Alabdin, , shhabaz Zain, H., Abdullah Salih, S., Z. Khorshid, S. (2014). Study of the aquifer nature in study area basin between Tuz Khurmato and Ber ahmmad villege using Vertical Electrical Sounding (VES). Alustath, 19(6), 150-163.
Alabdin; Hasan shhabaz Zain; Sabbar Abdullah Salih; Salman Z. Khorshid. "Study of the aquifer nature in study area basin between Tuz Khurmato and Ber ahmmad villege using Vertical Electrical Sounding (VES)". Alustath, 19, 6, 2014, 150-163.
Alabdin, , shhabaz Zain, H., Abdullah Salih, S., Z. Khorshid, S. (2014). 'Study of the aquifer nature in study area basin between Tuz Khurmato and Ber ahmmad villege using Vertical Electrical Sounding (VES)', Alustath, 19(6), pp. 150-163.
Alabdin, , shhabaz Zain, H., Abdullah Salih, S., Z. Khorshid, S. Study of the aquifer nature in study area basin between Tuz Khurmato and Ber ahmmad villege using Vertical Electrical Sounding (VES). Alustath, 2014; 19(6): 150-163.

Study of the aquifer nature in study area basin between Tuz Khurmato and Ber ahmmad villege using Vertical Electrical Sounding (VES)

Tikrit Journal of Pure Science
Article 1, Volume 19, Issue 6, December 2014, Pages 150-163
Authors
; Hasan shhabaz Zain; Sabbar Abdullah Salih; Salman Z. Khorshid
Abstract
Abstract
The studied area comprises (311km² ) within Salahaddin Governorate between Tuz Khurmato East and Tikrit
West between (448000 – 468000) East and (3870000– 3845000) North, The current study includes applying the
vertical electric sounding (VES) by using Schlumberger configuration, the measurements of apparent resistivity
measured in (25)VES points in located area, along four electric profiles, The apparent resistivity curves of field
data were drawn and interpreted qualitatively. The nature of the curves are grouped into twelve categories, Then
the curves were interpreted quantitatively by Auxiliary point method using Ebret method to find out the values of
quantitative resistivity and thickness of the electrical zones. After that, the sounding curves were interpreted
automatically by the computer program using (IPI2win) applying the Inverse interpretation method. The
estimated values of Transmissivity (T) in aquifer by using pumping tset results in (4) wells within study area
which is near of VES point while hydraulic conductivity (K) values of aquifer has been found from
Transmissivity (T) values of aquifer, the movement of direct ground water was limited in study area which was
from( north - east) to (south – west). Many empirical relations have been put between the geoelectrical
parameters, and the Hydraulic parameters, and using estimated Transmissivity (T) and hydraulic conductivity
(K) can be estimated from resistivity(p) or transverse resistivity (pt) relations or any extracted relations in this
study can be applied .
Keywords: VES , Apparent resistivity , Groundwater , Hydrogeologic characters , Geoelectrical sections
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