4.6 Article

The influence of dredging on estuarine hydrodynamics: Historical evolution of the Santos estuarine system, Brazil

Journal

ESTUARINE COASTAL AND SHELF SCIENCE
Volume 279, Issue -, Pages -

Publisher

ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
DOI: 10.1016/j.ecss.2022.108131

Keywords

Channel deepening; Tidal propagation; Numerical modelling

Funding

  1. Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [2011/50581-4]
  2. Office of Naval Research Global [N62909-14-1-N238]
  3. Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES) [001]
  4. Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)

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This study investigates the impact of deepening navigation channels by dredging on estuarine hydrodynamics in the Santos estuarine system (SES) in Brazil. The results show that the gradual deepening of the channels resulted in changes in tidal propagation, stratification of the water column, and transport of water and materials through the channels. It also led to increased saline intrusion, decreased water volume transported through the Santos channel, and an increased influence of tides in the system.
We assess changes in estuarine hydrodynamics due to the deepening of navigation channels by dredging. A validated numerical hydrodynamic model (Delft3D) was used to analyze scenarios (historical bathymetry data from 1876 to 2014) and applied to assess the hydrodynamic evolution of the Santos estuarine system (SES), Brazil. During the studied period, the SES underwent significant morphological changes, mainly related to the dredging of the Santos harbor navigation channel. The unprecedented results of the hydrodynamic evolution of the SES show that the gradual process of deepening the channels by dredging resulted in modified estuarine circulation parameters such as tidal propagation and stratification of the water column, as well as the residual water and materials transport through the SES channels. Channel deepening resulted in greater saline intrusion, a decrease in the volume of water transported through the Santos channel, an increase in the influence of the tide in the system and an increase in its asymmetry over the years in the upper estuary.

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