Processamento digital de imagens destinado ao mapeamento da ocupação humana do alto Bonfim e análise histórica dos remanescentes florestais entre os anos de 1965 a 2006.

Através do processamento de imagens digitais, mais especificamente as etapas de segmentação e classificação, foi possível analisar o processo de ocupação humana da bacia hidrográfica do rio Bonfim, localizada no município de Petrópolis, no estado do Rio de Janeiro. Este processo possibilitou a geração de mapas de uso da terra e cobertura vegetal e configurou-se numa importante etapa para avaliação ambiental capaz de auxiliar e dar fomento à execução de atividades de gestão e monitoramento do meio ambiente e de análise histórica dos remanescentes florestais ao longo dos últimos anos. Nesta pesquisa foram adotadas classes temáticas com o propósito de permitir a classificação das imagens digitais na escala 1/40.000. As classes adotadas foram: afloramento rochoso e vegetação rupestre; obras e edificações; áreas agrícolas e vegetação. Estudos foram feitos no sentido de indicar o melhor método de classificação. Primeiramente, efetuou-se a classificação no sistema SPRING, testando-se os melhores parâmetros de similaridade e área na detecção de fragmentos, somente da classe vegetação. Houve tentativa de classificar as demais classes de uso diretamente pelo sistema SPRING, mas esta classificação não foi viável por apresentar conflitos em relação às classes, desta forma, neste sistema foi feita somente a classificação e quantificação da classe vegetação. Visando dar continuidade a pesquisa, optou-se por executar uma interpretação visual, através do sistema ArcGis, para todas as classes de uso do solo, possibilitando o mapeamento da dinâmica de evolução humana, diante da floresta de mata atlântica na área de estudos e análise histórica de seus remanescentes entre os anos dos anos 1965, 1975, 1994 e 2006.

Fourteenth Annual Report for the year ended 31st March, 1965

This is the fourteenth Annual report of the Cumberland River Board on information of its activities and responsibilities on river management in its area between the beginning of April 1964, to the end of March 1965. The report contains 5 main sections on water resources, land drainage, fisheries, pollution, and finally the expenditure and income for the 12 month period. The first area that the report deals with is water resources, which includes information on the completion of gauging stations, abstraction of water and rainfall and river flow. The section on land drainage looks at work on improvement schemes, floods and information on maintenance work carried out on rivers including Wampool, Waver, Wiza, Ellen, Cocker, Keekle, Marron, Ehen, Bleng, Esk, Mite, Caldew and Petteril. The fisheries section covers 5 districts of the River Eden, Esk, Derwent, Ellen and South West Cumberland. It includes angling information and a general report for salmon and sea trout, brown trout and freshwater fish. Fish disease and fish hatchery are also covered as well as Byelaws and fisheries protection. The fourth section on pollution deals with water quality and information on sewage and trade effluents. The River Boards preceded the Environment Agency which came into existence in 1996.

River Dart Scale Reading Investigation Report on the 1965 Season

This is the fourth River Dart Scale Reading Investigation Report on the 1965 season by the Devon River Board. The object of this investigation is to examine, by means of scale-reading, the general biology of the salmon population of the River Dart. It reviews the methods used for the collection of scales and examination of the materials. It shows the results of the survey and the number of scales studied from each of the various sea-age classes, time of running with distribution of the sea-age groups throughout the season, fish sizes and smolt ages at migration. All it summarized in tables, and figures are included plotting weight distributions for each age classes and frequency distributions.

River Dart fisheries survey 1965

This is the first River Dart Fisheries Survey produced by the Devon River Authority; which was carried out from May to October 1965. The objective was to examine the distribution and relative abundance of salmonid fish in the River Dart, in order to assess the possibility or desirability, of increasing salmon smolt production of the river by artificial propagation or other means. Description, chemical, pollution and biological conditions of the River Dart along with fisheries catches, water extraction and spawning are briefly cited. The method includes the choice of sections and sampling techniques. The results go through the number/type/class of fishes counted while the survey took place, distribution patterns within the different transects/brooks, competition between salmon parr and trout and estimations of population. The section on the discussion and recommendations is introduced by a brief explanation of the bases for the Artificial Propagation Programme and the River Dart specific case-study. The annexes contains River Dart and tributaries maps, fish size distribution tables and figures, tables with totals of salmonid fish found and population density tables.

River Erme Fisheries Survey 1965

This is the River Erme Fisheries Survey, 1965 by the Devon River Authority. The survey was carried out during April and May 1965, with the principal object being the determination of the abundance and distribution of salmonid fish in the River Erme in relation to the discharge from Stowford Paper Mills, Ivybridge. It contains a brief introduction of general aspects of the catchment, chemistry, pollution, biology and fisheries in the river, methodology that looks at the selected transects and techniques for sampling, results and recommendations. It contains tables with totals of all salmonid fish found at each section, size distribution of trout, surface area of section and population density.

Evolution of the tectogene concept, 1930-1965

The tectogene, or crustal downbuckle, was proposed in the early 1930s by F.A. Vening Meinesz to explain the unexpected belts of negative gravity anomalies in island arcs. He attributed the isostatic imbalance to a deep sialic root resulting from the action of subcrustal convection currents. Vening Meinesz's model was initially corroborated experimentally by P.H. Kuenen, but additional experiments by D.T. Griggs and geological analysis by H.H. Hess in the late 1930s led to substantial revision in detail. As modified, the tectogene provided a plausible model for the evolution of island arcs into alpine mountain belts for another two decades. Additional revisions became necessary in the early 1950s to accommodate the unexpected absence of sialic crust in the Caribbean and the marginal seas of the western Pacific. By 1960 the cherished analogy between island arcs and alpine mountain belts had collapsed under the weight of the detailed field investigations by Hess and his students in the Caribbean region. Hess then incorporated a highly modified form of the tectogene into his sea-floor spreading hypothesis. Ironically, this final incarnation of the concept preserved some of the weaker aspects of the 1930s original, such as the ad hoc explanation for the regular geometry of island arcs.