Chemistry of primary and secondary phases in intraplate basalts and volcaniclastic sediments at DSDP Leg 89 Holes

Electron microprobe data are presented for clinopyroxenes, plagioclases, palagonites, smectites, celadonites, and zeolites in Hole 462A sheet-flow basalts and Site 585 volcaniclastic sediments. Glomerocrystic clinopyroxenes in Hole 462A are predominantly Ti-poor augites with minor fractionation to ferroaugites in rim portions. Quenched plumose clinopyroxenes show considerable variation from Ca-rich to Ca-poor augites, although all are characterized by being Tirich and Cr-poor relative to the glomerocrysts. Two differentiated series of Site 585 pyroxene compositions, calcic augite and diopside-salite, demonstrate the coexistence, in the vitric and lithic clasts, of tholeiitic and alkali basalt types, respectively. Plagioclase compositions in all samples are mainly labradorites, although some zoned Hole 462A glomerocrysts range from An73 to An20 and are characterized by high Mg and Fe contents in the more calcic varieties. The K content of the plagioclases is highest in the more sodic crystals, although the overall higher orthoclase component of Site 585 plagioclases reflects the generally higher bulk-rock K content. The compositions of both secondary smectites and celadonites are similar irrespective of the alteration location (glass, matrix, vesicles, etc.), although brown smectites replacing interstitial glass have marginally higher total Fe contents than pale green and yellow smectites. Analyzed zeolites are mainly phillipsites with variable alkali content, and, together with associated celadonite, represent late-stage alteration repositories for K under mildly oxidizing conditions. The compositions of both early and late secondary minerals are typical of those formed by the submarine alteration of basaltic rocks at low temperatures.

Sulfur isotopic variations in nodular and disseminated pyrite at DSDP Hole 93-603B

Analyses of modern marine sediments have suggested that availability and type of organic matter, sedimentation rate, and openness of the sulfate system influence the degree of isotopic fractionation between seawater sulfate and sedimentary iron sulfides. Isotopic studies of ancient sulfides should, therefore, provide insights into conditions of deposition and early diagenesis. Analysis of d34S of disseminated pyrite from Cretaceous sediments of Hole 603B yielded fractionations relative to coeval seawater sulfate ranging from 40 to 55 per mil, which are within the range for modern oxic marine sediments reported by others. Sulfur/carbon ratios are similar to those found from modern marine sediments and suggest that disseminated pyrite formation was dependent upon available organic carbon. These results imply that depositional and early diagenetic conditions during the Cretaceous in Hole 603B were similar to those occurring in initially oxic marine environments today. Macroscopic (nodular) pyrite from Hole 603B is isotopically variable (d34S values = - 48 to + 33 per mil), but generally more positive than disseminated pyrite. The isotopic evidence suggests that macroscopic pyrite formed during late stages of sulfate reduction in a system closed with respect to sulfate. However, detailed analyses of large pyrite nodules did not yield a consistent pattern of isotopic variation from center to rim.

Nematode abundance in cold seep sediments of the Darwin mud volcano

During the JC-10 cruise (2007), we sampled the Darwin mud volcano (MV) for meiofaunal community and trophic structure in relation of pore-water geochemistry along a 10 m transect from a seep site on the rim of the crater towards the MV slope. Sediment samples were retrieved by the ROV Isis using push cores. On board and after the pore water extraction, the top 10 cm of the cores were sliced into 1 cm sections and fixed them in 4% formaldehyde for meiofaunal community analysis. In the home laboratory, the formaldehyde-fixed samples were washed over a 32 µm mesh sieve and extracted the meiofauna from the sediment by Ludox centrifugation (Heip et al. 1985). Meiofauna was then sorted, enumerated and identified at coarse taxonomic level. From each slice, ca. 100 nematodes were identified to genus level. Afterwards, abundance of Nematoda were depth integrated over the top 5 cm to gain individual abundances per 10 cm**2. Overall, total nematode biomass in the top 5 cm of the seep sediment core was ~10x higher than that in the core taken 1100 m away. Nematode genus composition varied little among cores and was mainly dominated by Sabatieria.

High resolution in situ microsensor measurements of oxygen and temperature at a vesicomyid clam colony in the Japan Deep Sea Trench

Oxygen penetration depth and temperature at the rim of the clam colony was measured with a small deep-sea microprofiler module (Treude et al., 2009), carrying 3 oxygen Clark-type microelectrodes (Revsbech et al., 1980) and one temperature sensor (Pt100, UST Umweltsensorentechnik GmbH, Germany). High-resolution microprofiles across the sediment-water interface were measured with a vertical resolution of 100 µm on a total length of 15 cm. Oxygen electrodes had a linear response to the oxygen concentration in seawater and were calibrated in situ using constant readings in the bottom water (oxygen concentration determined by Winkler titration) and the anoxic parts of the sediment.

Evolution and breakup of viscous rotating drops

We study the evolution of a viscous fluid drop rotating about a fixed axis at constant angular velocity $Omega$ or constant angular momentum L surrounded by another viscous fluid. The problem is considered in the limit of large Ekman number and small Reynolds number. The analysis is carried out by combining asymptotic analysis and full numerical simulation by means of the boundary element method. We pay special attention to the stability/instability of equilibrium shapes and the possible formation of singularities representing a change in the topology of the fluid domain. When the evolution is at constant $Omega$, depending on its value, drops can take the form of a flat film whose thickness goes to zero in finite time or an elongated filament that extends indefinitely. When evolution takes place at constant L and axial symmetry is imposed, thin films surrounded by a toroidal rim can develop, but the film thickness does not vanish in finite time. When axial symmetry is not imposed and L is sufficiently large, drops break axial symmetry and, depending on the value of L, reach an equilibrium configuration with a 2-fold symmetry or break up into several drops with a 2- or 3-fold symmetry. The mechanism of breakup is also described

An Efficient Hybrid GO-PWS Algorithm to Analyze Conformal Serrated-Edge Reflectors for Millimeter-Wave Compact Range

A method to analyze parabolic reflectors with arbitrary piecewise rim is presented in this communication. This kind of reflectors, when operating as collimators in compact range facilities, needs to be large in terms of wavelength. Their analysis is very inefficient, when it is carried out with fullwave/MoM techniques, and it is not very appropriate for designing with PO techniques. Also, fast GO formulations do not offer enough accuracy to reach performance results. The proposed algorithm is based on a GO-PWS hybrid scheme, using analytical as well as non-analytical formulations. On one side, an analytical treatment of the polygonal rim reflectors is carried out. On the other side, non-analytical calculi are based on efficient operations, such as M2 order 2-dimensional FFT. A combination of these two techniques in the algorithm ensures real ad-hoc design capabilities, reached through analysis speedup. The purpose of the algorithm is to obtain an optimal conformal serrated-edge reflector design through the analysis of the field quality within the quiet zone that it is able to generate in its forward half space.

1000x shadow-free mirror-based Köhler concentrator

A new design for a photovoltaic concentrator, the most recent advance based on the Kohler concept, is presented. The system is mirror-based, and with geometry that guaranties a maximum sunlight collection area (without shadows, like those caused by secondary stages or receivers and heat-sinks in other mirror-based systems). Designed for a concentration of 1000x, this off axis system combines both good acceptance angle and good irradiance uniformity on the solar cell. The advanced performance features (concentration-acceptance products ?CAP- about 0.73 and affordable peak and average irradiances) are achieved through the combination of four reflective folds combined with four refractive surfaces, all of them free-form, performing Köhler integration 2 . In Köhler devices, the irradiance uniformity is not achieved through additional optical stages (TIR prisms), thus no complex/expensive elements to manufacture are required. The rim angle and geometry are such that the secondary stage and receivers are hidden below the primary mirrors, so maximum collection is assured. The entire system was designed to allow loose assembly/alignment tolerances (through high acceptance angle) and to be manufactured using already well-developed methods for mass production, with high potential for low cost. The optical surfaces for Köhler integration, although with a quite different optical behavior, have approximately the same dimensions and can be manufactured with the same techniques as the more traditional secondary optical elements used for concentration (typically plastic injection molding or glass molding).

Numerical analysis of deflagration initation by a hot jet

Numerical simulations of axisymmetric reactive jets with one-step Arrhenius kinetics are used to investigate the problem of deflagration initiation in a premixed fuel–air mixture by the sudden discharge of a hot jet of its adiabatic reaction products. For the moderately large values of the jet Reynolds number considered in the computations, chemical reaction is seen to occur initially in the thin mixing layer that separates the hot products from the cold reactants. This mixing layer is wrapped around by the starting vortex, thereby enhancing mixing at the jet head, which is followed by an annular mixing layer that trails behind, connecting the leading vortex with the orifice rim. A successful deflagration is seen to develop for values of the orifice radius larger than a critical value a c in the order of the flame thickness of the planar deflagration δL. Introduction of appropriate scales provides the dimensionless formulation of the problem, with flame initiation characterised in terms of a critical Damköhler number Δc=(a d/δL)2, whose parametric dependence is investigated. The numerical computations reveal that, while the jet Reynolds number exerts a limited influence on the criticality conditions, the effect of the reactant diffusivity on ignition is much more pronounced, with the value of Δc increasing significantly with increasing Lewis numbers. The reactant diffusivity affects also the way ignition takes place, so that for reactants with the flame develops as a result of ignition in the annular mixing layer surrounding the developing jet stem, whereas for highly diffusive reactants with Lewis numbers sufficiently smaller than unity combustion is initiated in the mixed core formed around the starting vortex. The analysis provides increased understanding of deflagration initiation processes, including the effects of differential diffusion, and points to the need for further investigations corporating detailed chemistry models for specific fuel–air mixtures.

Protein diagenesis in Patella shells: implications for amino acid racemisation dating

Se analiza la racemización de aminoácidos en proteínas inter e intracristalinas en conchas de Patella y su utilización como herramienta geocronológica, fundamentalmente empleadas en yacimientos arqueológicos.The inter- and intra-crystalline fractions of Patella vulgata limpets recovered from archaeological sites in Northern Spain (covering Neolithic, Mesolithic, Magdalenian, Solutrean, and Aurignacian periods) were examined for amino acid composition and racemisation over time. The calcitic apex and rim areas of the shells were found to probably be composed of similar proteins, as the D/L values and amino acids were comparable and varied in the same way with increasing age; however, the mineral structures present in these areas differed. The aragonitic intermediate part of the shell showed a distinctly different amino acid composition and mineral structure. The main protein leaching from the inter-crystalline fraction occurred within the first 6000 yr after the death of the organism. In contrast, the intra-crystalline fraction — comprised of a different protein composition than the inter-crystalline fraction — appeared to behave as a closed system for at least 34 ka, as reflected by the lack of a significant decrease in the amino acid content; however, changes in the amino acid percentages occurred during this period. The concentration of aspartic acid remained almost constant with age both in inter- and intra-crystalline proteins, and its contribution to the total amino acid content increased with age at the expense of other amino acids such as glutamic acid, serine, glycine and alanine. Temperature is thought to play a key role in the amino acid racemisation of P. vulgata and could explain why in the localities belonging to the Gravettian and Solutrean period, which formed during relatively cold conditions, D/L values were similar to those detected in shells from sites formed during the Magdalenian.

Mejora postpradial de un controlador basado en reglas

La Diabetes mellitus es una enfermedad caracterizada por la insuficiente o nula producción de insulina por parte del páncreas o la reducida sensibilidad del organismo a esta hormona, que ayuda a que la glucosa llegue a los tejidos y al sistema nervioso para suministrar energía. La Diabetes tiene una mayor prevalencia en los países desarrollados debido a múltiples factores, entre ellos la obesidad, la vida sedentaria, y disfunciones en el sistema endocrino relacionadas con el páncreas. La Diabetes Tipo 1 es una enfermedad crónica e incurable, en la que son destruidas las células beta del páncreas, que producen la insulina, haciéndose necesaria la administración de insulina de forma exógena para controlar los niveles de glucosa en sangre. El paciente debe seguir una terapia con insulina administrada por vía subcutánea, que debe estar adaptada a sus necesidades metabólicas y a sus hábitos de vida. Esta terapia intenta imitar el perfil insulínico de un páncreas sano. La tecnología actual permite abordar el desarrollo del denominado “páncreas endocrino artificial” (PEA), que aportaría precisión, eficacia y seguridad en la aplicación de las terapias con insulina y permitiría una mayor independencia de los pacientes frente a su enfermedad, que en la actualidad están sujetos a una constante toma de decisiones. El PEA consta de un sensor continuo de glucosa, una bomba de infusión de insulina y un algoritmo de control, que calcula la insulina a infusionar utilizando los niveles de glucosa del paciente como información principal. Este trabajo presenta una modificación en el método de control en lazo cerrado propuesto en un proyecto previo. El controlador del que se parte está compuesto por un controlador basal booleano y un controlador borroso postprandial basado en reglas borrosas heredadas del controlador basal. El controlador postprandial administra el 50% del bolo manual (calculado a partir de la cantidad de carbohidratos que el paciente va a consumir) en el instante del aviso de la ingesta y reparte el resto en instantes posteriores. El objetivo es conseguir una regulación óptima del nivel de glucosa en el periodo postprandial. Con el objetivo de reducir las hiperglucemias que se producen en el periodo postprandial se realiza un transporte de insulina, que es un adelanto de la insulina basal del periodo postprandial que se suministrará junto con un porcentaje variable del bolo manual. Este porcentaje estará relacionado con el estado metabólico del paciente previo a la ingesta. Además se modificará la base de conocimiento para adecuar el comportamiento del controlador al periodo postprandial. Este proyecto está enfocado en la mejora del controlador borroso postprandial previo, modificando dos aspectos: la inferencia del controlador postprandial y añadiendo una toma de decisiones automática sobre el % del bolo manual y el transporte. Se ha propuesto un controlador borroso con una nueva inferencia, que no hereda las características del controlado basal, y ha sido adaptado al periodo postprandial. Se ha añadido una inferencia borrosa que modifica la cantidad de insulina a administrar en el momento del aviso de ingesta y la cantidad de insulina basal a transportar del periodo postprandial al bolo manual. La validación del algoritmo se ha realizado mediante experimentos en simulación utilizando una población de diez pacientes sintéticos pertenecientes al Simulador de Padua/Virginia, evaluando los resultados con estadísticos para después compararlos con los obtenidos con el método de control anterior. Tras la evaluación de los resultados se puede concluir que el nuevo controlador postprandial, acompañado de la toma de decisiones automática, realiza un mejor control glucémico en el periodo postprandial, disminuyendo los niveles de las hiperglucemias. ABSTRACT. Diabetes mellitus is a disease characterized by the insufficient or null production of insulin from the pancreas or by a reduced sensitivity to this hormone, which helps glucose get to the tissues and the nervous system to provide energy. Diabetes has more prevalence in developed countries due to multiple factors, including obesity, sedentary lifestyle and endocrine dysfunctions related to the pancreas. Type 1 Diabetes is a chronic, incurable disease in which beta cells in the pancreas that produce insulin are destroyed, and exogenous insulin delivery is required to control blood glucose levels. The patient must follow a therapy with insulin administered by the subcutaneous route that should be adjusted to the metabolic needs and lifestyle of the patient. This therapy tries to imitate the insulin profile of a non-pathological pancreas. Current technology can adress the development of the so-called “endocrine artificial pancreas” (EAP) that would provide accuracy, efficacy and safety in the application of insulin therapies and will allow patients a higher level of independence from their disease. Patients are currently tied to constant decision making. The EAP consists of a continuous glucose sensor, an insulin infusion pump and a control algorithm that computes the insulin amount that has to be infused using the glucose as the main source of information. This work shows modifications to the control method in closed loop proposed in a previous project. The reference controller is composed by a boolean basal controller and a postprandial rule-based fuzzy controller which inherits the rules from the basal controller. The postprandial controller administrates 50% of the bolus (calculated from the amount of carbohydrates that the patient is going to ingest) in the moment of the intake warning, and distributes the remaining in later instants. The goal is to achieve an optimum regulation of the glucose level in the postprandial period. In order to reduce hyperglycemia in the postprandial period an insulin transport is carried out. It consists on a feedforward of the basal insulin from the postprandial period, which will be administered with a variable percentage of the manual bolus. This percentage would be linked with the metabolic state of the patient in moments previous to the intake. Furthermore, the knowledge base is going to be modified in order to fit the controller performance to the postprandial period. This project is focused on the improvement of the previous controller, modifying two aspects: the postprandial controller inference, and the automatic decision making on the percentage of the manual bolus and the transport. A fuzzy controller with a new inference has been proposed and has been adapted to the postprandial period. A fuzzy inference has been added, which modifies both the amount of manual bolus to administrate at the intake warning and the amount of basal insulin to transport to the prandial bolus. The algorithm assessment has been done through simulation experiments using a synthetic population of 10 patients in the UVA/PADOVA simulator, evaluating the results with statistical parameters for further comparison with those obtained with the previous control method. After comparing results it can be concluded that the new postprandial controller, combined with the automatic decision making, carries out a better glycemic control in the postprandial period, decreasing levels of hyperglycemia.

Eduardo Chillida, arquitecto

Es sabido que tras abandonar la carrera de arquitectura Chillida marcha a Paris a comenzar su carrera como escultor. De vuelta al País Vasco el hierro es el material en el que encuentra un camino propio. Toda la obra de su primera década está muy alejada en el aspecto formal de la arquitectura. Sin embargo, las líneas de fuerza que los hierros configuran muestran un interés espacial que queda manifiesto en una obra de 1953 denominada Consejo al espacio I. A partir de aquí su obra gira en torno al vacío. Las formas cambiarán con los materiales pero no el propósito. En sus dibujos, las manos expresan, más allá de su condición figurativa, la búsqueda del espacio cóncavo que los dedos encierran. El espacio que encuentra en la palma de la mano es equivalente al que construye con dedos gigantes de madera u hormigón. Chillida observa sus obras con una mirada cuya idea de escala se distancia del concepto de dimensión. Adquieren así una posibilidad de crecer que facilita imaginar sus espacios como arquitectura. Tras el hierro, el trabajo en madera y alabastro aproxima -en el aspecto formal- la obra de Chillida a la arquitectura. Los títulos de numerosas obras hacen referencia a ella o a conceptos con ella relacionados. Elogio de la arquitectura, Homenaje a la arquitectura, Arquitectura heterodoxa, Modulación del espacio, construcción heterodoxa, Alrededor del vacío, Mesa del arquitecto o Casa de luz, son algunos de ellos. La introducción del vacío en el alabastro da comienzo a un proceso tendente a que el espacio interior tenga una importancia inversamente proporcional a su presencia en la forma exterior. Un proceso de progresivo hermetismo donde pequeños espacios interiores son expresados mediante grandes masas envolventes. El espacio interior es el principal motivo por el que vemos la obra de Eduardo Chillida como arquitectura. La condición de interior, apreciable igualmente en sus grandes obras en el espacio público, hace que estas no constituyan únicamente hitos visuales sino espacios de protección con los que cuerpo interactúa estableciendo una nueva relación con el paisaje, el horizonte o el cosmos. La búsqueda de un interior vacío tiene como consecuencia la evolución hacia la desaparición de la forma exterior. Tal evolución comienza con el diálogo entre el bolo natural de alabastro y el vacío tallado de Homenaje a Goethe, y, como muestra de la inter-escalabilidad de la obra de Chillida, concluye con la introducción de un vacío oculto en la montaña sagrada de Tindaya. El gran vacío de Tindaya nos hace mirar la obra de pequeño formato a través de su filtro de aumento. Nos permite entender que el límite entre arquitectura y escultura es difuso en la obra del escultor vasco. Que la arquitectura puede estar en el origen de su escultura. Que su escultura puede ser el germen de muchas arquitecturas. ABSTRACT It is well known that after leaving his architectural studies Chillida went to Paris in order to begin his career as a sculptor. Back again to the Basque Country, iron is the material in which he finds his own way. In terms of form, his work from the very first ten years is far away from architecture. However, the strength lines set by the iron show a spatial will that is clearly evident in a 1953 piece called Advice to space I. From there on, his work focuses on void. Different materials will set different forms but the purpose will remain the same. In his drawings, hands are expressing, beyond its figurative condition, the search of the concave space that fingers are enclosing. The space founded in the palm of the hand is equivalent to the one built with giant wood or concrete fingers. Chillida faces his work with a look where the idea of scale takes distance to the concept of dimension. His works gets then a possibility to grow that allow us to imagine his spaces as architecture. Following iron, wood and alabaster pieces, in the formal aspect, approaches Chillida´s work to architecture. The titles of many sculptures are referred to it or to the concept related to it. In praise of architecture, Homage to architecture, Heterodox architecture, Modulation of space, Heterodox construction, Around the void, Architect’s table, or House of light, are some of them. The introduction of void in alabaster begins a process leading to the interior space has a presence inversely proportional to its importance in the external form. A process of progressive secrecy where small interior spaces are expressed through large enveloping masses. The interior space is the main reason why we see the work of Eduardo Chillida as architecture. The condition of inner space, equally noticeable in his great works in public space, makes this not only constitute visual landmarks, but protection spaces that body interacts with establishing a new relationship with the landscape, the horizon or the cosmos. The search of an inner void leads to an evolution towards the disappearance of the external form. The evolution begins in the dialogue between the natural bolus of alabaster and the carved void of Homage to Goethe, and as a sign of inter-scalability of the work of Chillida, it concludes with the introduction of a hidden void in the sacred mountain of Tindaya. The great void of Tindaya makes us look at a small format work trough the filter of his increase filter. It allows us to understand that the boundary between architecture and sculpture is diffuse in the work of the Basque sculptor. That architecture can be at the origin of his sculpture. That his sculpture may be the seed of many architectures.

Sola romani: morteros hidráulicos romanos en la Península Ibérica

En esta investigación se han analizado morteros de cal de cronología romana en el interior de la Península Ibérica. Para ello, se seleccionó una serie de muestras procedentes de diversos yacimientos, y de estructuras de carácter industrial. Estas muestras presentan aditivos cerámicos y conglomerantes de cal, como característica principal. Desde un principio el esfuerzo debía de centrarse en los fragmentos cerámicos presentes en los morteros. Para ello se documentaron varios morteros con aditivos cerámicos, a fin de conocer sus características básicas (componentes, distribución, micro-estratigrafía, granulometría, etc.). Por ello, y una vez tomadas las muestras, ésta fueron tratadas y procesadas para desarrollar una primera fase de estudio por medio de macroscopía. Se obtuvieron buenos resultados en cuanto a la caracterización visual de los morteros, localizando y documentando los fragmentos cerámicos. Durante la observación de dichos aditivos se observó que los fragmentos cerámicos tenían unas coronas o anillos de coloración que recorrían el borde, justo al contacto con la matriz de cal. Fueron seleccionados algunos fragmentos en los que eran más visibles dichos anillos. A fin de conocer la posible relación entre algunos yacimientos cercanos y la presencia de dicho anillo cromáticos se desarrolló una microscopía óptica polarizada, realizando láminas delgadas de las muestras y sobre los fragmentos cerámicos más determinantes, en concreto de una serie de enclaves del valle del Henares. Además de caracterizar microscópicamente los morteros, se observó que los anillos no eran un defecto visual ni una alteración física, producida tal vez por la extracción, la fase del corte o por la cocción de la cerámica. Tras analizar varios ejemplares se pudo apreciar que esos anillos eran habituales en todas las muestras y que se presentaban de diferente manera, es decir, que se observaban en granos cerámicos de diferentes características físicas (cochura, tamaño, situación con respecto del conglomerante, etc.). A fin de conocer los aspectos químicos de dicha alteración se seleccionó un grupo de muestras en las que los resultados macroscópicos habían sido muy claros, y en las que la microscopía óptica polarizada había determinado en los bordes, áreas adecuadas para otros análisis. Se realizó un mapeado o mapping de elementos químicos, a fin de saber qué podía estar sucediendo en esa interfaz entre el fragmento cerámico y la matriz de cal. Gracias a los resultados obtenidos se comprobó que existía una acumulación potencial de calcio tanto en el interior de los granos cerámicos como en el exterior, justo en la zona de contacto con el conglomerante, formando manchas que recorrían longitudinalmente el borde. Estos datos fueron muy útiles para llevar a cabo la siguiente fase de estudio, que permitiría conocer puntualmente qué estaba sucediendo químicamente en esa zona de contacto. Finalmente y con el objetivo de describir química y puntualmente este efecto en las adiciones cerámicas, se volvió a seleccionar una serie de muestras, escogidas esta vez en función de los granos cerámicos que cumpliesen unas variables estadísticas. Se eligieron granos con distintos tipos de cocciones, así como granos con tamaños diversos y granos con aditivo ceniciento en la matriz de cal, pensando que podrían ser las variables más útiles de interpretar de existir algún tipo de cambio químico entre la arcilla cocida y la matriz de cal. Tales variables se adaptaron a un sistema estadístico multi-varial y geométrico, con el objetivo de sintetizar los resultados y visualizar de forma óptima los datos en conjunto, como se ha comentado en varias ocasiones en este trabajo. Una vez seleccionados los granos por variables se procedió a realizar un análisis lineal y espectral semi-cuantitativo de SEM-EDX, con el que se caracterizaba químicamente una sección lineal del grano, desde la matriz de arcilla cocida de la cerámica hasta la matriz de cal –del interior al exterior del grano- pasando por el centro de la banda de reacción. Este análisis permitió determinar que se había producido una serie de cambios químicos porcentuales en los granos de cerámica. Dichos cambios se resumen en un incremento global de los porcentajes de calcio en el interior de las bandas de reacción de la cerámica, desde el borde mismo del anillo hasta el exterior. Así también se observaron picos porcentuales en el interfaz del fragmento cerámico con la matriz de cal, lo que confirmaba los resultados obtenidos por medio del mapping. Globalmente en todas las muestras se apreció un hombro en las gráficas de calcio a su paso por la zona de afección del anillo de reacción. Los restantes porcentajes de magnesio, silicio y aluminio se mantienen normales. En esta tesis se ha confirmado que dicho incremento global de calcio se acentúa en las muestras en donde no hay cenizas en la matriz de cal. Los casos correspondientes a estos granos sufren un incremento mayor que en el resto. La segunda variable que sufre un mayor incremento de calcio es la que corresponde a granos con buena cocción de la arcilla. Por lo tanto, parece que la tercera variable, la que corresponde con el tamaño del fragmento cerámico, no es decisiva. Por lo tanto, teniendo en cuenta la prueba visual de los anillos de reacción, y atendiendo a los resultados químicos, podríamos pensar que ese incremento de calcio en la banda de reacción de los fragmentos cerámicos se debió a una absorción de calcio en el interior de la arcilla cocida en la fase inmediatamente previa al fraguado, incluso durante el apagado de la cal. Es en este punto donde estaría la clave del cambio químico que se produce en esta interfaz, el calcio sílice-aluminato del que algunos autores ya han investigado. Esta absorción de calcio en el interior del grano no vendría sola, sino que generaría una costra de cal en el interfaz exterior de la cerámica, la cual ha sido observada químicamente por mapping y mineralógicamente por medio de microscopía óptica de polarización. La consecuencia de estos resultados es, primero, la mejora de nuestro conocimiento general acerca del factor hidráulico en los morteros. Asimismo se aprecia que la incorporación de materiales orgánicos como cenizas, puede alterar los porcentajes de calcio en el interior de los aditivos cerámicos, por lo que habría que sopesar, en trabajos futuros, si este tipo de material es adecuado o no en las mezclas destinadas a la restauración, así como seguir indagando en las propiedades de los morteros con la incorporación de aditivos orgánicos. Desde el punto de vista de la catalogación de los suelos industriales hidráulicos de época romana, además de mejorar la documentación incorporando micro-estratigrafías y granulometrías, la investigación de este material histórico constructivo mejora en cuanto a que se incorporan ensayos sencillos, que facilitan incluso la peritación de un estado de conservación por medio de una lupa binocular. Arqueológicamente hablando, es muy interesante correlacionar fábricas diferentes de estructuras situadas o bien en un mismo yacimiento, o bien en una misma área regional. Los estudios de caracterización y micro-estratigrafía no sólo aportan datos nuevos de cara a la restauración de morteros, sino que crean la posibilidad de generar patrones constructivos que sirvan de fósiles-guía para datar relativamente a unas estructuras o a otras. En lo referido a los resultados obtenidos en los diferentes complejos arqueológicos se ha observado una diferencia entre los morteros destinados a piletas y cubetas con respecto a los suelos industriales de uso indeterminado. La muestra correspondiente al yacimiento de Las Arenas no dispone de ninguna micro-estratigrafía, como sí por el contrario en las muestras obtenidas en Rotonda de Mejorada, Val de la Viña y La Magdalena. En estos enclaves las estructuras presentan grandes similitudes, con diferentes niveles constructivos empleando morteros de cal con áridos y gravas en las capas interiores, y áridos con adiciones cerámicas en las exteriores. En lo relativo a la granulometría las adiciones cerámicas de las muestras de Val de la Viña y La Magdalena presentan varias coincidencias en cuanto al tamaño de los granos y la distribución. Asimismo, de las muestras tomadas en La Magdalena, existe una gran diferencia entre las muestras MG1, MG2, MG3 y MG4 con respecto a las muestras MG5 y MG6, correspondientes éstas últimas a un mortero con fragmentos cerámicos de gran tamaño. Las estructuras EMG1 y EMG2, correspondientes a una cubeta y una pileta de La Magdalena, guardan similitud en lo referido a la micro-estratigrafía y a la granulometría. Se ha determinado que su función, así como su fabricación, debieron estar vinculadas a un mismo contexto cronocultural. Química y mineralógicamente, las muestras presentan características iguales, con presencia de un conglomerante de cal con áridos y aditivos cerámicos de diferentes cochuras. Destaca la muestra de Las Arenas, con un tamaño de los fragmentos cerámicos muy superior al resto, seguido de la estructura EMG3 de La Magdalena. Las muestras restantes de éste enclave, junto con las muestras recogidas en Val de la Viña y Rotonda de Mejorada presentan condiciones similares. En conclusión, los datos revelan que existían diferentes fábricas destinadas a distintas finalidades, y que las estructuras industriales empleaban aditivos cerámicos para la manipulación de productos con líquidos, de distintas densidades pero que requerían de cierto grado de hidraulicidad. ABSTRACT Lime Roman mortars from the Iberian Peninsula has been analyzed in this reesearch. A group of samples were selected from some sites and all the samples come from industrial structures. All this samples show ceramic additives. From the start, the effort was centered in the pieces of pottery that were found in the mortars. The samples were treated and processed to develop a first phase of the research using macroscopy. With this technique, great results were achieved in the characterization of mortars, the microstratigraphy and the location of the ceramic pieces. While observing these pieces, it was seen that the fragments of pottery had a ring bordering the piece. The pieces with the bigger and more vivid rings were chosen and they were analyzed by a polarized light microscope. The mortars were characterized microscopically and it also showed that the rings were not a physical alteration or a visual defect. After some more tests, the rings were a chemical change associated with the hydraulicity of the mortar. The best samples were selected and mappings of their chemical elements were performed in order to know what could be happening in the interface between the ceramic matrix fragment and lime. With the results obtained it was found that there was a potential; both calcium accumulation within the ceramic grains and outside, just in the area of contact with the binder, forming spots longitudinally along the edge. These data were very useful for carrying out the next phase of study, which would meet promptly what was happening chemically in the area of contact. Another group of samples were taken, and this time focused on ceramic grains that met a statistical variables. Grains were chosen with two types of cooking as well as grains with different sizes and grains with ash additive in the matrix of lime, thinking that might be the most logical to be some sort of chemical change between the baked clay and lime array variables . Such variables were adapted to a multi-varial and geometric statistical system in order to synthesize the results and optimally display the data together, as mentioned several times in this work. After selecting the variables grains proceeded to perform a linear and spectral analysis SEM-EDX. This analysis led to determine that the chemical changes were graduals. These changes are summarized in an increase in the percentages of calcium inside the reaction rim of ceramics, from the edge to the outer ring. So percentage increasing is also observed at the interface of the ceramic matrix fragment with lime, confirming the results obtained by the mapping. Overall in all samples can be seen a shoulder in graphic calcium through the area of the ring reaction condition. The remaining percentages of magnesium, silicon and aluminum are usual. We have promptly confirmed that the increase of calcium is accentuated in samples where there is no ash and lime matrix. Cases for these grains suffer a greater increase than the rest. The second variable suffering more calcium is increased corresponding to good cooking grains with clay. Therefore, it appears that the variable size of the fragment is not critical. Therefore, considering the visual tests to the rings and their response to chemical results, we might think that increasing calcium inside the ceramic fragments was due to an injection of calcium inside clay in the run-up to the setting phase. It is at this point that would be the key to the chemical change that occurs at this interface, silica-calcium aluminate some authors have already investigated. This injection of calcium into the grain does not come alone, but generate a lime crust on the outside interface of ceramics, which we tested for mapping is real in our samples. The consequence of these results is the improvement of our understanding of historical hydraulic factor in building materials, such as mortar. For example, knowing that the incorporation of organic materials such as ash powder, may be detrimental to the injection of calcium inside the ceramic additives. Archaeologically speaking, it's very interesting to correlate different factories or structures located on a single site, or in the same regional area. Characterization studies and microstratigraphy not only provide new information to help restore mortars, but create the possibility of generating constructive patterns that serve as guide fossils to determinate the age of the structures. With regard to the results obtained in different archaeological sites it has seen a difference between mortars of pools or sinks with respect to industrial floors of undetermined use. The sample of the site of Las Arenas does not have any micro-stratigraphy, as if instead in the samples obtained in Rotonda de Mejorada, Val de la Viña and La Magdalena sites. In these settlements the structures are really similar, with different construction levels using lime mortars with aggregates and gravel in the inner layers, and ceramic aggregates as external additions. With regard to the grain size of the ceramic additions Val de la Viña and La Magdalena samples has several coincidences about the size of grains and distribution. Also, samples taken at La Magdalena, there is a difference between the MG1, MG2, MG3 and MG4 samples and the MG5 and MG6 samples, so the last corresponding to a mortar samples with larger ceramic fragments. The EMG1 and EMG2 structures, corresponding to a bucket and a pool of La Magdalena settlement, have similarities with regard to micro-stratigraphy and grain size. It has been determined that the function and manufacturing must be linked with a same chronocultural context.

Influence of allelic prolamin variation and localities on durum wheat quality

Thirty-seven varieties of a Mediterranean durum wheat collection grown in Tunisia and Spain were analysed for their allelic composition in prolamins, as well as their protein concentration, sodium dodecyl sulphate sedimentation (SDSS) test and mixograph parameters. Genotype was a greater source of variation in all measurements than locality. Uncommon high and low molecular glutenin subunits (HMW-GS and LMW-GS) were found (V and 2? subunits at Glu-A1, 13 þ 16 at Glu-B1, 5* subunit and ax allele at Glu-A3). The rare combinations 2 þ 4þ14 þ 18 and 8 þ 9þ13 þ 16þ18 subunits at the Glu-B3 locus were found. Glu-A3ax had a positive influence on SDSS and mixograph parameters. Of all the prolamins, those that have the B-LMW-GS composition aaa (for Glu-A3, Glu-B3 and Glu-B2 loci, respectively), when associated with the Glu-A1c and Glu-B1d gave the best semolina quality. By contrast, semolina quality is poor when this same composition is associated with the Glu-A1c and Glu-B1e and even poorer when associated with the Glu-A1c and Glu-B1f. In addition, the cultivars with B-LMW-GS allelic composition aab (for Glu-A3, Glu-B3 and Glu-B2 loci, respectively), when associated with the Glu- A1c and Glu-B1d, gave high quality, whereas when associated with the Glu-A1c and Glu-B1e or with Glu- A1o and Glu-B1f, the quality was very poor.

mRNA binding protein mrnp 41 localizes to both nucleus and cytoplasm

We have identified and molecularly characterized a human protein with a Mr of 40,880 Da. After UV irradiation of HeLa cells, this protein was cross-linked to poly(A)-containing mRNA and was therefore designated mrnp 41 (for mRNA binding protein of 41 kDa). Cell fractionation and immunoblotting showed mrnp 41 in both the cytoplasm and the nucleus and particularly in the nuclear envelope. Immunofluorescence microscopy localized mrnp 41 to distinct foci in the nucleoplasm, to the nuclear rim, and to meshwork-like structures throughout the cytoplasm. The cytoplasmic meshwork staining was disrupted by prior treatment of cells with the actin filament- or microtubule-disrupting drugs cytochalasin or nocodazole, respectively, suggesting association of mrnp 41 with the cytoskeleton. Double immunofluorescence with antibodies against mrnp 41 and the cytoplasmic poly(A) binding protein showed colocalization to the cytoplasmic meshwork. Immunogold electronmicroscopy confirmed mrnp 41’s cytoplasmic and nucleoplasmic localization and revealed a striking labeling of nuclear pore complexes. Together these data suggest that mrnp 41 may function in nuclear export of mRNPs and/or in cytoplasmic transport on, or attachment to, the cytoskeleton. Consistent with a role of mrnp 41 in nuclear export are previous reports that mutations in homologs of mrnp 41 in Schizosaccharomyces pombe, designated Rae1p, or in Saccharomyces cerevisiae, designated Gle2p, result in mRNA accumulation in the nucleus although it is presently not known whether these homologs are mRNA binding proteins as well.