Andere Kunden interessierten sich auch für
![Variation des eaux souterraines dans la ville de Mubi au nord-est du Nigeria]( "Variation des eaux souterraines dans la ville de Mubi au nord-est du Nigeria")
Variation des eaux souterraines dans la ville de Mubi au nord-est du Nigeria26,99 €![Interpolating Beach Profile Data Using Linear and Non-linear Functions]( "Interpolating Beach Profile Data Using Linear and Non-linear Functions")
Interpolating Beach Profile Data Using Linear and Non-linear Functions26,99 €![Quantitative Analysis of Morphometric Parameters of Nayra River, India]( "Quantitative Analysis of Morphometric Parameters of Nayra River, India")
Quantitative Analysis of Morphometric Parameters of Nayra River, India26,99 €![Spatio-Temporal Variation of Natural Resources of KGP]( "Spatio-Temporal Variation of Natural Resources of KGP")
Spatio-Temporal Variation of Natural Resources of KGP23,99 €![Variation in Thickness & Ash Content-Coal Seam-Ii, Barjora, Wb, India.]( "Variation in Thickness & Ash Content-Coal Seam-Ii, Barjora, Wb, India.")
Variation in Thickness & Ash Content-Coal Seam-Ii, Barjora, Wb, India.32,99 €![Field Guide to the Geology of Northeastern Oman]( "Field Guide to the Geology of Northeastern Oman")
Field Guide to the Geology of Northeastern Oman29,90 €![Archean-Mesoproterozoic Crustal Evolution and Crust-Mantle Geodynamics of Western Liaoning-Northeastern Hebei Provinces, North China Craton]( "Archean-Mesoproterozoic Crustal Evolution and Crust-Mantle Geodynamics of Western Liaoning-Northeastern Hebei Provinces, North China Craton")
Archean-Mesoproterozoic Crustal Evolution and Crust-Mantle Geodynamics of Western Liaoning-Northeastern Hebei Provinces, North China Craton74,99 €
The study discussed sixteen physico-chemical parameters from thirty three groundwater samples on two dimensional maps along east-west central profile section. The results indicates the water at some points to reflecting the geologic formations through which it travelled, its residence time and man's interaction around some sampling points. Trough-like structures of about 2 mg/L and 4 m/L separate potassium ion concentration value of above 20 mg/L at the western side from those of about 16 mg/L at the central and eastern parts. A systematical rise of sodium ions concentration from the west to the east is attributed to increased domestic activity along the same direction. The low values of nitrate ions at the central part than at the two tails of the profile, the high chromium ions above and, the low sulphate ions below the international accepted limits should be checked at the sampling points they were obtained for accuracy of the analysis and/or sources of the anomalies, so as tooffer necessary remedial measures to the communities around such water points.