Impact of the Grand Ethiopian Renaissance Dam (GERD) on Gezira Groundwater, Sudan Abbas M. Sharaky, Hossam Eliwa, and Alaa Kassem Contents 1 Introduction 2 Material and Methods 2.1 Normalized Difference Vegetation Index (NDVI) 2.2 Stable Isotope Analysis 3 Climate Conditions 3.1 Precipitation 3.2 Temperature 3.3 Relative Humidity 4 Geological Setting 4.1 Basement Complex 4.2 Nubian Sandstone Formation 4.3 Gezira Formation 4.4 Recent Superficial Deposits 5 Hydrology and Hydrogeology 5.1 Surface Water 5.2 Groundwater Occurrence 6 Piezometric Characteristics of the Aquifer System 7 Physicochemical Parameters of Groundwater 7.1 Temperature (T) 7.2 pH Value 7.3 Total Dissolved Solids (TDS) 7.4 Total Hardness 7.5 Major Cations 7.6 Major Anions + 7.7 Ammonium (NH4 ) 7.8 Heavy Metals 7.9 Suitability of Groundwater for Different Purposes 7.10 Sodium Adsorption Ratio (SAR) 7.11 Soluble Sodium Percentage (SSP) A.M. Sharaky (*) and A. Kassem Department of Natural Resources, Institute of African Research and Studies, Cairo University, Giza, Egypt e-mail:
[email protected];
[email protected] H. Eliwa National Authority for Remote Sensing & Space Sciences, Cairo, Egypt A.M. Negm and S. Abdel-Fattah (eds.), Grand Ethiopian Renaissance Dam Versus Aswan High Dam, Hdb Env Chem, DOI 10.1007/698_2017_187, © Springer International Publishing AG 2017 1 A.M. Sharaky et al. 8 Impact of Land Use/Land Cover Changes on the Water Quality 8.1 Normalized Difference Vegetation Index (NDVI) 8.2 Land Use/Land Cover (LU/LC) Classification 9 Stable Isotopes of δ2H and δ18O 10 Summary and Conclusions 11 Recommendations References Abstract The Gezira area has one of the most massive agricultural projects in the world.