A avaliação das escolas: efeitos da avaliação externa nas dinâmicas de autoavaliação da escola

No contexto educativo português existem, atualmente, orientações legais para que as escolas sejam, por um lado, sujeitas a processos de avaliação externa e, por outro, induzidas a criar mecanismos de autoavaliação. Embora a escola seja, pelo menos em parte, um “locus de produção normativa”, na prática não tem sido fácil o diálogo entre a avaliação externa e os processos de mudança e melhoria, através da autoavaliação institucional. Num contexto onde as politicas nem sempre criam os estímulos e as condições adequadas, a ação organizacional em torno dos processos avaliativos acaba por refletir o jogo dos atores. Face à “natureza política” da avaliação, as escolas e os seus atores recorrem a “soluções organizacionais” que lhes permitem, em função dos interesses e dos objetivos individuais e organizativos, gerir as pressões e as expetativas do seu meio institucional. O presente trabalho pretende encontrar respostas sobre os efeitos do programa de avaliação externa das escolas (AEE) nas dinâmicas de autoavaliação e nos planos de ação para a melhoria da escola. Trata-se de uma investigação inserida numa matriz de cariz essencialmente qualitativo que opta pelo estudo de casos múltiplos. A informação foi recolhida através de várias fontes: observação direta, grupo focal (focus group), entrevistas, inquérito por questionário e análise documental. Os resultados tendem a evidenciar que as organizações educativas, nas respostas às prescrições externas para a avaliação e melhoria da escola recorrem a estratégias e táticas plurais, de tal modo que as mudanças que ocorrem, mais do que respostas à necessidade de eficácia e melhoria interna da escola, traduzem-se em processos de adaptação, que variam consoante as tensões existentes entre o contexto institucional e o ambiente competitivo onde as escolas estão inseridas; Abstract: The Evaluation of Schools: Effects of External Evaluation in the dynamics of Self-evaluation of Schools In the Portuguese educational context, there are currently legal guidelines for schools to be subject to external evaluation process, on the one hand, and on the other hand induced to create self-assessment mechanisms. Although the school is at least partly a "normative production locus", in practice the dialogue between the external evaluation and the processes of change and improvement through institutional self-assessment has not been easy. In a context where the policies do not always create the incentives and the right conditions, the organizational action around the evaluative process ends up reflecting the set of actors. Before the "political nature" of the evaluation, the schools and their actors recur to "organizational solutions" that allow them, in the interests of individual and organizational goals, to manage the pressures and expectations of its institutional environment. This work aims at finding answers to the effects of the External Schools Evaluation (ESE) programme, in the dynamics of self-evaluation and action plans for the improvement of school. It is an investigation inserted into an oriented matrix, essentially of qualitative nature that opts for multiple case studies. The information was collected through various sources: direct observation, focus group, interviews, questionnaire survey and document analysis. The results tend to show that educational organizations, in response to the external requirements for assessing and improving, use plural strategies and tactics. Similarly, the changes that occur in the structures, processes and practices, more than answers to the need for efficiency and indoor improvement of the school, result into adjustment processes, that change according to the existing tensions between the institutional context and the competitive environment where schools are located.

Inversion of ambient seismic noise HVSR to evaluate velocity and structural models of the Lower Tagus Basin, Portugal

During its history, several significant earthquakes have shaken the Lower Tagus Valley (Portugal). These earthquakes were destructive; some strong earthquakes were produced by large ruptures in offshore structures located southwest of the Portuguese coastline, and other moderate earthquakes were produced by local faults. In recent years, several studies have successfully obtained strong-ground motion syntheses for the Lower Tagus Valley using the finite difference method. To confirm the velocity model of this sedimentary basin obtained from geophysical and geological data, we analysed the ambient seismic noise measurements by applying the horizontal to vertical spectral ratio (HVSR) method. This study reveals the dependence of the frequency and amplitude of the low-frequency (HVSR) peaks (0.2–2 Hz) on the sediment thickness. We have obtained the depth of the Cenozoic basement along a profile transversal to the basin by the inversion of these ratios, imposing constraints from seismic reflection, boreholes, seismic sounding and gravimetric and magnetic potentials. This technique enables us to improve the existing three-dimensional model of the Lower Tagus Valley structure. The improved model will be decisive for the improvement of strong motion predictions in the earthquake hazard analysis of this highly populated basin. The methodology discussed can be applied to any other sedimentary basin.

Relatório no âmbito da unidade curricular "Prática de Ensino Supervisionada"

Este relatório, enquadrado na unidade curricular “Prática de Ensino Supervisionada” do Mestrado em Ensino de Português no 3.º ciclo do ensino básico e ensino secundário e de Espanhol nos ensinos básico e secundário, estrutura-se em torno de duas dimensões: uma dimensão teórica, respeitante aos documentos normativos e orientadores que norteiam a atividade docente e, mais especificamente, o processo de ensino-aprendizagem das disciplinas de Espanhol e de Português; uma dimensão prática que diz respeito à análise da prática de ensino desenvolvida na Escola E.B. 2, 3 André de Resende, no ano letivo de 2012/ 2013, no âmbito da planificação, condução de aulas, bem como da avaliação de aprendizagens. O principal objetivo deste relatório é relacionar criticamente essas duas dimensões no contexto da prática docente, na qual se englobam igualmente a participação nas estruturas da escola e o desenvolvimento profissional. ABSTRACT: This report, included in the course “Supervised Teaching Practice” of the Master Degree in Portuguese and Spanish Teaching in the middle and upper schools is organized according to two aspects: a theoretical aspect, concerning the normative and guiding documents that regulate the teaching activity and, more specifically, the teaching-learning process of Spanish and Portuguese courses; a practical aspect regarding the analysis of teaching practice developed in the School EB 2, 3 André Resende, in the school year 2012/2013, within lesson planning and organization and the learning assessment as well. The main goal of this report is to critically relate these two aspects in the teaching practice context which also includes the participation in school structures and professional development.

TECTONIC CONTROLS ON FLUVIAL LANDSCAPE DEVELOPMENT IN CENTRAL-EASTERN PORTUGAL: INSIGHTS FROM LONG PROFILE TRIBUTARY STREAM ANALYSES

This study examines the long profiles of tributaries of the Tejo (Tagus) and Zêzere rivers in central eastern Portugal (West Iberia) in order to provide new insights into the patterns, timing and controls on drainage development during the Pleistocene to Holocene incision stage. The long profiles were extracted from lower order tributary streams associated with the trunk drainage of the Tejo River and one main tributary, the Zêzere River (Fig. 1). These streams flow through a landscape strongly influenced by variations in bedrock lithology (mainly granites and metasediments), fault structures delimiting crustal blocks with distinct uplift rates, and a base-level lowering history (tectonic uplift / eustatic). The long profiles of the tributaries of the Tejo and Zêzere rivers record a series of transient and permanent knickpoints. The permanent knickpoints have direct correlation with the bedrock strength, corresponding to the outcropping of very hard quartzites or to the transition from softer (slates/metagreywaques) to harder (granite) basement. The analyzed streams/rivers record also an older transient knickpoint/knickzone separating: a) an upstream relict graded profile, with lower steepness and higher concavity, that reflects a long period of quasi-equilibrium conditions reached after the beginning of the incision stage; and b) a downstream reach displaying a rejuvenated long profile, with steeper gradient and lower concavity, particularly for the final segment, which is often convex (Fig. 2). The rejuvenated reaches testify the upstream propagation of several incision waves that are the response of each stream to continuous or increasing crustal uplift and dominant periods of base-level lowering by the trunk drainages, coeval of low sea level conditions. The long profiles and their morphological configurations enabled spatial and relative temporal patterns of incision to be quantified for each individual tributary stream. The incision values of streams flowing in uplifted blocks of the Portuguese Central Range (PCR) (ca.380-280 m) indicate differential uplift and are higher than the incision values of streams flowing on the adjacent South Portugal planation surface – the Meseta (ca. 200 m). The normalized steepness index, calculated using the method of Wobus et al. (2006), proved to be sensitive to active tectonics, as lower ksn values were found in relict graded profiles of streams located in less uplifted blocks, (e.g. Sertã stream in the PCR), or in those flowing through tectonic depressions. Fig. 1 – Geological map of the study area. 1 – fluvial terraces (Pleistocene); 2 – sedimentary cover (Paleogene and Neogene); 3 – slates and metasandstones (Devonian); 4 – slates and quartzites (Silurian); 5 – quartzites (Ordovician); 6 – slates and metagreywackes (Precambrian to Cambrian); 7 – slates, metagreywackes and limestones (Precambrian); 8 – granites and ortogneisses; 9 – diorites and gabros; 10 - fault. SFf – Sobreira Formosa fault; Sf – Sertã fault; Pf – Ponsul fault; Gf – Grade fault. The differential uplift indicated by the distribution of the ksn values and by the fluvial incision was likely accumulated on a few major faults, as the Sobreira Formosa fault (SFf), thus corroborating the tectonic activity of these faults. Due to the fact that the relict graded profiles can be correlated with other geomorphic references documented in the study area, namely the T1 terrace of the Tagus River (with an age of ca. 1 Myr), the following incision rates can be estimated: a) for the studied streams located in uplifted blocks of the PCR, 0.38 m/kyr to 0.28 m/kyr; b) for the streams flowing on the South Portugal planation surface, 0.20 m/kyr. The differential uplift inferred between crustal blocks in the study area corroborates the neotectonic activity of the bordering faults, which has been proposed in previous studies based upon less robust data. Fig. 2 – Longitudinal profile of the Nisa stream a tributary of the Tejo River. Note the equilibrium relict profile upstream the older transient knickpoint (hatched line) and the downstream rejuvenated profile (continuous line). Legend: tKP – transient knickpoint; rKp – resistant knickpoint; Mt – schist and phyllite; Gr – granite; Hf – hornfels; Og – orthogneisse. In the inset Distance – Slope plots, fill circles correspond to the relict graded profile, crosses correspond to the rejuvenated profile located downstream the older transient knickpoint (tKP).