Caracterização macro e micromorfológica do solo para compreensão de processos erosivos lineares, topossequência Manacá, São Carlos - SP

A presente pesquisa tem como objetivo compreender a dinâmica de comportamento do solo sob escala macro e micromorfológica visualizados em topossequência, no que concerne aos agentes morfológicos que condicionam e contribuem para deflagração de processos erosivos. A área de estudo está inserida na sub-bacia hidrográfica do Laranja Azeda localizada na região centro-leste do estado de São Paulo, no município de São Carlos/SP, e têm fundamental importância por pertencer à bacia hidrográfica do Ribeirão Feijão, importante manancial urbano para a cidade. O planejamento de uso e ocupação adequados aos fatores físicos que compõe a dinâmica desta paisagem são essenciais visando a conservação e preservação dos recursos hídricos ali existentes, onde a expressiva ocorrência de processos erosivos são objetos de preocupação, já que estes podem causar assoreamento de rios e reservatórios. Utilizando uma metodologia multiescalar para seleção da área de pesquisa em detalhe e compreensão da organização e dinâmica da cobertura pedológica, foram utilizados os procedimentos propostos pela Análise Estrutural da Cobertura Pedológica e conceitos e técnicas da micromorfologia de solos. Verifica-se que a distribuição dos solos na Topossequência Manacá está estritamente correlacionada à transformação vertical do materialde origem em solo, em cuja vertente existe uma diferenciação litológica que condiciona a morfologia diferenciada, tanto em escala macromorfológica quanto micromorfológica. O terço superior e médio da vertente está associado à depósitos colúvio-eluvionaresda Formação Itaqueri, onde desenvolve-se um Latossolo Vermelho Amarelo. Já o terço inferior da vertente corresponde a um solo formado a partir dos arenitos da Formação Botucatu, sendo enquadrado enquanto Neossolo Quartzarênico. Com o auxílio técnicas de análise bidimensional de imagens retiradas das lâminas delgadas de solo, foi possível visualizar e quantificar a macroposidade ao longo da vertente, importante atributo morfológico que controla os fluxos de água e são agentes condicionantes para o desenvolvimento de processos erosivos. Conclui-se que a ocorrência de voçorocas no terço médio inferior da vertente é a materialização em forma de processos erosivos deste comportamento diferencial da massa do solo, onde portanto, na Topossequência Manacá a busca de equilíbrio dinâmico na vertente é induzida pela dinâmica genética evolutiva das formações geológicas que sustentam a paisagem, desencadeada em processos erosivos que tendem a progredir em desequilíbrio, a depender do manejo estabelecido para o local.

Raluca L. Radulescu and Cory James Rushton, eds. 2009: A Companion to Medieval Popular Romance. Studies in Medieval Romance 10. Cambridge: D. S. Brewer. XIV + 209 pp. ISBN 9781843841920

This review is part of a research project funded by the Spanish Ministry of Science and Innovation (ref. FFI 2008-02165).

Ni bueno, ni bonito, ni barato. El problema de la simplificación de la naturaleza

Modern society has lost its natural connection with the environment. Present agriculture methods and city planning around the world support this fact. Humanity has always simplified nature in order to control it but, far from this, we have contributed to enhance current environmental issues as air and water pollution, soil fertility loss, species extinction and climate change. Therefore, it may be reasonable to change our point of view of nature. By assuming that we are an inseparable part of nature and vice versa, we may achieve a true conservation of the richness of our planet. We must synthesise nature because every living being is a part of a bigger whole. We need to live the complexity of life. Nowadays, we have reached a turning point after which we must decide either changing our ways or sacrificing our future. Hopefully, a slight impulse is sometimes enough to change the course of History.

Los planos del concurso para la ciudad de vacaciones Playa de San Juan en 1933

En 1933 se celebra el concurso de anteproyectos para la primera ciudad turística de España. Las bases de la convocatoria exigían una extensa documentación: planes, planos y perspectivas. El análisis de la propuesta vencedora —muy sensible a las preexistencias— pone de relieve la secuencia que liga la geografía con la ordenación urbana gracias al pensamiento y a las herramientas gráficas. Primero, se dibuja el territorio levantando acta del mismo recurriendo a los diagramas. Segundo, los datos y las vocaciones del suelo se transforman en una trama urbana zonificada en el espacio y programada en el tiempo. Y tercero, la fotografía del paisaje sugiere los enclaves panorámicos y algunas de las arquitecturas clave. En este hito de la planificación se dan cita las modernas técnicas gráficas y fotográficas que interactúan con el urbanismo moderno del zoning.

Proposed Parks and Parkways, Boston, Massachusetts, 1876 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Proposed parks and parkways. It was published by Park Dept., City of Boston in 1876. Scale [ca. 1:25,000]. Covers also parts of adjacent towns and cities, including all of Cambridge, Somerville, and Brookline.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Massachusetts State Plane Coordinate System, Mainland Zone (in Feet) (Fipszone 2001) 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, proposed parks, parkways, and roads, public grounds, sewer lines, railroad stations, radial distances from City Hall, and more.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.

Washington, D.C., 1791 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Plan of the city intended for the permanent seat of the government of t[he] United States : projected agreeable to the direction of the President of the United States, in pursuance of an act of Congress passed the sixteenth day of July, MDCCXC, "establishing the permanent seat on the bank of the Potowmac", by Peter Charles L'Enfant. It was published by U.S. Coast and Geodetic Survey in 1887. Scale ca. 1:15,840. Facsimile of L'Enfant's 1791 plan for Washington, D.C. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Maryland State Plane Coordinate System Meters NAD83 (Fipszone 1900). 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 proposed streets and government building locations, drainage, parks, and more. Includes notes, text, statistical data, and index to points of interest. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Washington, D.C., 1792 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Plan of the city of Washington in the territory of Columbia : ceded by the states of Virginia and Maryland to the United States of America, and by them established as the seat of their government, after the year MDCCC, engrav'd by Sam'l Hill, Boston ; in order to execute this plan, Mr. Ellicott drew a true meridional line. Andrew Ellicott plan of Washington, D.C. It was published in 1792. Scale [ca. 1:19,800]. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Maryland State Plane Coordinate System Meters NAD83 (Fipszone 1900). 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, block numbers and proposed government buildings, drainage, and more. Relief is shown by hachures. Depths shown by soundings. Includes text and notes. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.