870 resultados para syntatic transfer


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El reconocimiento temprano de anormalidades en la transferencia pasiva de inmunidad en equinos es importante para un manejo satisfactorio de los potrillos. La placenta de la yegua, epiteliocorial, no permite el pasaje de inmunoglobulinas.(Igs). La ingesta de calostro es vital ya que provee las Igs necesarias para alcanzar una concentración sérica de IgG mayor a 800 mg por ciento. Se considerara falla parcial con niveles de IgG entre 400 y 800 mgpor ciento; y total con niveles menores a 400 mg por ciento. La absorción de las Igs es máxima hasta 8 hs después del nacimiento y disminuye hasta hacerse nula a las 24 hs posparto. Los objetivos son: a) estudiar la cinética de la transferencia pasiva de Igs determinando la concentración de IgG sérica en potrillos en el primer trimestre de vida. b) relacionar la concentración de IgG del suero y calostro de la yegua con la concentración sérica de IgG en el potrillo. c) Relacionar en calostro la concentración de inmunoglobulina G con la densidad específica y la determinación semicuantitativa de inmunoglobulina G. d) Relacionar en el suero del potrillo a las 18 - 24 hs posparto la concentración de inmunoglobulina G con la densidad específica y la determinación semicuantitativa de inmunoglobulina G. Material y método: Diseño de estudio: de cohorte, observacional, descriptivo. Animales: 70 yeguas y 70 potrillos de raza Puro Polo. Calostros: 70 muestras Toma de muestras: Yeguas: se tomará una muestra de sangre en el periparto y una muestra de calostro posparto, antes del calostrado del potrillo. Potrillos: se tomarán muestras de sangre seriadas: al nacimiento (precalostrado), 6 hs posparto, 12 hs, 18 hs y 24 hs posparto y a los 21, 60 y 90 días posparto. Determinación de IgG (Suero y calostro): a) Técnica de inmunodifusión radial simple, los resultados se expresará en mg por ciento, en muestras seriadas en intervalos de tiempo preestablecidos. b)Refractometría (con refractómetro Modelo RHC-200/ATC- Arcano). c) Test de gluteralehído, Inmuno -G test. Análisis estadístico: Comparaciones de medias con prueba t apareada o de diferencia de medias, Se considera p significativa < 0,05. Se realizará un análisis de componentes principales. Se correlacionará la concentración de Ig G de suero y calostro de la yegua con la concentración en suero de potrillo. Con los resultados de este trabajo se determinarán los valores de inmunoglobulina en las yeguas y potrillos y su comportamiento en el tiempo, y se validará la sensibilidad y especificidad de las técnicas diagnósticas utilizadas. Los resultados permitirán obtener conocimientos para un manejo racional, desde la perspectiva inmunológica, de los potrillos, al establecer mediante técnicas cuantitativas y semicuantitativas los niveles de Igs séricos alcanzados, favoreciendo un diagnóstico precoz de inmunodeficiencia por fracaso de la transferencia de anticuerpos que pondría en riesgo la vida del potrillo.

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This thesis details the findings of a study relating the transfer of 238U, 228Ra (232Th), 226Ra, and 137Cs from soil to vegetation in an Atlantic blanket bog, upland blanket bog and semi-natural grassland situated along the north-west coast of Ireland. The results of this study provide information on the uptake of these radionuclides by the indigenous vegetation found present in these ecosystems. The ecosystems chosen are internationally recognizable ecosystems and provide a wide variety of vegetation species and contrasting soil physiochemical properties which allow the influence of these parameters on radionuclide uptake to be assessed. The levels of radionuclides in the soil and vegetation were measured using gamma spectrometry, alpha spectrometry and ICP-MS. The nutrient status of the vegetation and soil physiochemical properties were measured using atomic absorption, flame photometry and other analytical techniques. The results of the study indicate that the uptake of 238U and 228Ra (232Th) by vegetation from all three ecosystems was negligible as the levels in all vegetation was below the limits of detection for the methods used in this study. These results appear to indicate that the vegetation studied do not possess the ability to accumulate significant levels of these radionuclides however this assumption cannot be upheld in the case of the Atlantic blanket bog as the levels in the soil of this ecosystem were too low for detection. Similar results were obtained for 226Ra uptake in both the Atlantic blanket bog and grassland for all vegetation with the exception of H. lanatus from the grassland ecosystem. Radium-226 uptake in upland blanket bog was higher and was detectable in the majority of vegetation indigenous to this ecosystem. Transfer factor values ranged from 0.07 to 2.35 and the TF values for E. tetralix were significantly higher than all other vegetation studied. This species of heather demonstrated the ability to accumulate 226Ra to a greater extent than all other vegetation. The uptake of 226Ra by upland blanket bog vegetation appears to be significantly influenced by a range of soil physiochemical properties. The nutrient status of the vegetation, in particular the calcium content in the vegetation appears to have a negative impact on the uptake of this radionuclide. Potassium-40 was detectable in all vegetation present in the three ecosystems and the levels in the grassland soil were significantly higher than the levels in both bogland soils. Transfer factor values for Atlantic blanket bog vegetation ranged from 0.9 to 13 .8 and were significantly higher in E. vaginatum in comparison to C. vulgaris. Potassium-40 TF values for upland blanket bog vegetation on average ranged from 1.4 for C. vulgaris (stems) to 5.2 for E. vaginatum and were statistically similar for all species of vegetation. Transfer factor values for grassland vegetation ranged from 0.7 to 3.8 and were also statistically similar for all species of vegetation indicating that the transfer of 40K to vegetation within the upland bog and grassland ecosystem is not dependent on plant species. Comparisons of 40K TF values for all three ecosystems indicate that the uptake in E. vaginatum from the Atlantic blanket bog was statistically higher than all other vegetation studied. This appears to indicate that E. vaginatum has the ability to accumulate 40K, however, this species of vegetation was also present in the upland blanket and did not demonstrate the same behaviour. The uptake of 40K by vegetation from all three ecosystems was significantly affected by a range of soil physiochemical properties and in some cases the results were contradictory in nature possibly indicating that the affect of these parameters on 40K uptake is species dependent. The most obvious trend in the data was the influence of soil CEC and magnesium levels in vegetation on 40K TF values. A positive correlation was apparent between the CEC of the soil and 40K uptake in vegetation from both the Atlantic blanket bog and grassland ecosystem. A similar trend was apparent between magnesium levels in vegetation and 40K TF values for the upland blanket bog and grassland vegetation. Caesium-13 7 levels were found to be significantly higher in the two bogland soils in comparison to the grassland soil and levels of 137Cs decreased with increasing soil depth. Transfer factor values for Atlantic blanket bog vegetation ranged from 1.9 to 9.6 and TF values were significantly higher in the leaves o f C. vulgaris in comparison to all other vegetation from this ecosystem. Caesium-13 7 TF values for the upland blanket bog vegetation on average ranged from 0.29 for E. tetralix to 1.6 for C. vulgaris. Uptake by the leaves of C. vulgaris was significantly higher than all other vegetation present thereby supporting the trend found within the Atlantic blanket bog vegetation. These results appear to indicate that the leaves of C. vulgaris have the ability to accumulate significant quantities of 137Cs and also that the uptake of 137Cs by this vegetation is dependent on plant compartment as the stems of this vegetation contained significantly lower levels than the leaves in both ecosystems. The uptake of 137Cs by grassland vegetation was very low and was only detectable in a fraction of the vegetation sampled. Caesium-137 TF values for grassland vegetation were in general lower than 0.02. The impact of soil physiochemical properties and nutrient status of vegetation on 137Cs uptake by vegetation appears to be complex and in some cases contradictory. The most apparent trend in the data was the positive influence of vegetation nutrients on 137Cs uptake in particular the magnesium levels present in the vegetation and to a lesser extent the calcium levels present. The results in general indicate that the uptake of 226Ra, 40K and 137Cs by the chosen vegetation is varied and complex and is significantly dependent on the species of vegetation, soil radionuclide concentration, soil physiochemical properties and the nutrient status of the vegetation.

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Magdeburg, Univ., Fak. für Verfahrens- und Systemtechnik, Diss., 2011

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Membrane reactor, reactive membrane separation, arrheotrope, azeotrope, dusty gas model, esterification, residue curve map, distillation, kinetics, singular point, bifurcation

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Free Tube Jet - Impingemenet - Heat Transfer - Arrary - Infrared Techuique - Hole Channels - Heat Transfer Uniformaty

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Inorganic membranes, permeation, diffusion, heat transfer, mass transfer, axial dispersion

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Rotary kilns, Regenerative wall, heat transfer, directly fired, indirectly fired

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Distance learning, Canadian educational system, institution, medial learning, school system Saxony-Anhalt, system theory, qualitative research

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Magdeburg, Univ., Fak. für Geistes-, Sozial- und Erziehungswiss., Diss., 2007

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Magdeburg, Univ., Fak. für Verfahrens- und Systemtechnik, Diss., 2010

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Magdeburg, Univ., Fak. für Verfahrens- und Systemtechnik, Diss., 2013

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Magdeburg, Univ., Fak. für Humanwiss., Diss., 2013

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Magdeburg, Univ., Fak. für Verfahrens- und Systemtechnik, Diss., 2015

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Since the specific heat transfer coefficient (UA) and the volumetric mass transfer coefficient (kLa) play an important role for the design of biotechnological processes, different techniques were developed in the past for the determination of these parameters. However, these approaches often use imprecise dynamic methods for the description of stationary processes and are limited towards scale and geometry of the bioreactor. Therefore, the aim of this thesis was to develop a new method, which overcomes these restrictions. This new approach is based on a permanent production of heat and oxygen by the constant decomposition of hydrogen peroxide in continuous mode. Since the degradation of H2O2 at standard conditions only takes place by the support of a catalyst, different candidates were investigated for their potential (regarding safety issues and reaction kinetic). Manganese-(IV)-oxide was found to be suitable. To compensate the inactivation of MnO2, a continuous process with repeated feeds of fresh MnO2 was established. Subsequently, a scale-up was successfully carried out from 100 mL to a 5 litre glass bioreactor (UniVessel®)To show the applicability of this new method for the characterisation of bioreactors, it was compared with common approaches. With the newly established technique as well as with a conventional procedure, which is based on an electrical heat source, specific heat transfer coefficients were measured in the range of 17.1 – 24.8 W/K for power inputs of about 50 – 70 W/L. However, a first proof of concept regarding the mass transfer showed no constant kLa for different dilution rates up to 0.04 h-1.Based on this, consecutive studies concerning the mass transfer should be made with higher volume flows, due to more even inflow rates. In addition, further experiments are advisable, to analyse the heat transfer in single-use bioreactors and in larger common systems.

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Thermal systems interchanging heat and mass by conduction, convection, radiation (solar and thermal ) occur in many engineering applications like energy storage by solar collectors, window glazing in buildings, refrigeration of plastic moulds, air handling units etc. Often these thermal systems are composed of various elements for example a building with wall, windows, rooms, etc. It would be of particular interest to have a modular thermal system which is formed by connecting different modules for the elements, flexibility to use and change models for individual elements, add or remove elements without changing the entire code. A numerical approach to handle the heat transfer and fluid flow in such systems helps in saving the full scale experiment time, cost and also aids optimisation of parameters of the system. In subsequent sections are presented a short summary of the work done until now on the orientation of the thesis in the field of numerical methods for heat transfer and fluid flow applications, the work in process and the future work.