969 resultados para enthalpy of formation


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The seasonal appearance of a deep chlorophyll maximum (DCM) in Lake Superior is a striking phenomenon that is widely observed; however its mechanisms of formation and maintenance are not well understood. As this phenomenon may be the reflection of an ecological driver, or a driver itself, a lack of understanding its driving forces limits the ability to accurately predict and manage changes in this ecosystem. Key mechanisms generally associated with DCM dynamics (i.e. ecological, physiological and physical phenomena) are examined individually and in concert to establish their role. First the prevailing paradigm, “the DCM is a great place to live”, is analyzed through an integration of the results of laboratory experiments and field measurements. The analysis indicates that growth at this depth is severely restricted and thus not able to explain the full magnitude of this phenomenon. Additional contributing mechanisms like photoadaptation, settling and grazing are reviewed with a one-dimensional mathematical model of chlorophyll and particulate organic carbon. Settling has the strongest impact on the formation and maintenance of the DCM, transporting biomass to the metalimnion and resulting in the accumulation of algae, i.e. a peak in the particulate organic carbon profile. Subsequently, shade adaptation becomes manifest as a chlorophyll maximum deeper in the water column where light conditions particularly favor the process. Shade adaptation mediates the magnitude, shape and vertical position of the chlorophyll peak. Growth at DCM depth shows only a marginal contribution, while grazing has an adverse effect on the extent of the DCM. The observed separation of the carbon biomass and chlorophyll maximum should caution scientists to equate the DCM with a large nutrient pool that is available to higher trophic levels. The ecological significance of the DCM should not be separated from the underlying carbon dynamics. When evaluated in its entirety, the DCM becomes the projected image of a structure that remains elusive to measure but represents the foundation of all higher trophic levels. These results also offer guidance in examine ecosystem perturbations such as climate change. For example, warming would be expected to prolong the period of thermal stratification, extending the late summer period of suboptimal (phosphorus-limited) growth and attendant transport of phytoplankton to the metalimnion. This reduction in epilimnetic algal production would decrease the supply of algae to the metalimnion, possibly reducing the supply of prey to the grazer community. This work demonstrates the value of modeling to challenge and advance our understanding of ecosystem dynamics, steps vital to reliable testing of management alternatives.

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Knowledge taught at schools, everyday skills and practical know-how. The relevancy of formation for local elites and the corporative self-government of Early Modern Switzerland Daniel Schläppi, Bern There were different kinds of rural elites in Early Modern Switzerland. The diverse parts of the country developed in very dissimilar ways politically and economically. Some regions were dominated by traditional types of agriculture. Some territories were ruled by major cities. In some of the rural Cantons like Uri, Schwyz, Unterwalden, Glarus and Zug a political elite took control over generations and practiced a cultural lifestyle comparable to the famous aristocracies in cities like Bern, Basel, Freiburg, Luzern, Solothurn and Zurich. Intense proto-industrialization formed a completely different sort of elite with strong affinities to industry and trade in other regions. Meanwhile the habitants of the valley close-by stayed farmers like their ancestors (like in Appenzell). In the most conservative parts of the country mercenary business played an important role till the very end of the Ancien Regime and even furthermore. In summery the variety of historical circumstances caused heterogeneous elites all over. Such socio-political diversity provoked a variety of educational backgrounds. I an academic understanding of the term we know only little about literacy in local rural elites. But there is strong evidence that a lively culture of reading and story-telling existed. This means that even simple countrymen seem to have been in possession of some books. The organisation and capacity of the school system is subject of controversial discussions among up to date researchers. The state of research makes us suppose that the people designed to political careers learned their essential skills not only in school but also in everyday life or on the job. Based on the fact that every community and countless public corporations managed their affairs by their own it’s evident that the local elite’s key-players had a large repertoire of techniques and skills like writing, calculating, strategic thinking or knowledge of oral tradition, old usage or important rituals. Unfortunately the historical actors left not that many sources that would tell us precisely how knowledge and know-how were transferred in former times. Hardly any private account books or common correspondence have been conserved. But a huge bunch of sources that originate from corporative self-administration shows us that most local elites were well-educated and had the necessary skills anyway. Above all other sources like for instance the «Topographische Beschreibungen» (topographic descriptions) that were initiated by the «Ökonomische Gesellschaft» of Berne since the sixties of the 18th century provide an insight into pre-modern classrooms. More important information on the historical formation-reality can be gained by the autobiography of the famous poor peasant Ulrich Bräker (1735‒1798) or some of the novels by Albert Bitzius (1797‒1854, better known as Jeremias Gotthelf). The pedagogic writings by Johann Heinrich Pestalozzi (1746‒1827) and the influences by his mentors Johann Rudolf Tschiffeli (1716‒1780) or Philipp Emanuel von Fellenberg (1771‒1884) are quite illustrative as well.

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Multichronometric analyses were performed on samples from a transect in the French-Italian Western Alps crossing nappes derived from the Briançonnais terrane and the Piemonte-Liguria Ocean, in an endeavour to constrain the high-pressure (HP) metamorphism and the retrogression history. 12 samples of white mica were analysed by 39Ar-40Ar stepwise heating, complemented by 2 samples from the Monte Rosa 100 km to the NE and also attributed to the Briançonnais terrane. One Sm-Nd and three Lu-Hf garnet ages from eclogites were also obtained. White mica ages decrease from ca. 300 Ma in the westernmost samples (Zone Houillère), reaching ca. 300 °C during Alpine metamorphism, to < 48 Ma in the internal units to the East, which reached ca. 500 °C during Alpine orogeny. The conventional “thermochronological” interpretation postulates Cretaceous Eo-Alpine HP metamorphism and younger “cooling ages” in the higher-temperature samples. However, Eocene Lu-Hf and Sm-Nd ages from the same samples cannot be interpreted as post-metamorphic cooling ages, which makes a Cretaceous eclogitization untenable. The age date from this transect require instead to replace conventional “thermochronology” by an approach combining age dating with detailed geochemical, petrological and microstructural investigations. Petrology reveals important mineralogical differences along the transect. Samples from the Zone Houillère mostly contain detrital mica. White mica with Si > 6.45 atoms per formula unit becomes more abundant eastward. Across the whole traverse, HP phengitic mica forms the D1 foliation. Syn-D2 mica is Si-poorer and associated with nappe stacking, exhumation, and hydrous retrogression under greenschist facies conditions. D1 phengite is very often corroded, overgrown or intergrown by syn-D2 muscovite. Most importantly, syn-D2 recrystallization is not limited to S2 schistosity domains; microchemical fingerprinting shows that it also can form pseudomorphs after crystals that could be mistaken to have formed during D1 based on microstructural arguments alone. Thereby the Cl concentration in white mica is a useful discriminator, since D2 retrogression was associated with a less saline fluid than eclogitization. Once the petrological stage is set, geochronology is straightforward. All samples contain mixtures of detrital, syn-D1 and syn-D2 mica, and retrogression phases (D3) in greatly varying proportions according to local pressure-temperature-fluid activity-deformation conditions. The correlation of age vs. Cl/K clearly identifies 47 ± 1 Ma as the age of formation of syn-D1 mica along the entire transect, including the Monte Rosa nappe samples. The inferred age of the greenschist-facies low-Si syn-D2 mica generation ranges within 39-43 Ma, with local variations. Coexistence of D1 and D2 ages, and the constancy of non-reset D1 ages along the entire transect, are strong evidence that the D1 white mica ages are very close to formation ages. Volume diffusion of Ar in white mica (activation energy E = 250 kJ/mol; pressure-adjusted diffusion coefficient D’0 < 0.03 cm2 s-1) has a subordinate effect on mineral ages compared to both prograde and retrograde recrystallization in most samples. Eocene Lu-Hf and Sm-Nd garnet ages are prograde and predate the HP peak.

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Introduction: Cervical vertebral (C) malformation is rarely reported in large breed dogs. Congenital cervical kyphosis (CCK) may result from defects of vertebral segmentation, failure of formation or both. This report describes two cases of C3-C4 CCK in young sighthounds, treated surgically. Case description: An 18-month-old female Deerhound and a six-week-old female Borzoi dog were presented because of the complaints of reluctance to exercise and signs of of neck pain. Both dogs were neurologically normal. Diagnostic imaging revealed C3-C4 deformity, moderate kyphosis, and spinal canal stenosis associated with chronic spinal cord pressure atrophy. Both dogs underwent surgical treatment. Results: A staged two-step surgery starting with dorsal decompression was elected in the Deerhound. After the first surgical procedure, the dog developed focal myelomalacia and phrenic nerve paralysis and was euthanatized. A ventral distraction-fusion technique with two locking plates was performed in the Borzoi. This patient recovered uneventfully and long-term follow-up computed tomography revealed complete spondylodesis. Clinical significance: Until now, CCK has only been described in sighthounds. Congenital cervical kyphosis might be considered a differential diagnosis in these breeds that are presented with signs of cervical pain. Ventral realignment-fusion and bone grafting may be considered for surgical treatment, although the earliest age at which this procedure can and should be performed remains unclear.

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The interior of Hellas Basin displays a complex landscape and a variety of geomorphological domains. One of these domains, the enigmatic banded terrain covers much of the northwestern part of the basin. We use high-resolution (CTX and HiRISE) Digital Terrain Models to show that most of the complex viscous flowing behavior exhibited by the banded terrain is controlled by topography and flow-like interactions between neighboring banded terrain. Furthermore, the interior of the basin hosts several landforms suggestive of the presence of near-surface ice, which include polygonal patterns with elongated pits, scalloped depressions, isolated mounds and collapse structures. We suggest that thermal contraction cracking and sublimation of near-surface ice are responsible for the formation and the development of most of the ice-related landforms documented in Hellas. The relatively pristine form, lack of superposed craters, and strong association with the banded terrain, suggest an Amazonian (<3 Ga) age of formation for these landforms. Finally, relatively high surface pressures (above the triple point of water) expected in Hellas and summer-time temperatures often exceeding the melting point of water ice suggest that the basin may have recorded relatively “temperate” climatic conditions compared to other places on Mars. Therefore, the potentially ice-rich banded terrain may have deformed with lower viscosity and stresses compared to other locations on Mars, which may account for its unique morphology.

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Una de las propuestas centrales de este trabajo, como su título lo indica, es estudiar la correlación entre la configuración formal y semántica de la novela venezolana a partir del modernismo y el proceso de formación ("bildung") que se expresa a través de la revelación de la conciencia y de la subjetividad de sus personajes protagónicos. Considero esta correlación en algunas significativas novelas del modernismo y postmodernismo histórico en Venezuela: es decir, novelas de José Gil Fortoul, Manuel Díaz Rodríguez, Rómulo Gallegos y Teresa de la Parra.

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Deep sea drilling on four seamounts in the Emperor Seamount chain revealed that Paleogene shallow-water carbonate sediments of the "bryozoan-algal" facies crown the basalt edifices. According to the biofacies model of Schlanger and Konishi (1966, 1975), this bryozoan- algal assemblage suggests that the seamounts formed in cooler, more northerly waters than those presently occupied by the island of Hawaii; i.e., the paleolatitudes of formation were greater than 20 °N. Moving southward toward the youngest member of the seamount chain, a facies gradient indicative of warmer waters was observed. This gradient is interpreted as a reflection of a northward shift in isotherms during the time span in which the seamounts were progressively formed (Savin et al., 1975). On all seamounts, sedimentation at the drilling sites occurred in a high-energy environment with water depths of approximately 20 meters. Early-stage carbonate diagenesis began in the phreatic zone in the presence of meteoric water, but proceeded after subsidence of the seamounts into intermediate sea waters, where the bulk, stable isotopic composition was determined. The subsidence into intermediate waters was rapid, and permitted establishment of an isotopic equilibrium which, like the facies gradient, reflects the northward shift in isotherms during the Paleogene. Calcite and zeolite cements comprise the later-stage diagenesis, and originated from solutions arising from the hydrolysis of the underlying basalt. In conclusion, the results of this study of the shallow-water carbonate sediments are not inconsistent with a paleolatitude of formation for Suiko Seamount (Site 433) of 26.9 ±3.5 °N, as determined by paleomagnetic measurements (Kono, 1980).

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El presente trabajo da cuenta de una investigación llevada a cabo entre mediados y fines de los años `90 como parte de la acreditación académica del grado de Licenciatura en Ciencias de la Educación. La misma aborda como tema de estudio el campo de la Educación Superior y las Tecnologías Informáticas, particularmente el uso pedagógico-didáctico que se hace de dichas tecnologías a partir de su introducción en las prácticas de enseñanza. Metodológicamente se trabajó en dos etapas con de estilos de indagación diferenciados, pero a la vez imbricados. La primera consistió en recoger la mirada institucional respecto a la introducción de dichas tecnologías. A tales efectos, se seleccionó como población del estudio a miembros responsables de la conducción institucional de algunas de las Unidades Académicas de la Universidad Nacional de La Plata e Institutos Superiores de Formación Docentes -públicos y privados- de la provincia de Bs. As. Mientras que la segunda etapa se configuró a partir de los hallazgos de la anterior dando lugar a la necesidad de profundizar, mediante un estudio de casos, en el análisis de prácticas de enseñanza en las que se produce la inclusión de las tecnologías informáticas. Intentando visualizar en ellas, no sólo, la introducción de un artefacto novedoso sino la presencia de elementos de una cultura de innovación educativa que den cuenta de procesos de reflexión y de cambio en dichas prácticas. Las conclusiones arribadas posibilitaron integrar la dimensión institucional con la dimensión áulica; conocer prácticas de enseñanza que intentan, desde su espacio de trabajo, modificar la estructura de clase tradicional, acercando a los alumnos otras posibilidades de acceso al conocimiento y vislumbrar, en forma incipiente y en función de las posibilidades profesionales y personales de cada profesor, niveles de reflexión de su propia práctica con el propósito de mejorarlas.

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Esta tesis indaga en los textos escritos por la llamada generación del 37 (o "generación romántica" argentina) en el período de dominio rosista en el Río de la Plata (1830-1852). Se estudia el proceso simbólico de formación de una tradición y un canon literario nacional desde una perspectiva que toma en cuenta tanto los cruces genéricos como el contexto de enunciación de los distintos discursos analizados. En la primera parte, "Escribir (en) el desierto", se analiza el tratamiento del paisaje como forma simbólica en La cautiva de Echeverría, en el marco de los tópicos de la literatura de viaje de la época, y, en la segunda sección, los primeros ensayos dedicados a la formación de una literatura nacional en los periódicos románticos (La Moda, El Zonda, El Iniciador). En la segunda parte, "El tejido biográfico", se aborda el Facundo y el discurso modernizador de Sarmiento; en la tercera, "Linajes, memorias, influencias", se estudia la discusión sobre los límites de la nacionalidad a partir de las Investigaciones sobre la influencia social de la conquista y el sistema colonial de los españoles en Chile de José Victorino Lastarria, memoria presentada en 1844 en la Universidad de Chile, y a la que responden, desde distintos posicionamientos, Bello, Sarmiento y Alberdi.

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La tesis indaga las relaciones entre prensa periódica y cultura literaria que durante la primera mitad del siglo XIX, tanto en Chile como en el Río de la Plata, viabilizaron los procesos de formación de un imaginario y un público lector nacionales, y contribuyeron a la creación -temporal y territorialmente diferenciada- de un canon literario y estético. La tesis analiza las modalidades de construcción pública de las culturas literarias chilena y argentina ya consolidada la independencia, y especialmente los modos en que la prensa periódica incidió en los programas literarios de las respectivas élites letradas. Para ello, se estudia un amplio corpus de publicaciones periódicas que se extiende desde El Recopilador (1836) hasta El Talismán o El Corsario (1840) en el Río de la Plata, y desde El Semanario de Santiago (1842) hasta El Correo Literario (1858) o La Semana (1859) en Chile. Los límites de la periodización propuesta acompañan el itinerario de esas publicaciones de la primera mitad del siglo, y coinciden con el ingreso y la difusión de las ideas románticas que incentivaron la preocupación letrada por definir la problemática relación entre cultura y nacionalidad. El enfoque comparativo, por su parte, contempla particularidades, así como simetrías y divergencias, en la formación de imaginarios y tradiciones culturales de ambos territorios.

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The process of the family farmers' recognition as individuals with rights demonstrates having their first roots, in spite of being recent, if compared to the history of the Brazilian rural syndicalism, still in the constitution of the labor-syndical legislation in 1930. Therefore, seeking to explore that process the present paper has as objective to analyze the family farmers' emergence as individuals of rights in the contemporary Brazilian society, analyzing the processes of formation of the rural syndicalism and the expansion of the labor law for the rural workers as a form of accomplishment of a "regulated citizenship" until the decade of 1970; the urge to the official syndicalism, the structuring of a "new syndicalism" and the new social actors' appearance in the field, which made possible the enlargement of the citizenship spaces in the period of re-democratization in Brazil; the "crisis" of the new syndicalism, the creation of new syndical structures "apart" of the official structure (syndicalism of the family agriculture) and the emergency of the "family farmers" as subject of rights in the recent period.

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Este artículo analiza la población indígena del Bolívar Grande (Colombia) en el tercer cuarto del siglo XIX, en el contexto de formación de la nación y la expansión de la ganadería. Mostramos cómo los elementos discursivos sobre la nación mestiza y la identidad política ciudadana, más el fraccionamiento interno de las comunidades indígenas, facilitaron las acciones de ganaderos y poblaciones mestizas para intentar disolver la propiedad comunal de las tierras de los resguardos. También analizamos las formas de resistencia desplegadas por los indígenas, en especial la instrumentalización que realizaron del discurso liberal, y las negociaciones que establecieron con otros sectores sociales y políticos para defender sus intereses