Adesão aos refeitórios escolares no 2º, 3º ciclos e ensino secundário

Dissertação para obtenção do grau de Mestre no Instituto Superior de Ciências da Saúde Egas Moniz

A atitude dos professores do 2º, 3º ciclo e secundário face à inclusão de alunos com autismo

A educação inclusiva assume-se cada vez mais como um tema fulcral na sociedade contemporânea. Esta realidade confere responsabilidades acrescidas às instituições educativas e em especial aos docentes. Com o objetivo de averiguar as atitudes dos professores do 2º, 3º ciclo e secundário face à inclusão de alunos com autismo, este estudo foca-se na determinação do grau de aplicabilidade das considerações teóricas do movimento inclusivo na realidade escolar. Com uma metodologia mista (quantitativa e qualitativa), aplicada ao universo de 312 professores, concluiu-se que os docentes do 2º ciclo expressam uma atitude mais positiva face à inclusão de alunos com autismo nas aulas regulares, comparativamente com os professores do 3º ciclo e secundário. Este trabalho finaliza com breves orientações para futuras investigações.

Pentecôte et langues de feu : analyse structurelle et interprétation d’Actes des Apôtres 2,3

Le récit de la Pentecôte (Actes des Apôtres 2) présente au lecteur un élément particulier qui se retrouve rarement dans le canon biblique : les « langues comme de feu ». Seuls les passages d’Isaïe 5,24 et Actes 2,3 utilisent cette expression; pourtant, leurs contextes diffèrent largement. Nous trouvons certains commentaires rabbiniques et fragments de rouleaux de la Mer Morte qui emploient cette même expression, et la littérature gréco-romaine utilise une image similaire où un feu divin se pose sur la tête de certains personnages. Puisque la fonction de cet élément diffère d’un ouvrage littéraire à un autre, comment devons-nous interpréter les langues de feu dans le récit de la Pentecôte? Les commentaires bibliques qui examinent cet élément proposent différentes hypothèses sur la symbolique des langues de feu. Afin de répondre à cette problématique, nous commencerons notre étude avec une présentation sur l’état de la question et des approches synchroniques utilisées. Nous présenterons ensuite l’analyse structurelle du récit de la Pentecôte afin de percevoir la place que notre expression occupe dans cette péricope. Au chapitre trois, nous ferons une analyse grammaticale de notre segment afin de voir la fonction grammaticale de l’expression, et présenter une recension des ouvrages hébraïques et gréco-romains qui utilisent cette expression ou une image similaire. Enfin, l’analyse philologique des termes γλῶσσα et πῦρ sera élaborée et comparée à l’utilisation retrouvée dans le livre des Actes des Apôtres. Subséquemment, nous serons en mesure de porter un regard critique sur quelques interprétations proposées afin de percevoir que la mise en réseau structurel du membre γλῶσσαι ὡσεὶ πυρός, avec les termes répétitifs et synonymiques du récit, nous orientent à percevoir l’accomplissement de la promesse du Saint-Esprit, qui à son tour habilite le croyant à réaliser la mission donnée : la proclamation du message christologique à toutes les ethnies.

Tab. 2,3,4 Specific resistivity of calculated models for the soundings in Lapland

Geoelectrical soundings were carried out in 29 different places in order to find permafrost and to measure its thickness. In most places above timber Iine a permafrost thickness of 10-50 m was recorded. Permafrost was found at sites with thin snow cover during winter. Here, deflation phenomena on the summits of fjells indicate the occurence of permafrost, Vegetation type might be a good indicator of permafrost, too. It seems obvious that permafrost exists extensively on fjell summits of northern Finland.

(Tables 2, 3) Element ratios of planktonic foraminifera from western Pacific surface sediments

Accurately quantifying deep-sea calcite dissolution is crucial for understanding the role of the marine carbonate system in regulating atmospheric pCO2 over millennia. We compare a foraminifer-fragmentation-based calcite dissolution proxy (Globorotalia menardii fragmentation index (MFI)) to Mg/Ca, Sr/Ca, and Mg/Sr in several species of deep dwelling planktonic foraminifers. We conducted microfossil and geochemical analyses on the same core top samples taken at different depths on the Ontong Java Plateau to maximize the dissolution signal and minimize the temperature overprint on our data. We also compare elemental ratios from planktonic foraminifer tests to modern bottom water [CO3]2- undersaturation and model-derived estimates of percent calcite dissolved in deep-sea sediments. We find clear linear decreases in Mg/Ca or Mg/Sr in G. menardii and Pulleniatina obliquiloculata with increasing (1) bottom water [CO3]2- undersaturation, (2) percent calcite dissolved in sediments calculated with biogeochemical modeling, (3) MFI, and (4) percent calcite dissolved derived from MFI. These findings lend further support to MFI as a calcite dissolution proxy for deep-sea sediments. In contrast, we find no significant correlation between Sr/Ca and independent dissolution indicators. Our results suggest that Mg/Ca and Mg/Sr from deep dwelling foraminifers could potentially be used as calcite dissolution proxies in combination with independent water temperature estimates. Likewise, establishing the relationship between MFI and dissolution-induced changes in the Mg/Ca of surface-dwelling foraminifers could provide a tool to correct Mg/Ca-derived sea surface temperature reconstructions for calcite dissolution.

Major and trace element composition in the Central Indian Ocean Basin ferrobasalts (Table 2, 3)

We report the occurrence of ferrobasalts recovered from the Central Indian Ocean Basin crust generated at the Southeast Indian Ridge during a phase of moderate to fast spreading accretion (~110-190 mm/yr, full rate).The rocks are rich in plagioclase, FeO* (13/19 %), and TiO2 (2.27/2.76 %), poor in olivine and MgO (3.44/6.20%), and associated with topographic highs and increased amplitude magnetic anomalies corresponding to chrons A25 and A24. We suggest that secon dary eruptions from ancient N-MORB magma, which may have been trapped at a shallow depth in a horizon of neutral buoyancy, could have produced the ferrobasalts.

Status assessment of toxic chemicals : tris(2,3-dibromopropyl) phosphate /

Mode of access: Internet.

Performance characteristics of automotive engines in the United States. Second series--report no. 1. 1976 Chevrolet Vega 140 CID (2.3 liters), 2V. Interim report.

Transportation Systems Center, Cambridge, Mass.

Performance characteristics of automotive engines in the United States. Second series--report no. 5. 1977 Ford 140 CID (2.3 liters). 2V. Interim report.

Transportation Systems Center, Cambridge, Mass.

Health assessment document for 2,3,7,8-tetrachlorodibenzo-p-dioxin (TCDD) and related compounds.

"Draft, do not quote or cite."