Fuzzy control of a swells canal system

  • Authors:
  • Taieb Ben Romdhane;Raouf Ketata;Sofiene Hermi

  • Affiliations:
  • Département de Génie Physique et Instrumentation, Institut National des Sciences Appliquées et de Technologie, Centre Urbain Nord, BP No. 676, 1080 Tunis Cedex, Tunisia;Département de Génie Physique et Instrumentation, Institut National des Sciences Appliquées et de Technologie, Centre Urbain Nord, BP No. 676, 1080 Tunis Cedex, Tunisia and Research ...;Département de Génie Physique et Instrumentation, Institut National des Sciences Appliquées et de Technologie, Centre Urbain Nord, BP No. 676, 1080 Tunis Cedex, Tunisia

  • Venue:
  • Applied Soft Computing
  • Year:
  • 2008

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Abstract

This work forms a part of the research undertaken on the maritime developments behaviour submitted to the action of sea waves. To succeed in this objective, we have conceived and achieved a system of artificial wave generation in a swells channel (channel of 37.5m of length, 1m of width and 1m of depth). Indeed, the simulation of swells on scale model has many advantages. We can mention the construction of dykes for the protection of ports, the didactic interest of conception and generation of new models of waves and the construction of boat shells. The installed canal has to achieve tests of developments stability in the domain of the maritime hydraulics. Every work or scale model is constituted of several layers of ripraps of shapes and well-determined relative density. Thus, the survey of stability consists in reproducing in similitude (scale 1/20) in the swells canal to observe their effects on the holding of riprap (accumulation of boulder) or the artificial blocks of the scale model. Otherwise, the modelling of the process of swell generation is described by complicated physical laws and requires important means of computation. To solve this problem, we have conceived a system based on fuzzy logic permitting to assure the generation of coherent command data with the statistical parameters characterizing the oceanic waves, and to guarantee its conformity to the model of Pierson Moskowich spectrum.