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Geo-electric survey was applied to estimate water depth at the four selected points.
From geo-electric survey, Figs. 6 and 7 revealed that there are four layers.
Water depth distribution map in the study site was constructed using water depth collected from geo-electric survey (Table 1).
Although the measured depth to water is slightly different from that estimated from geo-electric survey, the expected flow net map gives consistent hydrological information about groundwater flow direction in the site.
The expected flow net map (Figs. 11, 12) was constructed based on data collected from the suggested methodology (Table 1), where the water level was calculated from depth to water estimated from geo-electric survey and elevations of points above sea level obtained from digital elevations from Google Earth with GPS (longitude, latitude) coordinates.
Although Todd (2005) suggested that surface geo-electric survey could not give an accurate water surface, many authors such as Nigm (2013), Sabet (1975) and Douglas (2013) indicated that inferred depth of water from resistivity survey could be consistent with the values measured in boreholes.
Open image in new window Fig. 11 Expected flow net map constructed using estimated water depth from geo-electric survey data from Table 1 Open image in new window Fig. 12 Actual flow net map from measured water depth in four boreholes.
I stood, awake in electric sight, performing a yellow-eyed survey of the day's odd revelations that brought me still closer to Steve Jobs.
An Electric resistivity survey was carried out to examine the distribution of weakness zones.
Open image in new window Fig. 8 Results of the electric resistivity survey.
Using the electric resistivity survey, it was discovered that the low resistivity zone is related to the tectonic zone and the characteristics of the strata.
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