2/12/2023 0 Comments Tecdoc 2013.2 insall![]() The first one is affected by the artesian well and it is not evaporated and it has high salinity. Its strong salinity is due to the dissolution and the lixiviation of the geological formation (ii) the Turonian, the Senonian and the Quaternary aquifers are not confined, and their stable isotope contents more or less important as the tritium, signifying that they receive recent recharge. The results show that (i) the stable isotope from the Infracenomanian is very poor and they are without tritium, confirming the fact that this aquifer is confined and it is not evaporated. The samples were collected once every 3 months from artesian groundwater of “the Infracenomanian” (4), the Turonian (4), the Senonian (1) and the Quaternary aquifer (5) and from the precipitation of the years 2001, 20. In the study area, a network of 20 water points has been the focus of the isotope analysis (δ 18O, δ 2H, 3H and 14C) and physical chemistry. Present study on the sustainable use of saline land and saline groundwater for agricultural production has been conducted in the pre-Saharian area of Ain El Atti through the application of environmental isotopes supported by the hydrochemistry.
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