Escalada deportiva en mini muro artificial : Estudio comparativo en la formación del Profesorado en Educación Física CRUB-UNCO

Para analizar el proceso de aprendizaje de los estudiantes en escalada se diseñó una práctica de escalada en muro (sistema abierto estilo americano) a través de un estudio comparativo entre estudiantes de dos asignaturas correlativas (Deportes Regionales Estivales 1 y 2). El objetivo es conocer la forma de resolución de problemas corporales y motrices en la escalada en el marco del mini muro como dispositivo de enseñanza. Se realizó a mitad del año académico en cada asignatura y para ello se elaboró una planilla de cotejo para registrar y comparar los resultados alcanzados. Se realizó un procesamiento cuantitativo sobre la cantidad de problemas resueltos por grupo. Se trabajó con enfoque cuali-cuantitativo para analizar las formas de resolución de los problemas motrices de los estudiantes. Se observa que los estudiantes de DRE 2 resuelven mayor cantidad de problemas en el muro que los estudiantes de DRE 1. La hipótesis que se sostiene tiene que ver con que los estudiantes más avanzados disponen de una mayor experiencia traducida en inteligencia motriz o disponibilidad corporal y motriz, que los estudiantes de la asignatura previa. Esta comunicación es parte del proyecto 04-B169 "El Andinismo en la Educación Física: Seguridad, enseñanza y formación docente". CRUB-UNCo

Escalada deportiva en mini muro artificial : Estudio comparativo en la formación del Profesorado en Educación Física CRUB-UNCO

Para analizar el proceso de aprendizaje de los estudiantes en escalada se diseñó una práctica de escalada en muro (sistema abierto estilo americano) a través de un estudio comparativo entre estudiantes de dos asignaturas correlativas (Deportes Regionales Estivales 1 y 2). El objetivo es conocer la forma de resolución de problemas corporales y motrices en la escalada en el marco del mini muro como dispositivo de enseñanza. Se realizó a mitad del año académico en cada asignatura y para ello se elaboró una planilla de cotejo para registrar y comparar los resultados alcanzados. Se realizó un procesamiento cuantitativo sobre la cantidad de problemas resueltos por grupo. Se trabajó con enfoque cuali-cuantitativo para analizar las formas de resolución de los problemas motrices de los estudiantes. Se observa que los estudiantes de DRE 2 resuelven mayor cantidad de problemas en el muro que los estudiantes de DRE 1. La hipótesis que se sostiene tiene que ver con que los estudiantes más avanzados disponen de una mayor experiencia traducida en inteligencia motriz o disponibilidad corporal y motriz, que los estudiantes de la asignatura previa. Esta comunicación es parte del proyecto 04-B169 "El Andinismo en la Educación Física: Seguridad, enseñanza y formación docente". CRUB-UNCo

Sulfur isotope rations in oceanic basement samples

Low temperature alteration of oceanic basement rocks is characterized by net gain of sulfur, which commonly yields low d34S values, suggesting involvement of microbial sulfate reduction. In order to test whether secondary sulfide minerals are consistent with a biogenic source, we apply high precision multiple sulfur isotope analysis to bulk rock sulfide and pyrite isolates from two contrasting types of altered oceanic basement rocks, namely serpentinized peridotites and altered basalts. Samples from two peridotite sites (Iberian Margin and Hess Deep) and from a basalt site on the eastern flank of the Juan de Fuca Ridge yield overlapping d34S values ranging from 0 per mil to -44 per mil. In contrast, sulfides in the basalt site are characterized by relatively low D33S values ranging from -0.06 per mil to 0.04 per mil, compared to those from peridotite sites (0.00 per mil to 0.16 per mil). The observed D33S signal is significant considering the analytical precision of 0.014 per mil (2 sigma). We present a batch reaction model that uses observed d34S and D33S relationships to quantify the effect of closed system processes and constrain the isotope enrichment factor intrinsic to sulfate reduction. The estimated enrichment factors as large as 61 per mil and 53 per mil, for peridotite and basalt sites respectively, suggest the involvement of microbial sulfate reduction. The relatively high D33S values in the peridotite sites are due to sulfate reduction in a closed system environment, whereas negative D33S values in the basalt site reflect open system sulfate reduction. A larger extent of sulfate reduction during alteration of peridotite to serpentinite is consistent with its higher H2 production capacity compared to basalt alteration, and further supports in-situ microbial sulfate reduction coupled with H2 production during serpentinization reactions.

(Table 2) Uranium and thorium isotopic composition, activity ratios and ages of bivalvia shells in sediment core GIK14350, northern Germany

A new chemical procedure for cleaning marine carbonates was applied to remove detritus as well as metaloxide contaminations of marine shells from Eemian deposits and adjoining succession of a sediment core from Dagebüll, Schleswig- Holstein. Hence, one can significantly reduce the contamination with detrital uranium and thorium. Thermal ionisation mass spectrometry was applied to determine the uranium and thorium activities used for 230Th/U dating of these shells. At least ten samples of marine bivalves of five different core sections were analysed. Samples located below a five meter thick clay layer at 19-24 m yielded an average age of 132±18 ka. Shells located above the clays at 15-20 m depth were strongly influenced by percolating groundwaters of an open system. Therefore, a reliable dating of these samples was not possible.

Geochemistry of silicate melt inclusions from ODP Holes 137-504B and 140-504B

Geochemical data from plagioclase-hosted silicate melt inclusions from Leg 140, Hole 504B diabase dikes are reported. Hand-picked plagioclase grains were heated to 1260°-1280°C to remelt the glass inclusions and to infer trapping temperatures. The samples were then polished to expose the inclusions, which were analyzed by electron and ion microprobes. Inclusion compositions are mainly in equilibrium with the host plagioclase and are more depleted in incompatible elements than the host rock. Simple crystal-liquid equilibrium calculations show that the melt inclusions could have been in equilibrium with depleted abyssal peridotite diopsides, whereas whole-rock basalt compositions generally could not have been. The melt inclusions are significantly more depleted than normal (N-type) mid-ocean-ridge basalt (MORB) and are consistent with being produced by 8%-16% incremental or open-system melting with 2% residual porosity in the peridotite source. These magmas were formed during pressure-release melting of the mantle over a range of depths between 30 and 15 km.

Escalada deportiva en mini muro artificial : Estudio comparativo en la formación del Profesorado en Educación Física CRUB-UNCO

Para analizar el proceso de aprendizaje de los estudiantes en escalada se diseñó una práctica de escalada en muro (sistema abierto estilo americano) a través de un estudio comparativo entre estudiantes de dos asignaturas correlativas (Deportes Regionales Estivales 1 y 2). El objetivo es conocer la forma de resolución de problemas corporales y motrices en la escalada en el marco del mini muro como dispositivo de enseñanza. Se realizó a mitad del año académico en cada asignatura y para ello se elaboró una planilla de cotejo para registrar y comparar los resultados alcanzados. Se realizó un procesamiento cuantitativo sobre la cantidad de problemas resueltos por grupo. Se trabajó con enfoque cuali-cuantitativo para analizar las formas de resolución de los problemas motrices de los estudiantes. Se observa que los estudiantes de DRE 2 resuelven mayor cantidad de problemas en el muro que los estudiantes de DRE 1. La hipótesis que se sostiene tiene que ver con que los estudiantes más avanzados disponen de una mayor experiencia traducida en inteligencia motriz o disponibilidad corporal y motriz, que los estudiantes de la asignatura previa. Esta comunicación es parte del proyecto 04-B169 "El Andinismo en la Educación Física: Seguridad, enseñanza y formación docente". CRUB-UNCo

Crafting a Third Space: Teacher Beliefs and Practices in Curriculum Reform for Multicultural Education

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

Petrology and geochemistry of early cretaceous bimodal continental flood volcanism of the NW Etendeka, Namibia. Part 2: Characteristics and petrogenesis of the high-Ti latite and high-Ti and low-Ti voluminous quartz latite eruptives

As a result of their relative concentration towards the respective Atlantic margins, the silicic eruptives of the Parana (Brazil)-Etendeka large igneous province are disproportionately abundant in the Etendeka of Namibia. The NW Etendeka silicic units, dated at similar to132 Ma, occupy the upper stratigraphic levels of the volcanic sequences, restricted to the coastal zone, and comprise three latites and five quartz latites (QL). The large-volume Fria QL is the only low-Ti type. Its trace element and isotopic signatures indicate massive crustal input. The remaining NW Etendeka silicic units are enigmatic high-Ti types, geochemically different from low-Ti types. They exhibit chemical affinities with the temporally overlapping Khumib high-Ti basalt (see Ewart et al. Part 1) and high crystallization temperatures (greater than or equal to980 to 1120degreesC) inferred from augite and pigeonite phenocrysts, both consistent with their evolution from a mafic source. Geochemically, the high-Ti units define three groups, thought genetically related. We test whether these represent independent liquid lines of descent from a common high-Ti mafic parent. Although the recognition of latites reduces the apparent silica gap, difficulty is encountered in fractional crystallization models by the large volumes of two QL units. Numerical modelling does, however, support large-scale open-system fractional crystallization, assimilation of silicic to basaltic materials, and magma mixing, but cannot entirely exclude partial melting processes within the temporally active extensional environment. The fractional crystallization and mixing signatures add to the complexity of these enigmatic and controversial silicic magmas. The existence, however, of temporally and spatially overlapping high-Ti basalts is, in our view, not coincidental and the high-Ti character of the silicic magmas ultimately reflects a mantle signature.

Geometric phases of scattering states in a ring geometry: adiabatic pumping in mesoscopic devices

Geometric phases of scattering states in a ring geometry are studied on the basis of a variant of the adiabatic theorem. Three timescales, i.e., the adiabatic period, the system time and the dwell time, associated with adiabatic scattering in a ring geometry play a crucial role in determining geometric phases, in contrast to only two timescales, i.e., the adiabatic period and the dwell time, in an open system. We derive a formula connecting the gauge invariant geometric phases acquired by time-reversed scattering states and the circulating (pumping) current. A numerical calculation shows that the effect of the geometric phases is observable in a nanoscale electronic device.

Gaussian phase-space representations for fermions

We introduce a positive phase-space representation for fermions, using the most general possible multimode Gaussian operator basis. The representation generalizes previous bosonic quantum phase-space methods to Fermi systems. We derive equivalences between quantum and stochastic moments, as well as operator correspondences that map quantum operator evolution onto stochastic processes in phase space. The representation thus enables first-principles quantum dynamical or equilibrium calculations in many-body Fermi systems. Potential applications are to strongly interacting and correlated Fermi gases, including coherent behavior in open systems and nanostructures described by master equations. Examples of an ideal gas and the Hubbard model are given, as well as a generic open system, in order to illustrate these ideas.

Reflective web interface agent

Web interface agent is used with web browsers to assist users in searching and interactions with the WWW. It is used for a variety of purposes, such as web-enabled remote control, web interactive visualization, and e-commerce activities. User may be aware or unaware of its existence. The intelligence of interface agent consists in its capability of learning and decision-making in performing interactive functions on behalf of a user. However, since web is an open system environment, the reasoning mechanism in an agent should be able to adapt changes and make decisions on exceptional situations, and therefore use meta knowledge. This paper proposes a framework of Reflective Web Interface Agent (RWIA) that is to provide causal connections between the application interfaces and the knowledge model of the interface agent. A prototype is also implemented for the purpose of demonstration.

O Fazer Teológico como Hermenêutica-Transdisciplinar: A Teologia desafiada pelo Pensamento Complexo de Edgar Morin

A pesquisa procura identificar como se dá a dinâmica relacional que deve existir entre o saber/fazer teológico e as demais formas de saberes na contemporaneidade, tendo como base o filósofo francês Edgar Morin em seu referencial teórico intitulado Pensamento Complexo . Nessa perspectiva, a pesquisa se delineará por uma hermenêutica complexa ou uma hermenêutica transdisciplinar. Este conceito (Hermenêutica-Transdisciplinar / Hermenêutica na Complexidade) não é um sistema dedutivo, e sim um sistema aberto, operacionalizado por uma razão aberta (racionalidade) que procura interpretar a realidade contemporânea observando a tradição. Também de forma criativa, interpreta a tradição como resposta emergente para a contemporaneidade em meio a uma realidade complexa. A partir desse conceito observam-se também as relações dinâmicas dos saberes deste mesmo tempo, e isso, não apenas observando pelas lentes da interdisciplinaridade, mas indo além, se tornando um saber transdisciplinar. A teologia cristã continua sendo amor à tradição-bíblica, sem jamais transformar-se num sistema completo e acabado do saber teológico. Passado e presente se completam e apenas lançam luz para o futuro. Para isso, na tradição teológica cristã, há na Bíblia fundamentos reflexivos e axiomas, a partir dos quais podemos refletir a respeito de todos os temas que os saberes vão impondo (complexidade na realidade) como tematização.

Knowledge maintenance and the frame problem

Knowledge maintenance is a major challenge for both knowledge management and the Semantic Web. Operating over the Semantic Web, there will be a network of collaborating agents, each with their own ontologies or knowledge bases. Change in the knowledge state of one agent may need to be propagated across a number of agents and their associated ontologies. The challenge is to decide how to propagate a change of knowledge state. The effects of a change in knowledge state cannot be known in advance, and so an agent cannot know who should be informed unless it adopts a simple ‘tell everyone – everything’ strategy. This situation is highly reminiscent of the classic Frame Problem in AI. We argue that for agent-based technologies to succeed, far greater attention must be given to creating an appropriate model for knowledge update. In a closed system, simple strategies are possible (e.g. ‘sleeping dog’ or ‘cheap test’ or even complete checking). However, in an open system where cause and effect are unpredictable, a coherent cost-benefit based model of agent interaction is essential. Otherwise, the effectiveness of every act of knowledge update/maintenance is brought into question.

The sedimentology and diagenesis of the Pendleside limestone group in the Craven Basin of Northern England. Available in 2 volumes.

This thesis describes the stratigraphy, sedimentology and diagenesis of the Pendleside Limestone (Asbian age), a sequence of limestones, shales and dolostones in the Clitheroe area of N. W. England. Field study of 19 measured sections indicates that it was deposited in a rhythmically subsiding basin (Craven Basin) because of movements on the Mid-Craven Fault which was active in Dinantian times. The sequence is up to 190m thick and consists mostly of distal turbidite deposits which have been reworked at horizons when sediment accumulation built up to the wave base. The original depositional fabric and mineralogy of the Pendleside Limestone Group has been extensively modified by diagenetic processes including cementation, authi­genesis, dolomitization and silicification. These processes have been studied using a wide variety of laboratory techniques. The carbonate cements of the PendIeside Limestone consist predominantly of ferroan calcite and non-ferroan calcite with microdolomite incIusions. The former is probably a stable replacement of original-high-magnesian calcite. Cementation was accompanied by the formation of authigenic albite and quartz. Much of the upper part of the Pendleside Limestone has been extensively dolomitized and chertified. Several distinct zones of dolomitization are found which increase in thickness and intensity towards the top of the Pendleside Limestone Group. The dolostone horizons correspond to coarser-grained lithologies deposited during periods of shallow water sedimentation. The composition of the dolomites changes from ferroan dolomite in the lower part of the Group to non-ferroan dolomite in the upper part. The low strontium and sodium content of the dolostones in association with the other evidence suggests that the dolomitization was brought about in an open system by the mixing of marine and fresh water in phreatic lens which were established at periodic intervals. The dolomitization was closely associated with chertification although this was initiated by the dissolution of siliceous spicules which provided the necessary source of silica.

Complete framework for efficient characterisation of non-Markovian processes

A non-Markovian process is one that retains `memory' of its past. A systematic understanding of these processes is necessary to fully describe and harness a vast range of complex phenomena; however, no such general characterisation currently exists. This long-standing problem has hindered advances in understanding physical, chemical and biological processes, where often dubious theoretical assumptions are made to render a dynamical description tractable. Moreover, the methods currently available to treat non-Markovian quantum dynamics are plagued with unphysical results, like non-positive dynamics. Here we develop an operational framework to characterise arbitrary non-Markovian quantum processes. We demonstrate the universality of our framework and how the characterisation can be rendered efficient, before formulating a necessary and sufficient condition for quantum Markov processes. Finally, we stress how our framework enables the actual systematic analysis of non-Markovian processes, the understanding of their typicality, and the development of new master equations for the effective description of memory-bearing open-system evolution.