972 resultados para SOCIETY SOURCE CLAYS
Resumo:
As more and more open-source software components become available on the internet we need automatic ways to label and compare them. For example, a developer who searches for reusable software must be able to quickly gain an understanding of retrieved components. This understanding cannot be gained at the level of source code due to the semantic gap between source code and the domain model. In this paper we present a lexical approach that uses the log-likelihood ratios of word frequencies to automatically provide labels for software components. We present a prototype implementation of our labeling/comparison algorithm and provide examples of its application. In particular, we apply the approach to detect trends in the evolution of a software system.
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Mainstream IDEs such as Eclipse support developers in managing software projects mainly by offering static views of the source code. Such a static perspective neglects any information about runtime behavior. However, object-oriented programs heavily rely on polymorphism and late-binding, which makes them difficult to understand just based on their static structure. Developers thus resort to debuggers or profilers to study the system's dynamics. However, the information provided by these tools is volatile and hence cannot be exploited to ease the navigation of the source space. In this paper we present an approach to augment the static source perspective with dynamic metrics such as precise runtime type information, or memory and object allocation statistics. Dynamic metrics can leverage the understanding for the behavior and structure of a system. We rely on dynamic data gathering based on aspects to analyze running Java systems. By solving concrete use cases we illustrate how dynamic metrics directly available in the IDE are useful. We also comprehensively report on the efficiency of our approach to gather dynamic metrics.
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Maintaining object-oriented systems that use inheritance and polymorphism is difficult, since runtime information, such as which methods are actually invoked at a call site, is not visible in the static source code. We have implemented Senseo, an Eclipse plugin enhancing Eclipse's static source views with various dynamic metrics, such as runtime types, the number of objects created, or the amount of memory allocated in particular methods.
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Mass spectrometric analysis of elemental and isotopic compositions of several NIST standards is performed by a miniature laser ablation/ionisation reflectron-type time-of-flight mass spectrometer (LMS) using a fs-laser ablation ion source (775 nm, 190 fs, 1 kHz). The results of the mass spectrometric studies indicate that in a defined range of laser irradiance (fluence) and for a certain number of accumulations of single laser shot spectra, the measurements of isotope abundances can be conducted with a measurement accuracy at the per mill level and at the per cent level for isotope concentrations higher and lower than 100 ppm, respectively. Also the elemental analysis can be performed with a good accuracy. The LMS instrument combined with a fs-laser ablation ion source exhibits similar detection efficiency for both metallic and non-metallic elements. Relative sensitivity coefficients were determined and found to be close to one, which is of considerable importance for the development of standard-less instruments. Negligible thermal effects, sample damage and excellent characteristics of the fs-laser beam are thought to be the main reason for substantial improvement of the instrumental performance compared to other laser ablation mass spectrometers.
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In the Lower Mekon Basin the extraordinary pace of economic development and growth contradicts with environmental protection. On base of the Watershed Classification Project (WSCP) and the inclusion of a DTM for the entire LMB the potential degradation risk was derived for each land unit. The risks were grouped into five classes, where classes one and two are considered critical with regard to soil erosion when the land is cleared of natural resources. For practical use the database has an enormous potential for further spatial analysis in combination with other datasets, as for example the NCCR North-South uses the WSCP within two research projects.
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Alpine heavy precipitation events often affect small catchments, although the circulation pattern leading to the event extends over the entire North Atlantic. The various scale interactions involved are particularly challenging for the numerical weather prediction of such events. Unlike previous studies focusing on the southern Alps, here a comprehensive study of a heavy precipitation event in the northern Alps in October 2011 is presented with particular focus on the role of the large-scale circulation in the North Atlantic/European region. During the event exceptionally high amounts of total precipitable water occurred in and north of the Alps. This moisture was initially transported along the flanks of a blocking ridge over the North Atlantic. Subsequently, strong and persistent northerly flow established at the upstream flank of a trough over Europe and steered the moisture towards the northern Alps. Lagrangian diagnostics reveal that a large fraction of the moisture emerged from the West African coast where a subtropical upper-level cut-off low served as an important moisture collector. Wave activity flux diagnostics show that the ridge was initiated as part of a low-frequency, large-scale Rossby wave train while convergence of fast transients helped to amplify it locally in the North Atlantic. A novel diagnostic for advective potential vorticity tendencies sheds more light on this amplification and further emphasizes the role of the ridge in amplifying the trough over Europe. Operational forecasts misrepresented the amplitude and orientation of this trough. For the first time, this study documents an important pathway for northern Alpine flooding, in which the interaction of synoptic-scale to large-scale weather systems and of long-range moisture transport from the Tropics are dominant. Moreover, the trapping of moisture in a subtropical cut-off near the West African coast is found to be a crucial precursor to the observed European high-impact weather.
Resumo:
Bentonite and iron metals are common materials proposed for use in deep-seated geological repositories for radioactive waste. The inevitable corrosion of iron leads to interaction processes with the clay which may affect the sealing properties of the bentonite backfill. The objective of the present study was to improve our understanding of this process by studying the interface between iron and compacted bentonite in a geological repository-type setting. Samples of MX-80 bentonite samples which had been exposed to an iron source and elevated temperatures (up to 115ºC) for 2.5 y in an in situ experiment (termed ABM1) at the Äspö Hard Rock Laboratory, Sweden, were investigated by microscopic means, including scanning electron microscopy, μ-Raman spectroscopy, spatially resolved X-ray diffraction, and X-ray fluorescence. The corrosion process led to the formation of a ~100 mm thick corrosion layer containing siderite, magnetite, some goethite, and lepidocrocite mixed with the montmorillonitic clay. Most of the corroded Fe occurred within a 10 mm-thick clay layer adjacent to the corrosion layer. An average corrosion depth of the steel of 22–35 μm and an average Fe2+ diffusivity of 1–26×10–13 m2/s were estimated based on the properties of the Fe-enriched clay layer. In that layer, the corrosion-derived Fe occurred predominantly in the clay matrix. The nature of this Fe could not be identified. No indications of clay transformation or newly formed clay phases were found. A slight enrichment of Mg close to the Fe–clay contact was observed. The formation of anhydrite and gypsum, and the dissolution of some SiO
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Über das Forschungsprogramm: The Philosophy of Western Society. Teilstück des allgemeinen Forschungsprogramms, veröffentlicht unter dem Untertitel: "The Philosophy of Social Science", in: "International Institute of Social Research. A Report of Its History, Aims and Activites, 1933-1938", New York (1938?), S. 19, Typoskript mit eigenhändiger Korrektur, 2 Blatt; Bericht über die Aktivitäten des Instituts für Sozialforschung für Robert M. MacIver, 1938-39: 1. Bericht vom 7.12.1939; a) Typoskript, englisch, 9 Blatt; b) Typoskript, als Brief von Pollock an Robert M. MacIver, Typoskript 10 Blatt; c) Entwurf Typoskript, englisch, 15 Blatt; d) Entwurf Typoskript, deutsch, 17 Blatt; MacIver, Robert M.: 1 Brief mit Unterschrift an Friedrich Pollock, New York, 27.04.1938, 1 Blatt; "Some data on the Institut`s Staff and Activities", 11.03.1938, zwei Typoskripte, je 2 Blatt; Über die Tätigkeiten des Instituts für Sozialforschung. Verschiedene Berichte. 1939; Aufstellung der Forschungsgebiete verschiedener Mitarbeiter des Instituts. Ohne Datum, Typoskript, 9 Blatt; Aufstellung der Forschungsgebiete verschiedener Mitarbeiter des Institutes, aus einem Bericht. Typoskript, 7 Blatt; Bericht an den Präsidenten des Columbia University. Typoskript, 2 Blatt; "Contribution of Dr. Franz Neumann to the Round Table Discussion, Chicago, Social Science Reaserach Building" Dezember 1939; a) Typoskript mit Handschriftlichen Korrekturen, 3 Blatt; b) Typoskript, 3 Blatt; "Statment on the objectives of the International Institut of Social Research". Typoskript, 2 Blatt; Stipendiaten des Instituts für Sozialforschung: Forschungsberichte, Ende 1939; Adorno, Theodor W.: a) Typoskript, englisch, mit eigenhändigen Korrekturen, 4 Blatt; b) Typoskript, deutsch, 3 Blatt; Beck, Maximilian: "Geschichte des Begriffs der Vernunft von Platon bis Husserl (Outline)". Typoskript, englisch und deutsch, mit handschriftlichen Korrekturen, 7 Blatt; Flechtheim, Ossip K.: Typoskript mit handschriftlichen Ergänzungen, 1 Blatt; Fried, Hans Ernest: Typoskript, 1 Blatt, 16.11.1939; Grossmann, Henryk: "Capitalism in the 13th Century"; a) Typoskript, englisch, mit handschriftlichen Korrekturen, 6 Blatt; b) Typoskript, englisch, 6 Blatt; c) Typoskript, deutsch, 4 Blatt; Grossmann, Henryk: "The Classical Theory and Marxism"; a) Typoskript, englisch, mit handschriftlichen Korrekturen, 2 Blatt; b) Typoskript, deutsch, mit handschriftlichen Korrekturen, 2 Blatt; Kirchheimer, Otto: Manuskript, 1 Blatt; Lauterbach, Albert: a) Typoskript, englisch, mit handschriftlichen Korrekturen, 2 Blatt; b) Typoskript, deutsch, mit handschriftlichen Korrekturen, 1 Blatt; Marcuse, Herbert: Typoskript mit handschriftlichen Korrekturen, 2 Blatt; Neumann, Franz L.: Typoskript, 2 Blatt; Wittfogel, Karl August: Typsokript, 2 Blatt; Zilsel, Edgar: Typoskript, 4 Blatt; Research Projects of the International Institute of Social Research. nicht vor 1939; Beschreibung der Forschungsprojekte: Pollock, Friedrich: "Economic and Social Cosequences of a Prepardness Economy". Neumann, Franz L.: "The Rule of Law". Fromm, Erich: "The German Worker in the Weiman Republic". Kirchheimer,Otto: "Criminal Law and Social Structure". Marcuse, Herbert: " A Text and Source Book for the History of Philosophy". Fromm, Erich: "Character Structure of Modern Man". Neumann, Franz L.: "The Theory and Practice of European Labor Law". Wittfogel, Karl August; Wittfogel-Lang, Olga: "The Chinese Family"; Dasselbe wie in "Beschreibung der Forschungsprojekte", ausgenommen Pollock, Friedrich: "Economic and Social Cosquences of a Prepardness Economy" und Fromm, Erich: "The German Worker in the Weimar Republic", zusätzlich Kirchner, Otto; Weil, Felix: "Changes in Social Stratification, National Income, and Living Standards of Germany since 1933"; 1 Ordner, Typoskript mit eigenhändigen Korrekturen, 49 Blatt;
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X-ray diffraction analyses have been carried out on 128 samples of Miocene to Quaternary sediments from ODP Sites 794, 795 and 797. Some clay fractions of samples from Site 797 have also been studied for rare earth elements and by Nd isotopic analyses. These three sites display similar lithological and clay assemblages (with dominant chlorite, illite and smectite) showing that the sedimentation was homogeneous throughout the whole Japan Sea Basin. Three mineralogical zones are recognized. The first zone (Lower Miocene sandy clay of Sites 794 and 797) is mainly composed of chlorite resulting from hydrothermal transformation of arc-derived smectite, due to sill injections during the initial oceanic spreading stage. The second zone (Lower Miocene to Lower Pliocene siliceous claystone and diatomaceous silty clay) is dominated by arc-derived smectite; the abundance of this mineral decreases upwards while illite and chlorite increase. This trend reflects a change of detrital source, from an eastern arc-derived source (epsilon -Nd**t>-3.3); variable LREE enrichment) to a western continental crust source (epsilon-Nd**t<-9.4; shale-like REE patterns); climatic modifications in the current dynamics are proposed as a cause for this change. The third zone (Upper Pliocene to Recent silty clay with minor diatom oozes) is characterized at Site 797 by increasing amounts of illite and chlorite. This reflects a more and more important western supply which is assumed to be related to tectonic rejuvenations of the Asian margin or climatic modifications affecting the alteration conditions or the current dynamics. At Sites 794 and 795, the more or less sharp supply of chlorite seems to be driven by the incipient subduction zone on the eastern margin of the Japan Sea.
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El cine como fuente historiográfica es utilizado a partir de la "batalla" que dio Marc Ferro hacia el interior de Annales. Cuando era difícil que se aceptaran otras fuentes que no fueran las gráficas, este historiador logró abrirse camino hasta llegar a ser el director de Annales en los años '70. El discurso de la imagen o el discurso audiovisual representa con mayor verosimilitud lo que el discurso gráfico no alcanza a expresar. Sin embargo, la sinécdoque y la generalización se encuentran a mitad de camino en un juego representativo para complementarse a la hora de comprender y reconstruir el pasado. El aporte del cine puede tomarse como reflejo o representación social y también como una alternativa discursiva. En este sentido, Rosenstone con el apoyo de Hayden White y su análisis de la "historiofotía" son los que incursionan en esta nueva dimensión, esto es la narración audiovisual de la historia
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To better understand the composition, characteristics of helium diffusion, and size distribution of interplanetary dust particles (IDPs) responsible for the long-term retention of extraterrestrial 3He, we carried out leaching, stepped heating, and sieving experiments on pelagic clays that varied in age from 0.5 Ma to ~90 Myr. The leaching experiments suggest that the host phase(s) of 3He in geologically old sediments are neither organic matter nor refractory phases, such as diamond, graphite, Al2O3, and SiC, but are consistent with extraterrestrial silicates, Fe-Ni sulfides, and possibly magnetite. Stepped heating experiments demonstrate that the 3He release profiles from the magnetic and non-magnetic components of the pelagic clays are remarkably similar. Because helium diffusion is likely to be controlled by mineral chemistry and structure, the stepped heating results suggest a single carrier that may be magnetite, or more probably a phase associated with magnetite. Furthermore, the stepped outgassing experiments indicate that about 20% of the 3He will be lost through diffusion at seafloor temperatures after 50 Myrs, while sedimentary rocks exposed on the Earth's surface for the same amount of time would lose up to 60%. The absolute magnitude of the 3He loss is, however, likely to depend upon the 3He concentration profile within the IDPs, which is not well known. Contrary to previous suggestions that micrometeorites in the size range of 50-100 µm in diameter are responsible for the extraterrestrial 3He in geologically old sediments [Stuart, F.M., Harrop, P.J., Knott, S., Turner, G., 1999. Laser extraction of helium isotopes from Antarctic micrometeorites: source of He and implications for the flux of extraterrestrial 3He flux to earth. Geochimica et Cosmochimica Acta, 63, 2653-2665, doi:10.1016/S0016-7037(99)00161-1], our sieving experiment demonstrates that at most 20% of the 3He is carried by particles greater than 50 µm in diameter. The size-distribution of the 3He-bearing particles implies that extraterrestrial 3He in sediments record the IDP flux rather than the micrometeorite flux.