Fuentes cartográficas para el estudio de la propiedad de la tierra de la Provincia de Buenos Aires : Chascomús, Ranchos y Monte, 1822-1864

En este trabajo se reconstruye el registro gráfico de 1864 y se comparan los resultados con otros ya desarrollados para 1822, 1830 y 1850, todos en la parte correspondiente a los partidos de Chascomús, Ranchos y Monte. Así, se correlacionan series completas de datos provenientes de duplicados de mensuras, solicitudes de tierras, protocolos de escribanos y testamentarias, con el fin de analizar la extensión de los campos y la tenencia de la tierra en estos partidos. De esta manera se aporta información para utilizar con mejores resultados la cartografía disponible para la época, revelando sus posibilidades expresivas en la comprensión de la ocupación y acceso a la propiedad legal de la tierra durante el siglo XIX, en ese sentido, aquí se evalúa el parcelamiento de los terrenos y el grado de concentración de la propiedad

Fuentes cartográficas para el estudio de la propiedad de la tierra de la Provincia de Buenos Aires : Chascomús, Ranchos y Monte, 1822-1864

En este trabajo se reconstruye el registro gráfico de 1864 y se comparan los resultados con otros ya desarrollados para 1822, 1830 y 1850, todos en la parte correspondiente a los partidos de Chascomús, Ranchos y Monte. Así, se correlacionan series completas de datos provenientes de duplicados de mensuras, solicitudes de tierras, protocolos de escribanos y testamentarias, con el fin de analizar la extensión de los campos y la tenencia de la tierra en estos partidos. De esta manera se aporta información para utilizar con mejores resultados la cartografía disponible para la época, revelando sus posibilidades expresivas en la comprensión de la ocupación y acceso a la propiedad legal de la tierra durante el siglo XIX, en ese sentido, aquí se evalúa el parcelamiento de los terrenos y el grado de concentración de la propiedad

Probabilistic models for the prediction of a ship performance in dynamic ice

We introduce two probabilistic, data-driven models that predict a ship's speed and the situations where a ship is probable to get stuck in ice based on the joint effect of ice features such as the thickness and concentration of level ice, ice ridges, rafted ice, moreover ice compression is considered. To develop the models to datasets were utilized. First, the data from the Automatic Identification System about the performance of a selected ship was used. Second, a numerical ice model HELMI, developed in the Finnish Meteorological Institute, provided information about the ice field. The relations between the ice conditions and ship movements were established using Bayesian learning algorithms. The case study presented in this paper considers a single and unassisted trip of an ice-strengthened bulk carrier between two Finnish ports in the presence of challenging ice conditions, which varied in time and space. The obtained results show good prediction power of the models. This means, on average 80% for predicting the ship's speed within specified bins, and above 90% for predicting cases where a ship may get stuck in ice. We expect this new approach to facilitate the safe and effective route selection problem for ice-covered waters where the ship performance is reflected in the objective function.

Framework for risk assessment for maritime transportation systems

Maritime accidents involving ships carrying passengers may pose a high risk with respect to human casualties. For effective risk mitigation, an insight into the process of risk escalation is needed. This requires a proactive approach when it comes to risk modelling for maritime transportation systems. Most of the existing models are based on historical data on maritime accidents, and thus they can be considered reactive instead of proactive. This paper introduces a systematic, transferable and proactive framework estimating the risk for maritime transportation systems, meeting the requirements stemming from the adopted formal definition of risk. The framework focuses on ship-ship collisions in the open sea, with a RoRo/Passenger ship (RoPax) being considered as the struck ship. First, it covers an identification of the events that follow a collision between two ships in the open sea, and, second, it evaluates the probabilities of these events, concluding by determining the severity of a collision. The risk framework is developed with the use of Bayesian Belief Networks and utilizes a set of analytical methods for the estimation of the risk model parameters. The model can be run with the use of GeNIe software package. Finally, a case study is presented, in which the risk framework developed here is applied to a maritime transportation system operating in the Gulf of Finland (GoF). The results obtained are compared to the historical data and available models, in which a RoPax was involved in a collision, and good agreement with the available records is found.

Characteristics of the Vernagtferner mass balance for the period from 1964 to 2014

The main characteristics of the Vernagtferner mass balance are sumarized in the table below. The mass balance years from 1964/65 to 2003/2004 are listed. The table includes the total area of the glacier (basis for the calculations), the equilibrium line altitude (ELA), percentage of the accumulation area in relation to the total area (AAR) and the specific net mass balance in mm w.e. (water equivalent) per year. It becomes clear that, after a rather minor growth period in the mid 1970's, the glacier continually lost mass since the beginning of the 1980's. Besides that, a clear increase of mass balance years with extreme mass losses could be observed in the last decade. The "glacier-friendly" summer with a well-balanced mass balance in 1999 could only interrupt the series of years with extreme mass losses, but this means no change in the trend. The minor mass loss in 1999 was caused by a winter snow cover above average, which prevented the glacier from becoming snow free over large areas and thus resulted in a lower ice melt. Although real summer conditions in 2000 were mainly restricted to August and produced a snow free area only slightly larger than in 1999, there have been further ice losses. This trend of negative mass balance continued also in the years 2001 and 2002. Nevertheless, the losses are moderate because a smaller part of the glacier became ice free until autumn (appr. 50 %). The summer 2003 caused a loss of ice in a dimension never seen since the beginning of the scientific investigations. This resulted from a combination of different factors: after only a moderate winter snowcover the glacier became snow free very early. For the first time the ablation area spanned over the entire glacier (blue fields in the mass balance tables!). Only one short snowfall event interrupted the ablation period, which lasted twice as long as in the years of large losses in the 1990's. The extreme mass loss in 2003 will also influence the mass balance in the following year 2004. The graphical representation of the elevation distribution of the specific mass balance together with the absolute mass balance can be found individually for each year by choosing one of the mass balance values from the table. These diagrams also include the area-height-distribution of the glacier and the ablation area. A tabular version of the numeric values in dependence of the elevation, provided separately for the accumulation area, the ablation area and the total glacier, can be found in colums "Persistent Identifier". The tables include the results for three different parts of the glacier and for the total glacier.

Large-Area Photo-Mosaicking tool (LAPM tool)

This paper presents a new tool for large-area photo-mosaicking (LAPM tool). This tool was developed specifically for the purpose of underwater mosaicking, and it is aimed at providing end-user scientists with an easy and robust way to construct large photo-mosaics from any set of images. It is notably capable of constructing mosaics with an unlimited number of images on any modern computer (minimum 1.30 GHz, 2 GB RAM). The mosaicking process can rely on both feature matching and navigation data. This is complemented by an intuitive graphical user interface, which gives the user the ability to select feature matches between any pair of overlapping images. Finally, mosaic files are given geographic attributes that permit direct import into ArcGIS. So far, the LAPM tool has been successfully used to construct geo-referenced photo-mosaics with photo and video material from several scientific cruises. The largest photo-mosaic contained more than 5000 images for a total area of about 105,000 m**2. This is the first article to present and to provide a finished and functional program to construct large geo-referenced photo-mosaics of the seafloor using feature detection and matching techniques. It also presents concrete examples of photo-mosaics produced with the LAPM tool.

Grain size investigations of sediments off the coast of Istria

Composition, grain-size distribution, and areal extent of Recent sediments from the Northern Adriatic Sea along the Istrian coast have been studied. Thirty one stations in four sections vertical to the coast were investigated; for comparison 58 samples from five small bays were also analyzed. Biogenic carbonate sediments are deposited on the shallow North Adriatic shelf off the Istrian coast. Only at a greater distance from the coast are these carbonate sediments being mixed with siliceous material brought in by the Alpine rivers Po, Adige, and Brenta. Graphical analysis of grain-size distribution curves shows a sediment composition of normally three, and only in the most seaward area, of four major constituents. Constituent 1 represents the washed-in terrestrial material of clay size (Terra Rossa) from the Istrian coastal area. Constituent 2 consists of fine to medium sand. Constituent 3 contains the heterogeneous biogenic material. Crushing by organisms and by sediment eaters reduces the coarse biogenic material into small pieces generating constituent 2. Between these two constituents there is a dynamic equilibrium. Depending upon where the equilibrium is, between the extremes of production and crushing, the resulting constituent 2 is finer or coarser. Constituent 4 is composed of the fine sandy material from the Alpine rivers. In the most seaward area constituents 2 and 4 are mixed. The total carbonate content of the samples depends on the distance from the coast. In the near coastal area in high energy environments, the carbonate content is about 80 %. At a distance of 2 to 3 km from the coast there is a carbonate minimum because of the higher rate of sedimentation of clay-sized terrestrial, noncarbonate material at extremely low energy environments. In an area between 5 and 20 km off the coast, the carbonate content is about 75 %. More than 20 km from the shore, the carbonate content diminishes rapidly to values of about 30 % through mixing with siliceous material from the Alpine rivers. The carbonate content of the individual fractions increases with increasing grain-size to a maximum of about 90 % within the coarse sand fractions. Beyond 20 km from the coast the samples show a carbonate minimum of about 13 % within the sand-size classes from 1.5 to 0.7 zeta¬? through mixing with siliceous material from the alpine rivers. By means of grain-size distribution and carbonate content, four sediment zones parallel to the coast were separated. Genetically they are closely connected with the zonation of the benthic fauna. Two cores show a characteristic vertical distribution of the sediment. The surface zone is inversely graded, that means the coarse fractions are at the top and the fine fractions are at the bottom. This is the effect of crushing of the biogenic material produced at the surface by predatory organisms and by sediment eaters. lt is proposed that at a depth of about 30 cm a chemical solution process begins which leads to diminution of the original sediment from a fine to medium sand to a silt. The carbonate content decreases from about 75 % at the surface to 65 % at a depth of 100 cm. The increase of the noncarbonate components by 10 % corresponds to a decrease in the initial amount of sediment (CaC03=75 %) by roughly 30 % through solution. With increasing depth the carbonate content of the individual fractions becomes more and more uniform. At the surface the variation is from 30 % to 90 %, at the bottom it varies only between 50 % and 75 %. Comparable investigations of small-bay sediments showed a c1ear dependence of sediment/faunal zonation from the energy of the environment. The investigations show that the composition and three-dimensional distribution of the Istrian coastal sediments can not be predicted only from one or a few measurable factors. Sedimentation and syngenetic changes must be considered as a complex interaction between external factors and the actions of producing and destroying organisms that are in dynamic equilibrium. The results obtained from investigations of these recent sediments may be of value for interpreting fossil sediments only with strong limitations.

Granulometry and Bulk Geochemistry of Nearshore Sediments, Herschel Island, Yukon Territory, Canada

This dataset contains the results of granulometric and bulk geochemical analyses of Van Veen surface samples obtained by the Alfred Wegener Institute (AWI) in the course of the 2012 and 2013 summer field seasons. The sampling was performed along transects in depths generally <13 m, to a distance of about <5 km off Herschel Island. In 2012, 75 samples in Pauline Cove and in the vicinity of Simpson Point were obtained. Sample collection was expanded in 2013, on transects established the previous year, with additional locations in Tetris Bay and Workboat Passage. Samples consisted of approximately 100 g of the top 3-6 cm of sediment, and were frozen in the field and freeze dried at the AWI before undergoing analytical procedures. Sample locations were recorded with the onboard global positioning system (GPS) unit. Grain size distributions in our study were obtained using laser diffractometry at the AWI (Beckman Coulter LS200) on the <1 mm fraction of samples oxidized with 30% H2O2 until effervescence ceased to remove organics. Some samples were also sieved using a sieve stack with 1 phi intervals. GRADISTAT (Blott and Pye, 2001) was used to calculate graphical grain size statistics (Folk and Ward, 1957). Grain diameters were logarithmically transformed to phi values, calculated as phi=-log2d, where d is the grain diameter in millimeters (Blott and Pye, 2001; Krumbein, 1934). Freeze dried samples were ground and ground using an Elemetar Vario EL III carbon-nitrogen-sulphur analyzer at the AWI to measure total carbon (TC) and total nitrogen (TN). Tungsten oxide was added to the samples as a catalyst to the pyrolysis. Following this analysis, total organic carbon (TOC) was determined using an Elementar VarioMax. Stable carbon isotope ratios of 13C/12C of 118 samples were determined on a DELTAplusXL mass spectrometer (ThermoFisher Scientific, Bremen) at the German Research Centre for Geosciences (GFZ) in Potsdam, Germany . An additional analysis on 69 samples was carried out at the University of Hamburg with an isotope ratio mass spectrometer (Delta V, Thermo Scientific, Germany) coupled to an elemental analyzer (Flash 2000, Thermo Scientific, Germany). Prior to analysis, soil samples were treated with phosphoric acid (43%) to release inorganic carbon. Values are expressed relative to Vienna Peedee belemnite (VPDB) using external standards (USGS40, -26.4 per mil VPDB and IVA soil 33802153, -27.5 per mil VPDB).

Kiel fjord pCO2 datasets between 2012 (July) and 2015 (January) measured using a HydroC® pCO2 sensor

The HydroC® CO2 sensor was deployed from a pontoon at the waterfront of the GEOMAR west shore building into Kiel Fjord, Western Baltic Sea (Kiel, Germany; 54°19'48.78"N, 010° 8'59.44"E). Since the pontoon is floating the deployment depth of the sensor was constant at 1m. Data of three deployment intervals are published here: 1) July 2012 - December 2012 2) April 2013 - June 2013 3) November 2013 - January 2015 Data are processed and corrected, for documentation and graphical overview see further details.

Learning an L1-regularized Gaussian Bayesian Network in the Equivalence Class Space

Learning the structure of a graphical model from data is a common task in a wide range of practical applications. In this paper, we focus on Gaussian Bayesian networks, i.e., on continuous data and directed acyclic graphs with a joint probability density of all variables given by a Gaussian. We propose to work in an equivalence class search space, specifically using the k-greedy equivalence search algorithm. This, combined with regularization techniques to guide the structure search, can learn sparse networks close to the one that generated the data. We provide results on some synthetic networks and on modeling the gene network of the two biological pathways regulating the biosynthesis of isoprenoids for the Arabidopsis thaliana plant

Las Infraestructuras de Datos Espaciales (IDE) como un recurso educativo TIC . Estrategias de formación y difusión para el profesorado de la Educación Secundaria Obligatoria

Desde mediados de los 90, gracias a las posibilidades de la World Wide Web, se liberó la cartografía de su dependencia del medio físico, posibilitando el acceso y visualización de millones de mapas almacenados en formatos gráficos a través de Internet. En este contexto, el papel de la Información Geográfica (IG) en la vida cotidiana adquirió relevancia en la medida que el acceso a la misma resultaba cada vez más fácil gracias a múltiples herramientas y aplicaciones para distribuir y acercar los mapas en distintos formatos a la sociedad en general. Sin embargo, dado que esa información enseguida pasaba a estar desactualizada, surgió una demanda desde distintos ámbitos (seguridad, medio ambiente transporte, servicios, etc.) y de la sociedad en general para disponer de la información más actual. Como respuesta a esta demanda, surgen las iniciativas denominadas Infraestructuras de Datos Espaciales (IDE). Estas iniciativas, mediante la acción coordinada de un conjunto de tecnologías, estándares, normas y políticas, brindan la posibilidad a los usuarios de acceder, a través de Internet, a IG actualizada producida por instituciones y organismos oficiales, en un marco colaborativo y sustentada en una estructura organizativa. En este contexto, el ámbito educativo no ha permanecido ajeno representando uno de los espacios más propicios para la difusión de las potencialidades y usos de las IDE. En esta tesis se propone la utilización de las IDE en el contexto educativo, específicamente en la Educación Secundaria Obligatoria (ESO). Utilizar las IDE en el contexto educativo implica asignarle un papel en el proceso de enseñanza-aprendizaje y en el marco de esta tesis se presentan los fundamentos teóricos que permiten afirmar que las IDE son un re-curso educativo que responde a las características de las Tecnologías de la Información y la Comunicación (TIC). Esto se explicita a través de un concepto más amplio que hemos denominado “recurso educativo TIC”. En este contexto se analizan las posibilidades que ofrece las IDE para alcanzar los objetivos de aprendizaje de asignaturas de la ESO relacionadas con IG y se identifican contenidos susceptibles de ser abordados utilizándolas. Por otra parte, atendiendo al modelo educativo del aprendizaje basado en competencias, se exponen las posibilidades y potencialidades que ofrecen las IDE para desarrollar la competencia digital. Una vez planteado el marco teórico se desarrollaron dos estrategias de formación y difusión de las IDE orientadas al profesorado de la ESO. En primer lugar, utilizando el Modelo de Diseño Instruccional ADDIE, se diseñaron, desarrollaron, implementaron y evaluaron tres cursos e-learning para el profesorado de ESO de las asignaturas Ciencias Sociales, Ciencias de la Naturaleza y Tecnología. En segundo lugar, con objetivo de complementar los resultados obtenidos de los cursos e-learning, se realizó una actividad en dos Institutos de Educación Secundaria orientada a difundir las IDE. La puesta en práctica de estas estrategias ofreció al profesorado la información necesaria sobre qué son las IDE y proporcionó ejemplos concretos de uso de las mismas en su asignatura, permitiéndoles disponer de los conocimientos e información para emitir una valoración sobre las posibilidades que ofrecen las IDE como un recurso educativo TIC. Since about the middle of the 1990 decade, owing to the potential of the World Wide Web, cartography freed itself from its dependence on its physical support, enabling the access and visualisation of millions of maps stored in graphical formats through the Internet. In this context, the role of Geographic Information (GI) in daily life became relevant in as much as its access turned out to be ever easier due to multiple tools and applications to distribute and bring maps in different formats closer to society in general. Yet, since the information available often became outdated, a demand for updated information arose from different specific fields (security, environment, transport, services, etc.) and from the general public. As a response to this demand, the so-called Spatial Data Infrastructure (SDI) initiatives arose which, through the coordinated action of a set of technologies, stan-dards, and policies, enabled users to access updated GI created by organisations and official institutions, through the Internet, within a cooperative framework and an organisational structure. In this context the educational world has not remained aloof, since it represented one of the most propitious scope for the dissemination of the potentials and uses of SDI. In this thesis the utilization of SDI in the educational context is proposed, specifically in the Spanish Compulsory Secondary Education (Educación Secundaria Obligatoria – ESO). This utilization implies assigning SDI a role in the teaching-learning process; here the theo-retical foundation is presented which allows asserting that SDI is an educational resource fitting in with the characteristics of the Information and Communication Technologies (ICT). This is made explicit by means of a broader concept we have called “ICT educa-tional resource”. The possibilities offered by SDI to reach the objective of learning ESO subjects related to GI are analyzed, and contents apt to be addressed by using them are identified. On the other hand, attending to the educational model of learning based on competences, the possibilities and potentials the SDI offer to develop the digital compe-tence are exposed. After having set forth the theoretical frame, two strategies of training and dissemination of SDI were developed, oriented to the ESO teaching staff. First, using the ADDIE Instruc-tional Design Model, three learning courses were designed, developed, implemented and evaluated for the ESO teaching staff in the subjects of Social Sciences, Natural Sciences and Technology. In the second place, with the purpose of supplementing the results ob-tained from the e-learning courses, an activity was carried out in two High Schools, ori-ented to disseminate the SDI. The implementation of these strategies offered the teaching staff the needed information concerning the SDI and provided specific instances of utilisa-tion thereof in their subject, thus enabling them to acquire the knowledge and information to issue an assessment of the possibilities the SDI offer as an ICT educational resource

Education and Training of Future Nuclear Engineers Through the use of an Interactive Plant Simulator

The successful experience of the Jose Cabrera Nuclear Power Plant Interactive Graphical Simulator implementation in the Nuclear Engineering Department in the Universidad Polite´cnica de Madrid, for the Education and Training of nuclear engineers is shown in this paper. The paper starts with the objectives and the description of the Simulator Aula, and the methodology of work following the recommendations of the IAEA for the use of nuclear reactor simulators for education. The practices and material prepared for the students, as well as the operational and accident situations simulated are provided.

Uniformly reweighted belief propagation for distributed Bayesian hypothesis testing

Belief propagation (BP) is a technique for distributed inference in wireless networks and is often used even when the underlying graphical model contains cycles. In this paper, we propose a uniformly reweighted BP scheme that reduces the impact of cycles by weighting messages by a constant ?edge appearance probability? rho ? 1. We apply this algorithm to distributed binary hypothesis testing problems (e.g., distributed detection) in wireless networks with Markov random field models. We demonstrate that in the considered setting the proposed method outperforms standard BP, while maintaining similar complexity. We then show that the optimal ? can be approximated as a simple function of the average node degree, and can hence be computed in a distributed fashion through a consensus algorithm.