Academic literature on the topic 'Geoelectric Layer'

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Journal articles on the topic "Geoelectric Layer"

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Falah, Muh Darwis. "Geoelectric Method Implementation in Measuring Area Groundwater Potential: A Case Study in Barru Regency." International Journal of Environment, Engineering and Education 2, no. 1 (2020): 1–8. http://dx.doi.org/10.55151/ijeedu.v2i1.22.

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Geoelectric measurements to detect the presence of groundwater aquifers in the study area by knowing the type of lithology, distribution, thickness, and depth of rock layers carrying groundwater (aquifer), both vertically and laterally. The research objective is to determine the location for drilling, if later in the study area, the groundwater potential maximally utilized. In this study, the linear symmetry electrode arrangement, the Schlumberger configuration method, is used. Data collection in the field done by using a resistivity meter. The number of geoelectric points is 12 measurement po
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Falah, Muh. Darwis. "Geoelectric Method Implementation in Measuring Area Groundwater Potential: A Case Study in Barru Regency." International Journal of Environment, Engineering & Education 2, no. 1 (2020): 1–8. https://doi.org/10.5281/zenodo.3752355.

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Geoelectric measurements to detect the presence of groundwater aquifers in the study area by knowing the type of lithology, distribution, thickness, and depth of rock layers carrying groundwater (aquifer), both vertically and laterally. The research objective is to determine the location for drilling, if later in the study area, the groundwater potential maximally utilized. In this study, the linear symmetry electrode arrangement, the Schlumberger configuration method, is used. Data collection in the field done by using a resistivity meter. The number of geoelectric points is 12 measurement po
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Bedair, Mohamed F., Rifai I. Rifai, Ahmed Gamal, and Mostafa S. M. Barseem. "Application of Geoelectric Technique in Groundwater Protection of Quaternary Aquifer in Wadi El Natrun, Egypt." Journal of Geography, Environment and Earth Science International 27, no. 2 (2023): 29–48. http://dx.doi.org/10.9734/jgeesi/2023/v27i2669.

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Qualitative and quantitative interpretations of the accessible geoelectrical resistivity data were conducted in the area located to the west of Nile Delta on both sides of the Cairo-Alexandria desert road, between latitudes 30.190816° and 30.745892° N and longitudes 29.797607° and 30.702070° E, in the northern Western Desert of Egypt. The study area is covered by thick sedimentary exposures ranging from the Miocene to the Quaternary period. Geological factors such as lithology and geological structures significantly influence the groundwater in the study area. The Quaternary, Pliocene, and Mio
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Syarifullah Bundang, George Belly Sahetapy, Dian Dwi Apriliyani Arsdinand, and Firman. "Interpretation of the Availability of Springs in Labuang Rano Village with a Geophysical Approach." Technium: Romanian Journal of Applied Sciences and Technology 17 (November 1, 2023): 149–52. http://dx.doi.org/10.47577/technium.v17i.10063.

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Geologically speaking, Labuang Rano Village, Mamuju City area is composed of rocks from the Adang Volcano Formation. Based on the results of the site survey, it was found that there is a spring with a slight discharge. The emergence of these springs is not yet known, so further analysis is needed. An approach used to determine subsurface conditions is the geophysical approach, especially the geoelectric method. This study aims to analyse the subsurface geological conditions using geoelectric to find the factors that influence the emergence of springs. Geoelectrical measurements, observations o
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Mudral, Hafiza, and Usman Malik. "PENGUKURAN RESISTIVITAS LAPISAN TANAH DI KELURAHAN TUAH KARYA MENGGUNAKAN KONFIGURASI SCHLUMBERGER." JOURNAL ONLINE OF PHYSICS 4, no. 2 (2019): 11–14. http://dx.doi.org/10.22437/jop.v4i2.7578.

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Geoelectric is one of the geophysical exploration methods that uses the earth's electrical properties to study subsurface conditions, the geoelectric method has several rules, one of which is Schlumberger's rule. This study aims to determine the composition of the soil layer, so that it can be known that the cause of difficult surface water seeps into the ground based on resistivity values at the HSB Indah Residence. Schlumberger configuration research uses a 300 meter stretch. Resistivity of soil constituent lithology in the study area was generated by processing geoelectric data using one-di
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Arif, Subhan, Nurul Dzakiya, Samuel Kristiyana, and Rohmad Bagus Abadi. "Identification of the Potential Quartz Sandstone in the Sambong Area By the Dipole-Dipole Configuration of Resistivity Method." Journal of Applied Geospatial Information 7, no. 1 (2023): 813–19. http://dx.doi.org/10.30871/jagi.v7i1.5276.

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The presence of quartz sandstone outcrops in the southeast of the study site suggests the presence of quartz sandstones in the northwest, according to the strike direction. This geoelectrical measurement aims to determine the distribution of these sandstones below the surface. The method used is geoelectric with a dipole dipole configuration.
 Measurements were made on four track lines. Tracks A and B indicate the existence of a layer of sandstone below the surface. Tracks C and D do not show any layers of quartz sandstone. This is caused by the presence of faults or folds that cause the
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Dinata, Indra A., M. Khalifah B. Y. Praja, Imam A. Sadisun, and Agus Kuswanto. "Geoelectric Analysis for Potential Slip Plane Interpretation in Labuan Bulan Hill, Salem District, Brebes Regency, Central Java." IOP Conference Series: Earth and Environmental Science 1227, no. 1 (2023): 012008. http://dx.doi.org/10.1088/1755-1315/1227/1/012008.

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Abstract Landslide is a natural disaster which often occurs in Indonesia. Based on National Disaster Management Agency (BNPB), there were 1,321 landslide incidents which occurred in 2021. Labuan Bulan Hill located on high susceptibility landslide seen from Landslide Susceptibility Zone of Brebes Regency, furthermore, soil tensile cracks presence with 5 - 50 cm width and 15 - 125 cm height at upper slope. In this study, the identification of subsurface lithologies and potential slip plane was carried out using geoelectric survey method with Wenner – Schlumberger configuration. The Wenner – Schl
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Sutasoma, Muwardi, Adi Susilo, and Eko Andi Suryo. "Penyelidikan Zona Longsor dengan Metode Resistivitas dan Analisis Stabilitas Lereng untuk Mitigasi Bencana Tanah Longsor." INDONESIAN JOURNAL OF APPLIED PHYSICS 7, no. 1 (2017): 35. http://dx.doi.org/10.13057/ijap.v7i1.8784.

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<p>Research using geoelectric resistivity dipole-dipole configuration and slope stability analysis has been done in the area Jawar, District Dampit to find out the sliding plane landslide, landslide direction and factor of safety. Tracks Retrieval of data by the method of geoelectric resistivity as much as 5 tracks with the direction of the southeast to the northwest three tracks with a length of 100 m - 200 m and southwest to northeast as many as two passes with a length of 200-300 m. While the slope stability analysis performed topographic map data retrieval and data collection sondir
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Gilbert, Idiegbe Onoriode, and Atumah Oyibo Lawrence. "Geophysical Investigation of Groundwater Level Using Vertical Electrical Sounding (A Case Study of Ewu in Edo State Nigeria)." International Journal of Research in Science 3, no. 2 (2017): 22. http://dx.doi.org/10.24178/ijrs.2017.3.2.22.

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Abstract- In this research work, four Vertical Electrical Soundings (VES) were carried out in Ewu Town at various locations: Eguare-Ewu, Idunwele-Ewu, Flour Mill Road-Ewu and Eko-Ewu using the ABEM terrameter, by employing the Schlumberger electrode configuration system to determine the level of groundwater. From the analysis of field data and results of computer iteration, a maximum of four geoelectric layers were obtained. The first layer of geoelectric section was the lateritic top soil with thickness of 1.21m and 11.1m, for VES 1 and VES 2, with apparent resistivity of 438Ωm and 183Ωm. The
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Ilaboya, Idowu, Eghosa Omosefe, and Esther Ambrose-Agabi. "Assessing aquifer vulnerability near cemeteries using dipole-dipole and vertical electrical sounding methods." CTU Journal of Innovation and Sustainable Development 16, no. 3 (2024): 112–23. http://dx.doi.org/10.22144/ctujoisd.2024.312.

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An integrated geophysical investigation of the second cemetery in Benin City was conducted with the view to determine the leachate flow direction and the geoelectrical layers that characterized the underlying aquifer. Eight vertical electrical soundings (VES) and two dipole-dipole profiling lines along two transverse sections were carried out. For the dipole-dipole profiling, ABEM Terrameter SAS 300C was employed, while the VES investigation utilized the Schlumberger array. The resistivity data collected during the field investigation were interpreted using DIPROWIN software version 4.01. Leac
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Dissertations / Theses on the topic "Geoelectric Layer"

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GIORDANO, CLAUDIA. "Applicazione della tomografia elettrica e di tecniche di rilievo tridimensionale nel Parco Archeologico di Egnazia (BR)." Doctoral thesis, Università degli studi del Molise, 2017. http://hdl.handle.net/11695/73682.

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Questo lavoro vuole essere un contributo per sottolineare l’importanza delle possibili applicazioni delle moderne metodologie geofisiche e di rilievo introdotte nel campo dei Beni Culturali e del loro potere risolutivo, mostrare come tali tecnologie siano utilizzabili ed efficaci in diversi contesti sia per la diagnostica ad alta risoluzione che per l’indagine del sottosuolo e la definizione dello stato di conservazione di un bene. L’obiettivo è stato quello di fornire il maggior numero possibile di elementi per una valutazione generale dei siti oggetto di ricerca; ciò ha permesso di dimostrar
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Book chapters on the topic "Geoelectric Layer"

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Ningsih, Jusna, Sriyati Ramadhani, Martini, Hendra Setiawan, Taufik Hidayat, and Dhiva Regina Putri. "Analysis of Soil Layer Structure Using Geoelectric Method on Tawaeli-Toboli Road Section Km 49+450." In Advances in Engineering Research. Atlantis Press International BV, 2025. https://doi.org/10.2991/978-94-6463-768-7_28.

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Kuchenbrod, Winfried. "How to Get the Structure of Waste Disposals and the Surface of Water Damming Layers with Geoelectrical Tomography." In Field Screening Europe. Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-009-1473-5_27.

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Przybyła, Marcin, Michał Podsiadło, and Piotr Gruba. "Badania magnetyczne i elektrooporowe na terenie kopalni krzemienia w Bęble, stan. 4, pow. krakowski / Magnetic survey and electrical resistivity tomography at the flint mine in Bębło, Site 4, Kraków district." In Nakopalniane pracownie krzemieniarskie z okresu neolitu w Bęble, stan. 4, woj. małopolskie / Neolithic flint workshops at the mine in Bębło, site 4, Małopolska. Muzeum Archeologiczne w Krakowie; Wydawnictwo Profil-Archeo, 2021. http://dx.doi.org/10.33547/bmak.10.2.

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The magnetic and electrical resistivity surveys have led to identifying the geological structure of Site 4 in Bębło, revealing varied limestone karren: karst grooves and clints, at a depth of one metre, under a shallow layer of humus and clayey loess. The bottom of those grooves may have been covered with flint concretions, and it is likely that flint was extracted exactly from there. The clarity of magnetic and geoelectrical anomalies in Bębło indicates that the test results reflect the true character of the mine. The absence of anomalies related to large and deep shafts seems to stem from th
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Trela-Kieferling, Elżbieta. "Zakończenie / Conclusion." In Nakopalniane pracownie krzemieniarskie z okresu neolitu w Bęble, stan. 4, woj. małopolskie / Neolithic flint workshops at the mine in Bębło, site 4, Małopolska. Muzeum Archeologiczne w Krakowie; Wydawnictwo Profil-Archeo, 2021. http://dx.doi.org/10.33547/bmak.10.8.

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The flint mine in Bębło is situated in the Ojców Upland within the Olkusz Upland. Its vast mining field lies on a slope of a crest facing south-east, rising above a small valley, now dry but once crossed by a watercourse, to a height of approx. 30 metres. In the late 5th millennium BC, irregular flint concretions were extracted there through small shallow pits located one next to the other and reaching the bottom of karst karren. The non-invasive exploration of the site has confirmed the presence of two separate sections: the workshop zone and the mining zone. The former zone covers a flat are
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Conference papers on the topic "Geoelectric Layer"

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Kushnir, Dmitry Yu, Nikolay N. Velker, and Darya V. Andornaya. "Neural network approximation of resistivity tool responses in three–layer formation model." In Недропользование. Горное дело. Направления и технологии поиска, разведки и разработки месторождений полезных ископаемых. Экономика. Геоэкология. Федеральное государственное бюджетное учреждение науки Институт нефтегазовой геологии и геофизики им. А.А. Трофимука Сибирского отделения Российской академии наук, 2020. http://dx.doi.org/10.18303/b978-5-4262-0102-6-2020-048.

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We apply neural networks function approximation method to the problem of resistivity data modeling on the example of a three–layer geoelectric formation model. The model parameters distribution of the training database depends on the relative position of the tool coils and the layer boundaries. It is obtained on a test database that the signals calculated using neural networks coincide with the synthetic ones within one measurement error for more than 99.9% of the test samples.
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Oluwaseun, Ojo Adebayo, Jun Xie, and Olorunfemi Martins Olu. "Investigating the resolution of inverted geoelectric layer parameters using the neighbourhood algorithm." In International Conference on Engineering Geophysics, Al Ain, United Arab Emirates, 9-12 October 2017. Society of Exploration Geophysicists, 2017. http://dx.doi.org/10.1190/iceg2017-031.

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Karangan, Rifnaldo, Muhammad Altin Massinai, Titien Haryani, and Nurul Fhaika. "Identification of underground aquifer layer using the geoelectric resistivity method, case study: Maros Regency, South Sulawesi, Indonesia." In PROCEEDINGS OF 5TH INTERNATIONAL CONFERENCE ON SUSTAINABLE INNOVATION IN ENGINEERING AND TECHNOLOGY 2023. AIP Publishing, 2024. http://dx.doi.org/10.1063/5.0164560.

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Bykov, Artem, Dmitry Surzhik, G. S. Vasilyev, O. R. Kuzichkin, and K. V. Bondarik. "APPLICATION OF THE PHASE-METRIC METHOD IN THE PROBLEMS OF GEOTECHNICAL CONTROL OF THE DRILLING PROCESS." In 22nd SGEM International Multidisciplinary Scientific GeoConference 2022. STEF92 Technology, 2022. http://dx.doi.org/10.5593/sgem2022/1.1/s06.068.

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During the process of drilling wells, it is necessary to have information about the composition of the soil layers through which the drill passes. This will optimize the parameters of rotation of the drill, the load on the drill, as a result of which equipment wear will be reduced. It will also make it possible to lay optimal trajectories during well drilling and track the penetration of the drill into the target layer. This issue is especially relevant for the oil industry, where production is carried out at great depths with a complex structure of soil and rocks. Obtaining this information b
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Puspita, T. R., D. P. E. Putra, A. H. Rafsanjani, and R. Farjrina. "BRACKISH WATER MAPPING BASED ON WATER QUALITY DATA AND GEOELECTRICAL SURVEY : CASE STUDY IN THE SHALLOW GROUNDWATER OF TEGAL CITY." In 7th International Conference on Sustainable Built Environment. Universitas Islam Indonesia, 2023. http://dx.doi.org/10.20885/icsbe.vol2.art9.

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Salty water in the aquifer influences changes in groundwater quality may cause by pumping activities and/or natural phenomena. This paper reported the result of salty water mapping in the shallow groundwater of Tegal city. The EC values of groundwater in the study area ranges between 510 µS/cm to 7610 µS/cm, and TDS values are between 300 mg/L to 2450 mg/L. The geoelectrical measurement on study area reveals a very low resistivity layer of 0.307 Ùm at a depth of 2.87 to 12 meters, indicating brackish water. Based on the EC and TDS also geoelectrical survey, a map of salty water is produced and
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Metwaly, M., G. El-Qady, A. El-Galladi, and K. Ushijima. "Evaluation of Peat Layer Using Geoelectrical Methods at Nile Delta– Egypt." In Near Surface 2005 - 11th European Meeting of Environmental and Engineering Geophysics. European Association of Geoscientists & Engineers, 2005. http://dx.doi.org/10.3997/2214-4609-pdb.13.p017.

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Gyulai, A., T. Ormos, and L. Dresen. "A joint inversion method to solve problems of layer boundaries, differently defined by seismics and geoelectrics." In 6th EAGE/EEGS Meeting. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406302.

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Yundari, Nurhasanah, Ryan Jonathan, Odilo Yupama Engkoe Nada, and Muhammad Irfan. "Space-time modeling in rock layers through resistivity data (case study: Resistivity geoelectric data in Pontianak city)." In INTERNATIONAL SEMINAR ON MATHEMATICS, SCIENCE, AND COMPUTER SCIENCE EDUCATION (MSCEIS) 2021. AIP Publishing, 2023. http://dx.doi.org/10.1063/5.0155344.

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Edigbue, Paul, Ismail Demirci, Hamdan Hamdan, et al. "Joint Inversion of Seismic and DC Geophysical Data Using Local and Global Optimization Algorithms." In International Petroleum Technology Conference. IPTC, 2022. http://dx.doi.org/10.2523/iptc-21877-ms.

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Abstract Geophysical inversion is usually carried out to quantitatively analyze the earth model and estimate its physical properties. Successful delineation of these properties such as layer boundaries, or other near-surface structures are crucial to understand the near-surface inhomogeneity. In this study, we focus on the use of joint inversion of seismic refraction and geoelectrical resistivity datasets using local and global optimization methods. The idea is to integrate the two optimization techniques to minimize the challenges faced by each algorithm when applied alone. This hybrid algori
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El Mahmoudi, A., Y. Al-Dakheel, A. Hussein, and M. Massoud. "Two Dimensional Geoelectrical Imaging of the Hardpan Layer at the Agricultural and Research Station of KFU, Al Hassa, KS." In First International Conference on Engineering Geophysics. EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20143979.

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