Gute Kabeljau- und Schellfischvorkommen bei der Bären Insel

Biological investigations were carried out onboard the commercial freezing trawler "Kiel" in the Bear Island area in May/June 1995. Data will be used as German contribution to the assessments of the ICES "Artic Fisheries Working Group". Concentrations of cod were found southwest of Bear Island. Catches ammounted to 5-60 t/haul. Relatively good catches (5-25 t) with high proportions of haddock (40-80 %) were observed to the northwest of the island. Length- and age distributions as well as preliminary results of stomach- and gonad- investigations are presented.

Geological evolution of two crustal scale shear zones. Part I. The Rand thrust complex, northwestern Mojave Desert, California. Part II. The Magdalena metamorphic core complex, north central Sonora, Mexico

The geology and structure of two crustal scale shear zones were studied to understand the partitioning of strain within intracontinental orogenic belts. Movement histories and regional tectonic implications are deduced from observational data. The two widely separated study areas bear the imprint of intense Late Mesozoic through Middle Cenozoic tectonic activity. A regional transition from Late Cretaceous-Early Tertiary plutonism, metamorphism, and shortening strain to Middle Tertiary extension and magmatism is preserved in each area, with contrasting environments and mechanisms. Compressional phases of this tectonic history are better displayed in the Rand Mountains, whereas younger extensional structures dominate rock fabrics in the Magdalena area.

In the northwestern Mojave desert, the Rand Thrust Complex reveals a stack of four distinctive tectonic plates offset along the Garlock Fault. The lowermost plate, Rand Schist, is composed of greenschist facies metagraywacke, metachert, and metabasalt. Rand Schist is structurally overlain by Johannesburg Gneiss (= garnet-amphibolite grade orthogneisses, marbles and quartzites), which in turn is overlain by a Late Cretaceous hornblende-biotite granodiorite. Biotite granite forms the fourth and highest plate. Initial assembly of the tectonic stack involved a Late Cretaceous? south or southwest vergent overthrusting event in which Johannesburg Gneiss was imbricated and attenuated between Rand Schist and hornblende-biotite granodiorite. Thrusting postdated metamorphism and deformation of the lower two plates in separate environments. A post-kinematic stock, the Late Cretaceous Randsburg Granodiorite, intrudes deep levels of the complex and contains xenoliths of both Rand Schist and mylonitized Johannesburg? gneiss. Minimum shortening implied by the map patterns is 20 kilometers.

Some low angle faults of the Rand Thrust Complex formed or were reactivated between Late Cretaceous and Early Miocene time. South-southwest directed mylonites derived from Johannesburg Gneiss are commonly overprinted by less penetrative north-northeast vergent structures. Available kinematic information at shallower structural levels indicates that late disturbance(s) culminated in northward transport of the uppermost plate. Persistence of brittle fabrics along certain structural horizons suggests a possible association of late movement(s) with regionally known detachment faults. The four plates were juxtaposed and significant intraplate movements had ceased prior to Early Miocene emplacement of rhyolite porphyry dikes.

In the Magdalena region of north central Sonora, components of a pre-Middle Cretaceous stratigraphy are used as strain markers in tracking the evolution of a long lived orogenic belt. Important elements of the tectonic history include: (1) Compression during the Late Cretaceous and Early Tertiary, accompanied by plutonism, metamorphism, and ductile strain at depth, and thrust driven? syntectonic sedimentation at the surface. (2) Middle Tertiary transition to crustal extension, initially recorded by intrusion of leucogranites, inflation of the previously shortened middle and upper crustal section, and surface volcanism. (3) Gravity induced development of a normal sense ductile shear zone at mid crustal levels, with eventual detachment and southwestward displacement of the upper crustal stratigraphy by Early Miocene time.

Elucidation of the metamorphic core complex evolution just described was facilitated by fortuitous preservation of a unique assemblage of rocks and structures. The "type" stratigraphy utilized for regional correlation and strain analysis includes a Jurassic volcanic arc assemblage overlain by an Upper Jurassic-Lower Cretaceous quartz pebble conglomerate, in turn overlain by marine strata with fossiliferous Aptian-Albian limestones. The Jurassic strata, comprised of (a) rhyolite porphyries interstratified with quartz arenites, (b) rhyolite cobble conglomerate, and (c) intrusive granite porphyries, are known to rest on Precambrian basement north and east of the study area. The quartz pebble conglomerate is correlated with the Glance Conglomerate of southeastern Arizona and northeastern Sonora. The marine sequence represents part of an isolated arm? of the Bisbee Basin.

Crosscutting structural relationships between the pre-Middle Cretaceous supracrustal section, younger plutons, and deformational fabrics allow the tectonic sequence to be determined. Earliest phases of a Late Cretaceous-Early Tertiary orogeny are marked by emplacement of the 78 ± 3 Ma Guacomea Granodiorite (U/Pb zircon, Anderson et al., 1980) as a sill into deep levels of the layered Jurassic series. Subsequent regional metamorphism and ductile strain is recorded by a penetrative schistosity and lineation, and east-west trending folds. These fabrics are intruded by post-kinematic Early Tertiary? two mica granites. At shallower crustal levels, the orogeny is represented by north directed thrust faulting, formation of a large intermontane basin, and development of a pronounced unconformity. A second important phase of ductile strain followed Middle Tertiary? emplacement of leucogranites as sills and northwest trending dikes into intermediate levels of the deformed section (surficial volcanism was also active during this transitional period to regional extension). Gravitational instabilities resulting from crustal swelling via intrusion and thermal expansion led to development of a ductile shear zone within the stratigraphic horizon occupied by a laterally extensive leucogranite sill. With continued extension, upper crustal brittle normal faults (detachment faults) enhanced the uplift and tectonic denudation of this mylonite zone, ultimately resulting in southwestward displacement of the upper crustal stratigraphy.

Strains associated with the two ductile deformation events have been successfully partitioned through a multifaceted analysis. R_f/Ø measurements on various markers from the "type" stratigraphy allow a gradient representing cumulative strain since Middle Cretaceous time to be determined. From this gradient, noncoaxial strains accrued since emplacement of the leucogranites may be removed. Irrotational components of the postleucogranite strain are measured from quartz grain shapes in deformed granites; rotational components (shear strains) are determined from S-C fabrics and from restoration of rotated dike and vein networks. Structural observations and strain data are compatable with a deformation path of: (1) coaxial strain (pure shear?), followed by (2) injection of leucogranites as dikes (perpendicular to the minimum principle stress) and sills (parallel to the minimum principle stress), then (3) southwest directed simple shear. Modeling the late strain gradient as a simple shear zone permits a minimum displacement of 10 kilometers on the Magdalena mylonite zone/detachment fault system. Removal of the Middle Tertiary noncoaxial strains yields a residual (or pre-existing) strain gradient representative of the Late Cretaceous-Early Tertiary deformation. Several partially destrained cross sections, restored to the time of leucogranite emplacement, illustrate the idea that the upper plate of the core complex bas been detached from a region of significant topographic relief. 50% to 100% bulk extension across a 50 kilometer wide corridor is demonstrated.

Late Cenozoic tectonics of the Magdalena region are dominated by Basin and Range style faulting. Northeast and north-northwest trending high angle normal faults have interacted to extend the crust in an east-west direction. Net extension for this period is minor (10% to 15%) in comparison to the Middle Tertiary detachment related extensional episode.

Perspectiva social de la infancia en algunas comunidades del País Vasco: Opiniones de las y los adolescentes de Santurtzi sobre sexismo

Resumen: El presente estudio ha intentado conocer la perspectiva que tienen las y los adolescentes de Santurtzi sobre el sexismo, eligiendo la adolescencia por su carácter fundamental en el desarrollo vital. Partimos de una investigación cualitativa llevada a cabo con 17 adolescentes a través de grupos de discusión sobre sexismo, patriarcado y alternativas de construcción personal, como son el movimiento feminista y el movimiento de nuevas masculinidades. Hemos podido corroborar el desconocimiento que todavía existe en materia de igualdad y la necesidad de intervenciones socioeducativas que de ello se desprenden, para así continuar con la lucha contra el patriarcado y contra la discriminación hacia la mujer, desde la perspectiva que nos aporta el sexismo ambivalente.

Ancillary ligand effects : from zirconium(IV)-catalyzed homogeneous propylene polymerization to platinum(II)-mediated C-H bond activation

A series of C_s- and C₁-symmetric doubly-linked ansa-metallocenes of the general formula {1,1'-SiMe₂-2,2'-E-('ƞ⁵-C₅H₂-4-R¹)-(ƞ⁵-C₅H-3',5'-(CHMe₂)₂)}ZrC₂ (E = SiMe₂ (1), SiPh₂ (2), SiMe₂ -SiMe₂ (3); R¹ = H, CHMe₂, C₅H₉, C₆H₁₁, C₆H₅) has been prepared. When activated by methylaluminoxane, these are active propylene polymerization catalysts. 1 and 2 produce syndiotactic polypropylenes, and 3 produces isotactic polypropylenes. Site epimerization is the major pathway for stereoerror formation for 1 and 2. In addition, the polymer chain has slightly stronger steric interaction with the diphenylsilylene linker than with the dimethylsilylene linker. This results in more frequent site epimerization and reduced syndiospecificity for 2 compared to 1.

C₁-Symmetric ansa-zirconocenes [1,1 '-SiMe₂-(C₅H₄)-(3-R-C₅H₃)]ZrCl₂ (4), [1,1 '-SiMe₂-(C₅H₄)-(2,4-R₂-C₅H₂)]ZrCl₂ (5) and [1,1 '-SiMe₂-2,2 '-(SiMe₂-SiMe₂)-(C₅H₃)-( 4-R-C₅H₂)]ZrCl₂ (6) have been prepared to probe the origin of isospecificity in 3. While 4 and 3 produce polymers with similar isospecificity, 5 and 6 give mostly hemi-isotactic-like polymers. It is proposed that the facile site epimerization via an associative pathway allows rapid equilibration of the polymer chain between the isospecific and aspecific insertion sites. This results in more frequent insertion from the isospecific site, which has a lower kinetic barrier for chain propagation. On the other hand, site epimerization for 5 and 6 is slow. This leads to mostly alternating insertion from the isospecific and aspecific sites, and consequently, a hemi-isotactic-like polymers. In comparison, site epimerization is even slower for 3, but enchainment from the aspecific site has an extremely high kinetic barrier for monomer coordination. Therefore, enchainment occurs preferentially from the isospecific site to produce isotactic polymers.

A series of cationic complexes [(ArN=CR-CR=NAr)PtMe(L)]⁺[BF₄]⁺ (Ar = aryl; R = H, CH₃; L = water, trifluoroethanol) has been prepared. They react smoothly with benzene at approximately room temperature in trifluoroethanol solvent to yield methane and the corresponding phenyl Pt(II) cations, via Pt(IV)-methyl-phenyl-hydride intermediates. The reaction products of methyl-substituted benzenes suggest an inherent reactivity preference for aromatic over benzylic C-H bond activation, which can however be overridden by steric effects. For the reaction of benzene with cationic Pt(II) complexes, in which the diimine ligands bear 3,5-disubstituted aryl groups at the nitrogen atoms, the rate-determining step is C-H bond activation. For the more sterically crowded analogs with 2,6-dimethyl-substituted aryl groups, benzene coordination becomes rate-determining. The more electron-rich the ligand, as reflected by the CO stretching frequency in the IR spectrum of the corresponding cationic carbonyl complex, the faster the rate of C-H bond activation. This finding, however, does not reflect the actual C-H bond activation process, but rather reflects only the relative ease of solvent molecules displacing water molecules to initiate the reaction. That is, the change in rates is mostly due to a ground state effect. Several lines of evidence suggest that associative substitution pathways operate to get the hydrocarbon substrate into, and out of, the coordination sphere; i.e., that benzene substitution proceeds by a solvent- (TFE-) assisted associative pathway.

Dynamic rupture simulation integrated with earthquake observations

Dynamic rupture simulations are unique in their contributions to the study of earthquake physics. The current rapid development of dynamic rupture simulations poses several new questions: Do the simulations reflect the real world? Do the simulations have predictive power? Which one should we believe when the simulations disagree? This thesis illustrates how integration with observations can help address these questions and reduce the effects of non-uniqueness of both dynamic rupture simulations and kinematic inversion problems. Dynamic rupture simulations with observational constraints can effectively identify non-physical features inferred from observations. Moreover, the integrative technique can also provide more physical insights into the mechanisms of earthquakes. This thesis demonstrates two examples of such kinds of integration: dynamic rupture simulations of the M_w 9.0 2011 Tohoku-Oki earthquake and of earthquake ruptures in damaged fault zones:

(1) We develop simulations of the Tohoku-Oki earthquake based on a variety of observations and minimum assumptions of model parameters. The simulations provide realistic estimations of stress drop and fracture energy of the region and explain the physical mechanisms of high-frequency radiation in the deep region. We also find that the overridding subduction wedge contributes significantly to the up-dip rupture propagation and large final slip in the shallow region. Such findings are also applicable to other megathrust earthquakes.

(2) Damaged fault zones are usually found around natural faults, but their effects on earthquake ruptures have been largely unknown. We simulate earthquake ruptures in damaged fault zones with material properties constrained by seismic and geological observations. We show that reflected waves in fault zones are effective at generating pulse-like ruptures and head waves tend to accelerate and decelerate rupture speeds. These mechanisms are robust in natural fault zones with large attenuation and off-fault plasticity. Moreover, earthquakes in damaged fault zones can propagate at super-Rayleigh speeds that are unstable in homogeneous media. Supershear transitions in fault zones do not require large fault stresses. In the end, we present observations in the Big Bear region, where variability of rupture speeds of small earthquakes correlates with the laterally variable materials in a damaged fault zone.

Valley evolution by meandering rivers

Fluvial systems form landscapes and sedimentary deposits with a rich hierarchy of structures that extend from grain- to valley scale. Large-scale pattern formation in fluvial systems is commonly attributed to forcing by external factors, including climate change, tectonic uplift, and sea-level change. Yet over geologic timescales, rivers may also develop large-scale erosional and depositional patterns that do not bear on environmental history. This dissertation uses a combination of numerical modeling and topographic analysis to identify and quantify patterns in river valleys that form as a consequence of river meandering alone, under constant external forcing. Chapter 2 identifies a numerical artifact in existing, grid-based models that represent the co-evolution of river channel migration and bank strength over geologic timescales. A new, vector-based technique for bank-material tracking is shown to improve predictions for the evolution of meander belts, floodplains, sedimentary deposits formed by aggrading channels, and bedrock river valleys, particularly when spatial contrasts in bank strength are strong. Chapters 3 and 4 apply this numerical technique to establishing valley topography formed by a vertically incising, meandering river subject to constant external forcing—which should serve as the null hypothesis for valley evolution. In Chapter 3, this scenario is shown to explain a variety of common bedrock river valley types and smaller-scale features within them—including entrenched channels, long-wavelength, arcuate scars in valley walls, and bedrock-cored river terraces. Chapter 4 describes the age and geometric statistics of river terraces formed by meandering with constant external forcing, and compares them to terraces in natural river valleys. The frequency of intrinsic terrace formation by meandering is shown to reflect a characteristic relief-generation timescale, and terrace length is identified as a key criterion for distinguishing these terraces from terraces formed by externally forced pulses of vertical incision. In a separate study, Chapter 5 utilizes image and topographic data from the Mars Reconnaissance Orbiter to quantitatively identify spatial structures in the polar layered deposits of Mars, and identifies sequences of beds, consistently 1-2 meters thick, that have accumulated hundreds of kilometers apart in the north polar layered deposits.

Selective plankton feeding by the coregonid ”bondella” (Coregonus sp.) of Lake Maggiore [Translation from: Translation from: Memorie dell'Istituto Italiano di Idrobiologia Dott.Marco de Marchi 31 181-203, 1974]

In recent times, some specialists have begun to study the subject of food selection of fish in an organized way, thus highlighting its importance. In the present work, the author intends to evaluate the impact of predation on the eupelagic zooplanktonic biocenosis of Lake Maggiore, producing, in this way, as far as possible, a basis for a better understanding of the population dynamics of the species of zooplankton directly involved. Another aspect which has been studied is that related to the mechanism of selective capture set in action by the predator. To this end the study tries to bear in mind that the subject should be interpreted as a function of numerous factors acting contemporaneously, that is as the interaction of characters peculiar to the predator and to the prey. The species studied, locally called ”bondella”, belongs to the family Salmonidae, subfamily Coregoninae and was introduced into Lake Maggiore in 1950.

The connection between single species and ecosystems

Ecosystem level models are motivated by some combination of scientific and practical concerns. Those models motivated by practical concerns are likely to bear little historical relation to previous models. Mechanisms of interaction between particular species and their ecosystems vary enormously. Some species literally construct their own ecosystems. Others have more or less complex and important interactions with other species so that their presence or absence may alter the ecosystem. Prior information about the natural history of particular species can make ecosystem investigations quicker, cheaper, and more effective. The optimal resource for preparing to deal with the unlimited diversity of questions asked of ecologists would be a large' computerized databank of natural history observations for as many species as possible.

The kingdom of the shore: achievement of good ecological potential in reservoirs

The European Water Framework Directive requires member states to restore aquatic habitats to good ecological status (quality) by 2015. Good ecological status is defined as slightly different from high status, which, according to the Directive, means negligible human influence. This poses problems enough for restoration of natural habitats but artificial reservoirs are not excluded from the Directive. They must be restored to good ecological potential. The meaning of good ecological status is linked to that of 'high' ecological status, the pristine reference condition for aquatic habitats under the Directive. From the point of view of an ecologist, this is taken to mean the presence of four fundamental characteristics: nutrient parsimony, characteristic biological and physical structure, connectivity within a wider system and adequate size to give resilience of the biological communities to environmental change. These characteristics are strongly interrelated. Ecological potential must bear some relationship to ecological status but since the reference state for ecological quality is near absence of human impact, it is difficult to see how the criteria for ecological status can be applied to a completely man-made entity where the purpose of the dam is deliberately to interfere with the natural characteristics of a river or former natural lake. Rservoirs are disabled lakes, ususally lakcing the diversity and function provided by a littoral zone. Nonetheless, pragmatic approaches to increasing the biodiversity of reservours are reviewed and conclusions drawn as to the likely effectivemess of the legislation.

A imagem social de mulheres negras universitárias: a silhueta esculpida durante o processo de formação

Este estudo aborda a temática das relações existentes entre a formação universitária e a imagem social de mulheres negras universitárias da área da saúde e suas possíveis transformações pessoais e sociais. Considerando que a formação universitária produz uma valorização social e os seus desdobramentos influenciam nos papéis sociais vividos por este grupo. Buscamos assim, descrever a imagem social de mulheres negras na perspectiva de mulheres negras universitárias e sua autoimagem social; e analisar a influencia da formação universitária na autoimagem social das mesmas. Metodologia: Pesquisa descritivo-exploratória com abordagem qualitativa, realizada com roteiro de entrevista semi estruturada com dez entrevistadas que se autodeclararam pretas ou pardas matriculadas em Programa de Pós-graduação (Mestrado) de uma universidade pública estadual no município do Rio de Janeiro (Brasil). Os dados produzidos foram analisados e interpretados à luz da análise de conteúdo de Bardin. Deste processo emergiram três categorias. A primeira categoria A imagem social da mulher negra na perspectiva de mulheres negras universitárias descreve a condição desigual da mulher negra na sociedade a partir da desvalorização do gênero feminino e da raça (sexismo e o racismo) e o corpo da mulher negra como objeto de sensualidade. A segunda categoria - A formação universitária na vida de mulheres negras desdobrou-se em duas categorias intermediárias: Situações positivas vivenciadas durante a formação (formação universitária como veículo para as transformações sociais e pessoais a partir da ampliação do conhecimento científico e a melhora na inserção social); Situações negativas (desigualdades de classes, sentimentos de indecisão, frustração frente à escolha do curso e limitações na aprendizagem e adaptação). A terceira categoria A autoimagem social de mulheres universitárias negras desenvolve a percepção das entrevistadas acerca da sua autoimagem a partir do processo de formação universitária, e desdobra-se em visões positivas e negativas sobre sua autoimagem. A visão positiva destaca o empoderamento diante da sua condição étnica caracterizado por atitudes perseverantes e demonstração de competência no cotidiano, favorecendo o fortalecimento de posições sociais; algumas inclusive não identificam vivenciar diferenças sociais pela etnia. A visão negativa foi descrita a partir dos sentimentos de baixa estima, insegurança no posicionamento nos espaços sociais e a dificuldade de falar sobre a sua autoimagem. Para as depoentes a autoimagem se traduz não no estereótipo, mas, nas conquistas sociais que elas alcançam decorrente da formação universitária. A formação universitária se torna condição fundamental para transpor os estigmas sociais que interferem na imagem social deste grupo populacional na sociedade.

Necessidades de autocuidado à qualidade de vida de clientes com câncer de cabeça e pescoço: contribuição da enfermagem

Aborda-se a consulta de enfermagem como estratégia de pesquisa, visando identificar necessidades de autocuidado (AC) em clientes com câncer de cabeça e pescoço em tratamento paliativo ambulatorial. Tem-se como objetivos: identificar o perfil sociodemográfico e nosológico dos clientes com câncer de cabeça e pescoço atendidos no ambulatório para cuidados paliativos; identificar a qualidade de vida (QV) dessas pessoas através da consulta de enfermagem; avaliar as mudanças no sistema de autocuidado, considerando a intervenção de enfermagem. O estudo fundamenta-se nos conceitos, protocolos e instrumentos específicos da temática escolhida, e na Teoria do Déficit de Autocuidado de Orem. Escolheu-se o método quantitativo, descritivo, com delineamento pré-experimental tempo-série anterior e posterior em grupo único, que recebeu orientações para o autocuidado na consulta de enfermagem (CE). Foram sujeitos do estudo 77 clientes cadastrados no ambulatório especializado em tratamento paliativo, do INCA do Rio de Janeiro, no período de março a agosto de 2011. Variáveis sociodemográficas e nosológicas compõem o instrumento de produção de dados; enquanto as etapas da sistematização da assistência de enfermagem compõem o formulário para a implementação da CE. Para avaliar a QV aplicou-se o formulário QLQ30-H&N45, sendo os dados produzidos tratados mediante a estatística descritiva. Constatou-se, que a maioria dos 77 (100%) sujeitos do estudo é do sexo masculino e situam-se na faixa etária de 50 a 60 anos. Predominam os residentes na Baixada Fluminense, com ensino fundamental e aposentados. Têm união estável, cuidador informal e referem pouca realização de lazer. A maioria possuía hábito de tabagismo e alcoolismo. Quanto ao perfil nosológico, a maioria possui lesão tumoral inodora, sendo a cavidade oral o sítio mais acometido por câncer, e a metástase local a mais frequente. Quanto à capacidade para AC, a maioria se alimenta, se veste e se locomove sem auxilio. Ressalte-se que, na avaliação da QV, os escores predominantes apontam indicativos de controle de sintomas e funcionalidade. Foram formulados 33 diagnósticos de enfermagem, destacando-se nos domínios: físico, a deglutição prejudicada; no psicológico, a baixa autoestima crônica; no social, a interação social prejudicada; no cognitivo, conhecimento deficiente da doença. Concluiu-se que os objetivos da pesquisa foram alcançados, identificando-se que os clientes com câncer de cabeça e pescoço, em tratamento paliativo, possuem diferentes necessidades de autocuidado, sendo o enfermeiro o profissional responsável pela sua educação em saúde e consequente identificação de demandas para outros profissionais da equipe multiprofissional.

Temperature dependence of thermal properties of Ag8In14Sb55Te23 phase-change memory materials

The dependence of thermal properties of Ag8In14Sb55Te23 phase-change memory materials in crystalline and amorphous states on temperature was measured and analyzed. The results show that in the crystalline state, the thermal properties monotonically decrease with the temperature and present obvious crystalline semiconductor characteristics. The heat capacity, thermal diffusivity, and thermal conductivity decrease from 0.35 J/g K, 1.85 mm(2)/s, and 4.0 W/m K at 300 K to 0.025 J/g K, 1.475 mm(2)/s, and 0.25 W/m K at 600 K, respectively. In the amorphous state, while the dependence of thermal properties on temperature does not present significant changes, the materials retain the glass-like thermal characteristics. Within the temperature range from 320 K to 440 K, the heat capacity fluctuates between 0.27 J/g K and 0.075 J/g K, the thermal diffusivity basically maintains at 0.525 mm(2)/s, and the thermal conductivity decreases from 1.02 W/m K at 320 K to 0.2 W/m K at 440 K. Whether in the crystalline or amorphous state, Ag8In14Sb55Te23 are more thermally active than Ge2Sb2Te5, that is, the Ag8In14Sb55Te23 composites bear stronger thermal conduction and diffusion than the Ge2Sb2Te5 phase-change memory materials.

Upconversion luminescence of TM3+/Yb3+ codoped oxyfluoride glasses

Novel oxyfluoride glasses are developed with the composition of 30SiO(2)-15Al(2)O(3)-28PbF(2)-22CdF(2)-0.1TmF(3)-xYbF(3) -(4.9-x) AlF3(x = 0, 0.5, 1.0, 1.5, 2.0) in mol fraction. Furthermore, the upconversion luminescence characteristics under a 970nm excitation are investigated. Intense blue, red and bear infrared luminescences peaked at 453nm, 476nm, 647nm and 789nm, which correspond to the transitions of Tm3+: D-1(2) -> F-3(4), (1)G(4) -> H-3(6), (1)G(4) -> F-3(4), and H-3(4) -> H-3(6), respectively, are observed. Due to the sensitization of Yb3+ ions, all the upconversion luminescence intensities are enhanced considerably with Yb3+ concentration increasing. The upconversion mechanisms are discussed based on the energy matching rule and quadratic dependence on excitation power. The results indicate that the dominant mechanism is the excited state absorption for those upconversion emissions.

A política de formação dos Agentes Comunitários de Saúde: memória de uma formulação em disputa nos anos 2003-2005

Este estudo trata da formulação da política de formação do agente comunitário de saúde (ACS), buscando compreender as disputas que então se travaram, a partir dos processos políticos relativos à gestão da educação e do trabalho do ACS, implementados no período compreendido entre o início de 2003 e meados de 2005. Para tal fim, foram analisados os documentos debatidos nessa formulação, no intervalo de tempo compreendido entre março de 2003 e julho de 2004, o qual se revelou um período intenso de produção conceitual em torno dessa política. Nos documentos analisados, revelaram-se posições acerca do perfil social do ACS e do trabalho que este deve realizar, articuladas a concepções de ensino e formação em saúde, que disputaram o conteúdo e a forma que a política de formação desses trabalhadores deveria assumir. Tais disputas guardam relação também com o modo como esta função se instituiu no SUS e as contradições geradas desde então; ao mesmo tempo, as posições conflitantes apontam para distintos projetos de saúde, educação e trabalho. Esse processo resultou na publicação do Referencial Curricular para Curso Técnico de Agente Comunitário de Saúde, que consolidou a proposta de formação técnica, mas cuja implementação não tem se dado integralmente, configurando a prevalência de uma qualificação inicial, conforme determina a legislação que orienta o exercício da profissão de ACS. Entretanto, a dissertação indica que o processo não se esgotou, sendo a atual política de formação dos ACS objeto de disputas e demandas, tanto pela sua conservação, quanto pela sua transformação.

Vivenciando lugares prenhes de significados e decifrando simbologias da rua Sacadura Cabral e Morro da Conceição (RJ), arenas de vida e de pertencimento

A cidade do Rio de Janeiro atravessa um momento de intensas metamorfoses. O porto da cidade, que outrora era conhecido com um túmulo de estrangeiros, hoje procura ostentar a alcunha de Porto Maravilha. Com base nos preceitos da Geografia Humanística - vertente que exploraos dramas, alegrias, entusiasmos e decepções ocorridos no mundo vivido, no âmbito das relações do homem com o espaço - procuramos investigar o poder da identidade e do pertencimento de moradores e frequentadores da Zona Portuária da cidade, marcadamente da rua Sacadura Cabral e do Morro da Conceição. Os lugares em tela atravessam um instigante processo de toporreabilitação, que transborda seus impactos no mundo vivido dos indivíduos, nos elos dos mesmos e para com seus lugares de significado, plenos de simbolismo. Neste contexto, o lugar deve ser visto como um contínuo dinâmico, pleno de nuances, fragrâncias, simbolismos e identidades. Afinados com princípios fenomenológicos, buscamos entender as relações dos indivíduos com seus lares, traduzindo assim a alma dos seus lugares, identidade e simbiose. Apoiado em depoimentos, que portam identidades e traduzem culturas pulsantes, procuramos elucidar a força das vivências e o poder do lugar face às transformações ocorridas nas localidades em destaque.