de las glaciaciones cuaternarias. Consideramos al geólogo alemán Ilugo Obermaier como el introductor de la moderna glaciología en España enire 1914-17, seguido por otros científicos: II uguet del Villar, J. Carandell, L. Fernández Navarro y E. Ilernández Pacheco, quienes trabajaron en el Sistema Ibérico, Sistema Central y Sierra Nevada. Por tanto, este artículo no recoge la glaciología pirenaica, llevada también a cabo por geólogos franceses.

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En el presente artículo se advierte de la presencia del pseudococcino Rhizoecus cacticans (HAMBLETON) en la zona de Valencia, atacando a raíces de cactáceas. Se dan algunas características del género y se describe la especie, así como algunos datos sobre los daños que causa. Se indican procedimientos posibles de control.

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Urbano Fos fue uno de los mejores representantes del Barroco valenciano. En este estudio atribuimos a su pincel un lienzo inédito de gran calidad. Se trata de una magnífica representación de San Pascual Bailón. Con nuestra investigación hemos demostrado sus filiaciones técnico-artísticas y resaltado aquellos aspectos por los que se popularizó su pintura.

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Los modelos de crecimiento de frutos describen la evolución de su tamaño a lo largo del período de desarrollo. Con fines de pronóstico, estos modelos permiten estimar en forma anticipada el tamaño que alcanzarán los frutos al momento de la cosecha. Para lograr estimaciones insesgadas del tamaño de frutos a cosecha es necesario un diseño adecuado de muestreo en la etapa de recolección de datos. El objetivo del presente trabajo fue determinar el tamaño óptimo de muestra, compuesta por árboles (n) y frutos (m), para establecer modelos de crecimiento de frutos de naranjo 'Valencia late', que permitan estimar la distribución de tamaño a la cosecha. Se trabajó con el diámetro ecuatorial de frutos previo a la cosecha, proveniente de dos huertos comerciales ubicados en la provincia de Corrientes, Argentina, durante tres temporadas. Mediante modelos mixtos se estimaron las componentes de varianzas entre árboles y frutos, y posteriormente a partir de dos tipos de metodologías se determinó el tamaño de muestra óptimo. La variabilidad entre frutos fue superior a la variabilidad entre árboles. Para la determinación del patrón de crecimiento de frutos de naranjo 'Valencia late' mediante un muestreo bietápico, se sugiere seleccionar 7 árboles y 30 frutos de cada árbol, para lograr estimaciones del diámetro ecuatorial de frutos con una precisión entre el 2 y 3%.

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Mesozoic and Neogene carbonates located in the Valencia Trough (offshore Spain, western Mediterranean Sea)are oil reservoirs. This paper investigates the diagenetic evolution of the Upper Jurassic limestones, currently dolomitized, that constitute the main reservoir of the Casablanca oil field. Core samples from Casablanca-1A well have been studied to determine the diagenetic products and their relation with porosity evolution, and to reconstruct the fluid flow history prior to and during oil emplacement. On the basis of petrological observations and geochemical analyses (major, minor and trace element composition and oxygen, carbon and strontium isotope composition), a major dolomitization event is recognized postdating subaerial exposure, erosion and karstification. The dolomitization event originated two replacive dolomites (RD1 and RD2) and two dolomite cements (saddle dolomite cement, SDC, and milky-white dolomite cement, MDC)which are partially cogenetic. RD1, RD2 and SDC precipitated at increasing temperatures (over 60ºC and below 110ºC), probably from meteoric water mixed with marine water. The last dolomite type milky-white dolomite cement) precipitated with increasing burial conditions and by arrival of hydrothermal fluids during the Miocene. The post-dolomitization sequence comprises precipitation of calcite cement and partial calcitization of all previous dolomites. The oxygen, carbon and strontium isotope compositions suggest that this calcite cementation occurred from meteoric waters mixed with Burdigalian - Langhian marine waters trapped in the sediments and expelled by compaction in the moderate to deep burial realm. Normal faults were the conduits for upward migration of these fluids as well as for later oil expulsion from the Burdigalian - Langhian source rocks. Late corrosion associated with organic acid-enriched fluids took place prior or simultaneously to oil migration during the Pliocene, enhancing porosity and increasing eservoir quality.

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El Triásico Superior del sector central valenciano de la Cordillera Ibérica presenta una facies germánica (Keuper) integrada por dos secuencias evaporíticas separadas por un episodio detrítico principal. Los datos preliminares obtenidos de una investigación palinológica en curso revelan una edad Karniense para todos estos materiales.