Evaluación de la ingesta de líquido, pérdida de peso y tasa de sudoración en jóvenes triatletas

Introducción: El triatlón es un deporte de resistencia que comprende tres disciplinas: natación, ciclismo y carrera a pie. Es necesario establecer pautas de hidratación para prevenir deshidrataciones durante entrenamientos o competiciones y mantener un buen estado de hidratación antes, durante y después del ejercicio. El objetivo de este estudio es evaluar la ingesta de líquido, pérdida de peso y tasa de sudoración en jóvenes triatletas, durante diferentes entrenamientos. Material y Métodos: Estudio descriptivo-observacional en 14 triatletas (7 chicos y 7 chicas) durante una sesión de natación, otra de ciclismo y otra de carrera a pie. Se valoró la ingesta de líquido, pérdida de peso, % agua corporal total, % deshidratación y tasa de sudoración. Los triatletas bebieron agua en sus respectivos bidones de 750 ml y se realizó una medición de orina en containers. Resultados: Los resultados del estudio siguiendo el orden de natación, ciclismo y carrera a pie fueron: ingesta agua 2,66±1,94ml/min, 7,91±7,69ml/min y 7,08±4,13ml/min en chicos y 3,43±1,53ml/min, 6,39±5,36ml/min y 8,33±2,74ml/min en chicas; pérdida de peso 0,83±0,5kg, 0,47±0,3kg y 0,98±0,4kg en chicos y 0,79±0,3kg, 0,47±0,58kg y 0,28±0,21kg en chicas; y tasa sudoración 4,44±4,9ml/min, 11,81±6,46ml/min y 5,29±3,13ml/min en chicos y 3,89±2,4ml/min, 4,69±4,20ml/min y 7,96±5,06ml/min en chicas. Conclusiones: Se comparó el porcentaje de agua corporal y deshidratación, la pérdida de peso y la tasa de sudoración con otros estudios y se observa que nuestros resultados son inferiores a los estudios comparados, además están por debajo de la media de recomendaciones de líquido establecidas por el consenso de hidratación.

Sharḥ-i Qaṣīdah-ʼi Burdah : manuscript, 1661

Written in one column, 19 lines per page, in black rubricated in red. Portions of text underlined or punctuated in red

Just Need Some Satisfaction: Examining the Relationship between Passion for Exercise and the Basic Psychological Needs

Individuals often pursue activities for which they are passionate about, and this passion is operationalized as being harmonious (an autonomous desireto engage in the activity) or obsessive (a controlled desire to engage in the activity) in nature (Vallerand et al., 2003). With regard to harmonious passion, Vallerand et al. (2003) suggests that it is fostered in environments that nurture innate needs for autonomy, competence, and relatedness. The purpose of the present study was to explore the nature of the passion-basic psychological needs (competence, autonomy, relatedness) relationship. Kinesiology students (N = 917; Mage = 18.54 SD = 1.66) completed the Passion Scale (Vallerand et al., 2003) and the Psychological Need Satisfaction in Exercise Scale (Wilson et al., 2006). Results from the SEM path analysis indicated that harmonious passion was positively related to competence (SPE = .43) and relatedness (SPE = .43) and obsessive passion was negatively related to autonomy (SPE = -.18)(CFI = .90, RMSEA = .07, SRMR = .07). Implications for exercise participation/enjoyment are discussed.

Data compilation of ESOP

The work in this sub-project of ESOP focuses on the advective and convective transforma-tion of water masses in the Greenland Sea and its neighbouring areas. It includes observational work on the sub-mesoscale and analysis of hydrographic data up to the gyre-scale. Observations of active convective plumes were made with a towed chain equipped with up to 80 CTD sensors, giving a horizontal and vertical resolution of the hydrographic fields of a few metres. The observed scales of the penetrative convective plumes compare well with those given by theory. On the mesoscale the structure of homogeneous eddies formed as a result of deep convection was observed and the associated mixing and renewal of the intermediate layers quantified. The relative importance and efficiency of thermal and haline penetrative convection in relation to the surface boundary conditions (heat and salt fluxes and ice cover) and the ambient stratification are studied using the multi year time series of hydro-graphic data in the central Greenland Sea. The modification of the water column of the Greenland Sea gyre through advection from and mixing with water at its rim is assessed on longer time scales. The relative contributions are quantified using modern water mass analysis methods based on inverse techniques. Likewise the convective renewal and the spreading of the Arctic Intermediate Water from its formation area is quantified. The aim is to budget the heat and salt content of the water column, in particular of the low salinity surface layer, and to relate its seasonal and interannual variability to the lateral fluxes and the fluxes at the air-sea-ice interface. This will allow to estimate residence times for the different layers of the Greenland Sea gyre, a quantity important for the description of the Polar Ocean carbon cycle.

Sedimentology of surface samples from the Weddell Sea, Antarctica

Mineralogical and granulometric properties of glacial-marine surface sediments of the Weddell Sea and adjoining areas were studied in order to decipher spatial variations of provenance and transport paths of terrigenous detritus from Antarctic sources. The silt fraction shows marked spatial differences in quartz contents. In the sand fractions heavy-mineral assemblages display low mineralogical maturity and are dominated by garnet, green hornblende, and various types of clinopyroxene. Cluster analysis yields distinct heavy-mineral assemblages, which can be attributed to specific source rocks of the Antarctic hinterland. The configuration of modern mineralogical provinces in the near-shore regions reflects the geological variety of the adjacent hinterland. In the distal parts of the study area, sand-sized heavy minerals are good tracers of ice-rafting. Granulometric characteristics and the distribution of heavy-mineral provinces reflect maxima of relative and absolute accumulation of ice-rafted detritus in accordance with major iceberg drift tracks in the course of the Weddell Gyre. Fine-grained and coarse-grained sediment fractions may have different origins. In the central Weddell Sea, coarse ice-rafted detritus basically derives from East Antarctic sources, while the fine-fraction is discharged from weak permanent bottom currents and/or episodic turbidity currents and shows affinities to southern Weddell Sea sources. Winnowing of quartz-rich sediments through intense bottom water formation in the southern Weddell Sea provides muddy suspensions enriched in quartz. The influence of quartz-rich suspensions moving within the Weddell Gyre contour current can be traced as far as the continental slope in the northwestern Weddell Sea. In general, the focusing of mud by currents significantly exceeds the relative and absolute contribution of ice-rafted detritus beyond the shelves of the study area.