Estudo das camadas de lama fluida em portos e canais de navegação

Detalhes bibliográficos
Ano de defesa: 2018
Autor(a) principal: Carneiro, Juliane Castro
Orientador(a): Não Informado pela instituição
Banca de defesa: Não Informado pela instituição
Tipo de documento: Tese
Tipo de acesso: Acesso aberto
Idioma: por
Instituição de defesa: Universidade Federal do Rio de Janeiro
Brasil
Instituto Alberto Luiz Coimbra de Pós-Graduação e Pesquisa de Engenharia
Programa de Pós-Graduação em Engenharia Oceânica
UFRJ
Programa de Pós-Graduação: Não Informado pela instituição
Departamento: Não Informado pela instituição
País: Não Informado pela instituição
Palavras-chave em Português:
Link de acesso: http://hdl.handle.net/11422/12564
Resumo: Many ports and navigation channels around the world suffer from silting and the presence of fluid mud layers and this continuous mud deposition can cause reductions in nautical depth. In this context, the existence of fluid mud layers makes the definition of the bottom location ambiguous because the location of interfaces between water, fluid mud and consolidated mud is dynamic and difficult to identify. The present work presents an integrated approach to the study of the fluid mud layers in different port regions and under controlled conditions in a laboratory column. In situ measurements were obtained with acoustic equipment, seismic, density profiles and sampling to characterize the grain size and rheology of the material. The study of the fluid mud is dependent on the rheological characteristics of the sediments, which showed the need to calibrate the methodology individually for each site to be studied. Regarding the detection of mud layers by means of echo-sounder measurements, high frequency return (HF) is associated with the water-mud interface (lutocline), and low frequency return (LF) is a more unstable signal, but correlated with changes in gradients and similar to the values of critical densities identified by the rheological transition measured in the laboratory. Regarding the measurement of the layers, specifically for the Port of Santos, the rheological tests revealed an increase in the yield stress of the samples in the internal region of the estuary. The combination of density profiles and rheological data allowed estimating a potential draft increase of 1.5 m, depending on the location, nautical depth criterion and tide condition. It is expected that the combination of detection and measurement techniques will allow the development of tools for navigation in fluid mud, with potential increase in draft for port areas for safe navigation.