9 resultados para Ozó

em Consorci de Serveis Universitaris de Catalunya (CSUC), Spain


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Amoz Oz en su ensayo 'Sobre la naturaleza del fanatismo' reivindica la literatura como antídoto contra esa enfermedad venenosa que se está convirtiendo en pandemia...

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Aquest treball planteja treballar en recirculació utilizant ozó per a la desinfecció o reducció de les colònies bacterianes de l'aigua marina. El sistema de recirculació en aqüicultura (SRA) és un procés que millora la qualitat físico-química de l'aigua. D'altra banda, la ozonització permet l'eliminació de compostos tant orgànics com inorgànics, desinfectant i reduint l'lor i la terbolesa de l'aigua, entre d'altres, amb l'inconvenient que l'ozó genera productes residuals en l'aigua salada. S'han realitzat diferents casos d'experimentació (peixos, zooplancton i un biofiltre) per a avaluar l'efecte de l'ozó, tant positiu com negatiu, sobre els organismes marins i l'aigua de cultiu.

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El treball presenta els resultats de l’avaluació de dues noves tècniques en el tractament de les aigües de piscina. Una d’elles es basa en l’aplicació d’ozó per a desinfectar l’aigua, que redueix considerablement la quantitat d’hipoclorit sòdic utilitzada en les piscines convencionals i conseqüentment aporta diversos beneficis. La segona tècnica estudiada es basa en la utilització de diòxid de carboni per a regular el pH, a diferència del típic àcid clorhídric que s’aplica en la majoria de piscines. L’estudi s’ha centrat en les piscines del Servei d’Activitat Física de la UAB i s’ha dividit en tres etapes, definides per l’aplicació de diferents tractaments químics. La utilització d’ozó enfront de l’hipoclorit sòdic ha revelat la variació d’alguns paràmetres de control de qualitat de l’aigua com la concentració d’oxigen dissolt o de subproductes de la desinfecció. L’addició de diòxid de carboni enfront de l’àcid clorhídric ha resultat molt efectiva, en tant que s’han desenvolupat propostes per a optimitzar el sistema i minimitzar el seu consum, fins ara excessiu. Tant una com l’altre, aquestes dues tècniques són una nova proposta que, si bé encara no han estat suficient diversificades i estudiades en el nostre país, sembla que redueixen els impactes ambientals, disminueixen el risc dels problemes de salut i augmenten la confortabilitat i seguretat dels usuaris i treballadors de les piscines.

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The purpose of this work is determine the extent of closure between measurements and models of UV irradiances at diverse sites using state of the art instruments, models, and the best available data as inputs to the models. These include information about aerosol optical depth (unfortunately not extending down as far into the UVB region as desirable because such information is not generally available), ozone column amounts, as well as vertical profiles of temperature. We concentrate on clear-sky irradiances, and report the results in terms of UV Index (UVI)

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To perform a climatic analysis of the annual UV index (UVI) variations in Catalonia, Spain (northeast of the Iberian Peninsula), a new simple parameterization scheme is presented based on a multilayer radiative transfer model. The parameterization performs fast UVI calculations for a wide range of cloudless and snow-free situations and can be applied anywhere. The following parameters are considered: solar zenith angle, total ozone column, altitude, aerosol optical depth, and single-scattering albedo. A sensitivity analysis is presented to justify this choice with special attention to aerosol information. Comparisons with the base model show good agreement, most of all for the most common cases, giving an absolute error within 0.2 in the UVI for a wide range of cases considered. Two tests are done to show the performance of the parameterization against UVI measurements. One uses data from a high-quality spectroradiometer from Lauder, New Zealand [45.04°S, 169.684°E, 370 m above mean sea level (MSL)], where there is a low presence of aerosols. The other uses data from a Robertson–Berger-type meter from Girona, Spain (41.97°N, 2.82°E, 100 m MSL), where there is more aerosol load and where it has been possible to study the effect of aerosol information on the model versus measurement comparison. The parameterization is applied to a climatic analysis of the annual UVI variation in Catalonia, showing the contributions of solar zenith angle, ozone, and aerosols. High-resolution seasonal maps of typical UV index values in Catalonia are presented

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The aim of this work is to study the tropospheric ozone concentrations and daily peak cycles in the Lisbon MetropolitanArea (LMA) during the summer season (June, July and August, JJA) covering the 4-yr study period 2002-2005. Theresults show that all the stations have the same pattern: a minimum in the early morning followed by an increase at 1000UTC reaching to a peak at 1300-1400 UTC, dropped again to minimum values 1800 UTC but with different concentrationsdue to regional and local wind circulations and complex dynamic interactions. We identified in Lisbon city the ozone “weekendeffect”. Finally, we studied an episode of very high levels of tropospheric ozone and related daily ozone concentrationswith some meteorological variables.

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We study large N SU(N) Yang-Mills theory in three and four dimensions using a one-parameter family of supergravity models which originate from non-extremal rotating D-branes. We show explicitly that varying this angular momentum parameter decouples the Kaluza-Klein modes associated with the compact D-brane coordinate, while the mass ratios for ordinary glueballs are quite stable against this variation, and are in good agreement with the latest lattice results. We also compute the topological susceptibility and the gluon condensate as a function of the "angular momentum" parameter.

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The strong influence of the winter North Atlantic Oscillation (NAO) on the total ozone column (TOC) in the Northern Hemisphere has been reported in a number of previous studies. In this study we show that this influence is not restricted to the winter season but is also significant in summer. Especially interesting effects of the summer NAO (SNAO) on the TOC are observed over the eastern Mediterranean region, where a strongly positive SNAO index is related to the creation of a geopotential height-negative anomaly over Greece with maximum amplitude at 200 hPa. Another anomaly was observed west of the Iberian Peninsula with similar effects on the TOC. Analyzing 26 years of Total Ozone Mapping Spectrometer (TOMS) and Ozone Monitoring Instrument (OMI) data from the equator to midlatitudes (60°) in the Northern Hemisphere, we demonstrate that the SNAO accounts for up to 30% of the TOC variability with a strong latitudinal and longitudinal dependence. Additionally, we obtain significant correlations between the NAO index and the thermal tropopause pressure and also with the geopotential heights at 200 and 500 hPa. Finally, some indirect connections between NAO and the TOC through teleconnections are also discussed.

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We present a detailed evaluation of the seasonal performance of the Community Multiscale Air Quality (CMAQ) modelling system and the PSU/NCAR meteorological model coupled to a new Numerical Emission Model for Air Quality (MNEQA). The combined system simulates air quality at a fine resolution (3 km as horizontal resolution and 1 h as temporal resolution) in north-eastern Spain, where problems of ozone pollution are frequent. An extensive database compiled over two periods, from May to September 2009 and 2010, is used to evaluate meteorological simulations and chemical outputs. Our results indicate that the model accurately reproduces hourly and 1-h and 8-h maximum ozone surface concentrations measured at the air quality stations, as statistical values fall within the EPA and EU recommendations. However, to further improve forecast accuracy, three simple bias-adjustment techniques mean subtraction (MS), ratio adjustment (RA), and hybrid forecast (HF) based on 10 days of available comparisons are applied. The results show that the MS technique performed better than RA or HF, although all the bias-adjustment techniques significantly reduce the systematic errors in ozone forecasts.