Programa de electricidad b??sica

Proyecto Experiencias en el Aula, curso 97-98. Ayudas a la Innovaci??n Educativa, 1997-98. Anexo Memoria en C-Innov. 79

Matem??ticas de primero de Bachillerato con DERIVE : memoria final

Ayudas a la Innovaci??n Educativa, 1997-98. Anexo Memoria en C-Innov. 80

Mamá lee el periódico y papá friega los platos ¿y por qué no? rechaza los materiales sexistas.

Premios Educación y Sociedad 1995. El ejemplar con R.111495 no tiene el cartel ni el ejemplar fotocopiado. Anexo Memoria en C- Innov.56

Nuestro colegio : un centro saludable.

Ayudas concedidas a proyectos de innovación educativa para el curso 1997-1998. Contiene: el proyecto, anexos y nõ 5 de la Revista Escolar La Cigüeña

A systematic and feasible method for computing nuclear contributions to electrical properties of polyatomic molecules

An analytic method to evaluate nuclear contributions to electrical properties of polyatomic molecules is presented. Such contributions control changes induced by an electric field on equilibrium geometry (nuclear relaxation contribution) and vibrational motion (vibrational contribution) of a molecular system. Expressions to compute the nuclear contributions have been derived from a power series expansion of the potential energy. These contributions to the electrical properties are given in terms of energy derivatives with respect to normal coordinates, electric field intensity or both. Only one calculation of such derivatives at the field-free equilibrium geometry is required. To show the useful efficiency of the analytical evaluation of electrical properties (the so-called AEEP method), results for calculations on water and pyridine at the SCF/TZ2P and the MP2/TZ2P levels of theory are reported. The results obtained are compared with previous theoretical calculations and with experimental values

Vida y obra de Pere Torroella

"ADVERTIMENT. La versió definitiva d'aquesta tesi doctoral està en premsa a l'editorial Barcino, Col·lecció Els Nostres Clàssics, Barcelona. En la nova versió s'hi han introduit nombroses millores, nous capítols i correccions importants. Es prega que, per a qualsevol citació, s'utilitzi la versió definitiva" Pere de Torroella ingresó en la corte de Juan de Navarra (luego Juan II de Aragón) en 1436, a quien sirvió como escudero y copero tanto en las escaramuzas de Castilla como en la corte de Navarra, donde fue sirviente de Carlos de Aragón, Príncipe de Viana e hijo del rey Juan. A finales de 1450 se trasladó a Nápoles junto don Juan de Aragón, hijo bastardo de Juan de Navarra. Permaneció allí hasta la muerte del rey Alfonso el Magnánimo en 1458. Durante esos años entabló amistad con humanistas como Giovanni Pontano, y ejerció de mayordomo del príncipe bastardo Juan II de Aragón, a quien Pere Torroella sirvió durante toda su vida. A finales de 1450 se trasladó a Nápoles junto don Juan de Aragón, hijo bastardo de Juan de Navarra. Permaneció allí hasta la muerte del rey Alfonso el Magnánimo en 1458. Durante esos años entabló amistad con humanistas como Giovanni Pontano, y ejerció de mayordomo del príncipe bastardo. En 1458, tras la muerte del rey Alfonso y el ascenso al trono de su hermano Juan, Pere Torroella se trasladó a Zaragoza y Barcelona como emisario de Carlos de Viana, a quien sirvió hasta su muerte, en 1461. Un año después, en 1462, estalló la guerra civil catalana (que enfrentó a la Generalitat de Catalunya y a la monarquía aragonesa), y Torroella luchó en los primeros años junto a los rebeldes. En 1464 se pasó al bando real, al que permaneció fiel hasta el final de la guerra, en 1472. Desde 1472 hasta su muerte (acaecida seguramente en 1492), Pere Torroella ejerció de consejero del rey Juan II en Barcelona, pero tras la muerte del rey en 1479 se retiró a sus dominios en el Ampurdán, donde murió. Pere Torroella es autor de obra en catalán y en castellano. En la primera lengua compuso lais, canciones al estilo de Ausiàs March, un soneto (el primero documentado en lengua catalana) y un ambicioso poema colectivo que empieza con el verso Tant mon voler. En castellano, es autor de decires amorosos, canciones y esparzas. También mantuvo un intenso intercambio epistolar con influyentes personalidades de las cortes aragonesas, como Francesc Ferrer, Hugo de Urríes, Bernat Hug de Rocabertí y Pedro de Urrea. Compuso, finalmente, varias composiciones en prosa de alto interés histórico y literario, como la Complanta por la muerte de Inés de Clèves (1448), la Consolatoria por la muerte de mosén Martín de Ansa (1451) y el Razonamiento en defensión de las donas, donde el autor se excusa por haber compuesto las famosas coplas de Maldezir de mugeres. Torroella fue una figura central en las cortes aragonesas de la época, y su obra literaria alcanzó gran difusión y estima entre los hombres de su siglo, como muestran sus epistolarios y los autores que decidieron imitar sus versos. Fue, por otro lado, un poeta sensible a las novedades líricas del momento. Asimiló los aspectos más superficiales de la poesía de Ausiàs March, conoció y admiró los versos de Petrarca, leyó con fruición la lírica francesa (y especialmente Oton de Grandson y Guillaume de Machaut), e imitó con destreza las poesía musical de Jordi de Sant Jordi y Martí Garcia. No siempre su gran cultura se vio reflejada en la calidad de sus obras, que presentan, sin embargo, un indudable interés para la historia de la literatura.

Recognizing emotion in illustrations and photographs: Comparing responses of children who are deaf or hard of hearing with those of children with normal hearing

Recognizing emotions are something children do everyday, whether it is identifying that mom is sad because she lost her job or that a character in a story is mad because no one will listen to him. The purpose of this study is to find out if recognizing emotions is easier to do with realistic photographs or illustrations.

Tactile localization of acoustic stimuli with an earmold vibratrory aid

This study examines the tactile localization of sound sources utilizing an earmold vibratory hearing aid.

Does reactive surface area depend on grain size? Results from pH 3, 25 circle C far-from-equilibrium flow-through dissolution experiments on anorthite and biotite

Laboratory determined mineral weathering rates need to be normalised to allow their extrapolation to natural systems. The principle normalisation terms used in the literature are mass, and geometric- and BET specific surface area (SSA). The purpose of this study was to determine how dissolution rates normalised to these terms vary with grain size. Different size fractions of anorthite and biotite ranging from 180-150 to 20-10 mu m were dissolved in pH 3, HCl at 25 degrees C in flow through reactors under far from equilibrium conditions. Steady state dissolution rates after 5376 h (anorthite) and 4992 h (biotite) were calculated from Si concentrations and were normalised to initial- and final- mass and geometric-, geometric edge- (biotite), and BET SSA. For anorthite, rates normalised to initial- and final-BET SSA ranged from 0.33 to 2.77 X 10(-10) mol(feldspar) m(-2) s(-1), rates normalised to initial- and final-geometric SSA ranged from 5.74 to 8.88 X 10(-10) mol(feldspar) m(-2) s(-1) and rates normalised to initial- and final-mass ranged from 0.11 to 1.65 mol(feldspar) g(-1) s(-1). For biotite, rates normalised to initial- and final-BET SSA ranged from 1.02 to 2.03 X 10(-12) mol(biotite) m(-2) s(-1), rates normalised to initial- and final-geometric SSA ranged from 3.26 to 16.21 X 10(-12) mol(biotite) m(-2) s(-1), rates normalised to initial- and final-geometric edge SSA ranged from 59.46 to 111.32 x 10(-12) mol(biotite) m(-2) s(-1) and rates normalised to initial- and final-mass ranged from 0.81 to 6.93 X 10(-12) mol(biotite) g(-1) s(-1). For all normalising terms rates varied significantly (p <= 0.05) with grain size. The normalising terms which gave least variation in dissolution rate between grain sizes for anorthite were initial BET SSA and initial- and final-geometric SSA. This is consistent with: (1) dissolution being dominated by the slower dissolving but area dominant non-etched surfaces of the grains and, (2) the walls of etch pits and other dissolution features being relatively unreactive. These steady state normalised dissolution rates are likely to be constant with time. Normalisation to final BET SSA did not give constant ratios across grain size due to a non-uniform distribution of dissolution features. After dissolution coarser grains had a greater density of dissolution features with BET-measurable but unreactive wall surface area than the finer grains. The normalising term which gave the least variation in dissolution rates between grain sizes for biotite was initial BET SSA. Initial- and final-geometric edge SSA and final BET SSA gave the next least varied rates. The basal surfaces dissolved sufficiently rapidly to influence bulk dissolution rate and prevent geometric edge SSA normalised dissolution rates showing the least variation. Simple modelling indicated that biotite grain edges dissolved 71-132 times faster than basal surfaces. In this experiment, initial BET SSA best integrated the different areas and reactivities of the edge and basal surfaces of biotite. Steady state dissolution rates are likely to vary with time as dissolution alters the ratio of edge to basal surface area. Therefore they would be more properly termed pseudo-steady state rates, only appearing constant because the time period over which they were measured (1512 h) was less than the time period over wich they would change significantly. (c) 2006 Elsevier Inc. All rights reserved.

The three-dimensional vortical nature of atmospheric and oceanic turbulent flows

Using a novel numerical method at unprecedented resolution, we demonstrate that structures of small to intermediate scale in rotating, stratified flows are intrinsically three-dimensional. Such flows are characterized by vortices (spinning volumes of fluid), regions of large vorticity gradients, and filamentary structures at all scales. It is found that such structures have predominantly three-dimensional dynamics below a horizontal scale LLR, where LR is the so-called Rossby radius of deformation, equal to the characteristic vertical scale of the fluid H divided by the ratio of the rotational and buoyancy frequencies f/N. The breakdown of two-dimensional dynamics at these scales is attributed to the so-called "tall-column instability" [D. G. Dritschel and M. de la Torre Juárez, J. Fluid. Mech. 328, 129 (1996)], which is active on columnar vortices that are tall after scaling by f/N, or, equivalently, that are narrow compared with LR. Moreover, this instability eventually leads to a simple relationship between typical vertical and horizontal scales: for each vertical wave number (apart from the vertically averaged, barotropic component of the flow) the average horizontal wave number is equal to f/N times the vertical wave number. The practical implication is that three-dimensional modeling is essential to capture the behavior of rotating, stratified fluids. Two-dimensional models are not valid for scales below LR. ©1999 American Institute of Physics.