• Corpus ID: 53655451

Interpretation of Hydro Deep Aquifers in parts of Port Harcourt , Eastern Niger

@inproceedings{Nwankwoala2013InterpretationOH,
  title={Interpretation of Hydro Deep Aquifers in parts of Port Harcourt , Eastern Niger},
  author={H. O. Nwankwoala},
  year={2013}
}

• H. Nwankwoala
• Published 2013
• Geology

-geochemical characteristics of deep boreholes i StatistiXL 1.5 which is an add-in to Microsoft Excel, -chemical variables that would otherwise not -way analysis of variance and further plots of group means -chemical parameters for the deep boreholes show the following – 7.72), EC (350.60 – 618.20μS/cm), TDS (122.70 – 36.00mg/l), Cl (115.00 – 410.00mg/l), Eh (123.22 /l), Salinity (12.00 – 355.00mg/l), NO3 (0.201 – 6.300mg/l), HCO + (0.834 – 3.400mg/l), Mg 2+ (0.445 – 5.677mg/l), K 2+ (0.011 – 0.727mg/l), F (0.411 – 2.310mg/l), SiO – 0.06mg/l) and Br (12.50 – 79.70mg/l). corded (2.50 EC, TDS, salinity as well as chloride contents in -freshwater interface should be delineated -chemical properties of -hoc structure detection of group means 22.30), Cl (300.00) and EC (513. elation to the dynamic movement of freshwater), resulted in the presence of relict saline components in the -geochemistry, saltwater intrusion, contamination. ----------------------------------