Estudi teòric pràctic de la solubilitat de noves mescles aquoses de nitrats alcalins per climatització per absorció accionada tèrmicament a alta temperatura

Investigación realizada a partir de una estancia como profesor visitante en el Departamento de Ingeniería Mecánica de la Universitat Rovira i Virgili. Las soluciones acuosas de LiNO3 tienen una gran potencialidad para ser utilizadas como fluidos de trabajo en ciclos de absorción a altas temperaturas. La adición de otros nitratos y/o nitritos alcalinos mejora, entre otras propiedades, su solubilidad en H2O, el principal inconveniente de estas soluciones. La información bibliográfica sobre la solubilidad de estas es prácticamente inexistente, por eso, en este trabajo se ha realizado un estudio teórico-práctico de la solubilidad de algunos de estos sistemas.(...)

Contact melting of a three-dimensional phase change material on a flat substrate

In this paper a model is developed to describe the three dimensional contact melting process of a cuboid on a heated surface. The mathematical description involves two heat equations (one in the solid and one in the melt), the Navier-Stokes equations for the flow in the melt, a Stefan condition at the phase change interface and a force balance between the weight of the solid and the countering pressure in the melt. In the solid an optimised heat balance integral method is used to approximate the temperature. In the liquid the small aspect ratio allows the Navier-Stokes and heat equations to be simplified considerably so that the liquid pressure may be determined using an igenfunction expansion and finally the problem is reduced to solving three first order ordinary differential equations. Results are presented showing the evolution of the melting process. Further reductions to the system are made to provide simple guidelines concerning the process. Comparison of the solutions with experimental data on the melting of n-octadecane shows excellent agreement.

Análisis de la dimensión social y económica de la relación de la comunidad de Cumbe con el manglar y los impactos de la industria camaronera

En los últimos años la industria camaronera ha adquirido mucha importancia en Brasil y genera presiones sobre ecosistemas y comunidades tradicionales que viven en equilibrio con su entorno. En Cumbe, una comunidad tradicional del municipio de Aracati, Ceará, Brasil, el ecosistema que rodea a su población es el manglar. Debido a esta fuerte presión, tanto el manglar como los servicios ambientales que la población local se beneficia, están transformándose. En este trabajo, la población local de Cumbe identifica, valora y caracteriza los servicios ambientales que les proporciona el manglar dándole así una vital importancia, que puede servir de precedente para una posible protección. Por otra parte, se hace una aproximación en términos económicos de la pesca artesanal y las granjas de camarón para discutir a corto y a largo plazo cuál es el modelo más sostenible a seguir.

Evaluación ambiental de la acuicultura de camarón sobre el ecosistema manglar en el tramo bajo del río Juguaribe

En los últimos años la acuicultura de camarón se ha desarrollado como industria potencial en Brasil y sus actividades generan presiones sobre ecosistemas y comunidades tradicionales que viven en equilibrio con su entorno. En Cumbe, una comunidad tradicional del municipio de Aracati, Ceará, Brasil, el ecosistema que rodea a su población es el manglar. Debido a esta fuerte presión, tanto el manglar como los servicios ambientales de los que la población local se beneficia, están en peligro. Este estudio pretende evaluar las diferencias entre tres áreas de manglar que están afectadas en diferente grado por la presión de las industrias camaroneras. Se evalúan parámetros biológicos y la estructura de los manglares para observar las posibles diferencias y relacionarlas con las diferentes variables.

Comparativa de equipos de síntesis mecánica : aleaciones de base Al-Cu y Fe-Ni

La síntesis mecánica es un proceso basado en la molturación de una mezcla de polvosometida a altas energías que se producen por los choques entre las partículas y lasbolas de un micromolino, entre las partículas y las paredes del recipiente y entre lasmismas partículas. Los dos procesos involucrados en el proceso de síntesis mecánicason la soldadura en frío y la fractura.El proyecto que se presenta es una continuación de los diferentes estudios realizadosen el departamento de Recerca de Materials i Termodinàmica de la Universidad deGirona sobre el proceso de aleado mecánico, en especial del proyecto de Ivan Darnés(Abril 2005) donde se realizaba un estudio comparativo de los micromolinosPulverisette 7 (P7) y SPEX8000 a partir de dos aleaciones en polvo de base Fe.El presente proyecto tiene como objetivo principal realizar nuevamente unacomparación de los equipos P7 y SPEX8000, pero utilizando otras mezclas de polvoiniciales y modificando los parámetros del proceso. Para tal comparación se estudiaránlas muestras obtenidas a nivel estructural, térmico y morfológico

Full Exploration of the Diels–Alder Cycloaddition on Metallofullerenes M3N@C80 (M=Sc, Lu, Gd): The D5h versus Ih Isomer and the Influence of the Metal Cluster

In this work a detailed investigation of the exohedral reactivity of the most important and abundant endohedral metallofullerene (EMF) is provided, that is, Sc3N@Ih-C80 and its D5h counterpart Sc3N@D5h-C80, and the (bio)chemically relevant lutetium- and gadolinium-based M3N@Ih/D5h-C80 EMFs (M=Sc, Lu, Gd). In particular, we analyze the thermodynamics and kinetics of the Diels–Alder cycloaddition of s-cis-1,3-butadiene on all the different bonds of the Ih-C80 and D5h-C80 cages and their endohedral derivatives. First, we discuss the thermodynamic and kinetic aspects of the cycloaddition reaction on the hollow fullerenes and the two isomers of Sc3N@C80. Afterwards, the effect of the nature of the metal nitride is analyzed in detail. In general, our BP86/TZP//BP86/DZP calculations indicate that [5,6] bonds are more reactive than [6,6] bonds for the two isomers. The [5,6] bond D5h-b, which is the most similar to the unique [5,6] bond type in the icosahedral cage, Ih-a, is the most reactive bond in M3N@D5h-C80 regardless of M. Sc3N@C80 and Lu3N@C80 give similar results; the regioselectivity is, however, significantly reduced for the larger and more electropositive M=Gd, as previously found in similar metallofullerenes. Calculations also show that the D5h isomer is more reactive from the kinetic point of view than the Ih one in all cases which is in good agreement with experiments

Irreversible thermodynamics of Poisson processes with reaction

A kinetic model is derived to study the successive movements of particles, described by a Poisson process, as well as their generation. The irreversible thermodynamics of this system is also studied from the kinetic model. This makes it possible to evaluate the differences between thermodynamical quantities computed exactly and up to second-order. Such differences determine the range of validity of the second-order approximation to extended irreversible thermodynamics

Predictions from information-theoretical models of nonequilibrium radiation

The radiation distribution function used by Domínguez and Jou [Phys. Rev. E 51, 158 (1995)] has been recently modified by Domínguez-Cascante and Faraudo [Phys. Rev. E 54, 6933 (1996)]. However, in these studies neither distribution was written in terms of directly measurable quantities. Here a solution to this problem is presented, and we also propose an experiment that may make it possible to determine the distribution function of nonequilibrium radiation experimentally. The results derived do not depend on a specific distribution function for the matter content of the system

Anàlisi tèrmica de l’obtenció d’òxids de bari a partir de precursors moleculars

Aquest projecte, que col•labora amb el Grup de Recerca en Materials i termodinàmica,tractarà de com obtenir òxids de bari purs per incloure en la matriu del superconductorYBCO a partir de diversos precursors moleculars tals com l’acetat de bari, el propionatde bari i l’etil hexaonat de bari. La dificultat rau en la descomposició tèrmica d’aquestsprecursors a òxid, ja que solen descompondre’s a carbonat. L’estudi consistirà encercar les condicions que evitin la formació de carbonat i per tant afavoreixin l’obtencióde l’òxid.L’estudi es realitza fent ús de les tècniques d’anàlisi tèrmica tals com latermogravimetria i l’anàlisi tèrmica diferencial. A posteriori, també hem utilitzat ladifracció de Raigs-X que ens permetrà analitzar el residu sòlid resultat de ladescomposició i per tant saber quin compost tenim, si òxid o carbonat. Tot i això, caltenir en compte que aquesta tècnica s’ha d’aplicar en finalitzar l’anàlisi tèrmica ja quesinó l’òxid que es forma reacciona amb el CO2 de l’atmosfera amb molta facilitat ialeshores s’observa només carbonat en el resultat

Determinació de la calor de combustió d’una closca d’arròs

Determinació mitjançant una bomba calorimètrica de la calor de combustió d'una closca d'arròs.

Information-theoretical derivation of an extended thermodynamical description of radiative systems

A radiative equation of the Cattaneo–Vernotte type is derived from information theory and the radiative transfer equation. The equation thus derived is a radiative analog of the equation that is used for the description of hyperbolic heat conduction. It is shown, without recourse to any phenomenological assumption, that radiative transfer may be included in a natural way in the framework of extendedirreversible thermodynamics

Entropy Production In Thermodynamic Climate Models

We present a non-equilibrium theory in a system with heat and radiative fluxes. The obtained expression for the entropy production is applied to a simple one-dimensional climate model based on the first law of thermodynamics. In the model, the dissipative fluxes are assumed to be independent variables, following the criteria of the Extended Irreversible Thermodynamics (BIT) that enlarges, in reference to the classical expression, the applicability of a macroscopic thermodynamic theory for systems far from equilibrium. We analyze the second differential of the classical and the generalized entropy as a criteria of stability of the steady states. Finally, the extreme state is obtained using variational techniques and observing that the system is close to the maximum dissipation rate

The second law of thermodynamics and the global climate system : A review of the maximum entropy production principle

The long-term mean properties of the global climate system and those of turbulent fluid systems are reviewed from a thermodynamic viewpoint. Two general expressions are derived for a rate of entropy production due to thermal and viscous dissipation (turbulent dissipation) in a fluid system. It is shown with these expressions that maximum entropy production in the Earth s climate system suggested by Paltridge, as well as maximum transport properties of heat or momentum in a turbulent system suggested by Malkus and Busse, correspond to a state in which the rate of entropy production due to the turbulent dissipation is at a maximum. Entropy production due to absorption of solar radiation in the climate system is found to be irrelevant to the maximized properties associated with turbulence. The hypothesis of maximum entropy production also seems to be applicable to the planetary atmospheres of Mars and Titan and perhaps to mantle convection. Lorenz s conjecture on maximum generation of available potential energy is shown to be akin to this hypothesis with a few minor approximations. A possible mechanism by which turbulent fluid systems adjust themselves to the states of maximum entropy production is presented as a selffeedback mechanism for the generation of available potential energy. These results tend to support the hypothesis of maximum entropy production that underlies a wide variety of nonlinear fluid systems, including our planet as well as other planets and stars

Second differential of the entropy as a criterion for the stability in low-dimensional climate models

The second differential of the entropy is used for analysing the stability of a thermodynamic climatic model. A delay time for the heat flux is introduced whereby it becomes an independent variable. Two different expressions for the second differential of the entropy are used: one follows classical irreversible thermodynamics theory; the second is related to the introduction of response time and is due to the extended irreversible thermodynamics theory. the second differential of the classical entropy leads to unstable solutions for high values of delay times. the extended expression always implies stable states for an ice-free earth. When the ice-albedo feedback is included, a discontinuous distribution of stable states is found for high response times. Following the thermodynamic analysis of the model, the maximum rates of entropy production at the steady state are obtained. A latitudinally isothermal earth produces the extremum in global entropy production. the material contribution to entropy production (by which we mean the production of entropy by material transport of heat) is a maximum when the latitudinal distribution of temperatures becomes less homogeneous than present values

States of maximum entropy production in a onedimensional vertical model with convective adjustment

We investigate the hypothesis that the atmosphere is constrained to maximize its entropy production by using a one-dimensional (1-D) vertical model. We prescribe the lapse rate in the convective layer as that of the standard troposphere. The assumption that convection sustains a critical lapse rate was absent in previous studies, which focused on the vertical distribution of climatic variables, since such a convective adjustment reduces the degrees of freedom of the system and may prevent the application of the maximum entropy production (MEP) principle. This is not the case in the radiative–convective model (RCM) developed here, since we accept a discontinuity of temperatures at the surface similar to that adopted in many RCMs. For current conditions, the MEP state gives a difference between the ground temperature and the air temperature at the surface ≈10 K. In comparison, conventional RCMs obtain a discontinuity ≈2 K only. However, the surface boundary layer velocity in the MEP state appears reasonable (≈3 m s-¹). Moreover, although the convective flux at the surface in MEP states is almost uniform in optically thick atmospheres, it reaches a maximum value for an optical thickness similar to current conditions. This additional result may support the maximum convection hypothesis suggested by Paltridge (1978)