893 resultados para Salt marshes.
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Resumen tomado del autor. Se muestran dibujos de posiciones en anilla y p??rtiga
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Resumen tomado de la publicación
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Módulo segundo del primer crédito para el área de Educación Física del ciclo 12-16. Presenta un esquema de todo el módulo con la ordenación de los bloques de contenido propuestos, los objetivos didácticos, las actividades de aprendizaje y de evaluación así como una temporalización indicativa y los procedimientos de trabajo del material incluido. El modulo trabaja la mejora de los alumnos en sus cualidades físicas básicas, los sistemas de entrenamiento, las carreras de vallas, el salto de longitud y la velocidad. Divide el módulo en veinte unidades didácticas y presenta las actividades de aprendizaje que se proponen en cada una de ellas y que, básicamente, consisten en ejercicios de velocidad, salto y calentamiento. Incluye una serie de consideraciones previas y recomendaciones metodológicas para el profesor a la hora de llevar a cabo las actividades de aprendizaje.
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Resumen tomado de la revista
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Pla de ciutadania sobre el municipi de Salt. Per què Salt necessita un Pla de Ciutadania? En primer lloc, pel canvi poblacional sobtat, ja que en menys d’una dècada (1999-2009) s’ha passat d’un 6% de població nouvinguda, a més del 40%. Tot un repte per a la convivència quotidiana, per una resposta de qualitat des dels serveis públics i per a la cohesió com a poble. Determinants que es necessiten anys per consolidar en el desenvolupament com a societat, voluntat política i planificació estratègica
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Crònica del Museu de l'Aigua de Salt, instal·lat a l'edifici del mas Llorens, dedicat bàsicament a la sèquia Monar i al curs mitjà del Ter i obert l'any 1990
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Zooplankton community structure (composition, diversity, dynamics and trophic relationships) of Mediterranian marshes, has been analysed by means of a size based approach. In temporary basins the shape of the biomass-size spectra is related to the hydrological cycle. Linear shape spectra are more frequent in flooding situations when nutrient input causes population growth of small-sized organisms, more than compensating for the effect of competitive interactions. During confinement conditions the scarcity of food would decrease zooplankton growth and increase intra- and interspecific interactions between zooplankton organisms which favour the greatest sizes thus leading to the appearance of curved shape spectra. Temporary and permanent basins have similar taxonomic composition but the latter have higher species diversity, a more simplified temporal pattern and a size distribution dominated mainly by smaller sizes. In permanents basins zooplankton growth is not only conditioned by the availability of resources but by the variable predation of planktivorous fish, so that the temporal variability of the spectra may also be a result of temporal differences in fish predation. Size diversity seems to be a better indicator of the degree of this community structure than species diversity. The tendency of size diversity to increase during succession makes it useful to discriminate between different succession stages, fact that is not achieved by analysing only species diversity since it is low both under large and frequent or small and rare disturbances. Amino acid composition differences found among stages of copepod species indicate a gradual change in diet during the life cycle of these copepods, which provide evidence of food niche partitioning during ontogeny, whereas Daphnia species show a relatively constant amino acid composition. There is a relationship between the degree of trophic niche overlap among stages of the different species and nutrient concentration. Copepods, which have low trophic niche overlap among stages are dominant in food-limited environments, probably because trophic niche partitioning during development allow them to reduce intraspecific competition between adults, juveniles and nauplii. Daphnia species are only dominant in water bodies or periods with high productivity, probably due to the high trophic niche overlap between juveniles and adults. These findings suggest that, in addition to the effect of interspecific competition, predation and abiotic factors, the intraspecific competition might play also an important role in structuring zooplankton assemblages.
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Els assentaments de gambians, tal com succeeix amb la majoria dels assentaments d'immigrats, tendeixen a la concentració en zones determinades. Per aquest motiu, aquesta tesi se centra en les comarques de Girona, perquè és on s'hi troba l'índex més alt d'aquesta població de tot l'Estat espanyol i es posa el focus d'atenció als municipis de la demarcació que acullen més gambians, concretament Banyoles, Olot i Salt. De la mateixa manera, aquesta tesi vol introduir específicament el grup ètnic soninké o sarahule, bàsicament perquè a la demarcació de Girona és l'ètnia majoritària. Abans d'ubicar els assentaments, ens endinsem en el context d'origen dels immigrats gambians, posant èmfasi especial en l'escolarització a Gambia i també en les migracions soninké. Un cop analitzem els assentaments, ens aproximem a les trajectòries migratòries gambianes, així com en les estratègies que s'utilizen per portar a terme el projecte migratori, l'accés als canals d'informació sobre l'existència de diferents destins on hi ha oportunitats de treball, etc. Ens aproximem també a la integració dels immigrats gambians a la demarcació de Girona fent una aproximació de la inserció d'aquest col·lectiu en la societat de destí, abordant diferents vessants de la seva integració laboral, espaial, entre d'altres. Una integració que dependrà tant del resultat de la voluntat individual de cada immigrant, com també dels serveis que possibilitin la integració, així com de l'accés als propis mecanismes d'integració que té la nostra societat (accés al treball, a un habitatge, etc.) Molts dels immigrats gambians instal·lats a les comarques gironines tenen i han tingut fills i filles, podent parlar, per tant, d'una "segona generació" de gambians. Es fa una aproximació als fills i filles d'aquest col·lectiu introduint-nos en la socialització d'aquests nens i nenes, en els valors dels pares i mares en relació amb l'educació dels seus fills i filles, als canvis en l'estructura familiar un cop realitzat l'assentament en el país de destí i en les relacions de la familia amb amics i parents del mateix grup ètnic. Es fa una anàlisi de la situació escolar dels tres municipis d'estudi, analitzant la distribució d'alumnat d'origen estranger en aquests municipis, així com les estratègies educatives dels mestres que escolaritzen alumnat d'origen gambià. Es posa èmfasi especial en una estratègia bastant seguida pel col·lectiu gambià, fonamentalment d'ètnia sarahule, que ha estat la d'enviar els fills i filles a Gàmbia per temporades lllargues.
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The improved empirical understanding of silt facies in Holocene coastal sequences provided by such as diatom, foraminifera, ostracode and testate amoebae analysis, combined with insights from quantitative stratigraphic and hydraulic simulations, has led to an inclusive, integrated model for the palaeogeomorphology, stratigraphy, lithofacies and biofacies of northwest European Holocene coastal lowlands in relation to sea-level behaviour. The model covers two general circumstances and is empirically supported by a range of field studies in the Holocene deposits of a number of British estuaries, particularly, the Severn. Where deposition was continuous over periods of centuries to millennia, and sea level fluctuated about a rising trend, the succession consists of repeated cycles of silt and peat lithofacies and biofacies in which series of transgressive overlaps (submergence sequences) alternate with series of regressive overlaps (emergence sequences) in association with the waxing and waning of tidal creek networks. Environmental and sea-level change are closely coupled, and equilibrium and secular pattern is of the kind represented ideally by a closed limit cycle. In the second circumstance, characteristic of unstable wetland shores and generally affecting smaller areas, coastal erosion ensures that episodes of deposition in the high intertidal zone last no more than a few centuries. The typical response is a series of regressive overlaps (emergence sequence) in erosively based high mudflat and salt-marsh silts that record, commonly as annual banding, exceptionally high deposition rates and a state of strong disequilibrium. Environmental change, including creek development, and sea-level movement are uncoupled. Only if deposition proceeds for a sufficiently long period, so that marshes mature, are equilibrium and close coupling regained. (C) 2002 Elsevier Science B.V. All rights reserved.
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Although numerous field studies have evaluated flow and transport processes in salt marsh channels, the overall role of channels in delivering and removing material from salt marsh platforms is still poorly characterised. In this paper, we consider this issue based on a numerical hydrodynamic model for a prototype marsh system and on a field survey of the cross-sectional geometry of a marsh channel network. Results of the numerical simulations indicate that the channel transfers approximately three times the volume of water that would be estimated from mass balance considerations alone. Marsh platform roughness exerts a significant influence on the partitioning of discharge between the channel and the marsh platform edge, alters flow patterns on the marsh platform due to its effects on channel-to-platform transfer and also controls the timing of peak discharge relative to marsh-edge overtopping. Although peak channel discharges and velocities are associated with the flood tide and marsh inundation, a larger volume of water is transferred by the channel during ebb flows, a portion of which transfer takes place after the tidal height is below the marsh platform. Detailed surveys of the marsh channels crossing a series of transects at Upper Stiffkey Marsh, north Norfolk, England, show that the total channel cross-sectional area increases linearly with catchment area in the inner part of the marsh, which is consistent with the increase in shoreward tidal prism removed by the channels. Toward the marsh edge, however, a deficit in the total cross-sectional area develops, suggesting that discharge partitioning between the marsh channels and the marsh platform edge may also be expressed in the morphology of marsh channel systems.
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The study of the morphology of tidal networks and their relation to salt marsh vegetation is currently an active area of research, and a number of theories have been developed which require validation using extensive observations. Conventional methods of measuring networks and associated vegetation can be cumbersome and subjective. Recent advances in remote sensing techniques mean that these can now often reduce measurement effort whilst at the same time increasing measurement scale. The status of remote sensing of tidal networks and their relation to vegetation is reviewed. The measurement of network planforms and their associated variables is possible to sufficient resolution using digital aerial photography and airborne scanning laser altimetry (LiDAR), with LiDAR also being able to measure channel depths. A multi-level knowledge-based technique is described to extract networks from LiDAR in a semi-automated fashion. This allows objective and detailed geomorphological information on networks to be obtained over large areas of the inter-tidal zone. It is illustrated using LIDAR data of the River Ems, Germany, the Venice lagoon, and Carnforth Marsh, Morecambe Bay, UK. Examples of geomorphological variables of networks extracted from LiDAR data are given. Associated marsh vegetation can be classified into its component species using airborne hyperspectral and satellite multispectral data. Other potential applications of remote sensing for network studies include determining spatial relationships between networks and vegetation, measuring marsh platform vegetation roughness, in-channel velocities and sediment processes, studying salt pans, and for marsh restoration schemes.
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The European research project TIDE (Tidal Inlets Dynamics and Environment) is developing and validating coupled models describing the morphological, biological and ecological evolution of tidal environments. The interactions between the physical and biological processes occurring in these regions requires that the system be studied as a whole rather than as separate parts. Extensive use of remote sensing including LiDAR is being made to provide validation data for the modelling. This paper describes the different uses of LiDAR within the project and their relevance to the TIDE science objectives. LiDAR data have been acquired from three different environments, the Venice Lagoon in Italy, Morecambe Bay in England, and the Eden estuary in Scotland. LiDAR accuracy at each site has been evaluated using ground reference data acquired with differential GPS. A semi-automatic technique has been developed to extract tidal channel networks from LiDAR data either used alone or fused with aerial photography. While the resulting networks may require some correction, the procedure does allow network extraction over large areas using objective criteria and reduces fieldwork requirements. The networks extracted may subsequently be used in geomorphological analyses, for example to describe the drainage patterns induced by networks and to examine the rate of change of networks. Estimation of the heights of the low and sparse vegetation on marshes is being investigated by analysis of the statistical distribution of the measured LiDAR heights. Species having different mean heights may be separated using the first-order moments of the height distribution.
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The kinetics of reactive uptake of gaseous N2O5 on sub-micron aerosol particles composed of aqueous ammonium sulfate, ammonium hydrogensulfate and sodium nitrate has been investigated. Uptake was measured in a laminar flow reactor, coupled with a differential mobility analyser (DMA) to obtain the aerosol size distribution, with N2O5 detection using NO chemiluminescence. FTIR spectroscopy was used to obtain information about the composition and water content of the aerosol particles under the conditions used in the kinetic measurements. The aerosols were generated by the nebulisation of aqueous salt solutions. The uptake coefficient on the sulfate salts was in the range [gamma]=0.0015 to 0.033 depending on temperature, humidity and phase of the aerosol. On sodium nitrate aerosols the values were much lower, [gamma]<0.001, confirming the inhibition of N2O5 hydrolysis by nitrate ions. At high humidity (>50% r.h.) the uptake coefficient on liquid sulfate aerosols is independent of water content, but at lower humidity, especially below the efflorescence point, the reactivity of the aerosol declines, correlating with the lower water content. The lower uptake rate on solid aerosols may be due to limitations imposed by the liquid volume in the particles. Uptake on sulfate aerosols showed a negative temperature dependence at T>290 K but no significant temperature dependence at lower temperatures. The results are generally consistent with previous models of N2O5 hydrolysis where the reactive intermediate is NO2+ produced by autoionisation of nitrogen pentoxide in the condensed phase.
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The kinetics of uptake of gaseous N2O5 on submicron aerosols containing NaCl and natural sea salt have been investigated in a flow reactor as a function of relative humidity (RH) in the range 30-80% at 295±2K and a total pressure of 1bar. The measured uptake coefficients, γ, were larger on the aerosols containing sea salt compared to those of pure NaCl, and in both cases increased with increasing RH. These observations are explained in terms of the variation in the size of the salt droplets, which leads to a limitation in the uptake rate into small particles. After correction for this effect the uptake coefficients are independent of relative humidity, and agree with those measured previously on larger droplets. A value of γ=0.025 is recommended for the reactive uptake coefficient for N2O5 on deliquesced sea salt droplets at 298K and RH>40%.