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Potential Energy Power from Tidal Current in Lagoon System – The Case of Oualidia Lagoon, Morocco
 
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Ukryj
1
Marine Geosciences and Soil Science Laboratory (URAC-45), Earth Sciences Department, Faculty of Sciences, Chouaib Doukkali University, Av. des Facultés, El Jadida 24000, Morocco
 
2
Departement of Oceanography, Faculty of Fisheries and Marine Science, Diponegoro University, Jl. Prof. Sudarto No.13, Tembalang, Kec. Tembalang, Kota Semarang, Java Tengah 50275, Indonesia
 
3
Highet School of Technology [ESTE], Cadi Ayyad University, Km 9, Route d'Agadir, Essaouira Aljadida BP. 383, Ghazoua, Essaouira 44000, Morocco
 
4
Nautical Science and Naval Engineering Department, Institut Supérieur d’Etudes Maritimes, Km 7, Road El Jadida, Casablanca B.P. 20520, Morocco
 
 
Autor do korespondencji
Mohammed Bouchkara   

Marine Geosciences and Soil Science Laboratory (URAC-45), Earth Sciences Department, Faculty of Sciences, Chouaib Doukkali University, Av. des Facultés, El Jadida 24000, Morocco
 
 
Ecol. Eng. Environ. Technol. 2023; 4:116-127
 
SŁOWA KLUCZOWE
DZIEDZINY
STRESZCZENIE
The lagoon is a natural system protected from the sea by a dune barrier creating energy from the movement of rising and falling tides, thus providing a sustainable option for extracting energy from tidal currents. The energy that can be extracted is one of the most potential renewable energy sources. Therefore, the interaction of tidal currents with stratification layers has become important to optimize the efficiency of energy conversion at each depth layer in water masses. We have chosen as a case study, the Oualidia lagoon (Atlantic coast of Morocco). This ecosystem is characterized by hydrodynamics relatively favored by tides and tidal currents which are the main intra-lagoon currents, with a predominance of the semi-diurnal component M2 (period of 12 h 25) with 2.1 to 3.4m of tidal range. The Multicell Argonaut-XR ADCP is used to measure the current velocity in the Oualidia lagoon at three different stations to study tidal patterns in a vertical layer of water depth. At each station, current velocities were recorded in each 0.5 m layer over a depth of about 5 m. As a result, this study showed that current velocity measurements to be used as renewable energy are found at station 1 located at a depth of 3.5 meters (~layer 5) with a current velocity of 0. 771 m/s and a power density value of 235.344 Watt/m2, station 2 located at a depth of 3.5 meters (~layer 5) with a current velocity of 0.4 m/s and a power density value of 32.86 Watt/m2 and station 3 is located at a depth of 3 meters (~layer 6) with a current velocity of 0.527 m/s and a power density value of 75.157 Watt/m2. The variation in current velocities between the different stations is mainly influenced by tides (Flood/ebb), the period of the measurements and the location of the stations (far or near the lagoon inlets). This work presents a model for extracting electrical energy through the use of tidal and current flow variations in such semi-enclosed natural system including lagoons.
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