Lateral Constrained Inversion of DC-Resistivity Data Observed at the Area North of Tenth of Ramadan City, Egypt for Groundwater Exploration
In the arid climate area north of Tenth of Ramadan City, southeast of the Nile Delta, Egypt, it is necessary to search for additional water resources for sustainable developments such as agricultural and industrial activities. Thirty two vertical electrical soundings (VES) of a electrical resistivit...
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MDPI AG
2021-06-01
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| Series: | Geosciences |
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| Online Access: | https://www.mdpi.com/2076-3263/11/6/248 |
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| author | Mohamed Genedi Hosni Ghazala Adel Mohamed Usama Massoud Bülent Tezkan |
| author_facet | Mohamed Genedi Hosni Ghazala Adel Mohamed Usama Massoud Bülent Tezkan |
| author_sort | Mohamed Genedi |
| collection | DOAJ |
| description | In the arid climate area north of Tenth of Ramadan City, southeast of the Nile Delta, Egypt, it is necessary to search for additional water resources for sustainable developments such as agricultural and industrial activities. Thirty two vertical electrical soundings (VES) of a electrical resistivity (DC) survey were carried out along four main profiles by using the Schlumberger array with electrode distances (AB/2) up to 500 m, to explore the shallow Pleistocene groundwater aquifer. The collected data was interpreted by a one-dimensional laterally constrained inversion (1D-LCI) and two-dimensional inversion algorithms to derive a best fit layered-earth resistivity model. The derived resistivity sections are geologically well interpreted based on information taken from the available water boreholes (P2-Well and P3-Well). The lateral constraints are part of the inversion where all data sets are inverted simultaneously, and consequently the output models are balanced between the constraints and the data-model fit. The 1D-LCI offers good analysis of the model parameters, which was successfully used to characterize a zone of groundwater aquifer, as it produces a laterally smooth model with sharp layer boundaries. The 1D-LCI inversion results show that the study area is subdivided into five geo-electrical layers of varied resistivity and thickness. In particular, the resistivity values of the last layer range between 9.3 and 110 Ωm representing the existing shallow Pleistocene aquifer located at depths between 134.5 and 118.4 m. Such results are tied and confirmed well with the results of the 2D inversion of the DC data. It reveals three interpreted geo-electric layers along the four profiles and shows that the area is affected by some normal faults striking nearly in the E–W direction. The very low resistivities of the groundwater aquifer beneath the agricultural part of the survey area probably indicates contamination due to the possible effect of irrigation operated in the cultivated lowlands. The results obtained could help the stakeholder to find additional information about the ground water aquifers in the newly reclaimed arid area and possible locations of new sites for drilling new water wells as additional water resources. |
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| publishDate | 2021-06-01 |
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| series | Geosciences |
| spelling | doaj.art-8c0315458cf94dbabdb1d28f8d02bc222023-11-21T23:04:35ZengMDPI AGGeosciences2076-32632021-06-0111624810.3390/geosciences11060248Lateral Constrained Inversion of DC-Resistivity Data Observed at the Area North of Tenth of Ramadan City, Egypt for Groundwater ExplorationMohamed Genedi0Hosni Ghazala1Adel Mohamed2Usama Massoud3Bülent Tezkan4Geology Department, Faculty of Science, Mansoura University, Mansoura 35516, EgyptGeology Department, Faculty of Science, Mansoura University, Mansoura 35516, EgyptGeology Department, Faculty of Science, Mansoura University, Mansoura 35516, EgyptNational Research Institute of Astronomy and Geophysics (NRIAG), Helwan 11722, EgyptInstitute of Geophysics and Meteorology, University of Cologne, 50969 Cologne, GermanyIn the arid climate area north of Tenth of Ramadan City, southeast of the Nile Delta, Egypt, it is necessary to search for additional water resources for sustainable developments such as agricultural and industrial activities. Thirty two vertical electrical soundings (VES) of a electrical resistivity (DC) survey were carried out along four main profiles by using the Schlumberger array with electrode distances (AB/2) up to 500 m, to explore the shallow Pleistocene groundwater aquifer. The collected data was interpreted by a one-dimensional laterally constrained inversion (1D-LCI) and two-dimensional inversion algorithms to derive a best fit layered-earth resistivity model. The derived resistivity sections are geologically well interpreted based on information taken from the available water boreholes (P2-Well and P3-Well). The lateral constraints are part of the inversion where all data sets are inverted simultaneously, and consequently the output models are balanced between the constraints and the data-model fit. The 1D-LCI offers good analysis of the model parameters, which was successfully used to characterize a zone of groundwater aquifer, as it produces a laterally smooth model with sharp layer boundaries. The 1D-LCI inversion results show that the study area is subdivided into five geo-electrical layers of varied resistivity and thickness. In particular, the resistivity values of the last layer range between 9.3 and 110 Ωm representing the existing shallow Pleistocene aquifer located at depths between 134.5 and 118.4 m. Such results are tied and confirmed well with the results of the 2D inversion of the DC data. It reveals three interpreted geo-electric layers along the four profiles and shows that the area is affected by some normal faults striking nearly in the E–W direction. The very low resistivities of the groundwater aquifer beneath the agricultural part of the survey area probably indicates contamination due to the possible effect of irrigation operated in the cultivated lowlands. The results obtained could help the stakeholder to find additional information about the ground water aquifers in the newly reclaimed arid area and possible locations of new sites for drilling new water wells as additional water resources.https://www.mdpi.com/2076-3263/11/6/248DC resistivity soundingSchlumberger arraylateral constrained (1D-LCI) inversiongroundwater aquifercontaminationNile delta |
| spellingShingle | Mohamed Genedi Hosni Ghazala Adel Mohamed Usama Massoud Bülent Tezkan Lateral Constrained Inversion of DC-Resistivity Data Observed at the Area North of Tenth of Ramadan City, Egypt for Groundwater Exploration Geosciences DC resistivity sounding Schlumberger array lateral constrained (1D-LCI) inversion groundwater aquifer contamination Nile delta |
| title | Lateral Constrained Inversion of DC-Resistivity Data Observed at the Area North of Tenth of Ramadan City, Egypt for Groundwater Exploration |
| title_full | Lateral Constrained Inversion of DC-Resistivity Data Observed at the Area North of Tenth of Ramadan City, Egypt for Groundwater Exploration |
| title_fullStr | Lateral Constrained Inversion of DC-Resistivity Data Observed at the Area North of Tenth of Ramadan City, Egypt for Groundwater Exploration |
| title_full_unstemmed | Lateral Constrained Inversion of DC-Resistivity Data Observed at the Area North of Tenth of Ramadan City, Egypt for Groundwater Exploration |
| title_short | Lateral Constrained Inversion of DC-Resistivity Data Observed at the Area North of Tenth of Ramadan City, Egypt for Groundwater Exploration |
| title_sort | lateral constrained inversion of dc resistivity data observed at the area north of tenth of ramadan city egypt for groundwater exploration |
| topic | DC resistivity sounding Schlumberger array lateral constrained (1D-LCI) inversion groundwater aquifer contamination Nile delta |
| url | https://www.mdpi.com/2076-3263/11/6/248 |
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