Desmantelamiento del experimento EB

Este proyecto consiste en la fase de desmantelamiento de un experimento que se ha ido desarrollando por la empresa AITEMIN en colaboración con multitud de empresas internacionales del ámbito de la eliminación de residuos radioactivos de alta actividad y se desarrolla en el laboratorio subterráneo de Mont Terri en Suiza. En el proyecto se describirán todas las partes del experimento y se procederá a establecer el procedimiento a utilizar para su desmantelamiento, explicando exhaustivamente los pasos a realizar por las personas responsables de la desmantelamiento. ABSTRACT This project involves the dismantling phase of an experiment that has been developed by the company AITEMIN in collaboration with many international companies in the field of radioactive waste disposal and develops high activity in the Mont Terri underground laboratory in Switzerland. The project will describe all parts of the experiment and proceed to establish the procedure to be used for dismantling, thoroughly explaining the steps to be performed by the persons responsible for the dismantling

Modeling and optimization of frequencies on congested bus lines

In this paper some mathematical programming models are exposed in order to set the number of services on a specified system of bus lines, which are intended to assist high demand levels which may arise because of the disruption of Rapid Transit services or during the celebration of massive events. By means of this model two types of basic magnitudes can be determined, basically: a) the number of bus units assigned to each line and b) the number of services that should be assigned to those units. In these models, passenger flow assignment to lines can be considered of the system optimum type, in the sense that the assignment of units and of services is carried out minimizing a linear combination of operation costs and total travel time of users. The models consider delays experienced by buses as a consequence of the get in/out of the passengers, queueing at stations and the delays that passengers experience waiting at the stations. For the case of a congested strategy based user optimal passenger assignment model with strict capacities on the bus lines, the use of the method of successive averages is shown.

Demonstracion legal, de los motiuos, que precisaron al ... señor D. Manuel Salvador y del Olmo ... por el ... señor Don Ascensio Sales, Obispo de Barcelona ..., a declarar y mandar publicar incursa en las censuras a la ..

Contiene: Epitome de los motiuos juridicos que assistieron a la Curia Eclesiastica de Barcelona para resistirse a firmar la contencion que le propuso la Real Audiencia a instancia de la ... abadesa de S. Pedro de las Puellas de la misma ciudad

Reglamento para el govierno del Monte-Pio de Viudas, y pupilos de los abogados del ... Colegio de la ciudad de Valencia ... [Texto impreso] : aprobado por los señores del ... Consejo de Castilla, en 20 de Marzo de 1778

Hay un ejemplar encuadernado con: Alegación en hecho y derecho por la... Duquesa del Infantado... posseedora de la Baronia de Alberique... contra el Dr.Juan Fronti,... Felix Pasqual Garcia..., Joseph Ortiz...y demas litis consortes... en el pleyto que pende ante... la Real Audiencia ... (XVIII/510).

New Hampshire, 1816 (Image 4 of 6) (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: New Hampshire by recent survey : made under the supreme authority and published according to law by Philip Carrigain ; J.J. Barralet, del. ; W. Harrison, sct., Philada. It was published by Philip Carrigain in 1816. Scale [ca. 1:200,000]. This layer is image 4 of 6 total images, representing the southwest portion of the six sheet source map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the New Hampshire State Plane coordinate system (NAD 1983 in Feet) (Fipszone 2800). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, public buildings, schools, churches, industry locations (e.g. mills, factories, mines, etc.), selected private buildings with names of property owners, town boundaries, land grants, and more. Relief shown pictorially and by hachures. Includes area notes, text, and table of population. Also includes illustrations: View of the Great Boars Head and Hampton Beach -- The Cap of the White Mountains -- View of the White Mountains from Shelburne; inset maps: States of the Union east of the Hudson with the adjacent British colonies. Scale [ca. 1:1,920,000] -- The middle, southern and western sections of the United States with the territories. Scale [ca. 1:4,900,000]. Includes: ms. additions with updated county boundary & township names.This layer is part of a selection of digitally scanned and georeferenced historic maps of New England from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of regions, originators, ground condition dates, scales, and map purposes.

Hillsborough County, New Hampshire, 1858 (Image 2 of 4) (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of Hillsboro Co., New Hampshire, from actual surveys by J. Chace, Jr. It was published by Smith, Mason & Co. in 1858. Scale [ca. 1:53,000]. This layer is image 2 of 4 total images, representing the southwest portion of the four sheet source map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the New Hampshire State Plane coordinate system (NAD 1983 in Feet) (Fipszone 2800). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, railroads, drainage, public buildings, schools, churches, cemeteries, industry locations (e.g. mills, factories, mines, etc.), private buildings with names of property owners, town and school district boundaries, and more. Relief shown by hachures. Includes table of distances, agricultural goods, religious affiliations, business directory, statistics of education and other information, and a list of county officers.This layer is part of a selection of digitally scanned and georeferenced historic maps of New England from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of regions, originators, ground condition dates, scales, and map purposes.

Southern, Central, & Eastern Africa, ca. 1730 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Carte de l'Afrique meridionale : ou pays entre la ligne & le cap de Bonne Esperance et l'isle de Madagascar, par la veuve de Nicolas Visscher avec privilege. It was published by Chez Henry de Leth, Marchand de l'Estampes près de la Boursse ca. 1730. Scale [ca. 1:12,250,000]. Covers portions of Southern, Central, and Eastern Africa. Map in French and Dutch.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Africa Sinusoidal projected coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, territorial boundaries, shoreline features, and more. Relief shown pictorially. Includes notes and insets: [Cabo de Bon Esperanca], Elevation du port et Mont Table au Cap de Bonne Esperance and Plan du port et Mont Table au Cap de Bonne Esperance.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Magnetic anisotropy reveals Neogene tectonic overprint in highly strained carbonate mylonites from the Morcles nappe, Switzerland

The anisotropy of magnetic susceptibility (AMS) has been measured with low- and high-field methods, in deformed carbonate rocks along the Morcles nappe shear zone (Helvetic Alps). High-field measurements at room temperature and 77 K enable the separation of the ferrimagnetic, paramagnetic and diamagnetic anisotropy. The ferrimagnetic sub-fabric is generally insignificant in these rocks, contributing less than 10% to the total AMS. AMS results for both the separated diamagnetic and paramagnetic subfabrics are consistent with the regional shear movement in the late-stage formation of the Helvetic nappes, as seen in the Morcles nappe, whose inverted limb indicate shear displacement towards the northwest. The diamagnetic anisotropy correlates well quantitatively with the calculated magnetic anisotropy based on the calcite texture. There is a gradational change in the degree of anisotropy related to the strain gradient along the shear zone. A more complex magnetic fabric, resulting from partial overprinting due to displacement along the Simplon–Rhône fault, is evident at one site near the root zone of the nappe. Partial overprinting of the magnetic fabric appears to have taken place in two locations farther up the shear zone as well. This late phase deformation is associated with recent exhumation of the Mont Blanc and Belledonne external massifs and orogen parallel extension, and is reflected by the AMS. Rocks with bulk susceptibility ∼0 SI, and simple mineral compositions are ideal for low temperature high-field torque, as this method helps to enhance the paramagnetic susceptibility and anisotropy, which may otherwise be masked by the mixed magnetic contributions of the composite magnetic fabric.

Dissolved CO2 and Alkane Gas in Clay Formations

Characterization of dissolved CO2 and alkane gas in clayrocks may help assessing the confinement properties of geological barriers considered as potential host rocks for a deep geological disposal as well as for caprocks of gas storages. A monitoring of alkanes with CO2, combined with carbon isotopes was performed on core samples coming from Underground Research Laboratories (Bure, Mont Terri, Tournemire) and the Schlattingen borehole in France and Switzerland. Composition of hydrocarbon gas and delta C-13 of methane strongly suggest a dominant thermogenic origin of methane which is mixed with a bacterial origin for the Toarcian shales, Pliensbachien and Callovian-Oxfordian clayrocks. Results also evidence the contrasted behavior of CO2, which is controlled by chemical equilibrium between pore water and carbonate mineralogy, compared to the alkanes which are present in the porosity as a stock of dissolved gases which can be depleted during degassing experiments. (C) 2015 The Authors. Published by Elsevier B.V.

Vislumbres.

Poems.

Metal bioaccumulation in fishes and aquatic invertebrates : a literature review /

Mode of access: Internet.

Aqueous ammonia equilibrium : tabulation of percent un-ionized ammonia /

Mode of access: Internet.

Trends in selected water-quality characteristics, Powder River and tributaries, Montana and Wyoming, water years 1968-88 and 1975-88 /

Mode of access: Internet.

CETIS, Complex Effluents Toxicity Information System : data encoding guidelines and procedures /

"CR807240."