981 resultados para General Strike, Mexico, 1921.


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The span of the bridge was assumed as 100 feet. The type of bridge used is the timber Howe Truss. The height of truss was taken as 20 feet between center lines of top and bottom chords. The width was taken as 18 feet center to center of trusses. The truss was divided up into five panels 20 feet long.

It was designed according to the "General Specifications for Steel Highway Bridges" by Ketchum. For the live load for the floor and its supports, a load of 80 pounds per square foot of total floor surface or a 15 ton traction engine with axles 10 feet centers and 6 feet gage, two thirds of load to be carried by rear axles.

For the truss a load of 75 pounds per square foot of floor surface.

For the wind load the bottom lateral bracing is to be designed to resist a lateral wind load of 300 pounds per foot of span; 150 pounds of this to be treated as a moving load.

The top lateral bracing is to be designed to resist a lateral wind force of 150 pounds per foot of span.

The timber to be used in the bridge is to be Douglas fir.

The unit stresses used for timber are those of the American Railway Engineering Association.

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Some of the metallogenic provinces of the southwestern United States and northern Mexico are defined by the geographic distribution of trace elements in the primary sulfide minerals chalcopyrite and sphalerite. The elements investigated include antimony, arsenic, bismuth, cadmium, cobalt, gallium, germanium, indium, manganese, molybdenum, nickel, silver, tellurium, thallium, and tin. Of these elements, cobalt, gallium, germanium, indium, nickel, silver, and tin exhibit the best defined geographic distribution.

The data indicate that chalcopyrite is the preferred host for tin and perhaps molybdenum; sphalerite is the preferred host for cadmium, gallium, germanium, indium, and manganese; galena is the preferred host for antimony, bismuth, silver, tellurium, and thallium; and pyrite is the preferred host for cobalt, nickel, and perhaps arsenic. With respect to the two minerals chalcopyrite and sphalerite, antimony, arsenic, molybdenum, nickel, silver, and tin prefer chalcopyrite; and bismuth, cadmium, cobalt, gallium, germanium, indium, manganese, and thallium prefer sphalerite. This distribution probably is the result of the interaction of several factors, among which are these: the various radii of the elements, the association due to chemical similarities of the major and trace elements, and the degree of ionic versus covalent and metallic character of the metal-sulfur bonds in chalcopyrite and sphalerite. The type of deposit, according to a temperature classification, appears to be of minor importance in determining the trace element content of chalcopyrite and sphalerite.

A preliminary investigation of large single crystals of sphalerite and chalcopyrite indicates that the distribution within a single crystal of some elements such as cadmium in sphalerite and indium and silver in chalcopyrite is relatively uniform, whereas the distribution of some other elements such as cobalt and manganese in sphalerite is somewhat less uniform and the distribution of tin in sphalerite is extremely erratic. The variations in trace element content probably are due largely to variations in the composition of the fluids during the growth of the crystals, but the erratic behavior of tin in sphalerite perhaps is related to the presence of numerous cavities and inclusions in the crystal studied.

Maps of the geographic distribution of trace elements in chalcopyrite and sphalerite exhibit three main belts of greater than average trace element content, which are called the Eastern, Central, and Western belts. These belts are consistent in trend and position with a beltlike distribution of copper, gold, lead, zinc, silver, and tungsten deposits and with most of the major tectonic features. However, there appear to be no definite time relationships, for as many as four metallogenic epochs, from Precambrian to late Tertiary, are represented by ore deposits within the Central belt.

The evidence suggests that the beltlike features have a deep seated origin, perhaps in the sub-crust or outer parts of the mantle, and that the deposits within each belt might be genetically related through a beltlike compositional heterogeneity in the source regions of the ores. Hence, the belts are regarded as metallogenic provinces.

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Bassenthwaite (Lake) is one of the larger Cumbrian lakes, certainly one of the most distinctive, and of considerable conservation and amenity value. Although its shores lack sizeable settlements, its main inflow receives sewage effluent from a major tourist centre (Keswick) and is subject to episodic floods. These influences, the growing development of leisure activities at the lake (e.g. sailing, time-share units), and recent road-construction, have led to past appraisals of ecological impacts and lake management. The lake has not been the subject of intense and long-term ecological study, but much scattered information exists that is relevant to future management decisions. In the present Report, commissioned by North West Water, such information - published and unpublished - is surveyed. Especial attention is given to evidence bearing on susceptibility to change, affecting the lake environment and its biota or species of conservation interest. Extensive use has been made of the results of a recent (1986-7) seasonal survey by the FBA.

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Bassenthwaite (Lake) is one of the larger Cumbrian lakes, certainly one of the most distinctive, and of considerable conservation and amenity value. Although its shores lack sizeable settlements, its main inflow receives sewage effluent from a major tourist centre (Keswick) and is subject to episodic floods. These influences, the growing development of leisure activities at the lake (e.g. sailing, time-share units), and recent road-construction, have led to past appraisals of ecological impacts and lake management. The lake has not been the subject of intense and long-term ecological study, but much scattered information exists that is relevant to future management decisions. In the present Report, commissioned by North West Water, such information - published and unpublished - is surveyed. Especial attention is given to evidence bearing on susceptibility to change, affecting the lake environment and its biota or species of conservation interest. Extensive use has been made of the results of a recent (1986-7) seasonal survey by the FBA.

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[ES]La adaptación de la Universidad Española al Espacio Europeo de Educación Superior (EEES) ha supuesto un cambio en los estudios universitarios que se advierte en su estructura (títulos de grado de cuatro años,) y que debe manifestarse también en las metodologías utilizadas. En los estudios de Magisterio la nueva ordenación de las enseñanzas ha supuesto la unificación de las anteriores especialidades en dos títulos de grado: Maestro de Educación Infantil y Maestro de Educación Primaria. En estos nuevos títulos las Prácticas de Enseñanza continúan teniendo un importante papel y constituyen un momento privilegiado de integración entre la teoría y la realidad de las aulas. El Practicum es el conjunto de actividades en las que diversas instituciones colaboran con la Escuela Universitaria de Magisterio, a fin de poner al alumnado en contacto con el mundo profesional. Supone la inmersión de los estudiantes en centros educativos con la finalidad de conocerlos directamente, integrar conocimientos teórico-prácticos, y adquirir competencias profesionales en todos los ámbitos de actuación.

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This report describes the general background to the project, defines the stations from which data sets have been obtained and lists the available data. The project had the following aims: To develop a more accurate and less labour-intensive system for the collection and processing of water temperature data from a number of stations within a stream/river system, and to use the River North Tyne downstream of the Kielder impoundment as a test bed for the system. This should yield useful information on the effects of impoundment upon downstream water temperatures.

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[ES]El Módulo de Practicum se organiza en dos materias: Prácticas escolares (38 créditos ECTS), y Trabajo fin de grado (12 créditos ECTS). Las prácticas escolares se realizarán en los dos ciclos de Educación Infantil (0-3, 3-6) y en los tres de Primaria (1ª-2º, 3º-4º, 5º-6º). Al tratarse de un Practicum progresivo, los estudiantes de los grados de Magisterio cursan la materia a lo largo del segundo, tercer y cuarto curso (Practicum I, Practicum II y Practicum III) con contenidos que tienen continuidad y que suponen un nivel de competencia superior respecto el anterior. El Practicum supone para el alumnado una oportunidad de adquirir e integrar las habilidades, los conocimientos, las competencias y la práctica necesarios para el ejercicio de su profesión, así como una ocasión para reflexionar de forma individual y grupal acerca del aprendizaje realizado. El Practicum I pretende que el alumnado establezca un primer contacto como futuros profesionales con un centro escolar, y realice una observación de carácter global, integrando los conocimientos aprendidos en la Escuela de Magisterio, ajustándolos a la diversidad del aula, a la escuela y al entorno social de ésta, y dedicando una especial atención al tratamiento de género. El Practicum II, al que se refiere esta guía, corresponde al tercer curso y se centra en el desarrollo docente de experiencias de enseñanza y aprendizaje con alumnado de la etapa, la implicación en la vida del ciclo y etapa y el ejercicio de la autocrítica y la reflexión en relación al propio desarrollo formativo y profesional. Se pretende que los estudiantes reflexionen de forma crítica sobre su conocimiento práctico inicial puesto en acción en esos contextos y sobre las condiciones que determinan su forma de pensar y actuar. El Practicum III está relacionado con las menciones (minor) y con la participación en proyectos de innovación.

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[ES]Las Prácticas Escolares se realizarán en los dos ciclos de Educación Infantil (0-3, 3-6) y en los tres de Educación Primaria (1º-2º, 3º-4º, 5º-6º). Al tratarse de un Prácticum progresivo, cada estudiante cursa la materia a lo largo del segundo, tercer y cuarto curso (Prácticum I, Prácticum II y Prácticum III) con contenidos que tienen continuidad y que suponen un nivel de competencia superior respecto el anterior. Además, el alumnado que en 4º curso se matricule en el minor de Educación Física deberá realizar su periodo de prácticas junto a una maestra o maestro especialista en esta materia, quien tutorizará sus prácticas. El Prácticum supone para el alumnado una oportunidad de adquirir e integrar las habilidades, los conocimientos, las competencias y la práctica necesarios para el ejercicio de su profesión, así como una ocasión para reflexionar de forma individual y grupal acerca del aprendizaje realizado y de la práctica llevada a cabo.

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On the basis of the space-time Wigner distribution function (STWDF), we use the matrix formalism to study the propagation laws for the intensity moments of quasi-monochromatic and polychromatic pulsed paraxial beams. The advantages of this approach are reviewed. Also, a least-squares fitting method for interpreting the physical meaning of the effective curvature matrix is described by means of the STWDF. Then the concept is extended to the higher-order situation, and what me believe is a novel technique for characterizing the beam phase is presented. (C) 1999 Optical Society of America [S0740-3232(99)001009-1].

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We demonstrate that it is possible to reduce the focal spot size by inserting a uniform nonlinear thin film at the aperture of a focusing lens. The reduction of spot size is tunable by adjusting the incoming laser power. In comparison with the original diffraction spot, the transverse spot size can be reduced 0.65 times. The nonlinear thin film acts effectively as a Toraldo filter, and the phase and amplitude modulation stems from the laser-induced variances in the transmission of the thin film. The proposed technique removes the need of fabricating annular pupil filters. (C) 2008 Optical Society of America.

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Introducción: La depresión representa una alta carga para la sociedad afectando a 121 millones de personas en el mundo, convirtiéndose en la tercera causa de carga mundial de morbilidad entre todas las enfermedades. En el campo de la enfermería las tasas de depresión son aun menos prometedoras. Diversos estudios a nivel internacional han considerado a la enfermería como una profesión con altas prevalencias en trastornos depresivos dando lugar a un efecto negativo sobre la fuerza de trabajo en el sector sanitario. Factores como los turnos rotatorios, mal ambiente laboral, bajo de nivel de autonomía o estar soltero o divorciado son algunos de los muchos agentes que aumentan el riesgo de padecer depresión. Objetivos: Aunque la depresión ha sido ampliamente estudiada, en la literatura actual los estudios realizados entre la depresión y la enfermería son relativamente escasos. Por lo tanto, el presente estudio será un esfuerzo para abordar esta cuestión y tendrá un doble propósito: determinar los niveles de depresión existentes entre las enfermeras del Servicio de Urgencias y de Cirugía General del Hospital de Galdakao y comparar los niveles de depresión entre las unidades anteriormente citadas. Metodología: Para ello se realizará un estudio descriptivo observacional de prevalencia. La población a estudio estará formada por los profesionales de enfermería que trabajan en las unidades de Urgencias y Cirugía General del Hospital de Galdakao. El instrumento que se utilizara para la recogida de datos será el Inventario de Depresión Beck (BDI) y el análisis estadístico se llevará a cabo mediante el programa informático SPSS.

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O principal objetivo deste trabalho foi à realização de um estudo geológico sobre os folhelhos fraturados da Formação Candeias que ocorrem em diferentes partes da Bacia do Recôncavo, sendo enfatizadas suas principais relações com a acumulação de petróleo. Este trabalho contempla, ainda, uma revisão bibliográfica acerca da evolução da campanha exploratória nesta bacia, desde seus primórdios, na década de trinta, além de uma análise sob as perspectivas na área de exploração e produção. A Bacia do Recôncavo, situada na região Nordeste do Brasil, está inserida numa grande bacia tafrogênica (Rifte abortado Recôncavo-Tucano-Jatobá), originada nos momentos iniciais de ruptura do paleocontinente Gondwana ocidental, no Eocretáceo, sob os campos de tensões que produziram o Oceano Atlântico. Em termos estratigráficos, a bacia guarda um importante registro geológico, compreendido por depósitos continentais (lacustres, fluvio-deltáicos, neríticos, eólicos e leques aluviais), sendo subdividido em seis seqüências sedimentares, referentes aos estágios pré-rifte e rifte. As principais acumulações de petróleo na bacia podem ser agrupadas em três grandes sistemas: pré-rifte, rifte-Candeias e rifte-Ilhas, representando plays exploratórios distintos. As perspectivas futuras para a Bacia do Recôncavo devem considerar a importância da identificação de novos plays exploratórios, através da caracterização de novos intervalos geradores e reservatórios, como é o caso dos folhelhos fraturados e do shale gas. Não menos importante é o desenvolvimento de novas técnicas de produção, aumentando o fator de recuperação de campos produtores.