Etude de l'hydrodunamique sédimentaire de la lagune de Bizerte

Authors

  • Mouldi BRAHIM Université de Carthage. Institut National des Sciences et Technologies de la Mer. Laboratoire du Milieu Marin. Tunisie
  • Bechir BEJAOUI Université de Carthage. Institut National des Sciences et Technologies de la Mer. Laboratoire du Milieu Marin. Tunis
  • A. ATOUI Université de Carthage. Institut National des Sciences et Technologies de la Mer. Laboratoire du Milieu Marin. Tunisie. Tunisie

Keywords:

Surveys, Sediment analysis, Sediment dynamics, Erosion, Hydrodynamic, Particle Size, Lagoons, Wind, Sediments, Marine, MED, Tunisia, Bizerte lagoon

Abstract

The results of the grain size analysis of the sediments of surface of the lagoon of Bizerte, taken with various depths, made it possible to identify the nature of its sediments and to specify the factors and the phenomena which intervene in their transport and their deposit. The sedimentological study showed that the detrital materials of continental origin and the sediments coming from the coastal erosion are subjected to a dynamics which is controlled primarily by the action of the currents due primarily to the winds.

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Published

2008-03-25

How to Cite

1.
BRAHIM M, BEJAOUI B, ATOUI A. Etude de l’hydrodunamique sédimentaire de la lagune de Bizerte. Bull. Inst. Natl. Sci. Technol. Mer [Internet]. 2008Mar.25 [cited 2024Apr.29];35:149-60. Available from: https://www.instm-bulletin.tn/index.php/bulletin/article/view/616

Issue

Vol. 35 (2008)

Section

Article

ARK

https://n2t.net/ark:/68747/INSTM.Bulletin.v35.616

License

Creative Commons License

This work is licensed under a Creative Commons Attribution 4.0 International License.

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