Pràctiques d'exclusió als locals nocturns del centre històric de Barcelona. El dret d'admissió com a tècnica de discriminació racista

La investigació se centra en l'ús discriminatori del dret d'admissió en els bars de nit del centre de Barcelona. En concret, el terreny de camp el conformen quatre bars situats en el Raval, un barri que està experimentant un procés d'ennobliment. El treball de camp ha tingut una durada de deu mesos i s¿ha basat fonamentalment en l'observació etnogràfica. L'objectiu principal ha estat constatar sobre el terreny la pràctica efectiva de la discriminació, i com es du a terme, quines són les formes que adopta i les argumentacions en què es basa. La qüestió fonamental que cal respondre és com es duen a terme els protocols d'acceptació o rebuig d¿aquells què pretenen ingressar als bars de nit, a partir de criteris de detecció de persones pertanyents a determinats grups socials considerats indesitjables, moralment contaminants o perillosos. Aquest és el cas dels i les immigrants, especialment els que provenen del Marroc o d'Algèria, als quals molt sovint se'ls impedeix l'entrada perquè són considerats com una font permanent d'ansietat. Això és bàsicament per un prejudici construït envers el que s¿entén popularment com la figura del moro. Molt sovint, els immigrants àrabs són relacionats amb la delinqüència, i això serveix com a pretext perquè es puguin justificar les pràctiques d'exclusió que s'executen envers aquest grup social en nom del dret d'admissió. En definitiva, aquestes pràctiques discriminatòries funcionarien com un mecanisme la missió del qual seria reafirmar la inferioritat moral atribuïda a aquest col·lectiu i garantir que en els espais d'oci nocturn del Raval els i les joves de classe mitjana no estiguin en contacte amb els i les immigrants àrabs. En conseqüència, podem afirmar que l'exercici discriminat del dret d'admissió sembla tenir relació amb el procés d'ennobliment que està experimentant el barri.

Generation and nonlinear evolution of shore-oblique/transverse sand bars

The coupling between topography, waves and currents in the surf zone may selforganize to produce the formation of shore-transverse or shore-oblique sand bars on an otherwise alongshore uniform beach. In the absence of shore-parallel bars, this has been shown by previous studies of linear stability analysis, but is now extended to the finite-amplitude regime. To this end, a nonlinear model coupling wave transformation and breaking, a shallow-water equations solver, sediment transport and bed updating is developed. The sediment flux consists of a stirring factor multiplied by the depthaveraged current plus a downslope correction. It is found that the cross-shore profile of the ratio of stirring factor to water depth together with the wave incidence angle primarily determine the shape and the type of bars, either transverse or oblique to the shore. In the latter case, they can open an acute angle against the current (upcurrent oriented) or with the current (down-current oriented). At the initial stages of development, both the intensity of the instability which is responsible for the formation of the bars and the damping due to downslope transport grow at a similar rate with bar amplitude, the former being somewhat stronger. As bars keep on growing, their finite-amplitude shape either enhances downslope transport or weakens the instability mechanism so that an equilibrium between both opposing tendencies occurs, leading to a final saturated amplitude. The overall shape of the saturated bars in plan view is similar to that of the small-amplitude ones. However, the final spacings may be up to a factor of 2 larger and final celerities can also be about a factor of 2 smaller or larger. In the case of alongshore migrating bars, the asymmetry of the longshore sections, the lee being steeper than the stoss, is well reproduced. Complex dynamics with merging and splitting of individual bars sometimes occur. Finally, in the case of shore-normal incidence the rip currents in the troughs between the bars are jet-like while the onshore return flow is wider and weaker as is observed in nature.

Self-organization mechanisms for the formation on nearshore crescentic and transverse sand bars

The formation and development of transverse and crescentic sand bars in the coastal marine environment has been investigated by means of a nonlinear numerical model based on the shallow-water equations and on a simpli ed sediment transport parameterization. By assuming normally approaching waves and a saturated surf zone, rhythmic patterns develop from a planar slope where random perturbations of small amplitude have been superimposed. Two types of bedforms appear: one is a crescentic bar pattern centred around the breakpoint and the other, herein modelled for the rst time, is a transverse bar pattern. The feedback mechanism related to the formation and development of the patterns can be explained by coupling the water and sediment conservation equations. Basically, the waves stir up the sediment and keep it in suspension with a certain cross-shore distribution of depth-averaged concentration. Then, a current flowing with (against) the gradient of sediment concentration produces erosion (deposition). It is shown that inside the surf zone, these currents may occur due to the wave refraction and to the redistribution of wave breaking produced by the growing bedforms. Numerical simulations have been performed in order to understand the sensitivity of the pattern formation to the parameterization and to relate the hydro-morphodynamic input conditions to which of the patterns develops. It is suggested that crescentic bar growth would be favoured by high-energy conditions and ne sediment while transverse bars would grow for milder waves and coarser sediment. In intermediate conditions mixed patterns may occur.