A Dynamic Route Planning Prototype for Cognitive Cities

A software prototype for dynamic route planning in the travel industry for cognitive cities is presented in this paper. In contrast to existing tools, the prototype enhances the travel experience (i.e., sightseeing) by allowing additional flexibility to the user. The theoretical background of the paper strengthens the understanding of the introduced concepts (e.g., cognitive cities, fuzzy logic, graph databases) to comprehend the presented prototype. The prototype applies an instantiation and enhancement of the graph database Neo4j . For didactical reasons and to strengthen the understanding of this prototype a scenario, applied to route planning in the city of Bern (Switzerland) is shown in the paper.

New algorithms for automated phylogenetic reconstruction using artificial intelligence and data mining techniques

Academic and industrial research in the late 90s have brought about an exponential explosion of DNA sequence data. Automated expert systems are being created to help biologists to extract patterns, trends and links from this ever-deepening ocean of information. Two such systems aimed on retrieving and subsequently utilizing phylogenetically relevant information have been developed in this dissertation, the major objective of which was to automate the often difficult and confusing phylogenetic reconstruction process. ^ Popular phylogenetic reconstruction methods, such as distance-based methods, attempt to find an optimal tree topology (that reflects the relationships among related sequences and their evolutionary history) by searching through the topology space. Various compromises between the fast (but incomplete) and exhaustive (but computationally prohibitive) search heuristics have been suggested. An intelligent compromise algorithm that relies on a flexible “beam” search principle from the Artificial Intelligence domain and uses the pre-computed local topology reliability information to adjust the beam search space continuously is described in the second chapter of this dissertation. ^ However, sometimes even a (virtually) complete distance-based method is inferior to the significantly more elaborate (and computationally expensive) maximum likelihood (ML) method. In fact, depending on the nature of the sequence data in question either method might prove to be superior. Therefore, it is difficult (even for an expert) to tell a priori which phylogenetic reconstruction method—distance-based, ML or maybe maximum parsimony (MP)—should be chosen for any particular data set. ^ A number of factors, often hidden, influence the performance of a method. For example, it is generally understood that for a phylogenetically “difficult” data set more sophisticated methods (e.g., ML) tend to be more effective and thus should be chosen. However, it is the interplay of many factors that one needs to consider in order to avoid choosing an inferior method (potentially a costly mistake, both in terms of computational expenses and in terms of reconstruction accuracy.) ^ Chapter III of this dissertation details a phylogenetic reconstruction expert system that selects a superior proper method automatically. It uses a classifier (a Decision Tree-inducing algorithm) to map a new data set to the proper phylogenetic reconstruction method. ^

Influencia del manejo del suelo y las coberturas vegetales en el microclima de la canopia de la vid, la composición de la uva y el vino

Para determinar la influencia del manejo del suelo sobre la composición de la uva y el vino se estableció un experimento en un viñedo de Cabernet Sauvignon conducido en doble cordón de pitones en espaldero alto. Se aplicaron tres tratamientos: TR-suelo sin maleza; CVP-cobertura de suelo espontánea y control del desarrollo vegetativo por desbrozado y CA-cobertura de flora espontánea y control del desarrollo vegetativo con aplicación de herbicida de contacto desecante. En la uva se determinó el contenido de azúcar, acidez total, pH y la composición fenólica (índice de polifenoles totales (IPT), grado de polimerización, flavonoles, flavan-3-oles, antocianos y proantocianidoles). Se elaboraron vinos que fueron evaluados físico-química y sensorialmente por jueces expertos. CVP tuvo el mayor contenido de antocianas y TR el de flavonoles, flavan-3-oles, proantocianidoles, IPT y grado de polimerización; CA presentó valores intermedios. Los vinos del tratamiento TR tuvieron mayor contenido de alcohol y menor de acidez total, con el color rojo (DO520) más bajo y una intensidad colorante más pequeña. Los vinos de CA y TR resultaron más amargos, más astringentes y más ásperos, y los de CVP tuvieron mayor carácter varietal. Resultó útil el empleo de coberturas de raíces superficiales y permanentemente desbrozadas para provocar cierta disminución en los valores de radiación reflejada y de la temperatura de la canopia. Las elevadas temperaturas y alta radiación solar son perjudiciales para la uva, porque aumentan la producción de quercetina y afectan el metabolismo y la degradación de antocianos.

Actores, argumentación y agenda en la gestión del territorio de la cuenca baja del río Luján

En el marco conceptual del análisis de políticas públicas, se identifican los actores del subsistema de gestión del suelo, sus lógicas, sus intereses y sus relaciones conflictivas en el proceso de transformación urbana y conformación del patrón de uso actual de la baja cuenca del río Lujan de los últimos diez años. Los discursos y argumentos de estos grupos de interés inciden en la formación de la agenda, entendida como proceso de agregación de intereses que refleja tanto el orden de prioridad de los problemas sociales como la visión que el gobierno tiene de la situación. El presente trabajo1 rastrea en las manifestaciones escritas y orales asociadas a los distintos actores del área de estudio, como factor que contribuye a explicar por qué ciertos temas se adoptan como problemas públicos y se incorporan a la agenda gubernamental.

Actores, argumentación y agenda en la gestión del territorio de la cuenca baja del río Luján

En el marco conceptual del análisis de políticas públicas, se identifican los actores del subsistema de gestión del suelo, sus lógicas, sus intereses y sus relaciones conflictivas en el proceso de transformación urbana y conformación del patrón de uso actual de la baja cuenca del río Lujan de los últimos diez años. Los discursos y argumentos de estos grupos de interés inciden en la formación de la agenda, entendida como proceso de agregación de intereses que refleja tanto el orden de prioridad de los problemas sociales como la visión que el gobierno tiene de la situación. El presente trabajo1 rastrea en las manifestaciones escritas y orales asociadas a los distintos actores del área de estudio, como factor que contribuye a explicar por qué ciertos temas se adoptan como problemas públicos y se incorporan a la agenda gubernamental.

Actores, argumentación y agenda en la gestión del territorio de la cuenca baja del río Luján

En el marco conceptual del análisis de políticas públicas, se identifican los actores del subsistema de gestión del suelo, sus lógicas, sus intereses y sus relaciones conflictivas en el proceso de transformación urbana y conformación del patrón de uso actual de la baja cuenca del río Lujan de los últimos diez años. Los discursos y argumentos de estos grupos de interés inciden en la formación de la agenda, entendida como proceso de agregación de intereses que refleja tanto el orden de prioridad de los problemas sociales como la visión que el gobierno tiene de la situación. El presente trabajo1 rastrea en las manifestaciones escritas y orales asociadas a los distintos actores del área de estudio, como factor que contribuye a explicar por qué ciertos temas se adoptan como problemas públicos y se incorporan a la agenda gubernamental.

Actores, argumentación y agenda en la gestión del territorio de la cuenca baja del río Luján

En el marco conceptual del análisis de políticas públicas, se identifican los actores del subsistema de gestión del suelo, sus lógicas, sus intereses y sus relaciones conflictivas en el proceso de transformación urbana y conformación del patrón de uso actual de la baja cuenca del río Lujan de los últimos diez años. Los discursos y argumentos de estos grupos de interés inciden en la formación de la agenda, entendida como proceso de agregación de intereses que refleja tanto el orden de prioridad de los problemas sociales como la visión que el gobierno tiene de la situación. El presente trabajo1 rastrea en las manifestaciones escritas y orales asociadas a los distintos actores del área de estudio, como factor que contribuye a explicar por qué ciertos temas se adoptan como problemas públicos y se incorporan a la agenda gubernamental.

Geochemistry of minerals at DSDP Hole 70-504B

Hole 504B, drilled into the 5.9 Ma crust of the southern flank of the Costa Rica Rift, tapped a hydrothermal system in its conductive stage. Three alteration zones were encountered along the 561.5 meters of basement drilled. The upper alteration zone, 274.5 to 584.5 meters below the seafloor (BSF), is characterized by the presence of color zonation in which red halos are located between dark gray inner rock portions and dark gray outer bands. The red halos are characterized by an abundance of iddingsite, and they have higher K2O contents and Fe3+/FeT ratios, but lower SiO2 contents, than the adjacent dark gray inner zones. The dark gray outer bands are characterized by the presence of celadonite-nontronite. Saponite is omnipresent in these three alteration bands. Phillipsite is the only zeolite that occurs in the upper alteration zone. The upper alteration zone is interpreted as being the result of low-temperature alteration, with large amounts of cold oxygenated seawater percolating through the upper ocean crust. In the upper alteration zone, the formation of red halos was both preceded and followed by formation of dark gray outer bands. Then followed formation of dark gray cores. The lower alteration zone (584.5-835.5 m BSF) is characterized by the absence of color zonation, the downward-increasing abundance of pyrite and saponite, and the presence of quartz, talc, and calcite. The chemical changes (downhole MgO enrichment and concomitant CaO depletion) observed in the basalts of the lower alteration zone are thought to result from reactions of oceanic basalts with evolved seawater (i.e., solutions derived from seawater that has already reacted with ocean crust), which is thus depleted in oxygen, potassium, and radiogenic strontium. This alteration process, which was responsible for saponite formation in both the upper and lower alteration zones, was rock dominated, and it took place under suboxic to anoxic conditions during a second stage of alteration. Reaction temperatures could have progressively increased with depth. There is also a zeolitic zone that essentially coincides with the lower part of the upper alteration zone (between 528.5 and 563 m BSF). The host rock adjacent to veins of zeolite exhibits a greenish discoloration due to the intensive replacement of the igneous minerals. The replacement minerals result in significant increases in the bulk rock K2O, MgO, CaO, CO2, and H2O+ contents. The solutions circulating along the newly opened fissures had high Ca activity, and minerals probably precipitated in these fissures at 60°C or 110°C. These hydrothermal solutions circulated later than those responsible for the formation of the minerals that characterize the upper and lower alteration zones.

Carbonate and terrigenous content and chemical composition of sediments in the Central Equatorial Pacific

This study addresses changes in the absolute magnitude and spatial geometry of particle flux and export production in a meridional transect across the central equatorial Pacific Ocean's upwelling system during oxygen isotope Stage 11 and Stage 12 and compares these time periods to the current Holocene interglacial system. Temporal and spatial variability in several chemical proxies of export production, and in particular the distributions of Ba, scavenged Al, and P, are studied in a suite of sediment cores gathered along a cross-equator transect at 5°S, 2°S, 0°, 2°N, and 4°N. Because this latitudinal range preserves strong gradients in biogenic particle flux in the modern equatorial Pacific Ocean, we are able to assess variations in the relative magnitude of export production as well as the meridional width of the equatorial system through the late Quaternary glacial/interglacial cycles. During interglacial oxygen isotope Stage 11 the chemical proxies each indicate lower particle flux and export production than during Stage 12. These records are consistent throughout the transect during this time period, but geographic narrowing (during the interglacial) and widening (during the glacial) of the meridional gradient also occurs. Although carbonate concentration varies dramatically through glacial/interglacial cycles at all latitudes studied, the productivity proxies record only minimal glacial/interglacial change at 5°S and 4°N, indicating that the carbonate minima at these latitudes is controlled dominantly by dissolution rather than production. The chemical data indicate that although the spatial geometry of the system during Stages 11 and 12 indicates maximum productivity at the equator during both glacial and interglacial conditions, the absolute magnitude of export production integrated from 5°S to 4°N during Stage 11 was 25-50% less than during Stage 12, and also was 25-50% less than it is now.

(Table 3) Leaf area and leaf nitrogen for deciduous, evergreen, forb and graminoid species at Barrow, Svalbard and Zackenberg

Arctic vegetation is characterized by high spatial variability in plant functional type (PFT) composition and gross primary productivity (P). Despite this variability, the two main drivers of P in sub-Arctic tundra are leaf area index (LT) and total foliar nitrogen (NT). LT and NT have been shown to be tightly coupled across PFTs in sub-Arctic tundra vegetation, which simplifies up-scaling by allowing quantification of the main drivers of P from remotely sensed LT. Our objective was to test the LT-NT relationship across multiple Arctic latitudes and to assess LT as a predictor of P for the pan-Arctic. Including PFT-specific parameters in models of LT-NT coupling provided only incremental improvements in model fit, but significant improvements were gained from including site-specific parameters. The degree of curvature in the LT-NT relationship, controlled by a fitted canopy nitrogen extinction co-efficient, was negatively related to average levels of diffuse radiation at a site. This is consistent with theoretical predictions of more uniform vertical canopy N distributions under diffuse light conditions. Higher latitude sites had higher average leaf N content by mass (NM), and we show for the first time that LT-NT coupling is achieved across latitudes via canopy-scale trade-offs between NM and leaf mass per unit leaf area (LM). Site-specific parameters provided small but significant improvements in models of P based on LT and moss cover. Our results suggest that differences in LT-NT coupling between sites could be used to improve pan-Arctic models of P and we provide unique evidence that prevailing radiation conditions can significantly affect N allocation over regional scales.

Geochemistry and ages of rock samples from Kirwanveggen, Antarctica

The basement of southern Kirwanveggen (western Dronning Maud Land) is formed by a SSW-dipping section consisting of (from SW to NE): migmatic gneisses; granitoid; low-grade/prograde meta-pelites, meta-psammites and meta-basalts (= "Polaris Formation"); ortho-gneiss; quartzite mylonite; Polaris Formation; quartzite mylonite; meta-turbidites. These units are (partly) separated by at least four SSW-dipping, NE to N directed major thrusts. Most probably, this thrust system is of Pan-African age. Towards north, the section is followed by the molasse-like Urfjell Group, deposited later than approx. 550 Ma and earlier than 450 Ma. Similarities with the Pan-African of the Shackleton Range (thrusting, molasse) led to the assumption, that the East/West Gondwana suture runs from the Shackleton Range towards Sor Rondane (eastern Dronning Maud Land) passing southern Kirwanveggen at its south-east.

New data on the specular reflectance of ores (VNIR: 400 - 1000 nm) and their significance for ore microscopy

This work is part of the project CAMEVA for the development of an expert system aimed at the automatic identification of ores [1, 2]. It relies on the measure of their reflectance values, R, on digital images. Software for calibration, acquisition and analysis of the multispectral data was designed by AITEMIN [3]; the research was also assessed by H.J. Bernhardt and E. Pirard [1].

Aplicación del análisis multi-espectral para el reconocimiento automatizado de menas metálicas

Traditional identification of ore minerals with reflected light microscopy relies heavily on the experience of the observer. Qualified observers have become a rarity, as ore microscopy is often neglected in today’s university training, but since it furnishes necessary and inexpensive information, innovative alternatives are needed, especially for quantification. Many of the diagnostic optical properties of ores defy quantification, but recent developments in electronics and optics allow new insights into the reflectance and colour properties of ores. Preliminary results for the development of an expert system aimed at the automatic identification of ores based on their reflectance properties are presented. The discriminatory capacity of the system is enhanced by near IR reflectance measures, while UV filters tested to date are unreliable. Interaction with image analysis software through a wholly automated microscope, to furnish quantitative and morphological information for geometallurgy, relies on automated identification of the ores based on the measured spectra. This methodology increases enormously the performance of the microscopist; nevertheless supervision by an expert is always needed.

Empowering and assisting natural human mobility: The simbiosis walker

This paper presents the complete development of the Simbiosis Smart Walker. The device is equipped with a set of sensor subsystems to acquire user-machine interaction forces and the temporal evolution of user's feet during gait. The authors present an adaptive filtering technique used for the identification and separation of different components found on the human-machine interaction forces. This technique allowed isolating the components related with the navigational commands and developing a Fuzzy logic controller to guide the device. The Smart Walker was clinically validated at the Spinal Cord Injury Hospital of Toledo - Spain, presenting great acceptability by spinal chord injury patients and clinical staff

Contribución al estudio de la incompatibilidad y otras medidas relacionadas en la lógica borrosa

Resumen La investigación descrita en esta memoria se enmarca en el campo de la lógica borro¬sa. Más concretamente, en el estudio de la incompatibilidad, de la compatibilidad y de la suplementaridad en los conjuntos borrosos y en los de Atanassov. En este orden de ideas, en el primer capítulo, se construyen, tanto de forma directa como indirecta, funciones apropiadas para medir la incompatibilidad entre dos conjuntos borro-sos. Se formulan algunos axiomas para modelizar la continuidad de dichas funciones, y se determina si las medidas propuestas, y otras nuevas que se introducen, verifican algún tipo de continuidad. Finalmente, se establece la noción de conjuntos borrosos compatibles, se introducen axiomas para medir esta propiedad y se construyen algunas medidas de compa¬tibilidad. El segundo capítulo se dedica al estudio de la incompatibilidad y de la compatibilidad en el campo de los conjuntos de Atanassov. Así, en primer lugar, se presenta una definición axiomática de medida de incompatibilidad en este contexto. Después, se construyen medidas de incompatibilidad por medio de los mismos métodos usados en el caso borroso. Además, se formulan axiomas de continuidad y se determina el tipo de continuidad de las medidas propuestas. Finalmente, se sigue un camino similar al caso borroso para el estudio de la compatibilidad. En el tercer capítulo, después de abordar la antonimia de conjuntos borrosos y de conjuntos de Atanassov, se formalizan las nociones de conjuntos suplementarios en estos dos entornos y se presenta, en ambos casos, un método para obtener medidas de suplementaridad a partir de medidas de incompatibilidad vía antónimos. The research described in this report pertains to the field of fuzzy logic and specifically studies incompatibility, compatibility and supplementarity in fuzzy sets and Atanassov's fuzzy sets. As such is the case, Chapter 1 describes both the direct and indirect construction of appropriate functions for measuring incompatibility between two fuzzy sets. We formulate some axioms for modelling the continuity of functions and determine whether the proposed and other measures introduced satisfy any type of continuity. Chapter 2 focuses on the study of incompatibility and compatibility in the field of Ata¬nassov's fuzzy sets. First, we present an axiomatic definition of incompatibility measure in this field. Then, we use the same methods to construct incompatibility measures as in the fuzzy case. Additionally, we formulate continuity axioms and determine the type of conti¬nuity of the proposed measures. Finally, we take a similar approach as in the fuzzy case to the study of compatibility. After examining the antonymy of fuzzy sets and Atanassov's sets, Chapter 3 formalizes the notions of supplementary sets in these two domains, and, in both cases, presents a method for obtaining supplementarity measures from incompatibility measures via antonyms.