Saint Teresa of Jesus Catholic University, , commonly known as the Catholic University of Ávila , is a private, Catholic university, located in Ávila, Castile and León, Spain. It's named after Saint Teresa of Ávila.The current rector of the university is Maria Rosario Sáez Yuguero. Wikipedia.
Pachon-Garcia F.T.,Catholic University of Avila
AEU - International Journal of Electronics and Communications | Year: 2016
This paper shows the calculation of electric field levels at MF band (medium frequency: 300. kHz-3. MHz) at different distances from the transmitter in environments where there are: (a) conductivity changes of the soil and (b) altitude variations. To assess the influence of these factors, a 2D tool named MF-FDTD (MF finite-difference time-domain) is implemented and it is calibrated and validated with the Millington method for flat land, and the FEM-PE (Finite Element Method-Parabolic Equation) for the inclusion of typified mountains. Then, this tool is also applied to real environments where certain AM (Amplitude Modulation) transmitters are located, selecting several profiles via a Geographic Information System. In our case, oscillations up to 10. dB have been obtained when comparing the results of irregular versus flat terrains with frequencies around 1. MHz. Part of the computation has been made using the Lusitania supercomputer, parallelizing tasks on multiple cores. © 2016 Elsevier GmbH.
Adjustment of SCS Curve Number tables for forest covers of the "Caldera de Taburiente" National Park (La Palma island, Spain) [Adaptación de las tablas del número de curva para las formaciones vegetales del parque nacional de la caldera de taburiente (isla de la Palma, España)]
Mongil Manso J.,Catholic University of Avila
Boletin Geologico y Minero | Year: 2010
SCS Curve Number Method estimates superficial runoff that a rainfall generates. Its practical application consists of locating in a table the curve number, which depends principally on soil use or type of vegetation, hydrological condition and type of soil (hydrologie soil groups). With this curve number, runoff is calculated through the equation proposed by the model. The mentioned tables are elaborated for the types of soils and vegetation of the United States. In this work, an adjustment of SCS Curve Number tables for forest covers of the "Caldera de Taburiente" National Park (La Palma island, Spain) is realized, through an analysis of factors that establish curve number.
Cottle D.J.,University of New England of Australia |
Romero C.,Technical University of Madrid |
Romero C.,Catholic University of Avila
Animal Feed Science and Technology | Year: 2014
It is difficult to measure pasture feed intake. A common method is based on naturally occurring, indigestible plant markers, such as long chain alkanes. Least-squares procedures are used to estimate diet composition and intake. If actual intake of a supplement is known, then total intake and the intake of all dietary components can be estimated. This 'labelled-supplement' approach requires an estimate of the faecal recoveries of the markers. The accuracy and precision of intake solutions for each animal is also affected by the sampling and measurement precision of the plant and faecal marker concentrations. This work was conducted to study whether weighting each marker's sums of squares in the least-squares procedure could be used to provide a more robust solution.Cluster and discriminant analyses of a plant marker database determined the contribution of each marker to discrimination between categories of plants. The markers' cluster or discriminant weights were used to weight the sums of squares in the least squares procedures. The actual individual dry matter intakes (DMI) of 20 cattle were arbitrarily assigned for three different diets. Measurement and sampling variations in marker concentrations and/or faecal recoveries were simulated to generate predicted total pasture intakes around the actual values.Six marker weighting methods were compared for their DMI prediction error values and correlations between predicted and actual DMI: (A) all markers weighted by one; (B) separate cluster analyses of z scores for alkanes and alcohols; (C) combined cluster analyses for alkanes and alcohols; (D) discriminant analyses of z score marker data for plants categorized into grasses, legumes, shrubs and trees; (E) discriminant analyses of plants categorized on origin and plant, photosynthesis and reproduction type; and (F) discriminant analyses of plants categorized on plant, photosynthesis and reproduction type.The standard approach of weighting all markers by one (A) was satisfactory when marker concentration error was set at zero, however intake predictions were poor when the error was non-zero, which is likely. The weighted least-squares intake solutions that were more robust to variance in measured marker concentrations or in assumed faecal recovery rates were those using weights derived by methods D and F. Marker weights from Methods D, E and F resulted in similar intake prediction error variances and correlations. Methods E and F required more botanical information about plant species and method D was simpler, so method D is recommended rather than other methods studied here, including the standard method A. There are problems with using weights derived from an analysis of all published marker data, so better weighting methods may still be found for specific plant and marker datasets. © 2013 Elsevier B.V.
Romero C.,Technical University of Madrid |
Romero C.,Catholic University of Avila |
Martinez E.,Technical University of Madrid
European Journal of Physics | Year: 2013
Among other skills, a capacity for abstraction and good spatial awareness are needed to succeed in physics courses. According to the prevailing low percentages of passed students on these courses, a great proportion of those students are likely to lack these skills. Our working hypothesis is that simulations could help engineering students visualize physical phenomena and thereby gain a better understanding of physical theoretical concepts and achieve higher grades. Two groups of students (n1 = 40 and n2 = 43) took the same fluid mechanics course at an engineering school. Both groups took the same end-of-course examination, but only group 1 was simulation-taught. For that purpose, 15 original simulations were created with GeoGebra software. Simulation-taught students completed a questionnaire on the interest of using simulations to teach fluid mechanics. Simulations designed in this work covered all the concepts taught on the course and overcame criticisms made on previous simulations also created to teach fluid mechanics. At the examination, the average grade and the percentage of passed students were higher in group 1 than in group 2. When surveyed, group 1 students declared that they enjoyed interacting with the simulations and considered them to be a good complement to the theoretical explanations because simulations helped them revise previously explained concepts. Simulations assisted students with difficulties to visualize and understand physical theoretical concepts but still students performed poorly on the examination. Additional strategies need to be adopted in order to help students develop the skills required to succeed in physics courses. © 2013 IOP Publishing Ltd.
Hevia J.N.,University of Valladolid |
de Araujo J.C.,Federal University of Ceara |
Manso J.M.,Catholic University of Avila
Earth Surface Processes and Landforms | Year: 2014
This paper presents the history of badland generated in the Saldaña region, Spain; as well as the main responses eight decades after the start of restoration - in terms of vegetation, soil and erosive processes. The restoration consisted of intense reforestation and construction of more than 100 check dams and numerous wattle fences. Presently, the dense vegetation (87% cover) contrasts markedly with the degraded landscape from the early 20th century (5% cover). The thickness of litter and the natural presence of some species (Quercus pyrenaica, Paeonia broteroi and Lactarius deliciosus) clearly indicate the recovery of the site. The development of the forest cover shows that the intervention has the potential to recover almost 90% of the area. There is also evidence of soil regeneration, although some properties (erodibility, resistance to penetration and shear-strength resistance) are not that different between the forested and degraded areas. In the restored zones, runoffis negligible, since a thick layer of moss covers the spillways of all the check dams. Erosion has almost been stopped by the effects of vegetation cover, litter and higher infiltration rates (infiltration rate in forested slopes is 43.4 times greater than in bare slopes). Sediment detachment, such as landslides, mudflows and piping, still occur, but are restricted to the degraded zones. Furthermore, even when sediments are mobilized from the upper degraded hillslopes during the larger storms events (2000-2010), check dams and the lower elevation restored forest-buffers effectively work to reduce the sediment yield into the Carrión River by almost three orders of magnitude (<102 mg L-1), compared with data from the 1930s and 1940s (>105 mg L-1). © 2014 John Wiley & Sons, Ltd.