Condensados de Bose-Einstein em redes óticas: a transição superfluido-isolante de Mott em redes hexagonais e a classe de universalidade superfluido-vidro de Bose em 3D

Estudamos transições de fases quânticas em gases bosônicos ultrafrios aprisionados em redes óticas. A física desses sistemas é capturada por um modelo do tipo Bose-Hubbard que, no caso de um sistema sem desordem, em que os átomos têm interação de curto alcance e o tunelamento é apenas entre sítios primeiros vizinhos, prevê a transição de fases quântica superfluido-isolante de Mott (SF-MI) quando a profundidade do potencial da rede ótica é variado. Num primeiro estudo, verificamos como o diagrama de fases dessa transição muda quando passamos de uma rede quadrada para uma hexagonal. Num segundo, investigamos como a desordem modifica essa transição. No estudo com rede hexagonal, apresentamos o diagrama de fases da transição SF-MI e uma estimativa para o ponto crítico do primeiro lobo de Mott. Esses resultados foram obtidos usando o algoritmo de Monte Carlo quântico denominado Worm. Comparamos nossos resultados com os obtidos a partir de uma aproximação de campo médio e com os de um sistema com uma rede ótica quadrada. Ao introduzir desordem no sistema, uma nova fase emerge no diagrama de fases do estado fundamental intermediando a fase superfluida e a isolante de Mott. Essa nova fase é conhecida como vidro de Bose (BG) e a transição de fases quântica SF-BG que ocorre nesse sistema gerou muitas controvérsias desde seus primeiros estudos iniciados no fim dos anos 80. Apesar dos avanços em direção ao entendimento completo desta transição, a caracterização básica das suas propriedades críticas ainda é debatida. O que motivou nosso estudo, foi a publicação de resultados experimentais e numéricos em sistemas tridimensionais [Yu et al. Nature 489, 379 (2012), Yu et al. PRB 86, 134421 (2012)] que violam a lei de escala $\\phi= u z$, em que $\\phi$ é o expoente da temperatura crítica, $z$ é o expoente crítico dinâmico e $ u$ é o expoente do comprimento de correlação. Abordamos essa controvérsia numericamente fazendo uma análise de escalonamento finito usando o algoritmo Worm nas suas versões quântica e clássica. Nossos resultados demonstram que trabalhos anteriores sobre a dependência da temperatura de transição superfluido-líquido normal com o potencial químico (ou campo magnético, em sistemas de spin), $T_c \\propto (\\mu-\\mu_c)^\\phi$, estavam equivocados na interpretação de um comportamento transiente na aproximação da região crítica genuína. Quando os parâmetros do modelo são modificados de maneira a ampliar a região crítica quântica, simulações com ambos os modelos clássico e quântico revelam que a lei de escala $\\phi= u z$ [com $\\phi=2.7(2)$, $z=3$ e $ u = 0.88(5)$] é válida. Também estimamos o expoente crítico do parâmetro de ordem, encontrando $\\beta=1.5(2)$.

Comprehensive Validation Of A Measure Of Student School Engagement: A Pilot Study Of Middle School Students

Although it may sound reasonable that American education continues to be more effective at sending high school students to college, in a study conducted in 2009, The Council of the Great City Schools states that "slightly more than half of entering ninth grade students arrive performing below grade level in reading and math, while one in five entering ninth grade students is more than two years behind grade level...[and] 25% received support in the form of remedial literacy instruction or interventions" (Council of the Great City Schools, 2009). Students are distracted with technology (Lei & Zhao, 2005), family (Xu & Corno, 2003), medical illnesses (Nielson, 2009), learning disabilities and perhaps the most detrimental to academic success, the very lack of interest in school (Ruch, 1963). In a Johns Hopkins research study, Building a Graduation Nation - Colorado (Balfanz, 2008), warning signs were apparent years before the student dropped out of high school. The ninth grade was often referenced as a critical point that indicated success or failure to graduate high school. The research conducted by Johns Hopkins illustrates the problem: students who become disengaged from school have a much greater chance of dropping out of high school and not graduating. The first purpose of this study was to compare different measurement models of the Student School Engagement (SSE) using Factor Analysis to verify model fit with student engagement. The second purpose was to determine the extent to which the SSE instrument measures student school engagement by investigating convergent validity (via the SSE and Appleton, Christenson, Kim and Reschly's instrument and Fredricks, Blumenfeld, Friedel and Paris's instrument), discriminant validity (via Huebner's Student Life Satisfaction Survey) and criterion-related validity (via the sub-latent variables of Aspirations, Belonging and Productivity and student outcome measures such as achievement, attendance and discipline). Discriminant validity was established between the SSE and the Appleton, Christenson, Kim and Reschly's model and Fredricks, Blumenfeld, Friedel and Paris's (2005) Student Engagement Instruments (SEI). When confirming discriminant validity, the SSE's correlations were weak and statistically not significant, thus establishing discriminant validity with the SLSS. Criterion-related validity was established through structural equation modeling when the SSE was found to be a significant predictor of student outcome measures when both risk score and CSAP scores were used. The third purpose of this study was to assess the factorial invariance of the SSE instrument across gender to ensure the instrument is measuring the intended construct across different groups. Conclusively, configural, weak and metric invariances were established for the SSE as a non-significant change in chi-square indicating that all parameters including the error variances were invariant across groups of gender. Engagement is not a clearly defined psychological construct; it requires more research in order to fully comprehend its complexity. Hopefully, with parental and teacher involvement and a sense of community, student engagement can be nurtured to result in a meaningful attachment to school and academic success.

Assistência estudantil no cenário da Universidade Federal do Triângulo Mineiro – UFTM

Este artigo foi organizado por meio da dissertação de mestrado cujo tema se concentra em é “Políticas Públicas Educacionais: uma análise sobre a Política Nacional de Assistência Estudantil no contexto da Universidade Federal do Triângulo Mineiro – UFTM”. O interesse pela temática vincula-se às políticas públicas educacionais tendo como objeto de estudo a sua implementação. O objetivo é demonstrar as formas como se dá a implementação da política de assistência estudantil e seus condicionantes políticos e sociais. O referencial teórico está pautado na teoria social crítica que busca a apreensão do processo histórico das relações sociais, repercutindo nas políticas públicas educacionais.

La modernisation de Tunis : un urbanisme et une architecture d’État au miroir d’une anthologie de la percée dans la médina (1881-1987)

Cette thèse traite de quelques moments clés dans l’histoire urbaine et architecturale moderne de la ville de Tunis. Elle les aborde conjointement à la problématique du percement de son noyau historique : la médina, née d’un projet de modernisation urbaine lancé par les beys de Tunis à la fin du XIXe siècle, poursuivi par le protectorat français de 1881 à 1956, puis par le gouvernement indépendant de 1956 à 1987. Partant, la recherche est répartie sur trois temps avec, au centre, le projet de la percée dite de la Casbah adopté par le Président Bourguiba à la fin de 1959. Pour plusieurs raisons, ce moment est cité rapidement dans la littérature malgré son importance dans la compréhension du visage actuel de la capitale tunisienne. Pour le saisir, on a dû retourner aux premières tentatives de percement de la médina de Tunis par le colonisateur français en 1887. Puis, on s’est progressivement approché de l’ancêtre direct de la percée bourguibienne paru sur le Plan directeur de Tunis en 1948. De ce premier temps, on a mis en valeur les stratégies coloniales dans leur gestion du territoire et leur rapport au processus de valorisation/dévalorisation du patrimoine issu de la civilisation arabo-islamique. Le second temps, qui correspond au plan de décolonisation mené par l’État indépendant dès 1955, est marqué par le lancement d’un « concours international ouvert pour une étude d’aménagement de la ville de Tunis » organisé par le Secrétariat d’État aux travaux publics en collaboration avec l’Union internationale des architectes. L’étude de cet événement et du colloque qui l’a suivi a ôté le voile sur ses raisons d’être politico-économiques que dissimulaient les usuels soucis de l’hygiène, de la circulation et de l’embellissement du Grand Tunis. Pour appuyer davantage ces constats, un troisième et dernier temps a été dédié au chantier de Tunis au lendemain du concours. L’accent mis sur les lieux symboliques du pouvoir et le désir obsessif des autorités à se les approprier ont réduit ce chantier à une redistribution concertée des symboles de la souveraineté nationale dans le but de centraliser et de personnifier le pouvoir en place. Le présent travail se situe dans le cadre des études postcoloniales et projette un regard critique sur la décolonisation en rapport avec ce qu’on a taxé d’urbanisme d’État. Propulsé par une certaine perception de la modernité, cet urbanisme est indissociable d’une instrumentalisation politique qui met l’accent sur les questions identitaires et patrimoniales, insiste sur la rupture avec le passé et tend à écarter l’opinion publique des questions inhérentes à l’aménagement du territoire et à la sauvegarde de la mémoire collective. En procédant par une analyse contextuelle de faits historiques et une lecture typomorphologique de la percée de la Casbah, cette recherche attire l’attention sur l’ampleur de certaines décisions gouvernementales concernant l’aménagement de l’espace urbain et la conservation de l’héritage architectural à court, moyen et long termes. Elle renseigne aussi sur le rôle des collectivités, de l’élite et des professionnels dans la canalisation de ces décisions pour ou contre leur droit à la ville.

Benchmarking numerical models of brittle thrust wedges

We report quantitative results from three brittle thrust wedge experiments, comparing numerical results directly with each other and with corresponding analogue results. We first test whether the participating codes reproduce predictions from analytical critical taper theory. Eleven codes pass the stable wedge test, showing negligible internal deformation and maintaining the initial surface slope upon horizontal translation over a frictional interface. Eight codes participated in the unstable wedge test that examines the evolution of a wedge by thrust formation from a subcritical state to the critical taper geometry. The critical taper is recovered, but the models show two deformation modes characterised by either mainly forward dipping thrusts or a series of thrust pop-ups. We speculate that the two modes are caused by differences in effective basal boundary friction related to different algorithms for modelling boundary friction. The third experiment examines stacking of forward thrusts that are translated upward along a backward thrust. The results of the seven codes that run this experiment show variability in deformation style, number of thrusts, thrust dip angles and surface slope. Overall, our experiments show that numerical models run with different numerical techniques can successfully simulate laboratory brittle thrust wedge models at the cm-scale. In more detail, however, we find that it is challenging to reproduce sandbox-type setups numerically, because of frictional boundary conditions and velocity discontinuities. We recommend that future numerical-analogue comparisons use simple boundary conditions and that the numerical Earth Science community defines a plasticity test to resolve the variability in model shear zones.

La modernisation de Tunis : un urbanisme et une architecture d’État au miroir d’une anthologie de la percée dans la médina (1881-1987)

Cette thèse traite de quelques moments clés dans l’histoire urbaine et architecturale moderne de la ville de Tunis. Elle les aborde conjointement à la problématique du percement de son noyau historique : la médina, née d’un projet de modernisation urbaine lancé par les beys de Tunis à la fin du XIXe siècle, poursuivi par le protectorat français de 1881 à 1956, puis par le gouvernement indépendant de 1956 à 1987. Partant, la recherche est répartie sur trois temps avec, au centre, le projet de la percée dite de la Casbah adopté par le Président Bourguiba à la fin de 1959. Pour plusieurs raisons, ce moment est cité rapidement dans la littérature malgré son importance dans la compréhension du visage actuel de la capitale tunisienne. Pour le saisir, on a dû retourner aux premières tentatives de percement de la médina de Tunis par le colonisateur français en 1887. Puis, on s’est progressivement approché de l’ancêtre direct de la percée bourguibienne paru sur le Plan directeur de Tunis en 1948. De ce premier temps, on a mis en valeur les stratégies coloniales dans leur gestion du territoire et leur rapport au processus de valorisation/dévalorisation du patrimoine issu de la civilisation arabo-islamique. Le second temps, qui correspond au plan de décolonisation mené par l’État indépendant dès 1955, est marqué par le lancement d’un « concours international ouvert pour une étude d’aménagement de la ville de Tunis » organisé par le Secrétariat d’État aux travaux publics en collaboration avec l’Union internationale des architectes. L’étude de cet événement et du colloque qui l’a suivi a ôté le voile sur ses raisons d’être politico-économiques que dissimulaient les usuels soucis de l’hygiène, de la circulation et de l’embellissement du Grand Tunis. Pour appuyer davantage ces constats, un troisième et dernier temps a été dédié au chantier de Tunis au lendemain du concours. L’accent mis sur les lieux symboliques du pouvoir et le désir obsessif des autorités à se les approprier ont réduit ce chantier à une redistribution concertée des symboles de la souveraineté nationale dans le but de centraliser et de personnifier le pouvoir en place. Le présent travail se situe dans le cadre des études postcoloniales et projette un regard critique sur la décolonisation en rapport avec ce qu’on a taxé d’urbanisme d’État. Propulsé par une certaine perception de la modernité, cet urbanisme est indissociable d’une instrumentalisation politique qui met l’accent sur les questions identitaires et patrimoniales, insiste sur la rupture avec le passé et tend à écarter l’opinion publique des questions inhérentes à l’aménagement du territoire et à la sauvegarde de la mémoire collective. En procédant par une analyse contextuelle de faits historiques et une lecture typomorphologique de la percée de la Casbah, cette recherche attire l’attention sur l’ampleur de certaines décisions gouvernementales concernant l’aménagement de l’espace urbain et la conservation de l’héritage architectural à court, moyen et long termes. Elle renseigne aussi sur le rôle des collectivités, de l’élite et des professionnels dans la canalisation de ces décisions pour ou contre leur droit à la ville.

Fluid compositions and mineralogy of precipitates from Mid Atlantic Ridge hydrothermal vents at 4°48'S

The effect of volcanic activity on submarine hydrothermal systems has been well documented along fast- and intermediate-spreading centers but not from slow-spreading ridges. Indeed, volcanic eruptions are expected to be rare on slow-spreading axes. Here we report the presence of hydrothermal venting associated with extremely fresh lava flows at an elevated, apparently magmatically robust segment center on the slow-spreading southern Mid-Atlantic Ridge near 5°S. Three high-temperature vent fields have been recognized so far over a strike length of less than 2 km with two fields venting phase-separated, vapor-type fluids. Exit temperatures at one of the fields reach up to 407°C, at conditions of the critical point of seawater, the highest temperatures ever recorded from the seafloor. Fluid and vent field characteristics show a large variability between the vent fields, a variation that is not expected within such a limited area. We conclude from mineralogical investigations of hydrothermal precipitates that vent-fluid compositions have evolved recently from relatively oxidizing to more reducing conditions, a shift that could also be related to renewed magmatic activity in the area. Current high exit temperatures, reducing conditions, low silica contents, and high hydrogen contents in the fluids of two vent sites are consistent with a shallow magmatic source, probably related to a young volcanic eruption event nearby, in which basaltic magma is actively crystallizing. This is the first reported evidence for direct magmatic-hydrothermal interaction on a slow-spreading mid-ocean ridge.

Environmental controls on the Emiliania huxleyi calcite mass

Although ocean acidification is expected to impact (bio)calcification by decreasing the seawater carbonate ion concentration, [CO3]2-, there exists evidence of non-uniform response of marine calcifying plankton to low seawater [CO3]2-. This raises questions on the role of environmental factors other than acidification and on the complex physiological responses behind calcification. Here we investigate the synergistic effect of multiple environmental parameters, including temperature, nutrient (nitrate and phosphate) availability, and seawater carbonate chemistry on the coccolith calcite mass of the cosmopolitan coccolithophore Emiliania huxleyi, the most abundant species in the world ocean. We use a suite of surface (late Holocene) sediment samples from the South Atlantic and southwestern Indian Ocean taken from depths lying well above the modern lysocline. The coccolith calcite mass in our results presents a latitudinal distribution pattern that mimics the main oceanographic features, thereby pointing to the potential importance of phosphorus and temperature in determining coccolith mass by affecting primary calcification and possibly driving the E. huxleyi morphotype distribution. This evidence does not necessarily argue against the potentially important role of the rapidly changing seawater carbonate chemistry in the future, when unabated fossil fuel burning will likely perturb ocean chemistry beyond a critical point. Rather our study highlights the importance of evaluating the combined effect of several environmental stressors on calcifying organisms to project their physiological response(s) in a high CO2 world and improve interpretation of paleorecords.

Integrated stratigraphy of the Messinian across the North Atlantic Ocean

The Messinian was a time of major climatic and paleoceanographic change during the late Cenozoic. It is well known around the Mediterranean region because of the giant anhydritelgypsum sequence and the suggested desiccation of the Mediterranean Sea. However, this interval is less constrained outside the Mediterranean region, where several paleoceanographic changes could have taken place because of the desiccation. Hence, we present an integrated stratigraphic framework for future Messinian paleoceanographic studies, determination of the effect of the Mediterranean desiccation on deep-water paleoceanography, and comparison of intra-Mediterranean paleoceanographic changes with those in the open oceans during the Messinian Stage. Four DSDP/ODP Holes (552A, 646B, 608, and 547A) from the North Atlantic Ocean and one land borehole from Morocco have been studied to integrate bio-, magneto-, and stable isotope Messinian stratigraphy with high resolution sampling. Our results produce the best assessment of the Tortonian/Messinian boundaries in all holes because they do not rely on any one signal. In paleomagnetic Subchronozone C3An1r in the Sale borehole and DSDP Site 609, a S/D coiling direction change of Neogloboquadrina pachyderma/acostaensis appears to indicate PMOW entering the northeastern Atlantic Ocean, at least reaching 50°N. Diachrony and synchrony of some important Messinian planktic foraminifera from these Atlantic DSDP/ODP holes and the Sale borehole, such as the LO of Gq. dehiscens, the LO of Gt. Eenguaensis, the FO and LO of Ct. conomiozea, the FO of Gt. margaritae s.s., the FO of Gt. puncticutata, and the FO of Gt. crassaformis are discussed for understanding some of the paleoceanographic changes. This integrated stratigraphic framework presented here allows much better North Atlantic correlations at this critical point in Messinian geologic history.

The Coordinated City’s Mutation Machine: Capitalism, Sympathy, and Urbanization in Seattle’s South Lake Union Neighborhood

Thesis (Ph.D.)--University of Washington, 2016-06

Intersectionality in the Language and Writing Classroom

Thesis (Ph.D.)--University of Washington, 2016-06

Local Actors in Donor-Funded Rule of Law Assistance in Indonesia: Owners, Partners, Agents?

Thesis (Ph.D.)--University of Washington, 2016-06

The possessive logic of patriarchal white sovereignty: The High Court and the Yorta Yorta decision

Race is fundamental in shaping the development of Australian law just as it has played its part in other former colonies, such as the United States, where a body of critical race theory has been established on the basis of this premise. Drawing on this theory I argue that the possessive logic of patriarchal white sovereignty works ideologically to naturalise the nation as a white possession by informing and circulating a coherent set of meanings about white possession as part of common sense knowledge and socially produced conventions in the High Court's Yorta Yorta decision.

Adsorption of ethylene on graphitized thermal carbon black and in slit pores: A computer simulation study

In this paper, we studied vapor-liquid equilibria (VLE) and adsorption of ethylene on graphitized thermal carbon black and in slit pores whose walls are composed of graphene layers. Simple models of a one-center Lennard-Jones (LJ) potential and a two-center united atom (UA)-LJ potential are investigated to study the impact of the choice of potential models in the description of VLE and adsorption behavior. Here, we used a Monte Carlo simulation method with grand canonical Monte Carlo (GCMC) and Gibbs ensemble Monte Carlo ensembles. The one-center potential model cannot describe adequately the VLE over the practical range of temperature from the triple point to the critical point. On the other hand, the two-center potential model (Wick et al. J. Phys. Chem. B 2000, 104, 8008-8016) performs well in the description of VLE (saturated vapor and liquid densities and vapor pressure) over the wide range of temperature. This UA-LJ model is then used in the study of adsorption of ethylene on graphitized thermal carbon black and in slit pores. Agreement between the GCMC simulation results and the experimental data on graphitized thermal carbon black for moderate temperatures is excellent, demonstrating that the potential of the GCMC method and the proper choice of potential model are essential to investigate adsorption. For slit pores of various sizes, we have found that the behavior of ethylene exhibits a number of features that are not manifested in the study of spherical LJ particles. In particular, the singlet density distribution versus distance across the pore and the angle between the molecular axis and the z direction provide rich information about the way molecules arrange themselves when the pore width is varied. Such an arrangement has been found to be very sensitive to the pore width.

Accelerating precursory activity within a class of earthquake analogue automata

A statistical fractal automaton model is described which displays two modes of dynamical behaviour. The first mode, termed recurrent criticality, is characterised by quasi-periodic, characteristic events that are preceded by accelerating precursory activity. The second mode is more reminiscent of SOC automata in which large events are not preceded by an acceleration in activity. Extending upon previous studies of statistical fractal automata, a redistribution law is introduced which incorporates two model parameters: a dissipation factor and a stress transfer ratio. Results from a parameter space investigation indicate that a straight line through parameter space marks a transition from recurrent criticality to unpredictable dynamics. Recurrent criticality only occurs for models within one corner of the parameter space. The location of the transition displays a simple dependence upon the fractal correlation dimension of the cell strength distribution. Analysis of stress field evolution indicates that recurrent criticality occurs in models with significant long-range stress correlations. A constant rate of activity is associated with a decorrelated stress field.