233 resultados para Manchas


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Contiene: Dia 23 de Octubre : octava de la Bienaventurada Vi[rge]n M[arí]a de aguas-vi[va]s / S[alvad]or Tudela Vallo

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Alcance y contenido: Ms. autógrafo firmado conteniendo las notas para el sermón en honor de las reliquias de san Bonifacio.

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Alcance y contenido: Ms. poético-jocoso dedicado al padre Puchol, por las discrepancias que tenía con su orden

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Contiene: Tabla o índice del contenido de un libro ya desaparecido(h. 1 r). -- Noticia sobre un terremoto acaecido en Valencia el día 15 de noviembre de 1775(h. 1 v - h. 2 r). -- Misas y demás oficios que se han de rezar durante el "Trentenario" de San Vicente Ferrer (h. 2-4)

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Tít. facticio sacado del principio del ms.

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Contiene: Dezimas que amanecio en Cadiz enla Lonja del Comercio (h. 2)

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Alcance y contenido: Copia ms. del documento que se posiblemente se envío al Congreso Nacional. Los nombres de los valencianos ilustres son: D. Joaquín Lorenzo Villanueva y Astengo, D. Mariano Liñán, D. Vicente Sancho, D. Francisco Ciscar, D. José Rovira, D. Simón de Roxas, D. Antonio Bernabeu, D. Felipe Benicio Navarro, D. Vicente Tomás Traver, D. Antonio Verdú, D. Nicolás Gareli y D. Gregorio Gisbert. Junto a los nombres, hay una breve nota biográfica y los atributos que acompañarán a las estatuas, todos relacionados con las profesiones de todos ellos.

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Aunque las primeras fábricas de tubos de poliéster reforzado con fibra de vidrio en España datan del año 1984, no es sino hasta el año 1996 cuando se comienza su utilización masiva como un sustituto de las tuberías de fribrocemento, que ya habían sido prohibidas por la legislación, debido a los efectos cancerígenos de este material. Desde entonces se ha prodigado la utilización de todas las diferentes tipologías de esta clase de tubería, de conformidad a los procesos de fabricación empleados que se encuentran recopilados en el AWWA Manual M45 (Fiberglass Pipe Design), obteniéndose muy diversos resultados. Durante estos años, ha surgido una creciente preocupación en los usuarios de este tipo de tuberías dadas las continuas y numerosas averías en todo el ámbito geográfico. Esto ha promovido el desarrollo de la presente investigaicón, que se ha dividido en dos partes y que ha concluido con la determinación de un nuevo mecanismo específico de fractura. La primera parte se centró en la obtención y desarrollo del modelo teórico que hemos venido a denominar como "Teoría de la Caja Mecánicamente Contaminada", y que está basado en la contaminación o separación por un impacto de dos de las tres capas que forman la tubería, la capa intermedia de arena y la capa más interna o "inner layer". La consecuencia es la disminución del canto resistente, la rotura del inner layer y la entrada de fluido a la capa de arena. Para la evaluación de la magnitud de esta separación se ha desarrollado un modelo analítico que ha determinado la existencia de una relación cuadrática que la rige, y que ha sido verificado mediante ensayos de impacto sobre probetas de tuberías, alcanzando ajustes de hasta el 92%. Así, se ha determinado que impactos de muy baja intensidad, del entorno de 90 a 160 Julios en tuberías Filament Winding continuo PN 16-20 (de 800 a 1000mm) pueden comprometer seriamente la integridad estructural de la tubería sin dejar, en un principio, muesca o traza alguna que pueda alertar del problema. Los siguientes pasos en el estudio se dirigieron a determinar qué otros mecanismos, aparte del golpe, podrían contaminar la tubería y a estudiar el consiguiente avance de la fractura a las capas externas. Se trataba además de analizar la aparición en el tubo de unas misteriosas manchas en forma de "piel de leopardo" y de otros fenómenos aparecidos en las averías como que algunas de las deformaciones de la rotura por presión interna son hacia el interior del tubo y no al revés, como habría sido de esperar a priori. Se optó entonces por comenzar la que ha constituido la segunda parte de la investigación. Para ello se recurrió a realizar ensayos hidráulicos en banco de pruebas a alta presión, cuyos resultados fueron sorprendentes al descubrir que en el proceso se producía la hidrólisis de la resina de poliéster no catalizada que fluía hacia el exterior del tubo. Como consecuencia se llevaron a cabo nuevos ensayos físicos y químicos para estudiar la migración del material y la hidrólisis producida en el proceso de fractura. En este estudio, resultó muy relevante el hecho de sobrepasar o no la presión que producía el desagarro entre las capas del tubo. En definitiva, en esta investigación, que ha constado de estudios analíticos y estudios experimentales, químicos y numéricos, se ha determinado un nuevo mecanismo de fractura que explica gran parte de los fallos acontecidos en las tuberías de poliéster reforzado con fibra de vidrio. Como aplicación se exponen recomendaciones para mejorar el comportamiento mecánico de esta tipología y evitar así los sobrecostes millonarios producidos por su reposición. Numerous and continuous failures in fiberglass reinforced polyester pipes of different companies and manufacturing processes of the AWWA Manual M45 (Fiberglass Pipe Design), have prompted the development of this research, that has concluded with a specific mechanism describing pipe fractures. This research was carried out via two independent studies. The first one is the development of the hypothesis that turned into the Mechanically Contaminated Layer Theory. This theory describes the fracture mchanism which explains a significant part of massive failures due to the existence of a sand layer placed near the neutral axis in the core making the composite very sensitive to impacts in fibreglass reinforced polyester pipes. These failures create interface delamination and consequently fluid can leak into supporting sand backfill thereby iniating the fracture process. In order to assess the delimination magnitude, an analytic method is developed and a squared root law between delamination and energy applied proposed. Vertical blunt ram testts on samples extracted from complete pipes have been carried out to verify this theory, reaching a goodness of fit up to 92%. It is concluded that low energy impacts, around 90-160J in 800-1000mm diameter PN 16-20 continuous filament winding pipes, can seriously compromise their structural integraty with no external trace. The next step in the study was to determine what other mechanism, apart from the brittle hit, could contaminate the pipe and to analyse the consequente advance of the fracture to the external layers. Another aim was to analyse two phenomena occurred in real pipe failures. The first one is the appearance on the tube of "leopard fur" stains on some of the analysed failures, and the other phenomenon is the "inverse fracture", in which the deformations of the failure due to internal pressure are towards the inside of the tube and not the other way round, as it would be expected. It was then chosen to follow a new branch of the investigation by hydraulic high-pressure bench tests that study seepage and load transmission. The results were very surprising as it was discovered that in the process, hydrolysis of the non-catalysed polyester resin occured, flowing towards the outer of the pipe, which entailed the development of chemical and physical tests of the exuded material to study material migration and hydrolysis of the fracture process. In this particular study it was relevant to exceed or not the pressure that produced the rip between the layers of the tube. In conclusion, a new breakage mechanism in FRP pies with sand-filled layer has been found, which explains a high part of the failure global cases. The whole failure process is justified by the Mechanically Contaminated Layer Theory, which has been corroborated by means of analytical, numerical and experimental studies. Several recommendations are also provided in order to improve the mechanical behaviour of this typology and avoid the millionaire overruns generated by its massive failures.

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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.

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The Amazon savannas occur as isolated patches throughout extensive areas of forest in the states of Amapá, Amazonas, Pará, and Roraima. There is a considerable variation in the composition of anuran assemblages in the localities and phytophysiognomies of Amazon savannas and given the absence of studies on reproductive behavior, a systematic and geographically wide sampling has been carried out in the Amapá savanna, located in the Eastern Amazon. The study was conducted in a savanna area in the state of Amapá to examine the composition, ecology, and reproductive behavior of anuran amphibians. We carried out 24 field trips in each phytophysiognomy (gramineous-woody savana, gramineous-herbaceous-woody savana, park savana, and arboreal savanna); for analysis of reproductive behavior observations were made during the period January to December 2013, lasting four consecutive days. Samples were collected by active and acoustic search along 20 plots of 100x50 meters. Twenty-one anuran species were recorded, of which four are new records for the state of Amapá: Dendropsophus walfordi, Scinax fuscomarginatus, Pseudopaludicola boliviana e Elachistocleis helianneae. The KruskalWallis ANOVA revealed significant differences between richness and species diversity in the phytophysiognomies (p < 0.05). The Bray-Curtis similarity coefficient divided the phytophysiognomies into three groups: arboreal savana, gramineous-woody savanna and gramineous-herbaceous-woody savanna, and park savanna. According to the non-metric multidimensional scaling, the structure of the anuran community resulted in a separation into three phytophysiognomies, with significant differences in the structure of communities (ANOSIM, R = 0.823; p < 0.001). In the study of community ecology, the results obtained for spatial, temporal, and trophic niche breadth suggest that the assemblage of anurans of the Amapá savanna is not composed of predominantly generalist species. Also, the presence of other specialist anurans may explain the processes of speciation associated with the isolation of habitats, resulting in heterogeneity and spatial discontinuity in the phytophysiognomies with open formations. The null model analysis revealed that the community is structured based on temporal and trophic niche, indicating a significant influence of contemporary ecological factors on the assemblage. The absence of structure based on spatial niche might be explained by the spatial segregation in the distribution and occupation of anurans in the different phytophysiognomies of the Amapá savanna. Regarding the reproductive behavior of anurans, 11 species were classified as having a long breeding season, intrinsically associated with the rainy season and the reproductive mode of most species that lay egg clutches in lentic water bodies. Six reproductive modes were recorded and parental care was observed in Leptodactylus macrosternum and L. podicipinus, whose reproductive mode is characterized by foam nests. Regarding behavioral reproductive strategies, calling males were observed in all species of anurans, satellite males were recorded only for D. walfordi, Hypsiboas multifasciatus, S. nebulosus and S. fuscomarginatus; active search for females was observed for Phyllomedusa hypochondrialis and L. fuscus, and male displacement was recorded only for Rhinella major and R. margaritifera. Of the reproductive behaviors observed, throat and vocal sac display is associated with courtship and territorial behavior exhibited by males. In addition to courtship behavior, visual signals associated with courtship strategies were recorded for the anurans of the Amapá savanna.

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Solar activity indicators, each as sunspot numbers, sunspot area and flares, over the Sun’s photosphere are not considered to be symmetric between the northern and southern hemispheres of the Sun. This behavior is also known as the North-South Asymmetry of the different solar indices. Among the different conclusions obtained by several authors, we can point that the N-S asymmetry is a real and systematic phenomenon and is not due to random variability. In the present work, the probability distributions from the Marshall Space Flight Centre (MSFC) database are investigated using a statistical tool arises from well-known Non-Extensive Statistical Mechanics proposed by C. Tsallis in 1988. We present our results and discuss their physical implications with the help of theoretical model and observations. We obtained that there is a strong dependence between the nonextensive entropic parameter q and long-term solar variability presents in the sunspot area data. Among the most important results, we highlight that the asymmetry index q reveals the dominance of the North against the South. This behavior has been discussed and confirmed by several authors, but in no time they have given such behavior to a statistical model property. Thus, we conclude that this parameter can be considered as an effective measure for diagnosing long-term variations of solar dynamo. Finally, our dissertation opens a new approach for investigating time series in astrophysics from the perspective of non-extensivity.

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Paisagens naturais tem sido afetadas dramaticamente pela perda de habitat e fragmentação, os quais transformam paisagens contínuas em manchas de habitat circundadas por áreas de não-habitat (matrizes). Essas matrizes, inóspitas ou não, afetam incontáveis processos ecológicos, como a dispersão. Uma das formas de compreender o efeito da matriz no processo de dispersão é estudando o alcance da percepção do habitat dos animais, o qual é definido como o alcance (distância) em que um animal pode perceber elementos da paisagem. Essa percepção está diretamente relacionada ao sucesso de chegada à um novo habitat, enquanto o animal navega por uma matriz. Nós avaliamos a percepção do habitat em Heliconius erato, uma borboleta tropical. Entretanto nós também estávamos interessados em avaliar o efeito da idade das borboletas e do tipo de matriz na percepção do habitat. Consequentemente, nós criamos borboletas em laboratório e pareamos com borboletas coletadas na floresta durante um experimento de soltura. Para determinar o alcance da percepção, nós realizamos solturas em duas diferentes matrizes (coqueiral e campo em regeneração) à três distâncias da floresta (0,30 e 100 metros) e medimos o ângulo final alcançado pelas borboletas. Nós encontramos que (I) borboletas soltas na borda se orientaram fortemente para a floresta; (II) quanto maior a distância de soltura, menor a habilidade de perceber o habitat e (III) há interação entre matriz e idade da borboleta. Borboletas inexperientes se orientaram melhor no campo aberto (alcance da percepção: 30-100 metros) e experientes se orientaram melhor no coqueiral (alcance da percepção entre 30-100 metros).

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In the primary visual cortex, neurons with similar physiological features are clustered together in columns extending through all six cortical layers. These columns form modular orientation preference maps. Long-range lateral fibers are associated to the structure of orientation maps since they do not connect columns randomly; they rather cluster in regular intervals and interconnect predominantly columns of neurons responding to similar stimulus features. Single orientation preference maps – the joint activation of domains preferring the same orientation - were observed to emerge spontaneously and it was speculated whether this structured ongoing activation could be caused by the underlying patchy lateral connectivity. Since long-range lateral connections share many features, i.e. clustering, orientation selectivity, with visual inter-hemispheric connections (VIC) through the corpus callosum we used the latter as a model for long-range lateral connectivity. In order to address the question of how the lateral connectivity contributes to spontaneously generated maps of one hemisphere we investigated how these maps react to the deactivation of VICs originating from the contralateral hemisphere. To this end, we performed experiments in eight adult cats. We recorded voltage-sensitive dye (VSD) imaging and electrophysiological spiking activity in one brain hemisphere while reversible deactivating the other hemisphere with a cooling technique. In order to compare ongoing activity with evoked activity patterns we first presented oriented gratings as visual stimuli. Gratings had 8 different orientations distributed equally between 0º and 180º. VSD imaged frames obtained during ongoing activity conditions were then compared to the averaged evoked single orientation maps in three different states: baseline, cooling and recovery. Kohonen self-organizing maps were also used as a means of analysis without prior assumption (like the averaged single condition maps) on ongoing activity. We also evaluated if cooling had a differential effect on evoked and ongoing spiking activity of single units. We found that deactivating VICs caused no spatial disruption on the structure of either evoked or ongoing activity maps. The frequency with which a cardinally preferring (0º or 90º) map would emerge, however, decreased significantly for ongoing but not for evoked activity. The same result was found by training self-organizing maps with recorded data as input. Spiking activity of cardinally preferring units also decreased significantly for ongoing when compared to evoked activity. Based on our results we came to the following conclusions: 1) VICs are not a determinant factor of ongoing map structure. Maps continued to be spontaneously generated with the same quality, probably by a combination of ongoing activity from local recurrent connections, thalamocortical loop and feedback connections. 2) VICs account for a cardinal bias in the temporal sequence of ongoing activity patterns, i.e. deactivating VIC decreases the probability of cardinal maps to emerge spontaneously. 3) Inter- and intrahemispheric long-range connections might serve as a grid preparing primary visual cortex for likely junctions in a larger visual environment encompassing the two hemifields.

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In the primary visual cortex, neurons with similar physiological features are clustered together in columns extending through all six cortical layers. These columns form modular orientation preference maps. Long-range lateral fibers are associated to the structure of orientation maps since they do not connect columns randomly; they rather cluster in regular intervals and interconnect predominantly columns of neurons responding to similar stimulus features. Single orientation preference maps – the joint activation of domains preferring the same orientation - were observed to emerge spontaneously and it was speculated whether this structured ongoing activation could be caused by the underlying patchy lateral connectivity. Since long-range lateral connections share many features, i.e. clustering, orientation selectivity, with visual inter-hemispheric connections (VIC) through the corpus callosum we used the latter as a model for long-range lateral connectivity. In order to address the question of how the lateral connectivity contributes to spontaneously generated maps of one hemisphere we investigated how these maps react to the deactivation of VICs originating from the contralateral hemisphere. To this end, we performed experiments in eight adult cats. We recorded voltage-sensitive dye (VSD) imaging and electrophysiological spiking activity in one brain hemisphere while reversible deactivating the other hemisphere with a cooling technique. In order to compare ongoing activity with evoked activity patterns we first presented oriented gratings as visual stimuli. Gratings had 8 different orientations distributed equally between 0º and 180º. VSD imaged frames obtained during ongoing activity conditions were then compared to the averaged evoked single orientation maps in three different states: baseline, cooling and recovery. Kohonen self-organizing maps were also used as a means of analysis without prior assumption (like the averaged single condition maps) on ongoing activity. We also evaluated if cooling had a differential effect on evoked and ongoing spiking activity of single units. We found that deactivating VICs caused no spatial disruption on the structure of either evoked or ongoing activity maps. The frequency with which a cardinally preferring (0º or 90º) map would emerge, however, decreased significantly for ongoing but not for evoked activity. The same result was found by training self-organizing maps with recorded data as input. Spiking activity of cardinally preferring units also decreased significantly for ongoing when compared to evoked activity. Based on our results we came to the following conclusions: 1) VICs are not a determinant factor of ongoing map structure. Maps continued to be spontaneously generated with the same quality, probably by a combination of ongoing activity from local recurrent connections, thalamocortical loop and feedback connections. 2) VICs account for a cardinal bias in the temporal sequence of ongoing activity patterns, i.e. deactivating VIC decreases the probability of cardinal maps to emerge spontaneously. 3) Inter- and intrahemispheric long-range connections might serve as a grid preparing primary visual cortex for likely junctions in a larger visual environment encompassing the two hemifields.