999 resultados para Diálogo experimental


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Resumen: La presente entrevista a Eugenio Guasta pertenece al proyecto de reconstrucción de la historia del diálogo entre literatura y teología en la Argentina, emprendido por el Seminario Interdisciplinario Permanente Literatura, Estética y Teología de la Facultad de Teología (UCA). En la misma línea de las entrevistas ya realizadas a Lucio Gera y Juan Carlos Scannone (cf. Teología 99 y 102), también ésta busca recoger la trama viva del interés de la teología por la literatura. El caso del actual entrevistado se distingue de los casos anteriores en el hecho de que se trata de un sacerdote y formador que proviene del ámbito literario y que mantiene una explícita vinculación con los escritores y académicos argentinos que signaron la cultura literaria de la segunda mitad del siglo XX.

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Este trabajo se estableció en la época de primera del 2010, en el Centro Experimental del Valle de Sébaco del Instituto Nicaragüense de Tecnología Agropecuaria, en el municipio de San Isidro, departamento de Matagalpa, con el objetivo de evaluar 10 líneas precoces de sorgo con buen comportamiento agronómico y productivo que se adapten a las condiciones ambientales de la zona. Se utilizó un diseño de bloques completos al azar (BCA) con 12 tratamientos y 4 repeticiones, evaluando variables de crecimiento, desarrollo y produccion, los datos obtenidos se sometieron al análisis de varianza (ANDEVA) y al análisis de agrupamiento a través de Tuckey (∞=0.05). Además se evaluaron variables cualitativas. El análisis de varianza no muestra diferencias estadísticas entre líneas para las variables peso de panoja, peso de mil granos y rendimiento de grano, sin embargo las demás variables de producción, crecimiento y desarrollo si presentaron diferencias estadísticamente significativas.

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Se evaluaron siete genotipos de tomate (Lycopersicum esculentum, Mill.) de los cuales AVTO1203, AVTO1883, AVTO1082, AVTO1031 y AVTO1173 provienen del Centro Mundial de Vegetales (AVDRDC) y dos variedades comerciales Shanty y Butero, que se usaron como testigos. El ensayo se estableció en el centro experimental ̈LAS MERCEDES̈ propiedad de la Universidad Nacional Agraria con el propósito de evaluar el comportamiento agronómico de los genotipos bajo sistema casa malla. El diseño experimental utilizado fue un bloque completo al azar, el análisis de la información se realizo utilizando análisis de varianza y separación de medias por TUKEY. Los genotipos mostraron diferencias estadísticamente significativas para las variables evaluadas, con excepción de los grados Brix, cuyos valores oscilaron entre 4.5 y 4.6. Los genotipos mostraron forma de fruto redondeada y redondo-alargada, en general el color de fruto fue rojo con distintas tonalidades oscuro e intermedio. Para el diámetro polar el carácter vario entre 6.36 cm y 3.8 cm; el diámetro ecuatorial vario de 4.89 cm y 2.72 cm. los genotipos presentaron números de lóculos de 6.6 a 2. Con respecto a frutos por plantas los valores oscilaron de 55.8 y 17.1 siendo los genotipos: A VTO1883, AVTO1203, y AVTO1082 los que estadísticamente se encontraron en la categoría superior con el testigo Shanty. El peso de los frutos vario entre 101.1 g y 58.1 g. Para el rendimiento los valores oscilaron entre 18.9 kg y 6 kg/parcela (la parcela fue de 2m2), los genotipos AVTO1203, AVTO1883, AVTO1082 y AVTO1173 se encontraron estadísticamente en la categoría superior con la variedad testigo Shanty. Basado a las características estudiadas se determinó que los genotipos AVTO1203 y AVTO1883 son promisorios por presentar similitud en rendimiento y características comerciales con el hibrido testigo Shanty.

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This work is devoted to study of the slip phenomenon between phases in water-oil two-phase flow in horizontal pipes. The emphasis is placed on the effects of input fluids flow rates, pipe diameter and viscosities of oil phase on the slip. Experiments were conducted to measure the holdup in two horizontal pipes with 0.05 m diameter and 0.025 m diameter, respectively, using two different viscosities of white oil and tap water as liquid phases. Results showed that the ratios of in situ oil to water velocity at the pipe of small diameter are higher than those at the pipe of big diameter when having same input flow rates. At low input water flow rate, there is a large deviation on the holdup between two flow systems with different oil viscosities and the deviation becomes gradually smaller with further increased input water flow rate. (C) 2008 Elsevier Inc. All rights reserved.

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Thermocapillary convection coupling with the evaporation effect of evaporating liquids is studied experimentally. This study focused on an evaporation liquid layer in a rectangular cavity subjected to a horizontal temperature gradient when the top evaporating surface is open to air, while most previous works only studied pure thermocapillary convection without evaporation. Two liquids with different evaporating rates are used to study the coupling of evaporation and thermocapillary convection, and the interfacial temperature profiles for different temperature gradients are measured. The experimental results indicate evidently the influence of evaporation effect on the thermocapillary convection and interfacial temperature profiles. The steady multicellular flow and the oscillatory multicellular flow in the evaporation liquid layer are observed by using the particle-image-velocimetry method.

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An on-board space experiment of bubble thermocapillary migration was performed in the Chinese 22nd recoverable satellite in 2005. Silicone oil of nominal viscosity 5cSt was used as the continuous phase in the experiment. Air bubbles were injected into the liquid in the same direction as the constant temperature gradient in the liquid. The velocities of bubbles were obtained by recording the paths of the bubbles. The results indicate that the scaled velocity of bubbles decreases with an increase of the Marangoni number extended to 9288, which agrees with the results of previous space experiments and numerical simulation. In addition, the interaction between two bubbles was also observed in the space experiment. The trajectories and the velocities of the bubbles were obtained. The two-bubble experiment results are also consistent with the theoretical analysis.

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An experimental investigation was conducted to study the holdup distribution of oil and water two-phase flow in two parallel tubes with unequal tube diameter. Tests were performed using white oil (of viscosity 52 mPa s and density 860 kg/m(3)) and tap water as liquid phases at room temperature and atmospheric outlet pressure. Measurements were taken of water flow rates from 0.5 to 12.5 m(3)/h and input oil volume fractions from 3 to 94 %. Results showed that there were different flow pattern maps between the run and bypass tubes when oil-water two-phase flow is found in the parallel tubes. At low input fluid flow rates, a large deviation could be found on the average oil holdup between the bypass and the run tubes. However, with increased input oil fraction at constant water flow rate, the holdup at the bypass tube became close to that at the run tube. Furthermore, experimental data showed that there was no significant variation in flow pattern and holdup between the run and main tubes. In order to calculate the holdup in the form of segregated flow, the drift flux model has been used here.

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Deformation twins have been observed in nanocrystalline (nc) fcc metals with medium-to-high stacking fault energies such as aluminum, copper, and nickel. These metals in their coarse-grained states rarely deform by twining at room temperature and low strain rates. Several twinning mechanisms have been reported that are unique to nc metals. This paper reviews experimental evidences on deformation twinning and partial dislocation. emissions from grain boundaries, twinning mechanisms, and twins with zero-macro-strain. Factors that affect the twinning propensity and recent analytical models on the critical grain sizes for twinning are also discussed. The current issues on deformation twinning in nanocrystalline metals are listed.

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With the PDPA (Phase Doppler Particle Analyzer) measurement technology, the probability distributions of particle impact and lift-off velocities on bed surface and the particle velocity distributions at different heights are detected in a wind tunnel. The results show that the probability distribution of impact and lift-off velocities of sand grains can be expressed by a log-normal function, and that of impact and lift-off angles complies with an exponential function. The mean impact angle is between 28 degrees and 39 degrees, and the mean lift-off angle ranges from 30 degrees to 44 degrees. The mean lift-off velocity is 0.81-0.9 times the mean impact velocity. The proportion of backward-impacting particles is 0.05-0.11, and that of backward-entrained particles ranges from 0.04 to 0.13. The probability distribution of particle horizontal velocity at 4 mm height is positive skew, the horizontal velocity of particles at 20 mm height varies widely, and the variation of the particle horizontal velocity at 80 mm height is less than that at 20 mm height. The probability distribution of particle vertical velocity at different heights can be described as a normal function.

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Results from a space experiment on bubble thermocapillary migration conducted on board the Chinese 22nd recoverable satellite were presented. Considering the temperature field in the cell was disturbed by the accumulated bubbles, the temperature gradient was corrected firstly with the help of the temperature measurement data at six points and numerical simulation. Marangoni number (Ma) of single bubble migrating in the space experiment ranged from 98.04 to 9288, exceeding that in the previous experiment data. The experiment data including the track and the velocity of two bubble thermocapillary migration showed that a smaller bubble would move slower as it was passed by a larger one, and the smaller one would even rest in a short time when the size ratio was large enough.

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Sand velocity in aeolian sand transport was measured using the laser Doppler technique of PDPA (Phase Doppler Particle Analyzer) in a wind tunnel. The sand velocity profile, probability distribution of particle velocity, particle velocity fluctuation and particle turbulence were analyzed in detail. The experimental results verified that the sand horizontal velocity profile can be expressed by a logarithmic function above 0.01 in, while a deviation occurs below 0.01 m. The mean vertical velocity of grains generally ranges from -0.2 m/s to 0.2 m/s, and is downward at the lower height, upward at the higher height. The probability distributions of the horizontal velocity of ascending and descending particles have a typical peak and are right-skewed at a height of 4 turn in the lower part of saltation layer. The vertical profile of the horizontal RMS velocity fluctuation of particles shows a single peak. The horizontal RMS velocity fluctuation of sand particles is generally larger than the vertical RMS velocity fluctuation. The RMS velocity fluctuations of grains in both horizontal and vertical directions increase with wind velocity. The particle turbulence intensity decreases with height. The present investigation is helpful in understanding the sand movement mechanism in windblown sand transport and also provides a reference for the study of blowing sand velocity. (C) 2007 Elsevier B.V All rights reserved.

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The relationship between hardness (H), reduced modulus (E-r), unloading work (W-u), and total work (W-t) of indentation is examined in detail experimentally and theoretically. Experimental study verifies the approximate linear relationship. Theoretical analysis confirms it. Furthermore, the solutions to the conical indentation in elastic-perfectly plastic solid, including elastic work (W-e), H, W-t, and W-u are obtained using Johnson's expanding cavity model and Lame solution. Consequently, it is found that the W-e should be distinguished from W-u, rather than their equivalence as suggested in ISO14577, and (H/E-r)/(W-u/W-t) depends mainly on the conical angle, which are also verified with numerical simulations. (C) 2008 American Institute of Physics.

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Benard-Marangoni convections of two-layer fluids heated from the bottom are investigated experimentally with a particle imagine velocimetry. The flows are visualized from the side, and various velocity fields near the onset of convection, such as three-layer vortex convective patterns, are observed when the depth ratio varies in a wide range. A new classification of the convective patterns is proposed with more detail than in previous studies. The analysis of the results indicates that the interface tension greatly influences the motion intensities of the bottom and top layers. The dimensionless wave number increases with the Bond number when the motion in the top layer is not more intense than that in the bottom layer, which agrees with the theoretical prediction.

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We investigate the surface deformations of buoyant-thermocapillary convection in a rectangular cavity clue to gravity and temperature gradient between the two sidewalls. The cavity is 52mm x 42mm in horizontal cross section, the thickness of liquid layer h is changed from 2.5mm to 6.5mm. Surface deformations of h = 3.5mm and 6.0mm are discussed and compared. Temperature difference is increased gradually, and the flow in the liquid layer will change from stable convection to unstable convection. Two kinds of optical diagnostic system with image processor are developed for study of the kinetics of buoyant-thermocapillary convection, they give out the information of liquid free surface. The quantitative results are calculated by Fourier transform and correlation analysis, respectively. With the increasing temperature gradient, surface deformations calculated are more declining. It is interesting phenomenon that the inclining directions of the convections in thin and thick liquid layers are different. For a thin layer, the convection is mainly controlled by thermocapillary effect. However, for a thick layer, the convection is mainly controlled by buoyancy effect. The surface deformation theoretically analysed is consistent with our experimental results. The present experiment proves that surface deformation is related to temperature gradient and thickness of the liquid layer. In other words, surface deformation lies on capillary convection and buoyancy convection.