930 resultados para Crayfish Neuromuscular-junction


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El presente trabajo es un macro ciclo de cinco meses que se realizó en la ACADEMIA DE FUTBOL ARNOLDO IGUARAN con niños en edades de los 6 a los 8 años pertenecientes al Municipio de La Villa de San Diego de Ubaté, Colombia; el objetivo principal fue determinar Incidencia de la aplicación de un programa de futbol, en actividades que se basan en el incremento de las unidades motoras activas, utilizando como herramienta un adecuado entrenamiento de la fuerza de tipo neuromuscular, haciendo énfasis en las acciones intermitentes y fundamental mente donde el niño este obligado a desarrollar fuerza y a entrenar con sobre cargas significativas

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El presente trabajo es un macro ciclo de cinco meses que se realizó en la ACADEMIA DE FUTBOL ARNOLDO IGUARAN con niños en edades de los 6 a los 8 años pertenecientes al Municipio de La Villa de San Diego de Ubaté, Colombia; el objetivo principal fue determinar Incidencia de la aplicación de un programa de futbol, en actividades que se basan en el incremento de las unidades motoras activas, utilizando como herramienta un adecuado entrenamiento de la fuerza de tipo neuromuscular, haciendo énfasis en las acciones intermitentes y fundamental mente donde el niño este obligado a desarrollar fuerza y a entrenar con sobre cargas significativas

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El presente trabajo es un macro ciclo de cinco meses que se realizó en la ACADEMIA DE FUTBOL ARNOLDO IGUARAN con niños en edades de los 6 a los 8 años pertenecientes al Municipio de La Villa de San Diego de Ubaté, Colombia; el objetivo principal fue determinar Incidencia de la aplicación de un programa de futbol, en actividades que se basan en el incremento de las unidades motoras activas, utilizando como herramienta un adecuado entrenamiento de la fuerza de tipo neuromuscular, haciendo énfasis en las acciones intermitentes y fundamental mente donde el niño este obligado a desarrollar fuerza y a entrenar con sobre cargas significativas

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This study focuses on mafic volcanic rocks from the Bouvet triple junction, which fall into six geochemically distinct groups: (1) N-MORB, the most widespread type, encountered throughout the study area. (2) Subalkaline volcanics, hawaiites and mugearites strongly enriched in lithophile elements and radiogenic isotopes and composing the Bouvet volcanic rise, and compositionally similar basalts and basaltic andesites from the Spiess Ridge, generated in a deeper, fertile mantle region. (3) Relatively weakly enriched basalts, T-MORB derived by the mixing of Type 1 and 2 melts and exposed near the axes of the Mid-Atlantic, Southwest Indian, and America-Antarctic Ridges. (4) Basalts with a degree of trace lithophile element enrichment similar to the Spiess Ridge and Bouvet Island rocks, but higher in K, P, Ti, and Cr. These occur within extensional structures: the rift valley of the Southwest Indian Ridge, grabens of the East Dislocation Zone, and the linear rise between the Spiess Ridge and Bouvet volcano. Their parental melts presumably separated from plume material that spread from the main channels and underwent fluid-involving differentiation in the mantle. (5) A volcanic suite ranging from basalt to rhyolite, characterized by low concentrations of lithophile elements, particularly TiO2, and occurring on the Shona Seamount and other compressional features within the Antarctic and South American plates near the Bouvet triple junction. Unlike Types 1 to 4, which display tholeiitic differentiation trends, this suite is calc-alkaline. Its parental melts were presumably related to the plume material as well but, subsequently, they underwent a profound differentiation involving fluids and assimilated surrounding rocks in closed magma chambers in the upper mantle. Alternatively, the Shona Seamount might be a fragment of an ancient oceanic island arc. (6) Enriched basalts, distinguished from the other enriched rock types in very high P and radiogenic isotope abundances and composing a tectonic uplift near the junction of the three rifts. It thus follows that the main factors responsible for the compositional diversity of volcanic rocks in this region include (i) mantle source heterogeneity, (ii) plume activity, (iii) an intricate geodynamic setup at the triple junction giving rise to stresses in adjacent plate areas, and (iv) the geological prehistory. The slow spreading rate and ensuing inefficient mixing of the heterogeneous mantle material result in strong spatial variations in basaltic compositions.

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After the successful implementation of a record performing dual-junction solar cell at ultra high concentration, in this paper we present the transition to a triple-junction device. The semiconductor structure of the solar cells is presented and the main changes in respect to a dual-junction design are briefly discussed. Cross-sectional TEM analysis of samples confirms that the quality of the triple-junction structures grown by MOVPE is good, revealing no trace of antiphase disorder, and showing flat, sharp and clear interfaces between the layers. Triple-junction solar cells manufactured on these structures have shown a peak efficiency of 36.2% at 700X, maintaining the efficiency over 35% from 300 to 1200 suns. With some changes in the structure and a fine tuning of its processing, efficiencies close to 40% at 1000 suns are envisaged.