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Journal articles on the topic 'Geoelectrical methods'

Author: Grafiati

Published: 4 June 2021

Last updated: 26 July 2025

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1

Anggita, Novia, Dwinanti Rika Marthanty, and Abdul Halim Hamdany. "Estimation of Hydraulic Conductivity Using Geoelectrical and Infiltrometer Observations." Nature Environment and Pollution Technology 24, S1 (2025): 125–36. https://doi.org/10.46488/nept.2024.v24is1.008.

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Hydraulic conductivity (K) as a parameter in surface and subsurface water interaction is an important study to research. Field observations using geoelectrics with the Schlumberger configuration and using infiltrometers with double ring were chosen as methods to estimate the (K) which aims to recognize the characteristics of the relationship between (K) obtained from different observation results. The estimated (K) obtained from infiltrometer observations are quite significant compared to geoelectric observations which range from 2.715 × 10-7 m/s to 6.132 × 10-7 m/s, while geoelectrical values

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Aweda, Abdulwahid Kolawole, Ibrahim Kagara Shehu, Olusegun Omoniyi Ige, Mohammed Umar Umar, and Joseph Barde David. "Application of geological and electrical resistivity methods for groundwater studies at Tatiko, North Central Nigeria." Global Journal of Geological Sciences 18 (June 25, 2020): 15–22. http://dx.doi.org/10.4314/gjgs.v18i1.2.

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The success probability of water wells constructed in crystalline rock terrains is largely dependent on the size, location and interconnectivity of the fractures present in them as well as the amount and nature of the material that may clog the fractures. Geological and geoelectrical studies were proposed and conducted at Tatiko to determine the structures in the underlying basement rocks and evaluate their groundwater potential. Geological study was used to delineate the structural control on groundwater availability while the geoelectrical study (Vertical Electrical Sounding) was used to inv

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Meju, M. A., S. L. Fontes, M. F. B. Oliveira, J. P. R. Lima, E. U. Ulugergerli, and A. A. Carrasquilla. "Regional aquifer mapping using combined VES-TEM-AMT/EMAP methods in the semiarid eastern margin of Parnaiba Basin, Brazil." GEOPHYSICS 64, no. 2 (1999): 337–56. http://dx.doi.org/10.1190/1.1444539.

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As part of a program to evaluate the utility of integrated geoelectrical methods for subsurface structural mapping and groundwater resource investigation in the semiarid eastern margin of the Parnaiba basin in Brazil, several vertical electrical soundings (VES) and transient electromagnetic (TEM) and tensorial audiomagnetotelluric (AMT) measurements were carried out along a 250-km-long east‐west transect (passing through major towns and cities) and a 127-km-long north‐south profile (passing through small farm settlements). The various data sets have been jointly processed using a novel integra

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Khasanov, І., and N. K. Haidai. "GEODYNAMICS." GEODYNAMICS 2(11)2011, no. 2(11) (2011): 323–25. http://dx.doi.org/10.23939/jgd2011.02.323.

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On the basis of interpretation of magnetotelluric sounding curves constructed geoelectric model of south-east of the Yana-Kolymskaya fold system. As a result of mapping of the deep geoelectrical parameters with data obtained by other methods, are identified generalized geological-geophysical criteria characterizing the gold units of the south-east of the Yana-Kolyma folded system.

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Vasilyev, G. S., D. I. Surzhik, O. R. Kuzichkin, M. D. Baknin, and A. O. Kovalenko. "METHOD FOR CALIBRATION OF GEOECOLOGICAL MONITORING SYSTEMS BASED ON GEOELECTRIC METHODS OF GEODYNAMIC CONTROL." Kontrol'. Diagnostika, no. 319 (January 2025): 56–61. https://doi.org/10.14489/td.2025.01.pp.056-061.

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The article discusses issues related to the development, research and testing of a new method of mathematical modeling and field testing of geoecological monitoring systems based on geoelectric methods of geodynamic control. The method being developed involves creating the effect of the presence of near-surface and deep-seated inhomogeneities using additional point or extended sources (electrodes of various shapes, cable sections of various lengths and shapes, etc.). The problem with the known methods of physical (full-scale) modeling of geoelectric sections is the rigid specification of the g

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6

Islami, Nur, and Mitri Irianti. "Integrated Very Low Frequency and Geoelectrical Resistivity Methods to Study Possibility Shallow Groundwater Pathway in Bedrock Area." Journal of Physics: Conference Series 2049, no. 1 (2021): 012056. http://dx.doi.org/10.1088/1742-6596/2049/1/012056.

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Abstract Exploration of groundwater movement has a specific challenge in thick forest area and cover with the shallow hard rock. The use of active and passive geophysical method is needed for groundwater exploration. This study aims to explore the prospect of groundwater zone especially for the groundwater pathway in the area around the hot spring zone. Geoelectrical resistivity and very low frequency (VLF) methods were used with electrode spacing of 2 meter and reading stations of about 5 meter, respectively. The geoelectrical resistivity was carried out using the Wenner configuration in the

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Mościcki, Włodzimierz Jerzy, Grzegorz Bania, Michał Ćwiklik, and Aleksandra Borecka. "DC Resistivity Studies of Shallow Geology in the Vicinity of Vistula River Flood Bank in Czernichów Village (Near Kraków in Poland)." Studia Geotechnica et Mechanica 36, no. 1 (2014): 63–70. http://dx.doi.org/10.2478/sgem-2014-0008.

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Abstract DC resistivity methods, soundings and Electrical Resistivity Tomography, were applied to study shallow geology in the place of planned construction of an experimental flood bank. The geoelectrical surveys provided quantitative information about the spatial presence of the various geoelectrical/geological layers: alluvial soils, sands, gravels and clays. ERT allowed maps to be constructed showing subsurface structure. A combination of geoelectrical and geological information resulted in a much better identification of the geological structure.

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Alfano, L. "Geoelectrical methods applied to structures of arbitrary shapes." Journal of Applied Geophysics 29, no. 3-4 (1993): 193–209. http://dx.doi.org/10.1016/0926-9851(93)90004-i.

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9

Rokityansky, I. I., and A. V. Tereshyn. "Donbas geoelectrical structure." Geofizicheskiy Zhurnal 44, no. 1 (2022): 158–72. http://dx.doi.org/10.24028/gzh.v44i1.253717.

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The Donbas was formed as the result of Late Devonian rifting of the East European craton. During the Carboniferous, the subsidence of the basin and sedimentation were at their maximum, and a 15-kilometer stratum of Carboniferous deposits formed in the Donbas. The total thickness of the deposits reaches more than 20 km. The next important event was folding, which occurred in the Late Triassic — Early Jurassic and Late Cretaceous — Early Tertiary. The inversion lifted the upper part of the folded Donbas and subsequent erosion exposed the Carboniferous coal-bearing strata on the surface of the ea

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10

Aryani, Ersa Shasqia, Inge Larisa Rahmadhani, Muhammad Yazid, and Setyo Dwi Kartika. "Wastewater leakage identification in WWTP and concrete pipelines using integrated geophysical imaging methods." E3S Web of Conferences 485 (2024): 02010. http://dx.doi.org/10.1051/e3sconf/202448502010.

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Industry and mining activities covers a broad spectrum of processes that dispose an abundant amount of wastewater. Given the vast array of industries, there are equally large number of heavy metals, organic solvents, and hydrocarbons pollutants associated with its wastewater, posing a great threat to aquifers, especially groundwater. Main contributor of this polluting scheme are from the leakage of underground/surface storage tanks, effluent pipework, industrial sewers, and waste injection system. To ascertain the presence of pollution in the subsoil and groundwater resources, an integrated ge

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11

Arnaut, Filip, and Branislav Sretenović. "Landslide investigations using the geoelectrical scanning method and ground penetrating radar: Case studies." Tehnika 76, no. 4 (2021): 419–25. http://dx.doi.org/10.5937/tehnika2104419a.

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Geotechnical investigations of landslides for future mitigation are a complex task. To obtain relevant information, various geophysical methods are used, with varying degrees of success. The geoelectrical scanning method, also known as Electrical Resistivity Tomography (ERT) has been successfully applied in several locations in Serbia in the las three decades. The geoelectrical scanning method was used during investigations of landslides: Umka, Lukovska banja, Tara, and Trandžament, while both geoelectrical scanning and Ground Penetrating Radar (GPR) were utilized at the Trandžament landslide.

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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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Oktaviana, Latif, Hazhiyah Ula, and Purnama Yoga. "Application of geoelectrical methods for identification of soil layer." Journal of Applied Engineering Science 19, no. 4 (2021): 874–79. http://dx.doi.org/10.5937/jaes0-29022.

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Landslide is a geological event caused by the movement of rock or land mass that can be defined as the displacement of slope-forming material, which is the original rock as well as the other material that is moving with the gravity. The factors that influence landslides are soil layer, slip surface and saturated soil. Mapping or determining the landslide area is done by identifying several parameters that can trigger landslide. The geophysical method that can be used to analyse soil layer is resistance type of geoelectrical. Variations of each rock or soil layer resistance below the measuring

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Carrier, A., F. Fischanger, J. Gance, G. Cocchiararo, G. Morelli, and M. Lupi. "Deep electrical resistivity tomography for the prospection of low- to medium-enthalpy geothermal resources." Geophysical Journal International 219, no. 3 (2019): 2056–72. http://dx.doi.org/10.1093/gji/ggz411.

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SUMMARY The growth of the geothermal industry sector requires innovative methods to reduce exploration costs whilst minimizing uncertainty during subsurface exploration. Until now geoelectrical prospection had to trade between logistically complex cabled technologies reaching a few hundreds meters deep versus shallow-reaching prospecting methods commonly used in hydro-geophysical studies. We present a recent technology for geoelectrical prospection, and show how geoelectrical methods may allow the investigation of medium-enthalpy geothermal resources until about 1 km depth. The use of the new

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Malik, Usman, Defrianto Defrianto, Zulfa Zulfa, Yohanes Dwi Saputra, and Juandi Muhammad. "One-dimensional analysis of underground water using geoelectric methods." Science, Technology and Communication Journal 4, no. 1 (2023): 11–14. http://dx.doi.org/10.59190/stc.v4i1.252.

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The regional development issues in Tambang Kampar District that are most important to solve are environmental issues related to surface water potential and limited clean water. Environmental potential through good environmental management can become potential natural resources that can be utilized to support the regional economic sector. Groundwater potential needs to be studied and interpreted in the matrix of groundwater resource management through geophysical studies, namely by using the geoelectric method. This matrix will be able to provide solutions to environmental problems with the pot

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Supper, R., A. Römer, B. Jochum, G. Bieber, and W. Jaritz. "A complex geo-scientific strategy for landslide hazard mitigation – from airborne mapping to ground monitoring." Advances in Geosciences 14 (January 2, 2008): 195–200. http://dx.doi.org/10.5194/adgeo-14-195-2008.

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Abstract. After a large landslide event in Sibratsgfäll/Austria several exploration methods were evaluated on their applicability to investigate and monitor landslide areas. The resulting optimised strategy consists of the combined application of airborne electromagnetics, ground geoelectrical measurements and geoelectrical monitoring combined with hydrological and geological mapping and geotechnical modelling. Interdisciplinary communication and discussion was the primary key to assess this complicated hazard situation.

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Telesca, L., G. Colangelo, K. Hattori, and V. Lapenna. "Principal component analysis of geoelectrical signals measured in the seismically active area of Basilicata Region (southern Italy)." Natural Hazards and Earth System Sciences 4, no. 5/6 (2004): 663–67. http://dx.doi.org/10.5194/nhess-4-663-2004.

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Abstract. Geoelectrical fluctuations are the end product of several geophysical phenomena. In particular geoelectrical signals measured in seismically active areas can be attributed to stress and strain changes, associated with earthquakes. The complexity of this problem has suggested the development of advanced statistical methods to investigate the heterogeneous nature of these fluctuations. In this paper we analysed the time dynamics of short-term variability of geoelectrical field measured at Giuliano station, located in Basilicata Region, one of the most seismically active areas of southe

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18

Gujahar, Rengje Danlami Rogers, and Ayegba Abdullahi. "Application of Satellite Remote Sensing, GIS and Geoelectrical Resistivity Methods for Groundwater Potential Mapping for Jos and Environs, Plateau State, North Central Nigeria." International Journal of Trend in Scientific Research and Development 1, no. 5 (2017): 1163–71. https://doi.org/10.31142/ijtsrd2452.

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An integrated approach of Remote sensing GIS and geoelectrical resistivity methods was employed to produce groundwater potential map for Jos and environs through theGISraster based Multi Criteria Evaluation MCE analysis of five thematic layers. These layers drainage density, lineament density, Landuse cover, slope steepness and overburden thickness wereextractedfrom Nigeria Sat X, ASTERGDEM and geoelectrical resistivity methods. The result revealed four categories of groundwater potential zones as, very high, high, moderate, and low. About 105km2 18.4 was classified as very high groundwater po

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Vu, Nguyen Trong, Nguyen Ba Duan, and Tran Dinh Tung. "Geoelectrical investigations on coastal aquifers to assess the saline water intrusion in Nghi Son, Thanh Hoa." Tạp chí Khoa học và Công nghệ biển 17, no. 4B (2017): 115–22. http://dx.doi.org/10.15625/1859-3097/17/4b/12999.

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This paper presents the results of geoelectrical investigations for delineation of the aquifers and determination the hydrogeological situation of the water bearing in Nghi Son economic zone. Following the geophysical investigations and the stratification of geological formation, the boundary between fresh and saline water is determined in study area. The geoelectrical measurements indicate that the saline water intrusion within the Pleistocene aquifer occurs along the coastline of the Northeast part of Nghi Son economic zone. The values of formation resistivity below 20 Ωm imply that the wate

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COLANGELO, GERARDO, VINCENZO LAPENNA, and LUCIANO TELESCA. "ANALYSIS OF CORRELATION PROPERTIES IN GEOELECTRICAL DATA." Fractals 11, no. 01 (2003): 27–38. http://dx.doi.org/10.1142/s0218348x03001471.

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This paper considers four geoelectrical time series, measured in a seismic area of Southern Italy. Lomb Periodogram method, Higuchi analysis, Detrended Fluctuation Analysis (DFA) and the mean distance spanned within time L are used to discuss the correlation properties of these signals. The values of the scaling exponents from these methods of the geoelectrical data indicate that the long-range correlations are present. Furthermore, it is found that these correlations are all linear.

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Azizah, Nurul, Nadya Hari Pratiwi, Annisa Permata Islami, and Nur Islami. "Application of Geoelectrical Resistivity Methods for Mapping of Seawater Intrusion." Journal of Physics: Conference Series 1351 (November 2019): 012094. http://dx.doi.org/10.1088/1742-6596/1351/1/012094.

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Appel, Erwin, Jörg Wilhelm, and Martin Waldhör. "Archaeological prospection of wall remains using geoelectrical methods and GPR." Archaeological Prospection 4, no. 4 (1997): 219–29. http://dx.doi.org/10.1002/(sici)1099-0763(199712)4:4<219::aid-arp84>3.0.co;2-d.

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Giamboro, Wrego Seno, Puji Pratiknyo, Ardian Novianto, and Lisna Tri Utami. "Analisa Persebaran Wetland Berdasarkan Metode Geolistrik di Kecamatan Pandak, Kab. Bantul, DIY." Jurnal Mineral, Energi, dan Lingkungan 4, no. 2 (2021): 1. http://dx.doi.org/10.31315/jmel.v4i2.3030.

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ABSTRAKWetland merupakan tanah lunak tersaturasi air yang berada di dekat permukaan yang menjadi permasalahan dalam pembangunan di sekitar daerah penelitian di Desa Gilangharjo, Kab. Bantul, DIY. Oleh karena itu dilakukan pengukuran metode geolistrik untuk mengetahui persebaran kedalaman wetland di sekitar daerah penelitian sebagai bahan kajian pendukung dalam program pembangunan desa. Dalam penelitian ini dilakukan pengukuran metode geolistrik sounding sebanyak lima titik sounding, kemudian data lapangan diproses menggunakan pemodelan inversi 1 Dimensi (1D) untuk mendapatkan kurva model 1D re

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Baban, Ezzadin, Abdulla Amin, and Kwestan Ahmed. "Combined Geoelectrical Tomography (ERT/IP) Methods and Geoelectrical ‎Parameters to Evaluate Groundwater in Qularaisi Area NW Sulaimani-Kurdistan Region-IRAQ." Iraqi National Journal of Earth Science (INJES) 23, no. 1 (2023): 1–34. http://dx.doi.org/10.33899/earth.2023.135144.1024.

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RĂDULESCU, Vlad, Florian RĂDULESCU, and Ioan STAN. "Geoelectrical Measurements Applied to the Assessment of Groundwater Quality." Geo-Eco-Marina No 12/2006 (December 31, 2006): 107–10. https://doi.org/10.5281/zenodo.57382.

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Abstract. The aim of this paper is to convince both the specialists in the drilling fields and those in the environmental protection field to use the geophysical methods of investigation, especially in the field of water supply. It is almost essential to use geophysical methods especially in the geoelectrical domain when you have drilled for water if you take into consideration the possibility this method gives of an optimum setting for estimating the quality of these waters. Below we are laying before you some examples of water quality estimation through geophysical methods. We are also menti

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Fauzan, M., Syafrizal, Deassy Siska, and Khalsiah. "Analysis of Area Potential Landslides on Elak Roads Using Geoelectrical Methods." Journal of Social Responsibility,Tourism and Hospitality, no. 22 (February 8, 2022): 6–13. http://dx.doi.org/10.55529/jsrth.22.6.13.

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A landslide is a geological event that occurs when rock masses move together. The combination of high rainfall and steep topography and weathered rock creates a landslide-prone environment The many deformations and cracks along Jalan Lintas Elak indicate that the area is prone to landslides. This condition is unquestionably linked to the lithological conditions beneath the surface: Resistivity data measurements were carried out using the electrical resistivity method of the Wenner-Schlumberger array on two-line with a length of each line of 220 m to determine these conditions. The presence of

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Ikard, S. J., A. Revil, M. Schmutz, M. Karaoulis, A. Jardani, and M. Mooney. "Characterization of Focused Seepage Through an Earthfill Dam Using Geoelectrical Methods." Groundwater 52, no. 6 (2013): 952–65. http://dx.doi.org/10.1111/gwat.12151.

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Ramazi, Hamidreza, and Kamran Mostafaie. "Application of integrated geoelectrical methods in Marand (Iran) manganese deposit exploration." Arabian Journal of Geosciences 6, no. 8 (2012): 2961–70. http://dx.doi.org/10.1007/s12517-012-0537-2.

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Sá, Gilvan, Anne Karine Nunes da Mata Silva, Ewerton Aparecido Rodrigues, and Marco Antonio da Silva Braga. "Assessment of Geoelectrical and Seismic Methods for Tailing Dams – Catalão GO." Revista de Geociências do Nordeste 11, no. 1 (2025): 696–707. https://doi.org/10.21680/2447-3359.2025v11n1id38814.

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Mining tailings dams are engineered structures designed for the disposal of waste materials generated during mineral processing. These structures require continuous geotechnical monitoring, including visual inspections and manual or automated instrumentation, to ensure their safety and stability. This paper presents the application and results of geophysical methods used to monitor and investigate a tailings dam. In Brazil, recent dam failures have prompted significant improvements in legislation, technical standards, and geotechnical investigation protocols. Electrical resistivity was employe

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Maurer, Hansruedi, Andrew Curtis, and David E. Boerner. "Recent advances in optimized geophysical survey design." GEOPHYSICS 75, no. 5 (2010): 75A177–75A194. http://dx.doi.org/10.1190/1.3484194.

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Survey design ultimately dictates the quality of subsurface information provided by practical implementations of geophysical methods. It is therefore critical to design experimental procedures that cost effectively produce those data that maximize the desired information. This review cites recent advances in statistical experimental design techniques applied in the earth sciences. Examples from geoelectrical, crosswell and surface seismic, and microseismic monitoring methods are included. Using overdetermined 1D and 2D geoelectrical examples, a minor subset of judiciously chosen measurements p

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Mycka, Mateusz, and Maciej Jan Mendecki. "An application of geoelectrical methods for contamination plume recognition in Urbanowice waste disposal." Contemporary Trends in Geoscience 2, no. 1 (2013): 42–47. http://dx.doi.org/10.2478/ctg-2014-0006.

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ABSTRACT The purpose of this work was to detect groundwater pollution and to identify the conditions of soil and groundwater near the Urbanowice landfill site using geoelectrical measurements. Presented measurements are preliminary results from tested site and are beginning of continuous monitoring. Contamination outflows detected by resistivity and IP technique show a good correlation with available hydrological data. Contamination plume were found in Eastern part of survey profil.

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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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Arisanto, Pranu, Daru Jaka Sasangka, Andi Patiroi, Didit Puji Riyanto, Wahyu Prasetyo, and Dinggatanta Dinggatanta. "Nilai Resistivitas dan Durabilitas Batu Lempung dan Batu Pasir pada Proyek Pembangunan Bendungan Jragung." Jurnal Talenta Sipil 8, no. 1 (2025): 393. https://doi.org/10.33087/talentasipil.v8i1.839.

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Each type of rock has different resistivity values as well as durability. Continuous geoelectrical data is highly beneficial for estimating the distribution of rocks based on their resistivity values. The purpose of this study is to observe the resistivity patterns of each rock unit, both subsurface and exposed in the field, where each rock unit has specific durability values. The geoelectrical survey was conducted using the Dipole-Dipole and Wenner-Schlumberger methods with the Multichannel Resistivity MAE X 612 EM+ instrument. A case study was carried out at one of the excavation sites at Jr

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Βαφείδης, Α., Μ. Μανούτσογλου, H. Hamdan, et al. "GEOPHYSICAL SURVEY AT THE OMALOS PLATEAU, CHANIA, CRETE." Bulletin of the Geological Society of Greece 36, no. 3 (2004): 1204. http://dx.doi.org/10.12681/bgsg.16463.

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This paper discusses the preliminary results of a geophysical survey that was carried out at the Omalos plateau in Chania, Crete. The geophysical survey included measurements of electrical tomography, electrical mapping, seismic refraction, georadar, VLF and gravity. The aim of this survey is to compare the results from different geophysical methods used in imaging dolines and karstic features. The processing of the measurements indicates three geoelectrical layers. The first layer of extremely high electrical resistivity is attributed to alluvial - dilluvial deposits. The second layer of very

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Høyer, Anne-Sophie, Ingelise Møller, and Flemming Jørgensen. "Challenges in geophysical mapping of glaciotectonic structures." GEOPHYSICS 78, no. 5 (2013): B287—B303. http://dx.doi.org/10.1190/geo2012-0473.1.

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Glaciotectonic complexes have been recognized worldwide — traditionally described on the basis of outcrops or geomorphological observations. In the past few decades, geophysics has become an integral part of geologic mapping, which enables the mapping of buried glaciotectonic complexes. The geophysical methods provide different types of information and degrees of resolution and thus, a different ability to resolve the glaciotectonic structures. We evaluated these abilities on the basis of an integrated application of four commonly used geophysical methods: airborne transient electromagnetics,

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Stoll, Johannes B., and Karsten Bahr. "Optimization of signal‐to‐noise ratio in dc soundings." GEOPHYSICS 65, no. 5 (2000): 1495–500. http://dx.doi.org/10.1190/1.1444838.

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Geoelectric (dc) sounding methods are usually limited to electrode spacings smaller than 1 km, which restrict the depth of investigation to only several hundreds of meters. Greater depths of investigation require both a larger electrode spacing and motor‐generator driven transmitters. In order to increase the depth of investigation into the middle crust, the distance between transmitter and receiver dipole must be increased up to 100 km as well. Instead of a Schlumberger electrode configuration, we use a dipole‐dipole electrode arrangement, which avoids cable connections of several tens of kil

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Sastrawan, F. D., and W. Romadhon. "Application of geoelectrical methods for estimating the availability of shallow aquifer layers." Journal of Physics: Conference Series 1763, no. 1 (2021): 012062. http://dx.doi.org/10.1088/1742-6596/1763/1/012062.

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Mitrofan, Horia, Ioan Povară, and Mihai Mafteiu. "Geoelectrical investigations by means of resistivity methods in karst areas in Romania." Environmental Geology 55, no. 2 (2007): 405–13. http://dx.doi.org/10.1007/s00254-007-0986-1.

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Ramazi, Hamidreza, Mohammad Reza Hossein Nejad, and Aenollah Azizzadeh Firoozi. "Application of integrated geoelectrical methods in Khenadarreh (Arak, Iran) graphite deposit exploration." Journal of the Geological Society of India 74, no. 2 (2009): 260–66. http://dx.doi.org/10.1007/s12594-009-0126-5.

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Frohlich, Reinhard K., Daniel W. Urish, James Fuller, and Mary O'Reilly. "Use of geoelectrical methods in groundwater pollution surveys in a coastal environment." Journal of Applied Geophysics 32, no. 2-3 (1994): 139–54. http://dx.doi.org/10.1016/0926-9851(94)90016-7.

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Piegari, Ester, Giorgio De Donno, Davide Melegari, and Valeria Paoletti. "A machine learning-based approach for mapping leachate contamination using geoelectrical methods." Waste Management 157 (February 2023): 121–29. http://dx.doi.org/10.1016/j.wasman.2022.12.015.

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Boyd, James P., Andrew Binley, Paul Wilkinson, Jessica Holmes, Edward Bruce, and Jonathan Chambers. "Practical considerations for using petrophysics and geoelectrical methods on clay rich landslides." Engineering Geology 334 (May 2024): 107506. http://dx.doi.org/10.1016/j.enggeo.2024.107506.

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Akinlabi I. A. and Olanrewaju S. A. "Assessment of Seepage in an Embankment Dam Using Very Low Frequency Electromagnetic and Geoelectrical Methods." Asian Journal of Environment & Ecology 23, no. 7 (2024): 114–24. http://dx.doi.org/10.9734/ajee/2024/v23i7568.

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Geoephysical surveys involving Very Low Frequency Electromagnetic (VLF-EM), Vertical Electrical Sounding (VES) and 2D resistivity imaging were conducted along the embankment of Asejire dam to detect potential seepage zones and assess the integrity of the dam. 750 VLF-EM measurements were made at 10 m station interval using the VLF-EM Equipment. 24 Schlumberger VES were conducted at 20 m interval using resistivity meter and its accessories. The current electrode spacing (AB/2) was varied from 1 m to 100 m. The 2D resistivity profiling employed the dipole-dipole configuration with electrode spac

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Somba, Bunga Elim, Saiful Darman, Rachmat Zainuddin, and Raihanda Dwimart Mangawe. "GEOLOGICAL MODELLING OF LITHOSEQUENT BASED ON DEM AND FINITE ELEMENT METHOD INVERSION OF VES DATA." AGROLAND The Agricultural Sciences Journal (e-Journal) 9, no. 2 (2022): 98–106. http://dx.doi.org/10.22487/agroland.v9i2.1476.

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The aims of this study are to develop interpretation of structural geology in lithosequent using DEM and finite elemen method based on VES data. This research was conducted on June 2021 untill January 2022 at Pasang District, North Toraja. Four main point location were selected and recorded in google earth. Those points were processed using software QGIS for developing 3D model, Saga-GIS for interpolated DEM and VES for generating 1D and 2D geoelectrical modelling. Data were interpolated using Universal Kriging method and analysed using IP2WIN software. The results of these research shows that

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Silva Filho, Antonio M., José R. S. Silva, Glaciano M. Fernandes, Lucas D. S. Morais, Antonio P. Coimbra, and Wesley P. Calixto. "Root System Analysis and Influence of Moisture on Soil Electrical Properties." Energies 14, no. 21 (2021): 6951. http://dx.doi.org/10.3390/en14216951.

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This paper proposes a methodology for plant root system and soil moisture analysis through the geoelectrical prospecting method. Overall, bench and field experiments are implemented to analyze the behavior of electrical conductivity of the soil in relation to moisture content and plant root system growth. Specifically, Wenner array and lateral profiling technique are used to stratify the soil in horizontal layers, performing in-depth analysis. Millet (Pennisetum glaucum L.), bean (Phaseolus vulgaris L.) and sorghum (Sorghum bicolor L. Moench) are used to analyze the root system behavior. Resul

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Khalilidermani, Mitra, Dariusz Knez, and Mohammad Ahmad Mahmoudi Zamani. "Empirical Correlations between the Hydraulic Properties Obtained from the Geoelectrical Methods and Water Well Data of Arak Aquifer." Energies 14, no. 17 (2021): 5415. http://dx.doi.org/10.3390/en14175415.

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A number of empirical correlations have been achieved between the hydraulic properties measured through geoelectrical methods and water well data of Arak Aquifer located in Markazi province, Iran. The geoelectrical method of Vertical Electrical Sounding (VES) technique was used to calculate the hydraulic properties of the aquifer. Through the VES technique, the pivotal hydraulic properties such as porosity, hydraulic conductivity, and specific yield of the layers were calculated. The results of VES technique were compared with the data obtained from seven observation water wells that were alre

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Hasan, M. F. R., A. Susilo, E. A. Suryo, et al. "The use of geoelectrical resistivity methods to detect the potential landslides in Payung, Batu City, Indonesia." IOP Conference Series: Earth and Environmental Science 1347, no. 1 (2024): 012003. http://dx.doi.org/10.1088/1755-1315/1347/1/012003.

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Abstract Landslides are a serious threat as they cause damage, loss of economic assets, infrastructure, and productive land. When entering the rainy season, several areas in Indonesia often experience landslides; one of them is Batu City, which has experienced 267 landslides in the last 4 years (2019-2022). This research aims to map landslide susceptibility areas in the research area using the geoelectrical resistivity method. This research uses the geoelectrical resistivity method with 10 measurement points, and the distance between electrodes is 10 meters. Data analysis is presented in 1D, t

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Thong, Kieu Duy. "Inversion of multiple data sets acquired by different array configuration of geoelectrical resistivity method." Journal of Mining and Earth Sciences 61, no. 1 (2020): 52–60. http://dx.doi.org/10.46326/jmes.2020.61(1).06.

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The geoelectrical resistivity method is one of the most commonly used geophysical methods. This method uses different electrodes configuration, electrode array, depending on the purpose and conditions of the field, each type of array has its advantages and disadvantages. Due to the development of data acquisition technology, it is common for geoelectrical instruments enable to record data arising from different electrode arrays with negligible real-time construction. However, current software’s only allows to process for each individual electrode array. Inverted models of different electrode a

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Raj, A. Stanley, D. Hudson Oliver, and Y. Srinivas. "Geoelectrical Data Inversion by Clustering Techniques of Fuzzy Logic to Estimate the Subsurface Layer Model." International Journal of Geophysics 2015 (2015): 1–11. http://dx.doi.org/10.1155/2015/134834.

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Soft computing based geoelectrical data inversion differs from conventional computing in fixing the uncertainty problems. It is tractable, robust, efficient, and inexpensive. In this paper, fuzzy logic clustering methods are used in the inversion of geoelectrical resistivity data. In order to characterize the subsurface features of the earth one should rely on the true field oriented data validation. This paper supports the field data obtained from the published results and also plays a crucial role in making an interdisciplinary approach to solve complex problems. Three clustering algorithms

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Rizzo, E., V. Giampaolo, L. Capozzoli, and S. Grimaldi. "Deep Electrical Resistivity Tomography for the Hydrogeological Setting of Muro Lucano Mounts Aquifer (Basilicata, Southern Italy)." Geofluids 2019 (February 27, 2019): 1–11. http://dx.doi.org/10.1155/2019/6594983.

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The proposed work concerns the application of a deep geoelectrical survey to a carbonate aquifer in order to define the best location for exploitation well drilling for increasing water supply. However, an optimal characterization of a groundwater resource is the necessary condition to reach the indicated aim. Therefore, the geoelectrical investigation was guided from the previous geological and hydrogeological characterization. Moreover, geophysical methods are good tools to improve the groundwater model when detailed information is necessary, such as the localization of a pumping well. The w

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