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Journal articles on the topic 'Geoelectric Layer'

Author: Grafiati

Published: 3 June 2025

Last updated: 31 July 2025

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1

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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2

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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4

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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8

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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9

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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A., O. Talabi, A. Abdu-Raheem Y., and O. Afolagboye L. "Application of Electrical Resistivity Method in Building Foundation Study around Ansarudeen Primary School Adehun Area of Ado-Ekiti, Southwestern Nigeria." International Journal of Innovative Research in Multidisciplinary Education 03, no. 11 (2024): 1838–46. https://doi.org/10.5281/zenodo.14233860.

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The study evaluated the structural competency of the subsurface geological materials around Ansarudeen Primaryschool in Bolorunduro community, Adehun area of Ado Ekiti, Ekiti State, Nigeria to delineate the area that is suitable for buildingdevelopment. The ABEM SAS 1000 was employed for transmitting current and recording the resistivity value of the subsurfacelayers across the two traverses using the dipole-dipole and the Schlumberger arrays for horizontal profiling and vertical electricalsounding of the survey area respectively. Five VES points were occupied along traverses 1 and 2 with AB/2

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Ishola, Sakirudeen Akinola, and S. T. Olufemi. "Groundwater Exploration using Geoelectric Technique in Oru-Ijebu, South-West Nigeria." Nigerian Journal of Theoretical and Environmental Physics 2, no. 1 (2024): 49–66. http://dx.doi.org/10.62292/njptep.v2i1.2024.20.

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Forty Vertical Electrical Soundings (VES) were carried out using Allied Ohmega resistivity meter with schlumberger configuration in parts of Oru-Ijebu to determine the necessary geoelectrical parameters for delineating the aquiferous zones. Four to five distinct geoelectric layers were delineated from the survey area except for VESORU21 which exhibited six geoelectric layers namely the top soil, clayey sand/laterite, clay and granite gneiss. The first layer serves as the topsoil with high variable resistivity ranging from 11.2Ωm (VESORU7) to 153.8Ωm (VESORU25) with their corresponding thicknes

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Markos, Mulugeta, Abel Saka, Leta Tesfaye Jule, N. Nagaprasad, and Krishnaraj Ramaswamy. "Groundwater Potential Assessment Using Vertical Electrical Sounding and Magnetic Methods: A Case of Adilo Catchment, South Nations, Nationalities and Peoples Regional Government, Ethiopia." Concepts in Magnetic Resonance Part A 2021 (December 8, 2021): 1–11. http://dx.doi.org/10.1155/2021/5424865.

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Vertical electrical sounding and magnetic methods were carried out to assess groundwater potential in Adilo catchment, Kembata Tembaro Zone, South Nations, Nationalities and Peoples Regional Government, Main Ethiopian Rift. The data were acquired from eight VES points using Schlumberger electrode arrays with maximum half current electrode spacing ( AB / 2 = 500 ) and 253 magnetic data points were analyzed. The qualitative analysis of VES data was accomplished by using curves, apparent resistivity, and pseudodepths, and the quantitative interpretations of the VES data were constructed by the VE

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14

Efendi, Aco Wahyudi. "Availability of the Sangatta Pelangi Hill Slide Using Geoelectric Correlation on the Borlog." Journal of Science and Education Research 2, no. 1 (2023): 7–15. http://dx.doi.org/10.62759/jser.v2i1.27.

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The earth's surface moves downward from a point in a process known as land subsidence, which causes the elevation of the ground surface to drop or become lower than it was. The geoelectric technique is one way to investigate soil. Depending on the electrical characteristics of the rock, this technique is one of the geophysical exploration methods that can give a generalized (map) of a rock layer or formation and the depth of the rock layers. The goals of this study were to model landslide behavior and identify the soil layers using geoelectric data. The rock or hard soil zone has a high resist

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15

Mahi, Shuaibu, Abubakar Yusuf, and Garba Lawal. "Geoelectrical Assessment of Groundwater Potential within Zamfara and its Environs, Northwestern Nigeria." Caliphate Journal of Science and Technology 4, no. 1 (2022): 54–70. http://dx.doi.org/10.4314/cajost.v4i1.8.

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Groundwater potential assessment was carried out within Zamfara environs, Northwestern Nigeria using geoelectrical technique with a view of solving the problem of incessant failure of boreholes in the study area. A total of one hundred and eighty-three (183) vertical electrical soundings (VES) were used to identify potential groundwater bearing zones capable of sustaining economic development of the study area. Two hydrogeological units were investigated (basement rock units and sedimentary rock unit), using Omega resistivity meter Model No. 122, to measure and record the resistance of the sub

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Eyankware, M. O., A. O. I. Selemo, P. N. Obasi, and O. M. Nweke. "EVALUATION Of GROUNDWATER VULNERABILITY IN FRACTURED AQUIFER USING GEOELECTRIC LAYER SUSCEPTIBILITY INDEX AT OJU, SOUTHERN BENUE TROUGH NIGERIA." Geological Behavior 4, no. 2 (2020): 63–67. http://dx.doi.org/10.26480/gbr.02.2020.63.67.

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A combination of geoelectric and hydrogeologic concept was used in the assessment of groundwater vulnerability in fractured aquifers of Oju and environs. The study area is underlain by the sediments of the Asu River Group, Southern Benue Trough Nigeria. A total of twenty-seven (27) Vertical Electrical Sounding (VES) was carried out within the study area. Geoelectric parameters (layer, resistivity and thickness) of the overlying layers across the study area were determined and used to evaluate the vulnerability of the underlying aquifers. Three charts were compared using geo-electrically derive

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17

Alaydrus, Alfina Taurida, Adi Susilo, Suhayat Minardi, Agus Naba, and Agus Wahid. "Analysis the Effect of Physical Parameters on Groundwater Salinity in the KEK Mandalika Lombok." Prisma Sains : Jurnal Pengkajian Ilmu dan Pembelajaran Matematika dan IPA IKIP Mataram 9, no. 2 (2021): 316. http://dx.doi.org/10.33394/j-ps.v9i2.4437.

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KEK Mandalika is located in a coastal area which is very vulnerable to changes in the quantity and quality of groundwater due to seawater intrusion. This study aims to detect the presence of aquifers (groundwater), seawater intrusion and analyze the effect of physical parameters to determine groundwater quality in the KEK Mandalika area. The physical parameters used are: resistivity, conductivity, Total Dissolved Solid (TDS) and salinity. The resistivity value was obtained using the geoelectric resistivity method with 10 lines using a dipole-dipole configuration, while the other parameters wer

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18

Atan Obeten Egor, Abong Augustine. Agwul, and Bisong Samson Asu. "Deployment of Geophysical Technique in Groundwater Search at Guinueaworm Endermic areas in Obubra local government area of cross river state, Nigeria." GSC Advanced Research and Reviews 16, no. 1 (2023): 268–79. http://dx.doi.org/10.30574/gscarr.2023.16.1.0317.

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This study was conducted in the Guineaworm prone areas in Obubra Local Government Area, the study entails the deployment of vertical electrical sounding technique in the search for groundwater. In doing this, measurement was made in 14 profiles of 500m long each, using the IGIS resistivity meter model SSR-MP-ATS. Resist software was used for analysis. The Geoelectric sounding data interpretation revealed characteristic curves with two to six geoelectric layer thicknesses. The predominant curve types in the area were the KH, HKH, and HK. The electrical resistivity of the first layer ranged betw

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Idris, Syafrizal, Dian Darisma, Agus Hari Pramana, Nurul Aflah, M. Sayuti, and Nanda Novita. "Identification of the Aquifer Layer using the Geoelectric Method in Teupin Batee Village, Aceh Besar." Bulletin of Computer Science and Electrical Engineering 3, no. 1 (2022): 40–46. http://dx.doi.org/10.25008/bcsee.v3i1.1155.

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The need for clean water around the world is related to the increasing population, especially in Teupin Batee Village, Aceh Besar District. In addition to surface water, groundwater is one of the potentials that can be utilized by the community, particularly for household needs. The purpose of this study is to identify the aquifer layer using the geoelectric method. One of the geophysical methods that can be used to map groundwater potential is the geoelectrical method based on the resistivity value of subsurface rocks. This study uses the Wenner-Schlumberger array because it can map subsurfac

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Atan, Obeten Egor, Augustine. Agwul Abong, and Samson Asu Bisong. "Deployment of Geophysical Technique in Groundwater Search at Guinueaworm Endermic areas in Obubra local government area of cross river state, Nigeria." GSC Advanced Research and Reviews 16, no. 1 (2023): 268–79. https://doi.org/10.5281/zenodo.8272237.

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This study was conducted in the Guineaworm prone areas in Obubra Local Government Area, the study entails the deployment of vertical electrical sounding technique in the search for groundwater. In doing this, measurement was made in 14 profiles of 500m long each, using the IGIS resistivity meter model SSR-MP-ATS. Resist software was used for analysis. The Geoelectric sounding data interpretation revealed characteristic curves with two to six geoelectric layer thicknesses. The predominant curve types in the area were the KH, HKH, and HK. The electrical resistivity of the first layer ranged betw

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21

Darwis, Muh. "Evaluasi Potensi Airtanah dengan Metode Geolistrik di Desa Lipukasi Kabupaten Barru." LaGeografia 18, no. 2 (2020): 160. http://dx.doi.org/10.35580/lageografia.v18i2.12808.

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The groundwater research area is included in the Lipempuan Village area. This research was conducted using the geoelectric method, using the Schlumberger linear symmetry configuration. Measurement of the type of resistivity was carried out at 12 geoelectric points. The research method uses qualitative methods. The measurement results show a cross section of resistors of types BR33-BR34-BR35-BR36-BR40-BR42 in general shows a layer of fresh shallow groundwater at depths (1.5 - 10) m, low productive productive groundwater at depths (10 - 75) m and local shows brackish-saltwater groundwater, produ

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22

Juandi, M., and S. A. Santoso. "Analysis of Groundwater Infiltration using the Schlumberger Geoelectric Method." Journal of Physics: Conference Series 2049, no. 1 (2021): 012070. http://dx.doi.org/10.1088/1742-6596/2049/1/012070.

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Abstract Groundwater is one of the best water resources for clean water, which can be used to meet the needs of people's lives, such as household, irrigation, and industrial needs. Based on the theory that changes in land use will have an impact on groundwater absorption. This study aims to see and analyze underground water absorption around the gate of the University of Riau using the geoelectric method of the Schlumberger configuration. Based on the results of measurements of resistivity values and groundwater infiltration in the Gate area of Riau University, Simpang Baru, Tampan, Pekanbaru,

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23

Lubis, Marwan, Luthfi Parinduri, Abdul Haris Nasution, and Darlina Tanjung. "PENENTUAN LOKASI TITIK BOR UNTUK MENDAPATKAN SUMBER AIR BERSIH DESA BANDAR RAHMAT KECAMATAN TANJUNG TIRAM KABUPATEN BATU BARA." Jurnal Pengabdian Mitra Masyarakat 1, no. 2 (2022): 39–47. http://dx.doi.org/10.30743/jurpammas.v1i2.5116.

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Availability of safe access to drinking water is one aspect of the slums of Bandar Rahmat Village. To build a good clean water well, reference data or information is needed regarding the investigation of groundwater potential around Bandar Rahmat Village, Tanjung Tiram Batubara District. This activity conducts geoelectrical testing using the resistivity method to be able to determine the value of rock resistivity which will later be used as a determination of the depth of shallow aquifers and deep aquifers. With the data obtained at each sounding point and correlated with other sounding points

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Olufemi, F. Ojo, O. Talabi Abel, O. Afolagboye Lekan, and A. Oyedele Akintunde. "Application of Electrical Resistivity in Building Foundation Study around Led School Area in Bishini, Northwestern Nigeria." Journal of Geography, Environment and Earth Science International 10, no. 3 (2017): 1–9. https://doi.org/10.9734/JGEESI/2017/34108.

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This study evaluated the structural competence of the subsurface geological materials around Led School Area in Bishini, NW Nigeria to delineate the area that is suitable for building development. Twenty Seven vertical electrical soundings (VES) points were occupied in the study area employing ABEM Terrameter SAS 300C with Schlumberger electrode configuration of maximum electrode separation AB/2=150 m. The field resistivity data were interpreted using Win RESIST software. The results from the 2-D interpretation of the VES data were used to prepare the geoelectric sections along four cross sect

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Woobaidullah, ASM, M. Moklesur Rahman, and M. Zohir Uddin. "Evaluation of hydrogeological conditions through vertical electrical soundings survey at Mankiganj pourashava, Manikganj, central part of Bangladesh." Bangladesh Journal of Scientific Research 27, no. 2 (2016): 109–20. http://dx.doi.org/10.3329/bjsr.v27i2.26229.

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The Pourashava area of Manikganj, located in the central part of Bangladesh is treated as arsenic hotspot in the country as the outcome of various studies concludes that almost 80% of the domestic tube wells at this area exceed arsenic level of Bangladesh standard (50 ?g/l) for drinking water. To enhance the potable water supply in the area, 15 geoelectric soundings survey using Schlumberger configuration with spreading AB/2 = 300 meters has been executed to decipher the subsurface lithology distribution and aquifers at different depths, to determine the lateral and vertical extent of aquifer

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Mirianrita, Ngozi Ossai, Nneka Okeke Francisca, Nnaemeka Obiora Daniel, and Cletus Ibuot Johnson. "Vulnerability assessment of hydrogeologic units in parts of Enugu North, Southeastern Nigeria, using integrated electrical resistivity methods." Indian Journal of Science and Technology 13, no. 34 (2020): 3495–509. https://doi.org/10.17485/IJST/v13i34.1366.

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Abstract <strong>Aim/objectives:</strong> This research is geared towards integrating Vertical Electrical Soundings (VES) and Electrical Resistivity Tomography (ERT) profiles constrained with geoelectric sections and borehole logs to assess the vulnerability of the aquifer units employing Aquifer Vulnerability Indexing (AVI) method.<strong>Method:</strong> The dataset used in this study comprises of fifty VES, five ERT profiles surveyed in parts of Enugu north in Enugu state, two geoelectric sections and three borehole logs. The computer and manual interpretation of VES resistivity d

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Khalil, Mohammad Ibrahim. "Coastal groundwater aquifer characterization from geoelectrical measurements- A case study at Kalapara, Patuakhali, Bangladesh." Journal of Applied Geology 5, no. 1 (2020): 1. http://dx.doi.org/10.22146/jag.55009.

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Vertical electrical sounding has been carried out in a coastal area in the southern part of Bangladesh to locate the groundwater aquifers containing fresh water. The Interpex1X1Dv3 computer program was used to process the field apparent resistivity data sets obtained from the vertical electrical sounding. Geoelectric layers were identified in the context of resistivity and thickness from the vertical electrical sounding data. From the initial parameters layered model was achieved using the inversion technique. Correlation of the obtained layer model with a nearby lithologic log concludes the g

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Inyang, Namdie J., and Idara O. Akpabio. "Geoelectric and Hydroelectric Parameters of Aquifers in Southern Parts of Akwa Ibom State." International Journal of Geology and Earth Sciences 3, no. 3 (2017): 23–32. https://doi.org/10.5281/zenodo.1612040.

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A Vertical Electrical resistivity Sounding (VES) survey was carried out, to study the geoelectric and hydroelectric parameters of aquifer in some locations in Part of Akwa Ibom State. A total of six (6) geoelectric soundings were acquired. The lithology of the aquifer layer can be said to compose of fine to gravelly sand, with sand and clay intercalation. The low resistivity values across most of the geoelectric layers can be attributed to conductive argillaceous geomaterials. Underlying aquiferous layer is likely unprotected from the surface contamination flow due to the fact that the protect

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Adeyemo, Igbagbo Adedotun, Andrew Ifeoluwa Afolayan, Bisola Stella Boluwade, and Samuel Kayode Alabi. "Subsurface Geotechnical Competence Evaluation Using Geoelectric Sounding and Direct Cone Penetrometer Test at Plural Garden Estate, Ilaramokin Southwestern Nigeria." Indonesian Journal of Earth Sciences 3, no. 2 (2023): A618. http://dx.doi.org/10.52562/injoes.2023.618.

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In order to evaluate the geotechnical competence of the subsurface soil materials at Plural Garden Estate, Ilaramokin Southwestern Nigeria, geotechnical investigations involving geoelectric sounding and Direct Cone Penetrometer Test (DCPT) was carried out in the estate. A total of 27 VES points and 8 DCPT points were occupied across the study area. A, H, K, Q and KH are the five sounding curve types delineated in the area. Resistivity values of the top soil, weathered layer, fractured layer and fresh bedrock vary from 65-864, 156-1698, 28-217, 433-12167 ohm-m respectively, while their thicknes

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Jonathan, R., Yundari, Nurhasanah, and O. Y. E. Nada. "Application of GSTAR(1,1) model for layer peat soil predicted based on resistivity log data." Journal of Physics: Conference Series 2106, no. 1 (2021): 012031. http://dx.doi.org/10.1088/1742-6596/2106/1/012031.

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Abstract In this study, GSTAR modeling was carried out with the inverse of distance weight matrix obtained from Geoelectrical Resistivity data at several peatland locations around the Universitas Tanjungpura, Pontianak. This data can identify the subsurface layer of the soil through the electric current that binds into the soil. However, due to the limitation of the tool to measure the resistivity value, it can only measure 1/5 of the depth of the observation length. To overcome this problem, predictions are made at the next depth using the GSTAR model. The study began by measuring the resisti

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Sudinda, Teddy Wartono. "STABILITY ANALYSIS FOR EMBANKMENTS WITH GEOELECTRICITY." Jurnal Sains dan Teknologi Mitigasi Bencana 15, no. 2 (2020): 114–22. http://dx.doi.org/10.29122/jstmb.v15i2.4333.

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Abstract The collapse of the embankment is a problem that needs attention to find the right solution, so that the risk can be minimized. The condition of the embankment is influenced by the strength of the soil layer of the embankment, groundwater flow in the embankment, the condition of the water level of the embankment and human activities around the embankment. Changes in the quality of soil density in the embankment can form cavity zones within the embankment which cause changes in groundwater flow patterns in the embankment. The degradation of the soil layer of the embankment can cause pi

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Santi, Narulita, Wahju K. Hidajat, Nur Adillah, Devina Trisnawati, and Nurakhmi Qadaryati. "Perhitungan Cadangan Batupasir di Derah Perencanaan Tambang Desa Pegongsoran, Kecamatan Pemalang, Kabupaten Pemalang, Jawa Tengah." MINERAL 6, no. 1 (2021): 1–5. http://dx.doi.org/10.33019/mineral.v6i1.3078.

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Indonesia has large number of sandstone reserves throughout the region. One of the potential reserves of Sandstones located in Pegongsoran, Pemalang. The purpose of the study is to know subsurface rock distribution so amount of Sandstones reserves can be determined for mining. The method used is Schlumberger arrays configuration geoelectrical method. Geoelectric measurements carried out at four points, geological mapping also conducted to know geological conditions and surface geomorphology.. From data processing in the field lithology found in the field are volcanic breccia, sandstones, and t

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Bawallah, M. A., A. A. Oyedele, S. O. Ilugbo, et al. "Evaluation of structural defects and the dynamic of stress and strain on a building along Oluwole Area, Southwestern Nigeria." Applied Journal of Physical Science 2, no. 2 (2020): 23–37. http://dx.doi.org/10.31248/ajps2020.027.

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This research was carried out within the Basement Complex terrain along Oluwole, off Akure High School, Akure, Ondo State, Nigeria, with the aim to ascertain the reasons for the major cracks and sign of apparent failures observed in a building few years after its construction and usage. The geophysical investigation involved two electrical resistivity techniques; Vertical Electrical Sounding (VES) using the Schlumberger configuration and 2-D electrical imaging using Dipole-dipole electrode configuration. Three traverses were established E–W direction cutting across geologic strike with a dista

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Okechukwu, E. Agbasi, and E. det Et uk Sunday. "Hydro-Geoelectric Study of Aquifer Potential in Parts of Ikot Abasi Local Government Area, Akwa Ibom State Using Electrical Resistivity Soundings." International Journal of Geology and Earth Sciences 2, no. 4 (2016): 43–54. https://doi.org/10.5281/zenodo.1560729.

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Geoelectric survey employing Vertical Electrical Sounding (VES) was carried out in parts of Ikot Abasi Local  Government Area, Akwa Ibom state, Nigeria. In this area there is no borehole that has been drilled until now, the main objectives of this study is to be a guide for the suitable position of borehole in order to avoid wild cat drilling and also to avoid salt intrusions using the VES geophysical techniques. Schlumberger electrode configuration was used in acquiring the data. Four to five geoelectric layers were delineated from the interpreted results. It shows the topsoil having res

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Lateef, T. A., Akinola B. Eluwole, and Dare J. Adewa. "Geoelectrical Assessment of the Impact of the Ilokun Dumpsite, Ado-Ekiti Southwestern Nigeria, on Surrounding Groundwater Aquifers." International Letters of Natural Sciences 40 (May 2015): 41–47. http://dx.doi.org/10.18052/www.scipress.com/ilns.40.41.

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The area around the Ilokun dumpsite, Ado-Ekiti was investigated with the aim of establishing the possible impact the contaminant plumes emanating from the dumpsite have on the subsurface aquifers. The Vertical Electrical Sounding (VES) field technique of the electrical resistivity method was adopted for the study, and the half-electrode spacing AB/2 varied from 1 to 65 m. A total of eight VES stations were occupied and a control VES point was located on the refuse dump. The VES data were interpreted quantitatively by partial curve matching and computer iteration, after which the geoelectric pa

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Lateef, T. A., Akinola B. Eluwole, and Dare J. Adewa. "Geoelectrical Assessment of the Impact of the Ilokun Dumpsite, Ado-Ekiti Southwestern Nigeria, on Surrounding Groundwater Aquifers." International Letters of Natural Sciences 40 (May 17, 2015): 41–47. http://dx.doi.org/10.56431/p-u6ea1b.

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The area around the Ilokun dumpsite, Ado-Ekiti was investigated with the aim of establishing the possible impact the contaminant plumes emanating from the dumpsite have on the subsurface aquifers. The Vertical Electrical Sounding (VES) field technique of the electrical resistivity method was adopted for the study, and the half-electrode spacing AB/2 varied from 1 to 65 m. A total of eight VES stations were occupied and a control VES point was located on the refuse dump. The VES data were interpreted quantitatively by partial curve matching and computer iteration, after which the geoelectric pa

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Zulfian, Zulfian. "APLIKASI METODE GEOLISTRIK DALAM PENDUGAAN KETEBALAN LAPISAN TANAH GAMBUT (STUDI KASUS: DAERAH DI SEKITAR JL. PERDANA, KOTA PONTIANAK)." Jurnal Kumparan Fisika 5, no. 1 (2022): 55–62. http://dx.doi.org/10.33369/jkf.5.1.55-62.

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ABSTRAK Tanah gambut merupakan jenis tanah yang tergolong memiliki daya dukung tanah yang lemah. Pendugaan ketebalan tanah gambut telah dilakukan dengan menerapkan metode geolistrik resistivitas. Konfigurasi yang digunakan pada metode ini yaitu konfiguruasi Wenner dengan spasi elektroda terkecil sebesar 3 m. Dalam pendugaan lapisan tanah gambut, lintasan survei geolistrik resistivitas dibuat berjumlah 2 buah lintasan dengan panjang tiap lintasan 72 m dan berjarak 15 m. Data lapangan selanjutnya diolah dan dilakukan inversi sehingga diperoleh penampang resisitivtas 2D lokasi penelitian. Dari pe

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Boubaya, Djamel. "Combining Resistivity and Aeromagnetic Geophysical Surveys for Groundwater Exploration in the Maghnia Plain of Algeria." Journal of Geological Research 2017 (January 18, 2017): 1–14. http://dx.doi.org/10.1155/2017/1309053.

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The Maghnia plain in western Algeria is filled by Plio-Quaternary and Miocene sediments that rest unconformably on a basement of Jurassic rocks. Electrical sounding (VES), magnetic data, well information, and hydrogeological data have been used to explore for groundwater potential in the Maghnia plain. The interpretation of Schlumberger sounding data was first calibrated with the lithology of available nearby wells. Four geoelectrical layers were identified within the study area. They are a thin near surface topsoil layer with variable resistivities, a moderate resistive aquifer (15–30 ohm-m),

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Gbadebo, Adewole Michael, Oluwaseun Tolu Olurin, Ganiyu Olabode Badmus, and Sikiru Salami. "Geoelectrical Investigation of the Groundwater Potential in Eti-Osa, Lagos State, Nigeria." ABUAD International Journal of Natural and Applied Sciences 4, no. 2 (2024): 1–6. https://doi.org/10.53982/aijnas.2024.0402.01-j.

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An electrical resistivity survey was conducted in Eti-Osa, Lagos State, Nigeria, to characterize the subsurface lithologic units, delineate the underlying aquifer, and assess groundwater potential. The study utilized an ABEM SAS 1000 terrameter for the data acquisition. Eight vertical electrical soundings were carried out using the Schlumberger electrode configuration. Data interpretation, both qualitative and quantitative, was presented through tables, charts, and sections. The interpreted geoelectric models revealed three to five layers with varying lithologies, including topsoil, sand, silt

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Mulyadi, Dudung, and Agung W. Biantoro. "Investigation of groundwater availability and geoelectric analysis to anticipate the scarcity of clean water in urban areas." IOP Conference Series: Earth and Environmental Science 1321, no. 1 (2024): 012037. http://dx.doi.org/10.1088/1755-1315/1321/1/012037.

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Abstract The need for housing makes suburban areas of Jakarta such as Tangerang Regency, Indonesia, a location that continues to grow. AG Housing is a developer in the area that continues to build housing. In housing development, it is very important to pay attention to the magnitude of water needs, both domestic water needs and non-domestic water needs. A problem that often occurs is that housing developers do not take into account the long-term water needs of their residents, especially in water-scarce areas. Developers often do not check the condition and location of water content in the so

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Fatoba, J. O., S. D. Omolayo, and E. O. Adigun. "Using Geoelectric Soundings for Estimation of Hydraulic Characteristics of Aquifers in the Coastal Area of Lagos, Southwestern Nigeria." International Letters of Natural Sciences 11 (February 2014): 30–39. http://dx.doi.org/10.18052/www.scipress.com/ilns.11.30.

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Electrical resistivity investigation was carried out at Ibeju Lekki, Southwestern Nigeria. The thrust of this study is to determine the geoelectrical parameters of the shallow aquifer and estimate the hydraulic characteristics of this aquifer unit from the surface geophysics. The area falls within the Dahomey basin of the Nigeria sedimentary terrain. Twenty-one VES were conducted using Shlumberger array with a maximum half current electrode (AB/2) of 100 m giving total spread of 200 m. Data were interpreted using partial curve matching technique and assisted 1-D forward modeling with WINRESIST

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Fatoba, J. O., S. D. Omolayo, and E. O. Adigun. "Using Geoelectric Soundings for Estimation of Hydraulic Characteristics of Aquifers in the Coastal Area of Lagos, Southwestern Nigeria." International Letters of Natural Sciences 11 (February 27, 2014): 30–39. http://dx.doi.org/10.56431/p-odo5d4.

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Electrical resistivity investigation was carried out at Ibeju Lekki, Southwestern Nigeria. The thrust of this study is to determine the geoelectrical parameters of the shallow aquifer and estimate the hydraulic characteristics of this aquifer unit from the surface geophysics. The area falls within the Dahomey basin of the Nigeria sedimentary terrain. Twenty-one VES were conducted using Shlumberger array with a maximum half current electrode (AB/2) of 100 m giving total spread of 200 m. Data were interpreted using partial curve matching technique and assisted 1-D forward modeling with WINRESIST

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Mantiri, Steven Yohanes Yulianus, Vinexa Alwendzani, Daniel Napitupulu, and Tatang Sutarman. "Analisis Struktur Lapisan Tanah Menggunakan Metode Geolistrik Resistivitas Konfigurasi Schlumberger Vertikal di Kompleks Perumahan Dosen Uncen Kali Acai, Kulurahan VIM, Distrik Abepura, Kota Jayapura." Jurnal Fisika Papua 2, no. 2 (2023): 124–33. http://dx.doi.org/10.31957/jfp.v2i2.88.

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Research on the analysis of the structure of the soil layer using the Vertical Schlumberger Geoelectric method in the Lecturer Housing Complex of Uncen Kali Acai, VIM Village, Abepura District, Jayapura City. This study aims to determine the soil layer, determine the location and depth of the soft soil layer, determine the soft and hard soil. Data retrieval using geoelectric resistivity method with vertical Schlumberger configuration. The instrument used for subsurface surveys is the HV 500 AK resistivity meter. Field measurements obtained electric current and voltage values and then calculate

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Fadilah, Fadilah. "Resistivitas Batuan Berdasarkan Metode Geolistrik Konfigurasi Schlumberger untuk Menentukan Potensi Air Tanah Sebagai Acuan Sumur Bor." Science, and Physics Education Journal (SPEJ) 4, no. 1 (2020): 31–37. http://dx.doi.org/10.31539/spej.v4i1.1783.

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The purpose of this study is to analyze rock resistivity based on the geoelectric method of the Schlumberger configuration to determine the potential for groundwater as a reference for boreholes. The method used in this research is the geoelectric resistivity method with a Schlumberger configuration. Data acquisition modeling was analyzed using Progress Version 3.0 to describe the subsurface based on measurement sounding points in the field. The main targets for these measurements are confined aquifer traps and sandstone stratigraphy. Field measurement points are at coordinates S 030 43 '52.2

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Salami, S. A., E. M. Babafemi, and F. E. Ossai. "Application of Electrical Resistivity Sounding Method for Groundwater Exploration in Ugboshi-Afe, Akoko-Edo, Southwestern Nigeria." Journal of Applied Sciences and Environmental Management 28, no. 5 (2024): 1345–53. http://dx.doi.org/10.4314/jasem.v28i5.3.

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Schlumberger configuration of Vertical Electrical Sounding (VES) was deplored for groundwater exploration in Ugboshi-Afe study location. A total of nine (9) vertical electrical sounding (VES) locations, spread across the community were occupied to gain insights on the hydrogeological settings within the area. Quantitative computer interpretation of the data yielded three to six geoelectrical layers. The geoelectrical interpretation models were geologically interpreted as: clayey sand/sandy topsoil with resistivity values ranging from 54 Ohm-m to 424 Ohm-m, this is underlain by a relatively hig

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Koesuma, Sorja, Daniel Afrian Pratama, and Budi Legowo. "Mapping of seawater intrusion in coastal areas using resistivity geoelectric method in Dukuhseti, Pati." Journal of Physics: Conference Series 2945, no. 1 (2025): 012028. https://doi.org/10.1088/1742-6596/2945/1/012028.

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Abstract Seawater mapping of the coastal area of the Dukuhseti District was carried out using the resistivity geoelectric method. The resistivity geoelectric method measures subsurface-specific resistance by passing an electric current into the ground. This geoelectric method uses a 1D Schlumberger configuration, and measurement is done at 12 points. Based on 1D data, seawater intrusion is present in shallow aquifers with a 5 to 50 meters depth range. Resistivity in shallow aquifers containing saltwater at 0.1Ωm - 2.5Ωm, low resistivity indicates the presence of saltwater rocks. Saltwater is n

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Simpen, I. Nengah, and Ni Made Widya Pratiwi. "Discovering ditch buried volcanic materials: geoelectric method assistance to minimize hazard loss." International journal of life sciences 3, no. 1 (2019): 48–55. http://dx.doi.org/10.29332/ijls.v3n1.258.

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The current study is aimed at discovering ditch buried volcanic materials: geoelectric method assistance to minimize hazard loss. The research has been conducted at Bugbug Karangasem Bali. This covered by volcanic material from the eruption of Mount Agung in 1963 and before. Of course, there is a ditch as a land boundary. Based on the measurement results of the geoelectric method, it was found that there was a low resistivity area of 26.5 ?.m at a depth of about 7 m area A and 23.5 m (area B). Based on the excavation at several points, the thickness of the volcanic material layer in the study

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Sehah, Muhammad, Mitha Syahfitri, and Sunardi Sunardi. "Pendugaan sebaran intrusi air laut melalui sungai di desa Ujungmanik kecamatan Kawunganten kabupaten Cilacap menggunakan metode geolistrik resistivitas konfigurasi Wenner." Jurnal Teras Fisika 4, no. 1 (2021): 176. http://dx.doi.org/10.20884/1.jtf.2021.4.1.3452.

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The estimation of the distribution of the sea water intrusion through the rivers in Ujungmanik Village, Kawunganten District, Cilacap Regency has been carried out using the Wenner configuration resistivity geoelectric. This research aims to estimate the distribution of sea water intrusion through rivers in Ujungmanik Village, Kawunganten District, Cilacap Regency based on geoelectric resistivity and conductivity data of groundwater. The geoelectric data acquisition was carried out on four lines. They were Wen1 Line, Wen2 Line, Wen3 Line, and Wen4 Line. Each line had a range of 200 meters. The

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Anwar, Samsul, Sri Cahyo Wahyono, and Fahruddin Fahruddin. "Identifikasi Lapisan Akuifer Tertekan Dengan Metode Geolistrik di Desa Lok Rawa Kecamatan Mandastana Kabupaten Barito Kuala Kalimantan Selatan." Jurnal Teori dan Aplikasi Fisika 8, no. 2 (2020): 151–58. http://dx.doi.org/10.23960/jtaf.v8i2.2447.

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One way to be able to identify rocks below the surface, depth, including groundwater aquifer layers is to do geophysical measurements using the schlumberger geoelectric method. This study aims to determine thickness and depth of aquifers in Lok Rawa Village, Mandastana District, Barito Kuala Regency. The results of the schlumberger configuration geoelectric study showed rock layers in Lok Rawa Village at the measurement points GL1, GL2 and GL3 consisting of weathered, sand, and fine clay (silt) layers. Lapiasan aquifers in Lok Rawa Village at the measurement points GL1, GL2 and GL3 consisting

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Kadri, Muhammad, and Teguh Febri Sudarma. "Penentuan Struktur Bawah Permukaan Daerah Geothermal Menggunakan Metode Geolistrik di Desa Penen Kecamatan Biru Biru Kabupaten Deli Serdang." Tunas Geografi 8, no. 1 (2019): 1. http://dx.doi.org/10.24114/tgeo.v8i1.13914.

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Abtract This study aimed to study the distribution of fluids, anomaly sightings and subsurface models from geothermal areas discussed in Penen village. Blue Biru District Deli Serdang Regency. The measurement of the geoelectric method is done by making the electrode path that injects current through the electrode. The potential difference that arises in the resistivity ABEM gauge can be measured by the apparent resistivity value obtained from the geoelectric device. Then the data is processed using Res2Div to get a 2D cross-section of the resistivity value of the rock layer. The analysis shows

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