Distribution and environmental geochemistry of some heavy metals in stream sediments of Wadi Allaqi, South Eastern Desert of Egypt

The study focuses on the lateral distribution and the environmental geochemistry of seven heavy metals: Fe, Mn, Cu, Co, Ni, Pb, and Zn in addition to Al in the stream sediments of Wadi Allaqi. Forty-two samples were collected from the upstream, the midstream, and the downstream of this Wadi. Results of the grain size analysis show that the sediments of Wadi Allaqi are fine to medium sand. The heavy metals content reflects the weathering impact on the hinterland. The highest concentrations of Fe, Al, Mn, Cu, Pb, and Zn are recorded in the midstream that is dominated by clastics of felsic and intermediate composition. Moreover, the downstream, occupied by ultrabasic–basic rocks, shows the highest averages of Co and Ni. These results suggest that the felsic and intermediate rocks are the main source of the former metals, whereas the ultrabasic–basic rocks are the source of later two metals. All the analyzed heavy metals have average concentrations lower than their backgrounds, except for Co and Pb. The pollution level by these heavy metals has been evaluated using enrichment ratio (ER), pollution load index (PLI), and index of geoaccumulation (Igeo). The calculated values of ER, CF, PLI, and Igeo indicate that Wadi Allaqi sediments are almost pristine except occasional feeble pollution level by Co and Pb.