949 resultados para North-east India
Resumo:
The political brinkmanship of the Liberation Tigers of the Tamil Eelam has been illustrated vividly by the way in which it brought forward its proposals for an Interim Self-Governing Authority by exploiting the vulnerabilities of the United National Front Government. In the proposals the LTTE articulated its political intentions in concrete constitutional terms for the first time. The Proposals rationalize the armed struggle and a contractual agreement outside the Constitution. The plenary powers of the ISGA exceed the federal formula; effectively exclude the institutions of the state of Sri Lanka from the North-East; and clear the route for a separate state. This situation demands a redirection of the peace process which requires a clear political vision and a proper strategy with alternative proposals on the part of the government. In the face of present impasse of the peace process the challenges before the new Freedom Alliance government are formidable.
Resumo:
The bridge over the Mittellandkanal is located in the municipality of Braunschweig, a city of Low Saxony located in Mid-North Germany, between Berlin and Hannover, 50 km away from this last city. The city of Braunschwig has 248.867 inhabitants (December 2010). The orography of the zone is practically even, with some slopes in the surrounding area, with a no important variation of the ground elevation, characterized by a big uniformity and a great visual quality. In this zone the canal flows from west to east, from the Dortmundkanal until the Elbe river, so it has a length of 325,3 km. The normal flora from the zone is farmland with some little forests not very big and not very important. But the Mittellandkanal lies at the North of Brauschweig, that means that in the zone of the canal there is a change between the urban area and the rural area. For this reason in the zone of the bridge we start to find farmlands and forest, however the constructions and buildings are still present in this area. The railway line that is going to be built will unite the North-center of Germany with the North-East of Germany because some of the following factors: •Overstress of the only existing line in the moment that connects Berlin with the North-East extreme of Germany. •No direct connection with the North-Easth Germany with other important German cities from South and West of Germany. •Replacement of the old existing one way line in the area that has to be renewed. •Modernization of the old railway lines of Germany. Schedule order by the European Union and the German Government. The actual lines of the zone do not have the necessary conditions and characteristics to satisfy the demand of the travelers that want to travel all over Germany with the railway avoiding using other transports like plan or car. For these reasons the necessity of the replacement of the old railway line and the aim to create a union with the North-East Germany that has a deficit of transport infrastructures and connections with the rest of the country and Europe. Although the new railway line provokes some disadvantages when constructing it is indispensable to build this railway line. The pass of the railway line through Braunschweig has not been random. The zone Braunschweig-Wolfsburg is a very industrialized area because of some companies like Wolkswagen and too because this zone is an important pass of important line from Berlin, South and East Germany. For all of these reasons the railway line goes through Braunschweig and connects to the city of Wolfsburg first, and after the North-East Germany zone.
Resumo:
The aim of this paper is to explain the chloride concentration profiles obtained experimentally from control samples of an offshore platform after 25 years of service life. The platform is located 12 km off the coast of the Brazilian province Rio Grande do Norte, in the north-east of Brazil. The samples were extracted at different orientations and heights above mean sea level. A simple model based on Fick’s second law is considered and compared with a finite element model which takes into account transport of chloride ions by diffusion and convection. Results show that convective flows significantly affect the studied chloride penetrations. The convection velocity is obtained by fitting the finite element solution to the experimental data and seems to be directly proportional to the height above mean sea level and also seems to depend on the orientation of the face of the platform. This work shows that considering solely diffusion as transport mechanism does not allow a good prediction of the chloride profiles. Accounting for capillary suction due to moisture gradients permits a better interpretation of the material’s behaviour.
Resumo:
The aim of this paper is to explain the chloride concentration profiles obtained experimentally from control samples of an offshore platform after 25 years of service life. The platform is located 12 km off the coast of the Brazilian province Rio Grande do Norte, in the north-east of Brazil. The samples were extracted at different orientations and heights above mean sea level. A simple model based on Fick’s second law is considered and compared with a finite element model which takes into account transport of chloride ions by diffusion and convection. Results show that convective flows significantly affect the studied chloride penetrations. The convection velocity is obtained by fitting the finite element solution to the experimental data and seems to be directly proportional to the height above mean sea level and also seems to depend on the orientation of the face of the platform. This work shows that considering solely diffusion as transport mechanism does not allow a good prediction of the chloride profiles. Accounting for capillary suction due to moisture gradients permits a better interpretation of the material’s behaviour
Resumo:
El trabajo ha sido desarrollado en un agrosistema tradicional del NE de la provincia de Alicante (SE España). La superficie total del área de estudio es de aproximadamente 59.000 ha. La zona presenta grandes contrastes, con un área interior de morfología montañosa, con pequeñas cuencas dedicadas a la agricultura de secano, mientras que la zona litoral se caracteriza por un relieve menos abrupto, con núcleos de población y explotaciones agrícolas de regadío. El estudio se basa en la información extraída a partir de encuestas realizadas a los gestores cinegéticos, obteniendo datos acerca de las abundancias y la evolución de las poblaciones de jabalí entre los años 1980 y la actualidad. Se construye una base de datos SIG con un total de 15 cotos de caza. La base de datos incluye las siguientes variables: usos del suelo a nivel de coto, abundancias y evolución temporal de la especie. Los resultados muestran que dos de los cotos presentan densidades de jabalí elevadas (15-25 ind/ha), dos cotos presentan densidades medias (10-15 ind/ha), cinco cotos muestran densidades bajas (5-10 ind/ha) y otros seis cotos densidades muy bajas (0-5 ind/ha). Los valores máximos se encuentran en cotos de interior y de montaña donde todavía se mantienen en activo cultivos de secano y se intercalan con cultivos abandonados y áreas naturales. También se observan densidades elevadas en el único coto de todos los analizados que se encuentra en la costa, donde la disponibilidad de hábitat es menor y, por lo tanto, hay una mayor concentración de individuos. Finalmente, el jabalí ha aumentado sus poblaciones desde la década de los años 1980 en la totalidad de los cotos estudiados.
Resumo:
This layer is a georeferenced raster image of the historic paper map entitled: Blachford & Co.'s new chart of the coast of Brazil : from the Equator to Rio Janeiro, drawn from the surveys made by order of the Portuguese government, including those of Jose Patriceo, Manoe Pimental & several other officers in the Royal Navy. It was published by R. Blachford & Co., chart sellers to the Admiralty, and East India Compny, etc., 115 Minories in 1830. Scale [ca. 1:1,700,000]. Covers a portion of coastal Brazil.The image inside the map neatline is georeferenced to the surface of the earth and fit to the South America Lambert Conformal Conic 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 coastal features such as rocks, channels, points, ports, coves, islands, flats, bottom types, anchorage points, and more. Includes also selected land features such as towns, drainage, and more. Relief shown by hachures. Depths shown by soundings. Includes notes and insets: Harbor of Cape Frio, Rio de Janeiro, Harbor of Bahia, or St. Salvador, Fernand de Noronha, Bay of Maranham and Pernambuco. Decorated with 10 views of harbor entrances to Rio de Janeiro, Cape Frio, Bahia, etc.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.
Resumo:
This layer is a georeferenced raster image of the historic paper map entitled: Ulma memorabilis ac permunita libera Imperii Civitas ad Danubium, ubi Ilara et Blavus ei miscentur = Ulm eine considerable Freye Reichs Statt in Schwaben, wo die Flüsse Iler u. Blau in die Donau fallen, verfertigt durch Matthaeum Seutter, Seiner Kayserl. u. Königl. Cathol. Majest. Geogr. in Augspurg. It was published by Matthaeus Seutter, ca. 1740. Scale [ca. 1:4,300]. Covers Ulm, Germany. Map in Latin and German. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Deutsches Hauptdreiecksnetz (DHDN) 3-degree Gauss-Kruger Zone 3 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 roads, drainage, built-up areas and selected buildings, fortifications, ground cover, and more. Relief shown pictorially. Includes also index, text, and panorama of Ulm seen from the North East.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.
Resumo:
This layer is a georeferenced raster image of the historic paper map entitled: A new map of the East India Isles from the latest authorities, by John Cary. It was published by J. Cary, Dec. 21, 1801. Scale [ca. 1:9,000,000]. Covers Southeast Asia. The image inside the map neatline is georeferenced to the surface of the earth and fit to the World Miller Cylindrical projection. 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 by hachures. This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection as part of the Open Collections Program at Harvard University project: Islamic Heritage Project. Maps selected for the project represent a range of regions, originators, ground condition dates, scales, and purposes. The Islamic Heritage Project consists of over 100,000 digitized pages from Harvard's collections of Islamic manuscripts and published materials. Supported by Prince Alwaleed Bin Talal and developed in association with the Prince Alwaleed Bin Talal Islamic Studies Program at Harvard University.
Resumo:
This layer is a georeferenced raster image of the historic paper map entitled: The Survey Districts of North Harbour & Blueskin, Lower Harbour West, North East Valley, Upper Harbour West, Tomahawk, Sawyers Bay, Andersons Bay, Portobello Bay, Otago Peninsula & Upper Harbour East, drawn by G.P. Wilson, April 1896. It was published by N.Z. Lands and Survey in 1896. Covers the Dunedin region, New Zealand. Scale [ca. 1:63,360]. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Universal Transverse Mercator (UTM Zone 59S, meters, WGS 1984) 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 property lot and block numbers, boundaries of survey districts and blocks, boroughs, townships and estates, drainage, selected roads, railroads and stations, selected buildings and industry locations, cemeteries, shoreline features, docks and wharves, and more. Relief shown by spot heights.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.