994 resultados para casa-1000
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大兴安岭摩天岭泥炭藓泥炭纤维素的δ13C 时间序列揭示了近1000 a 来该区气候的演变过程。区内1000 a 的气候经历了950700 a BP、700300 a BP 及300 a BP 以来三个阶段百年尺度的干湿波动,这些波动上又叠加了一系列数十年尺度的气候变化。该序列指示了大兴安岭地区近代气候向着偏干方向发展。
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A publicação apresenta uma estrutura móvel construída com lona e tubo de ferro que pode ser usada como uma casa de embalagem rudimentar, onde as hortaliças são armazenadas e preparadas entre a colheita e a expedição.
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Identificar genótipos resistentes ao cancro da haste, causado por Diaporthe phaseolorum f. sp. meridionalis, visando o melhoramento genético de soja (Glycine max) e o desenvolvimento de cultivares resistentes.
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Sims-Williams, Patrick, Studies on Celtic Languages before the Year 1000 (Aberystwyth, CMCS Publications, 2007) RAE2008
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De acuerdo a la normativa de TFEs el repositorio no puede dar acceso a este trabajo. Para consultarlo póngase en contacto con el tutor del trabajo. Puede acceder al resumen del mismo pinchando en el pdf adjunto
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Dissertação apresentada à Universidade Fernando Pessoa como parte dos requisitos para obtenção do grau de Mestre em Psicologia Jurídica
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89 hojas.
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24 hojas : ilustraciones, fotografías.
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[22] hojas : ilustraciones, fotografías.
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119 hojas : ilustraciones, fotografías a color.
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3 hojas : ilustraciones.
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126 hojas : ilustraciones.
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33 hojas : ilustraciones.
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16 hojas.
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The aim of this research was to make the first depth profiles of the microbial assimilation of methanol carbon and its oxidation to carbon dioxide and use as an energy source from the microlayer to 1000 m. Some of the highest reported methanol oxidation rate constants of 0.5–0.6 d−1 were occasionally found in the microlayer and immediately underlying waters (10 cm depth), albeit these samples also showed the greatest heterogeneity compared to other depths down to 1000 m. Methanol uptake into the particulate phase was exceptionally low in microlayer samples, suggesting that any methanol utilised by microbes in this environment is for energy generation. The sea surface microlayer and 10 cm depth also showed a higher proportion of bacteria with a low DNA content, and bacterial leucine uptake rates in surface microlayer samples were either less than or the same as those in the underlying 10 cm layer. The average methanol oxidation and particulate rates were however statistically the same throughout the depths sampled, although the latter were highly variable in the near-surface 0.25–2 m compared to deeper depths. The statistically significant relationship demonstrated between uptake of methanol into particles and bacterial leucine incorporation suggests that many heterotrophic bacteria could be using methanol carbon for cellular growth. On average, methanol bacterial growth efficiency (BGEm) in the top 25 m of the water column is 6% and decreases with depth. Although, for microlayer and 10 cm-depth samples, BGEm is less than the near-surface 25–217 cm, possibly reflecting increased environmental UV stress resulting in increased maintenance costs, i.e. energy required for survival. We conclude that microbial methanol uptake rates, i.e. loss from seawater, are highly variable, particularly close to the seawater surface, which could significantly impact upon seawater concentrations and hence the air–sea flux.