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Mohammed M . A L I AL-Hameedawi
  • BAGHDAD, Iraq
  • 009647702787525

Mohammed M . A L I AL-Hameedawi

  • Mohammed AL-Hameedawi was born in Baghdad city, Iraq on June 7, 1980. He graduated from Baghdad University / College of Science/ geology department in 2005 and he got his master... moreedit
The resistivity survey was carried out by using vertical electrical sounding (VES) and 2D imaging techniques in the northern Badra area, Eastern Iraq. Eleven VES points distributed on two parallel profiles and six 2D imaging stations were... more
The resistivity survey was carried out by using vertical electrical sounding (VES) and 2D imaging techniques in the northern Badra area, Eastern Iraq. Eleven VES points distributed on two parallel profiles and six 2D imaging stations were applied using long survey lines. In general, two types of aquifers are recognized in the study area. The first is the Quaternary aquifer, which appears in all geological sections and inverse model of 2D imaging stations (2DS).This aquifer can be divided into upper and lower aquifers as shown in (2DS1), (2DS3), and (2DS4). Generally, the thickness of this aquifer ranges between (30-200 m) which occurs at a depth of (10-30m) according to geological sections, while its thickness ranges between (35-180m) and occurs at depth (10-45m) according to the inverse model of 2D imaging stations. The second is the AL-Mukdadiya aquifer, which appears only in 2DS1 at a depth of (140m), and it thickness is more than (80m). The comparison between VES and 2D imaging ...
Research Interests:
The study area occupies about (101) Km2, and it is located within Wasit province, north Badra area, eastern Iraq. This area is bounded between latitude (33o 17'– 33o 07') north, and longitude (45º 53'-46º 04') east. The... more
The study area occupies about (101) Km2, and it is located within Wasit province, north Badra area, eastern Iraq. This area is bounded between latitude (33o 17'– 33o 07') north, and longitude (45º 53'-46º 04') east. The aims are to compare four electrode arrays to determine the best array in delineating the aquifers using 2D imaging technique, and then compare between 1D and 2D imaging techniques in delineating layers and aquifer boundaries in complex sedimentary deposits, and to determine the thickness and depth of aquifers in the study area. Six 2D imaging stations were applied in the study area. The first two stations (2DS1, and 2DS2) were selected to make the comparison between Dipole-Dipole, Wenner-Schlumberger, Schlumberger reciprocal, and Wenner arrays. The total length survey for each array in the (2DS1) was 1190m, while in the (2DS2) was 590m with electrode spacing of 10m. Also, cross Vertical Electrical Sounding technique was carried out in the same positio...
The study area occupies about (101) Km2, and it is located within Wasit province, north Badra area, eastern Iraq. This area is bounded between latitude (33o 17'– 33o 07') north, and longitude (45º 53'-46º 04') east. The... more
The study area occupies about (101) Km2, and it is located within Wasit province, north Badra area, eastern Iraq. This area is bounded between latitude (33o 17'– 33o 07') north, and longitude (45º 53'-46º 04') east. The aims are to compare four electrode arrays to determine the best array in delineating the aquifers using 2D imaging technique, and then compare between 1D and 2D imaging techniques in delineating layers and aquifer boundaries in complex sedimentary deposits, and to determine the thickness and depth of aquifers in the study area. Six 2D imaging stations were applied in the study area. The first two stations (2DS1, and 2DS2) were selected to make the comparison between Dipole-Dipole, Wenner-Schlumberger, Schlumberger reciprocal, and Wenner arrays. The total length survey for each array in the (2DS1) was 1190m, while in the (2DS2) was 590m with electrode spacing of 10m. Also, cross Vertical Electrical Sounding technique was carried out in the same positio...
The resistivity survey was carried out by using vertical electrical sounding (VES) and 2D imaging techniques in the northern Badra area, Eastern Iraq. Eleven VES points distributed on two parallel profiles and six 2D imaging stations were... more
The resistivity survey was carried out by using vertical electrical sounding (VES) and 2D imaging techniques in the northern Badra area, Eastern Iraq. Eleven VES points distributed on two parallel profiles and six 2D imaging stations were applied using long survey lines. In general, two types of aquifers are recognized in the study area. The first is the Quaternary aquifer, which appears in all geological sections and inverse model of 2D imaging stations (2DS).This aquifer can be divided into upper and lower aquifers as shown in (2DS1), (2DS3), and (2DS4). Generally, the thickness of this aquifer ranges between (30-200 m) which occurs at a depth of (10-30m) according to geological sections, while its thickness ranges between (35-180m) and occurs at depth (10-45m) according to the inverse model of 2D imaging stations. The second is the AL-Mukdadiya aquifer, which appears only in 2DS1 at a depth of (140m), and it thickness is more than (80m). The comparison between VES and 2D imaging techniques revealed that the VES technique is the best in delineating the boundaries between layers. However, the 2D imaging technique is better at delineating the aquifers, and at determining the vertical and horizontal changes in resistivity within layers and aquifers, and it also succeeded in recognizing the upper and lower aquifers of quaternary aquifer as shown in (2DS1), (2DS3), and (2DS4). Therefore, 2D imaging is better at recognizing more layers or aquifers than that of VES technique, especially with the gradual decrease (or increase) in resistivity values or layers with small thickness. Also, the VES technique showed a high depth of investigation (DOI) in comparison with 2D imaging technique.
Research Interests:
Research Interests: