Elementos de competitividad para la general Motors Colmotores, en el marco del TLC Colombia - USA

el primer capitulo de esta monografía, se va a entender de una manera concisa cual es la dinámica de funcionamiento de la industria automotriz en general, teniendo en cuenta sus diversas facetas, como lo son el ensamblaje automotriz y algunos aspectos de cómo se maneja en negocio en el ámbito comercial y su importancia dentro de la economía de los estados. En el segundo capitulo se contextualizara e ubicara dentro de un ámbito regional, pasando por como se estructura a nivel de la Comunidad Andina de Naciones (CAN), hasta llegar al panorama local colombiano, enfocándose en la General Motors Colmotores, como la ensambladora mas fuerte del mercado Colombiano en la actualidad. En el tercer capitulo se establecerá cual es el marco jurídico que rige al sector automotriz, partiendo desde una perspectiva subregional, con el estudio del convenio automotor andino, el cual se convierte en el piso jurídico del sector en el marco del TLC Estados Unidos – Colombia. En el cuarto capitulo se estudiara el caso de éxito de de la industria automotriz mexicana, bajo el marco del TLC México- Estados Unidos, el cual sirvió como factor de consolidación para el sector. Por ultimo se darán las conclusiones del estudio del tema y se emitirán unas pequeñas recomendaciones.

Manipulación manual de cargas y presencia de lumbalgia en los trabajadores de desempaque armada en General Motors Colmotores

Trabajo de grado enfocado a determinar la asociaciónexistente entre manipulación manual de cargas y la presencia de lumbalgia entrabajadores de un área determinada en una empresa ensambladora devehículos. Se abordan temas como anatomía y biomecánica de la columnalumbar, levantamiento manual de carga, lumbalgia y factores que contribuyen ala presencia de esta, los cuales sirvieron de soporte teórico en este trabajo.Esta es una investigación de tipo descriptivo, la cual se desarrolló en tres fases:revisión teórica, trabajo de campo y análisis y procesamiento de la información;concluyendo que existe una asociación entre la manipulación manual de cargasy la presencia de lumbalgia en los trabajadores del área estudiada, teniendoademás como resultados adicionales que la lumbalgia tiene un origenmultifactorial y los factores psicosociales juegan un papel importante en lapresencia de esta.

Recerca de jocs motors tradicionals a Catalunya i arreu del món : joc i diversitat intercultural, a l'educació infantil, primària i secundària. 'Investigación de juegos motores tradicionales en Cataluña y de todo el mundo : juego y diversidad intercultural, en la educación infantil, primaria y secundaria'.

Se confecciona un repertorio de juegos motores tradicionales. La secuencia lógica que sigue es partir de la realidad más cercana e+ inmediata para acercarse a otras culturas más alejadas. Se pone de manifiesto el carácter transcultural, casi universal, de esta manifestación humana. El estudio ofrece cincuenta juegos motores tradicionales de Cataluña y de todo el mundo. Se refuerza la utilización del juego como recurso y fuente de aprendizaje, con la intencionalidad educativa que en la práctica lúdica ayude a establecer relaciones basadas en el respeto y la tolerancia, favoreciendo la integración escolar y social con los alumnos, sobre todo de la población escolar con necesidades educativas específicas.

Els motors : rotors, aleps i pistons. La interpretació : l'esperit crític. 'Los motores : rotores, alabes y pistones. La interpretación : el espíritu crítico'.

Crédito de Tecnología del módulo nueve sobre motores. Contiene un conjunto de actividades destinadas a ayudar al niño a comprender el concepto de motor y a entrar dentro del funcionamiento de los motores más comunes de nuestro entorno y sus aplicaciones. El crédito incluye material de ayuda para el alumno, destinado a cubrir más de la mitad de las actividades de aprendizaje propuestas en el tercer nivel de concreción. Se dan pautas generales para la evaluación.

Benchmarking 2D hydraulic models for urban flooding

This paper describes benchmark testing of six two-dimensional (2D) hydraulic models (DIVAST, DIVASTTVD, TUFLOW, JFLOW, TRENT and LISFLOOD-FP) in terms of their ability to simulate surface flows in a densely urbanised area. The models are applied to a 1·0 km × 0·4 km urban catchment within the city of Glasgow, Scotland, UK, and are used to simulate a flood event that occurred at this site on 30 July 2002. An identical numerical grid describing the underlying topography is constructed for each model, using a combination of airborne laser altimetry (LiDAR) fused with digital map data, and used to run a benchmark simulation. Two numerical experiments were then conducted to test the response of each model to topographic error and uncertainty over friction parameterisation. While all the models tested produce plausible results, subtle differences between particular groups of codes give considerable insight into both the practice and science of urban hydraulic modelling. In particular, the results show that the terrain data available from modern LiDAR systems are sufficiently accurate and resolved for simulating urban flows, but such data need to be fused with digital map data of building topology and land use to gain maximum benefit from the information contained therein. When such terrain data are available, uncertainty in friction parameters becomes a more dominant factor than topographic error for typical problems. The simulations also show that flows in urban environments are characterised by numerous transitions to supercritical flow and numerical shocks. However, the effects of these are localised and they do not appear to affect overall wave propagation. In contrast, inertia terms are shown to be important in this particular case, but the specific characteristics of the test site may mean that this does not hold more generally.

Hydraulic modeling of runoff over a rough surface under partial inundation

This study presents a numerical method to derive the Darcy- Weisbach friction coefficient for overland flow under partial inundation of surface roughness. To better account for the variable influence of roughness with varying levels of emergence, we model the flow over a network which evolves as the free surface rises. This network is constructed using a height numerical map, based on surface roughness data, and a discrete geometry skeletonization algorithm. By applying a hydraulic model to the flows through this network, local heads, velocities, and Froude and Reynolds numbers over the surface can be estimated. These quantities enable us to analyze the flow and ultimately to derive a bulk friction factor for flow over the entire surface which takes into account local variations in flow quantities. Results demonstrate that although the flow is laminar, head losses are chiefly inertial because of local flow disturbances. The results also emphasize that for conditions of partial inundation, flow resistance varies nonmonotonically but does generally increase with progressive roughness inundation.

Automatic near real-time selection of flood water levels from high resolution Synthetic Aperture Radar images for assimilation into hydraulic models: a case study

Flood extents caused by fluvial floods in urban and rural areas may be predicted by hydraulic models. Assimilation may be used to correct the model state and improve the estimates of the model parameters or external forcing. One common observation assimilated is the water level at various points along the modelled reach. Distributed water levels may be estimated indirectly along the flood extents in Synthetic Aperture Radar (SAR) images by intersecting the extents with the floodplain topography. It is necessary to select a subset of levels for assimilation because adjacent levels along the flood extent will be strongly correlated. A method for selecting such a subset automatically and in near real-time is described, which would allow the SAR water levels to be used in a forecasting model. The method first selects candidate waterline points in flooded rural areas having low slope. The waterline levels and positions are corrected for the effects of double reflections between the water surface and emergent vegetation at the flood edge. Waterline points are also selected in flooded urban areas away from radar shadow and layover caused by buildings, with levels similar to those in adjacent rural areas. The resulting points are thinned to reduce spatial autocorrelation using a top-down clustering approach. The method was developed using a TerraSAR-X image from a particular case study involving urban and rural flooding. The waterline points extracted proved to be spatially uncorrelated, with levels reasonably similar to those determined manually from aerial photographs, and in good agreement with those of nearby gauges.

Developing a reliable strategy to infer the effective soil hydraulic properties from field evaporation experiments for agro-hydrological models

The Richards equation has been widely used for simulating soil water movement. However, the take-up of agro-hydrological models using the basic theory of soil water flow for optimizing irrigation, fertilizer and pesticide practices is still low. This is partly due to the difficulties in obtaining accurate values for soil hydraulic properties at a field scale. Here, we use an inverse technique to deduce the effective soil hydraulic properties, based on measuring the changes in the distribution of soil water with depth in a fallow field over a long period, subject to natural rainfall and evaporation using a robust micro Genetic Algorithm. A new optimized function was constructed from the soil water contents at different depths, and the soil water at field capacity. The deduced soil water retention curve was approximately parallel but higher than that derived from published pedo-tranfer functions for a given soil pressure head. The water contents calculated from the deduced soil hydraulic properties were in good agreement with the measured values. The reliability of the deduced soil hydraulic properties was tested in reproducing data measured from an independent experiment on the same soil cropped with leek. The calculation of root water uptake took account for both soil water potential and root density distribution. Results show that the predictions of soil water contents at various depths agree fairly well with the measurements, indicating that the inverse analysis is an effective and reliable approach to estimate soil hydraulic properties, and thus permits the simulation of soil water dynamics in both cropped and fallow soils in the field accurately. (C) 2009 Elsevier B.V. All rights reserved.

Sensitivity of a hydraulic model to changes in channel erosion during extreme flooding

Recent research into flood modelling has primarily concentrated on the simulation of inundation flow without considering the influences of channel morphology. River channels are often represented by a simplified geometry that is implicitly assumed to remain unchanged during flood simulations. However, field evidence demonstrates that significant morphological changes can occur during floods to mobilise the boundary sediments. Despite this, the effect of channel morphology on model results has been largely unexplored. To address this issue, the impact of channel cross-section geometry and channel long-profile variability on flood dynamics is examined using an ensemble of a 1D-2D hydraulic model (LISFLOOD-FP) of the 1:2102 year recurrence interval floods in Cockermouth, UK, within an uncertainty framework. A series of hypothetical scenarios of channel morphology were constructed based on a simple velocity based model of critical entrainment. A Monte-Carlo simulation framework was used to quantify the effects of channel morphology together with variations in the channel and floodplain roughness coefficients, grain size characteristics, and critical shear stress on measures of flood inundation. The results showed that the bed elevation modifications generated by the simplistic equations reflected a good approximation of the observed patterns of spatial erosion despite its overestimation of erosion depths. The effect of uncertainty on channel long-profile variability only affected the local flood dynamics and did not significantly affect the friction sensitivity and flood inundation mapping. The results imply that hydraulic models generally do not need to account for within event morphodynamic changes of the type and magnitude modelled, as these have a negligible impact that is smaller than other uncertainties, e.g. boundary conditions. Instead morphodynamic change needs to happen over a series of events to become large enough to change the hydrodynamics of floods in supply limited gravel-bed rivers like the one used in this research.

Modeling plant transpiration under limited soil water: comparison of different plant and soil hydraulic parameterizations and preliminary implications for their use in land surface models

Accurate estimates of how soil water stress affects plant transpiration are crucial for reliable land surface model (LSM) predictions. Current LSMs generally use a water stress factor, β, dependent on soil moisture content, θ, that ranges linearly between β = 1 for unstressed vegetation and β = 0 when wilting point is reached. This paper explores the feasibility of replacing the current approach with equations that use soil water potential as their independent variable, or with a set of equations that involve hydraulic and chemical signaling, thereby ensuring feedbacks between the entire soil–root–xylem–leaf system. A comparison with the original linear θ-based water stress parameterization, and with its improved curvi-linear version, was conducted. Assessment of model suitability was focused on their ability to simulate the correct (as derived from experimental data) curve shape of relative transpiration versus fraction of transpirable soil water. We used model sensitivity analyses under progressive soil drying conditions, employing two commonly used approaches to calculate water retention and hydraulic conductivity curves. Furthermore, for each of these hydraulic parameterizations we used two different parameter sets, for 3 soil texture types; a total of 12 soil hydraulic permutations. Results showed that the resulting transpiration reduction functions (TRFs) varied considerably among the models. The fact that soil hydraulic conductivity played a major role in the model that involved hydraulic and chemical signaling led to unrealistic values of β, and hence TRF, for many soil hydraulic parameter sets. However, this model is much better equipped to simulate the behavior of different plant species. Based on these findings, we only recommend implementation of this approach into LSMs if great care with choice of soil hydraulic parameters is taken