Las trayectorias de los estudiantes universitarios : un modelo integral = Les trajectoires des étudiants universitaires : un modèle intégré

Nous avons développé un modèle qui cherche à identifier les déterminants des trajectoires scolaires des élèves universitaires en articulant deux perspectives théoriques et en utilisant une approche méthodologique mixte en deux phases : quantitative et qualitative. La première phase est basée sur le modèle de Tinto (1992) avec l'incorporation d'autres variables de Crespo et Houle (1995). Cette étape a atteint deux objectifs. Dans le premier, on a identifié les différences entre les variables exogènes (indice économique, l'éducation parentale, moyen au lycée et moyenne dans l’examen d'entrée) et trois types de trajectoires: la persévérante, de décalage et d’abandon. Cette phase était basée sur les données d'un sondage administré à 800 étudiants à l'Université de Sonora (Mexique). Les résultats montrent que ceux qui ont quitté l'institution ont obtenu des scores significativement plus bas sur les variables exogènes. Le deuxième objectif a été atteint pour les trajectoires persévérantes et de décalage, en établissant que les étudiants ont une plus grande chance d’être persévérants lorsqu’ils présentent de meilleurs scores dans deux variables exogènes (l'examen d'entrée et être de genre féminin) et quatre viable endogènes (haute intégration académique, de meilleures perspectives d'emploi, ont une bourse). Dans la deuxième phase nous avons approfondi la compréhension (Verstehen) des processus d'articulation entre l'intégration scolaire et sociale à travers de trois registres proposés par Dubet (2005): l'intégration, le projet et la vocation. Cette phase a consisté dans 30 interviews avec étudiantes appartenant aux trois types de trajectoire. À partir du travail de Bourdages (1994) et Guzman (2004), nous avons cherché le sens de l'expérience attribuée par les étudiants au processus éducatif. Les résultats révèlent cinq groupes d’étudiantes avec des expériences universitaires identifiables : ceux qui ont une intégration académique et sociale plus grande, les femmes travailleuses intégrées académiquement, ceux qui ont les plus grandes désavantages économiques et d’intégration scolaire, ceux qui ont cherché leur vocation dans un autre établissement et ceux qui n'ont pas poursuivi leurs études. L'utilisation de différents outils statistiques (analyse de corrélation, analyse de régression logistique et analyse des conglomérats) dans la première phase a permis d’identifier des variables clés dans chaque type de trajectoire, lesquelles ont été validées avec les résultats de la phase qualitative. Cette thèse, en plus de montrer l'utilité d'une approche méthodologique mixte, étend le modèle de Tinto (1987) et confirme l'importance de l'intégration scolaire pour la persévérance à l'université.

Usages de la photographie chez Patrick Modiano

Mémoire numérisé par la Division de la gestion de documents et des archives de l'Université de Montréal

Résister à l'exploitation : une histoire de l'opposition péruvienne aux transnationales minières de 1901 à nos jours

Cette oeuvre est mise à disposition selon les termes de la licence Creative Commons Attribution - Pas d'utilisation commerciale - Pas de modification 2.5 Canada Vous avez donc le droit de : Partager - copier, distribuer et communiquer le matériel par tous les moyens et sous tous formats; Selon les conditions suivantes : Attribution — Vous devez créditer l'Oeuvre, intégrer un lien vers la licence et indiquer si des modifications ont été effectuées à l'Oeuvre. Vous devez indiquer ces informations par tous les moyens possibles mais vous ne pouvez pas suggérer que l'Offrant vous soutient ou soutient la façon dont vous avez utilisé son Oeuvre. Pas d’Utilisation Commerciale — Vous n'êtes pas autoriser à faire un usage commercial de cette Oeuvre, tout ou partie du matériel la composant. Pas de modifications — Dans le cas où vous effectuez un remix, que vous transformez, ou créez à partir du matériel composant l'Oeuvre originale, vous n'êtes pas autorisé à distribuer ou mettre à disposition l'Oeuvre modifiée. Pour voir une copie de cette licence, visitez http://creativecommons.org/licenses/by-nc-nd/2.5/ca/ ou écrivez à Creative Commons, 444 Castro Street, Suite 900, Mountain View, California, 94041, USA.

Quantum cavitation in liquid helium

Using a functional-integral approach, we have determined the temperature below which cavitation in liquid helium is driven by thermally assisted quantum tunneling. For both helium isotopes, we have obtained the crossover temperature in the whole range of allowed negative pressures. Our results are compatible with recent experimental results on 4He.

Provenance, Sedimentation and Geochemistry' of the Modern Sediments of time Mud Banks Off the Centrai Keraia Coast, India

This thesis is an attempt to Provenence, Sedimentetion and Geochemistry of the Modern Sediments of the Mud Banks off the Central Kerela Coast, India. In the present doctoral work, an attempt has been made to study in detail the mud banks of central Kerala, i.e. of Narakkal, Saudi and Purakkad areas which are reported as permanent mud banks, since olden days. The studies have been conducted during the years 1985 and 1986. The important findings of the study is stated as clay mineralogical studies of the rivers, lake and mud bank sediments reveal that the dominant clay mineral is kaolinite followed by montmorillonite, illite and gibbsite. Geochemical analysis of the Vembanad lake and mud bank sediments show that the iron and manganese are widely distributed both in the lake and mud bank sediments

Cavitation in 3He-4He liquid mixtures at low temperatures

Bubble formation in solutions of 3He and 4He is studied within a density-functional approach. In particular, the temperature dependence of the cavitation pressure for different 3He concentrations is calculated at low temperatures and compared to that of pure 4He. The presence of Andreev states lowers the surface tension and, consequently, nucleation barriers are drastically reduced. This fact means that even at low 3He concentrations the cavitation process takes place at higher pressures than the spinodal pressure, which is not the case for pure 4He.

Nucleation in supersaturated solutions 3He in 4He at negative pressure.

Depending on the 3He concentration, thermal nucleation in 3-4He supersaturated liquid mixtures at negative pressures may be originated either by bubble or by 3rich drop formation. We have investigated this phenomenon within a density-functional approach, determining the regions in the pressure¿3He-concentration plane where bubbles or drops likely drive the nucleation process. As an illustrative example, we also give the homogeneous nucleation pressure corresponding to 50 and 100 mK temperature.

Short-term effects of human urine fertiliser and wood ash on soil pH and electrical conductivity

The fertiliser value of human urine has been examined on several crops, yet little is known about its effects on key soil properties of agronomic significance. This study investigated temporal soil salinization potential of human urine fertiliser (HUF). It further looked at combined effects of human urine and wood ash (WA) on soil pH, urine-NH_3 volatilisation, soil electrical conductivity (EC), and basic cation contents of two Acrisols (Adenta and Toje series) from the coastal savannah zone of Ghana. The experiment was a factorial design conducted in the laboratory for 12 weeks. The results indicated an increase in soil pH by 1.2 units for Adenta series and 1 unit for Toje series after one week of HUF application followed by a decline by about 2 pH units for both soil types after twelve weeks. This was attributed to nitrification of ammonium to nitrate leading to acidification. The EC otherwise increased with HUF application creating slightly saline conditions in Toje series and non-saline conditions in Adenta series. When WA was applied with HUF, both soil pH and EC increased. In contrast, the HUF alone slightly salinized Toje series, but both soils remained non-saline whenWA and HUF were applied together. The application ofWA resulted in two-fold increase in Ca, Mg, K, and Na content compared to HUF alone. Hence, WA is a promising amendment of acid soils and could reduce the effect of soluble salts in human urine fertilizer, which is likely to cause soil salinity.

Microbial response to restoration of tantalite mine soils in western Rwanda

Artisanal columbite-tantalite (coltan) mining has had negative effects on the rural economy in the great Lakes region of Africa through labor deficits, degradation and loss of farmland, food insecurity, high cost of living, and reduced traditional export crop production alongside secondary impacts that remotely affect the quality of air, water, soil, plants, animals, and human wellbeing. The situation is multifaceted and calls for a holistic approach for short and long-term mitigation of such negative effects. This study focuses on the effects of mine land restoration on soil microbiological quality in the Gatumba Mining District of western Rwanda. Some coltan mine wastelands were afforested with pine and eucalyptus trees while farmers directly cultivated others due to land scarcity. Farmyard manure (FYM) is the sole fertilizer applied on the wastelands although it is insufficient to achieve the desired crop yields. Despite this, several multi-purpose plants such as Tithonia diversifolia, Markhamia lutea, and Canavalia brasiliensis thrive in the area and could supplement FYM. The potential for these “new” amendments to improve soil microbial properties, particularly in the tantalite mine soils was investigated. The specific objectives of the study were to: (a) evaluate the effects of land use on soil microbial indices of the tantalite mine soils; (b) investigate the restorative effects of organic amendments on a Technosol; and (c) estimate the short-term N and P supply potential of the soil amendments in the soils. Fresh soils (0-20 cm) from an unmined native forest, two mine sites afforested with pine and eucalyptus forests (pine and eucalyptus Technosols), an arable land, and two cultivated Technosols (Kavumu and Kirengo Technosols) were analyzed for the physicochemical properties. Afterwards, a 28-day incubation (22oC) experiment was conducted followed by measurements of mineral N, soil microbial biomass C, N, P, and fungal ergosterol contents using standard methods. This was followed by a 12-week incubation study of the arable soil and the Kavumu Technosol amended with FYM, Canavalia and Tithonia biomass, and Markhamia leaf litter after which soil microbial properties were measured at 2, 8, and 12 weeks of incubation. Finally, two 4-week incubation experiments each were conducted in soils of the six sites to estimate (i) potential mineralizable N using a soil-sand mixture (1:1) amended with Canavalia and goat manure and (ii) P mineralization mixtures (1:1) of soil and anion exchange resins in bicarbonate form amended with Tithonia biomass and goat manure. In study one, afforestation increased soil organic carbon and total N contents in the pine and eucalyptus Technosols by 34-40% and 28-30%, respectively of that in the native forest soil. Consequently, the microbial biomass and activity followed a similar trend where the cultivated Technosols were inferior to the afforested ones. The microbial indices of the mine soils were constrained by soil acidity, dithionite-extractable Al, and low P availability. In study two, the amendments substantially increased C and N mineralization, microbial properties compared with non-amended soils. Canavalia biomass increased CO2 efflux by 340%, net N mineralization by 30-140%, and microbial biomass C and N by 240-600% and 240-380% (P < 0.01), respectively after four weeks of incubation compared with the non-amended soils. Tithonia biomass increased ergosterol content by roughly 240%. The Kavumu Technosol showed a high potential for quick restoration of its soil quality due to its major responses to the measured biological parameters. In study three, Canavalia biomass gave the highest mineralizable N (130 µg g-1 soil, P < 0.01) in the Kavumu Technosol and the lowest in the native forest soil (-20 µg g-1 soil). Conversely, the mineralizable N of goat manure was negative in all soils ranging from -2.5 µg N g-1 to -7.7 µg N g-1 soil except the native forest soil. However, the immobilization of goat manure N in the “cultivated soils” was 30-70% lower than in the “forest soils” signifying an imminent recovery of the amended soils from N immobilization. The mineralization of goat manure P was three-fold that of Tithonia, constituting 61-71% of total P applied. Phosphorus mineralization slightly decreased after four weeks of incubation due to sulfate competition as reflected in a negative correlation, which was steeper in the Tithonia treatment. In conclusion, each amendment used in this research played a unique role in C, N, and P mineralization and contributed substantially to microbial properties in the tantalite mine soils. Interestingly, the “N immobilizers” exhibited potentials for P release and soil organic carbon storage. Consequently, the combined use of the amendments in specific ratios, or co-composting prior to application is recommended to optimize nutrient release, microbial biomass dynamics and soil organic matter accrual. Transport of organic inputs seems more feasible for smallholder farmers who typically manage small field sizes. To reduce acidity in the soils, liming with wood ash was recommended to also improve P availability and enhance soil biological quality, even if it may only be possible on small areas. Further, afforestation with mixed-species of fast-growing eucalyptus and legume or indigenous tree species are suggested to restore tantalite mine wastelands. It is emphasized most of this research was conducted under controlled laboratory conditions, which exclude interaction with environmental variables. Also fine fractions of the amendments were used compared with the usual practice of applying a mixture of predominantly coarser fractions. Therefore, the biological dynamics reported in the studies here may not entirely reflect those of farmers’ field conditions.

Geometría en los Reales Alcázares de Sevilla.

Se presenta para el alumnado el aprendizaje de la geometría, y propone abordar la enseñanza de este bloque mediante unidades didácticas interdisciplinares, apoyadas en el entorno cultural y con contenidos y actividades adaptadas a distintos niveles de la ESO y de ritmos de aprendizaje en el aula. Se contempla la creación de materiales didácticos para todos los cursos de la ESO, su aplicación en el aula y la evaluación de los resultados obtenidos.