Contribution des isotopes de l’environnement pour la comprehension du fonctionnement de l’aquifere mio-plioquaternaire du Haouz de Marrakech (Maroc)

Abstract

The study area «Haouz plain» is Located at the center of Morocco, it extend on a surface of 2800 km2, limited by the Jbilet hills in the North, the High-Atlas range in the South, R' dat wadi in the East and the Essaouira-Chichaoua plateau in the West. The area climate is semi-arid, characterized by low precipitations varying between 160 mm/year and 250mm/year and important variation in temperature between the winter and the summer with respectively 5°C and 45°C. Its hydrographic network is represented by the Tensift system which receives all the affluents of central and Westem Haouz. These affluents are characterized by weak flows with important seasonal variations. The Haouz plain is a sedimentary basin, being along the northern edge of the high atlas, it presents a geologic succession going from the primary to the recent Quaternary. The mio-plioquatemary formations, stemming from the dismantling of the atlasic chain, refuge an important and generalized water table on al1 the plain. This water table shows very variable hydrodynarnic characteristics, reflecting the complexity of the deep structures of the plain, 1986) and also the lithological variability of the mio-plioquatemary formations. The Haouz plain includes also the deep resemoirs of the Jurassic, Cretaceous and Eocene which finish some meters at the north of the Atlas, thus having a very limited extension and thereafter a low productivity. Five representative samples of water taken on the haouz water table were analyzed by the ABHT, the projection of these contents on the potability diagram enabled us to show that water of the water table generally has a good quality to passable. In the east quality becomes poor related to the existence of a zone arranged for agriculture (piezometer 1903/44). The nastiest potability is obsemed on the piezometer 3828/44 located at north of Marrakech at elazouzia zone of spreading of wom water of this city. The representation of the percentages of anions and major cations shows the prevalence of ions Ca2+ and HCO; and makes it possible to show up the Bicarbonate calcic facies of the water table. During these last decades, the use of stable isotopes, such oxygen 18 and deuterium, became necessary for the study of subsoil waters, it makes possible the estimation of the surfaces of refills, the determination of water origin. The samples taken on water points well distributed in the area of study allowed us a better comprehension of the function of the plioquatemary water table. The relation oxygen 18, deuterium shows that water is aligned on a line of slope 8.09, slightly different from the world meteoric line, thus characterizing precipitations of oceanic origin which did not endure notable isotopic fractionation therefore not important evaporation. Using the isotopic measures for the sarnples taken in January 2002 on wells well distributed in the area of study, allows us to show a variation of the contents of 018 with the altitude of the zones of refill. Thus we could delimit the surfaces of refill between 1500 and 800meters height. The relation oxygen-18 deuterium (δ2H = 8,9032 δ18O + 14,214 (R2 = 0,7449 ) translated an Atlantic mode of precipitations without remarkable evaporation.