6 resultados para geopolymeric recycled concret (GRC)

em Acceda, el repositorio institucional de la Universidad de Las Palmas de Gran Canaria. España


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[EN] Ammonium (NH4+) and nitrate (NO3-) are the main constituents of the inorganic nitrogen pool that supports primary production in marine systems. NH4+ release via glutamate deamination in heterotrophic organisms represents the largest recycled nitrogen source in the euphotic zone, supporting around the 80 % of the primary producers requirements (Harrison, 1992). Glutamate dehydrogenase (GDH) is the enzyme that catalyzes this process. This fact has lead to the use of GDH activity as an index, a proxy, for physiological NH4+ formation. The result is a measure of potential excretion that avoids incubation artefacts due to manipulation of the organisms. The relationship between GDH activity and NH4+ excretion in cultures of the marine mysid Leptomysis lingvura is analyzed here. With interspecific and environmental interferences minimized, the study shows that the relationship between GDH activity and NH4+ excretion in L. lingvura is similar to equivalent results measured on mixed assemblages of zooplankton.

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[EN] Nitrogen (N) is essential for life, but its availability is frequently limited in ocean ecosystems. Among all the compounds which influence the N pool, ammonium (NH4+) represents the major source of N for autotrophs. This NH4+ is provided by bacterial remineralization and heterotrophic grazers, with the mesozooplankton responsible for 12% to 33% of the total NH4+ recycled.  Quantifying the excretion physiology of zooplankton is then, necessary to understand the basis of an aquatic ecosystem’s productivity.
The measurement of glutamate dehydrogenase (GDH) activity has been widely used to assess the NH4+ excretion rates in planktonic communities. However, its relationship with the physiology varies with temperature and the nutritional status of the organisms, among other variables. Here we compare the GDH/RNH4+ ratio between oceanic regions with different trophic conditions.  Strengthening our knowledge of the relationship between GDH activities and the NH4+ excretion rates will lead to more meaningful interpretations of the mesoscale variations in planktonic NH4+ excretion.

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[EN]Nitrogen (N) is essential for life, but its availability is frequently limited in ocean ecosystems. Among all the compounds which influence the N pool, ammonium (NH4+) represents the major source of N for autotrophs. This NH4+ is provided by bacterial remineralization and heterotrophic grazers, with the mesozooplankton responsible for 12% to 33% of the total NH4+ recycled. Quantifying the excretion physiology of zooplankton is then, necessary to understand the basis of an aquatic ecosystem?s productivity. The measurement of glutamate dehydrogenase (GDH) activity has been widely used to assess the NH4+ excretion rates in planktonic communities. However, its relationship with the physiology varies with temperature and the nutritional status of the organisms, among other variables. Here we compare the GDH/RNH4+ ratio between oceanic regions with different trophic conditions. Strengthening our knowledge of the relationship between GDH activities and the NH4+ excretion rates will lead to more meaningful interpretations of the mesoscale variations in planktonic NH4+ excretion.

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[ES] En este artículo se analiza la constitución y evolución de la Confederación Hidrográfica del Ebro. Este hecho se enmarca en el contexto de la política hidráulica de oferta, predominante en la España de la Restauración y años posteriores. En efecto, la política de construcción de grandes presas tiene su raíz en las políticas reformistas impulsadas por los gobiernos de las Restauración desde principios del siglo XX; asimismo, la gestión supuso la creación de instituciones responsables, proceso que en el caso de la cuenca Ebro se concretó en la Confederación, entidad de índole corporativa que integraba a los usuarios del agua de este río. [EN] In this article is analysed the constitution and evolution of the Hydrographic Confederation of The River Ebro. This fact is in the line with a hydraulic policy of offer that was predominant in Spain within the Restoration and in the subsequent years. In this way, the construction of big reservoirs policy has its root on reformists politics boosted by the Restoration governments since the beginnings of 20th century; likewise, the management involved the creation of responsible institutions, and this was a process that in the case of the River Ebro basin meant the Confederation, an entity of corporate nature which drew together the water users of this river.

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[EN] It is generally assumed that episodic nutrient pulses by cyclonic eddies into surface waters support a significant fraction of the primary production in subtropical low-nutrient environments in the northern hemisphere. However, contradictory results related to the influence of eddies on particulate organic carbon (POC) export have been reported. As a step toward understanding the complex mechanisms that control export of material within eddies, we present here results from a sediment trap mooring deployed within the path of cyclonic eddies generated near the Canary Islands over a 1.5-year period. We find that, during summer and autumn (when surface stratification is stronger, eddies are more intense, and a relative enrichment in CaCO3 forming organisms occurs), POC export to the deep ocean was 2–4 times higher than observed for the rest of the year. On the contrary, during winter and spring (when mixing is strongest and the seasonal phytoplankton bloom occurs), no significant enhancement of POC export associated with eddies was observed. Our biomarker results suggest that a large fraction of the material exported from surface waters during the late-winter bloom is either recycled in the mesopelagic zone or bypassed by migrant zooplankton to the deep scattering layer, where it would disaggregate to smaller particles or be excreted as dissolved organic carbon. Cyclonic eddies, however, would enhance carbon export below 1000 m depth during the summer stratification period, when eddies are more intense and frequent, highlighting the important role of eddies and their different biological communities on the regional carbon cycle.

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[ES] Este artículo estudia la evolución de la historiografía obrera italiana, que surge del marxismo y vinculada al PCI. Esta historiografía militante se caracterizó por la recopilación de fuentes documentales y el estudio del movimiento organizado, al tiempo que se debatía sobre cuestiones socio-económicas. En una segunda fase, a partir de 1956, la historiografía obrera italiana avanzó en pos de un mayor rigor científico, propósito que se concretó en una mayor apertura de los archivos y en la ampliación de la investigación a temáticas políticamente sensibles. Posteriormente, al calor de los cambios experimentados por el país en los años sesenta y setenta, y favorecida por los contactos con historiografías foráneas, la historiografía obrera italiana perdió progresivamente su carácter militante y se renovó con nuevas interrogantes y metodologías. [EN] This article looks at the evolution of labour historiography in Italy, a movement that emerged from Marxism and was linked to the PCI. This militant historiography was characterized by the compilation of documentary sources and the study of the organised movement, while general socio-economic issues were under discussion. The second phase, from 1956 onward, saw Italian labour historiography making advances in achieving greater thoroughness, involving the opening of more archives and expanding the research to politically sensitive issues. Subsequently, in the light of changes experienced by the country in the 1960s and 1970s, and thanks to foreign historiographies, the Italian labour historiography lost its militant nature in a progressive way and developed new queries and methodologies.