952 resultados para Diffusion and lntermittency


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Pese a la amplia difusión y destacada calidad enológica del Torrontés riojano -perteneciente al grupo de cepajes "criollos"- no se disponía de una caracterización completa del mismo. Su estudio, como parte del programa "Caracterización ampelográfica, fenológica y bioclimática de cepajes" pone al día su descripción según normas actualizadas y homologadas internacionalmente. El método utilizado se basa en los Códigos de Caracteres Ampelográficos de la O.I.V., que incluyen una detallada observación de los órganos de la planta, sinónimos, origen, antecedentes, situación actual, características ampelográficas y diferenciales, comportamientos agronómico y fenológico, y aptitud. Los resultados conformaron una ficha complementada con fotografías de brotes, hoja, racimo, flor, baya y semilla, confrontada con descripciones de cepajes vinculables de las islas Canarias y España continental.

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Seawater that has been altered by reaction with basaltic basement has been sampled from Deep Sea Drilling Project Hole 504B, located on 5.9-m.y.-old crust on the southern flank of the Costa Rica Rift. Fourteen water samples have been collected on Legs 69, 70, and 83, both before and after renewed drilling on the latter two legs, at temperatures from 69 to 133°C and pressures from 390 to 425 bars. The water sampled prior to renewed drilling on Leg 83 had occupied the hole for nearly 2 yr. since it was last flushed with surface seawater at the end of Leg 70. Despite some contamination by seawater during sampling, the composition of two of these waters has been determined by using nitrate as a tag for the contaminant. Both the 80 and 115°C waters have seawater chlorinity, but have lost considerable Mg, Na, K, sulfate, and 02, and have gained Ca, alkalinity, Si, NH3 and H2S. The loss of sulfate is due to anhydrite precipitation, as indicated by the d34S value of the remaining dissolved sulfate. The 87Sr/86Sr ratio has been lowered to 0.7086 for the 80°C water and 0.7078 for the 115°C water, whereas the Sr concentration is nearly unchanged. The changes in major element composition relative to seawater are also larger for the 115°C water, indicating that the basement formation water at this site probably varies in composition with depth. Based on their direction relative to seawater, the compositional changes for the 80 and 115°C waters do not complement the changes inferred for the altered rocks from Hole 504B, suggesting that the bulk composition of the altered rocks, like their mineralogy, is largely unrelated to the present thermal and alteration regime in the hole. The exact nature of the reacted seawaters cannot be determined yet, however. During its 2 yr. residence in the hole, the surface seawater remaining at the end of Leg 70 would have reacted with the wall rocks and exchanged with their interstitial formation waters by diffusion and possibly convection. How far these processes have proceeded is not yet certain, although calculations suggest that diffusion alone could have largely exchanged the surface seawater for interstitial water. The d18O of the samples is indistinguishable from seawater, however, and the d14C of the 80°C sample is similar to that of ocean bottom water. Although the interpretation of these species is ambiguous, that of tritium should not be. Tritium analyses, which are in progress, should clarify the nature of the reacted seawaters obtained from the hole.

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En las coplas reunidas por Margit Frenk bajo el epígrafe: "Que si soy morena", así como en varias referidas a fiestas de la Virgen o agrupadas en otros temas, de índole amorosa, se cruzan varias tradiciones: el tema paneuropeo evocado por la misma investigadora de la afirmación del color moreno, la tradición asociada al nivel culto o noble de la belleza clara, incluso expresamente rubia y de ojos verdes estudiada desde Faral, Lecoy, Dámaso Alonso o María Rosa Lida y en fin una clara presencia bíblica, sobre todo del Cantar de los Cantares. Dada la intensa difusión y comentarios de este libro bíblico en los monasterios, especialmente benedictinos y cistercienses, y en la liturgia mariana, son muchas las vías posibles de interpenetración con la cultura popular.

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The growth of populations is known to be influenced by dispersal, which has often been described as purely diffusive (Kierstead and Slobodkin, 1953; Okubo, 1980). In the open ocean, however, the tendrils and filaments of phytoplankton populations provide evidence for dispersal by stirring (Gower et al., 1980, doi:10.1038/288157a0; Holligan et al., 1993, doi:10.1029/93GB01731). Despite the apparent importance of horizontal stirring for plankton ecology, this process remains poorly characterized. Here we investigate the development of a discrete phytoplankton bloom, which was initiated by the iron fertilization of a patch of water (7 km in diameter) in the Southern Ocean (Boyd et al., 2000, doi:10.1038/35037500). Satellite images show a striking, 150-km-long bloom near the experimental site, six weeks after the initial fertilization. We argue that the ribbon-like bloom was produced from the fertilized patch through stirring, growth and diffusion, and we derive an estimate of the stirring rate. In this case, stirring acts as an important control on bloom development, mixing phytoplankton and iron out of the patch, but also entraining silicate. This may have prevented the onset of silicate limitation, and so allowed the bloom to continue for as long as there was sufficient iron. Stirring in the ocean is likely to be variable, so blooms that are initially similar may develop very differently.