Enquête préliminaire et évaluation de la satisfaction globale des soins dans une structure ambulatoire psychiatrique pour enfants et adolescents

The complexity and difficulty of assessing psychiatric care for children and adolescents is a widely accepted reality. However, this should not discourage necessary efforts to stress the richness and efficiency of clinical practices, regardless of their theoretical models. We present the results of a quality-like survey addressing patient satisfaction and therapeutic alliance conducted in 2007 in an outpatient ward of the department of psychiatry for children and adolescents of the University of Lausanne (Service Universitaire de Psychiatrie de l'Enfant et de l'Adolescent - SUPEA, Lausanne). We developed a questionnaire on the basis of a "traditional" patient satisfaction survey, consisting of questions dealing with a range of different types of ambulatory settings and evaluating: access to care, quality of reception, patient's perception of the type of care and support offered, the therapeutic alliance and global satisfaction. Questions regarding the therapeutic alliance were based on the Revised Help Alliance Questionnaire (HAQ-II, Lester Luborski). Questionnaires were anonymous and self-administered by children from 10 years old up and parents separately. High levels of global satisfaction were reported (80% satisfied or very satisfied). Certain specific aspects seem to influence the global satisfaction level and therapeutic alliance. Patients with self-reported anxiety problems were less satisfied than those with selfreported conduct problems. The mode of reference of the patient, self or by parents versus by school or social workers, affected the perceived alliance. A higher frequency of sessions was also related to a better perceived alliance and satisfaction.

La manifestation

La manifestation est sans doute la forme la plus commune d'expression politique, tant dans les pays démocratiques, où sa légitimité le dispute avec plus ou moins de bonheur aux formes plus conventionnelles de participation comme le vote, que dans les pays non démocratiques, où elle accompagne les tentatives de révolte et de renversement.Dans cet ouvrage de synthèse, les auteurs proposent une analyse sociologique et historique de ce mode d'action politique, avec ses normes et ses règles, ses légendes et ses mythes, ses épisodes glorieux et ses heures sombres.Mais surtout, au-delà de l'interrogation classique sur la place de la manifestation dans le répertoire d'action contemporain et dans les luttes politiques, c'est aussi à une analyse au plus près des manifestants eux-mêmes et de «ce qui les fait courir» que cet ouvrage nous invite.

The cover basement contact beneath the Rawil axial depression (Western Alps) - True amplitude seismic processing, petrophysical properties, and modeling

Since 1986, several near-vertical seismic reflection profiles have been recorded in Switzerland in order to map the deep geologic structure of the Alps. One objective of this endeavour has been to determine the geometries of the autochthonous basement and of the external crystalline massifs, important elements for understanding the geodynamics of the Alpine orogeny. The PNR-20 seismic line W1, located in the Rawil depression of the western Swiss Alps, provides important information on this subject. It extends northward from the `'Penninic front'' across the Helvetic nappes to the Prealps. The crystalline massifs do not outcrop along this profile. Thus, the interpretation of `'near-basement'' reflections has to be constrained by down-dip projections of surface geology, `'true amplitude'' processing, rock physical property studies and modelling. 3-D seismic modelling has been used to evaluate the seismic response of two alternative down-dip projection models. To constrain the interpretation in the southern part of the profile, `'true amplitude'' processing has provided information on the strength of the reflections. Density and velocity measurements on core samples collected up-dip from the region of the seismic line have been used to evaluate reflection coefficients of typical lithologic boundaries in the region. The cover-basement contact itself is not a source of strong reflections, but strong reflections arise from within the overlaying metasedimentary cover sequence, allowing the geometry of the top of the basement to be determined on the basis of `'near-basement'' reflections. The front of the external crystalline massifs is shown to extend beneath the Prealps, about 6 km north of the expected position. A 2-D model whose seismic response shows reflection patterns very similar to the observed is proposed.