Integration of borehole and vertical electrical sounding data to characterise the sedimentation process and groundwater in Krueng Aceh basin, Indonesia

Rusydy, Ibnu; Ikhlas,; Setiawan, Bambang; Zainal, Muzakir; Idris, Syafrizal; Basyar, Khairil; Putra, Yusmardani Ariya

doi:10.1016/j.gsd.2020.100372

Cited by 21 publications

(11 citation statements)

References 14 publications

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“…The VES method is generally applied in geophysical exploration activities to determine the identification of aquifer layers [2], [3]. The VES method is also often integrated with borehole data such as in research to characterize sediment processes in Krueng Aceh [4], geotechnical investigations [5], and so on. The VES method with the Schlumberger array arrangement can provide an overview of the resistivity values of subsurface rocks [6]…”

Section: Introductionmentioning

confidence: 99%

Subsurface Layer Investigation Using The Vertical Electrical Sounding (VES) in Muara Batu and Dewantara Sub-districts

Syafrizal

Novita

Muliani

et al. 2023

Proceedings of Malikussaleh International Conference on Multidi

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Research has been carried out that aims to determine the structure of the subsurface layers in the Muara Batu and Dewantara sub-districts using the Schlumberger array Vertical Electrical Sounding method. This research was conducted at 3 location points with a track length at each point of 600 m. The data in this study were measured using the SuperSting R8/IP resistivity meter and processed using the Ip2win software. The results obtained show that the subsurface layer at point VES1 consists of alluvium with a very low resistivity value (1.2 – 5.1 Ωm), VES2 consists of top soil, clays, gravels, tuffaceous, limestones, sandstones, and calcareous mudstones with a resistivity value of 4.8 – 39.0 Ωm, and VES3 consists of clays, gravels, silty clay, sandy silty clays, tuffaceous, silt, sand, calcareous mudstones and hard rocks with a resistivity value of 8.0 – 18.7 Ωm. The subsurface of VES1 is a layer that is saturated with water and is not dense so it has liquefaction potential. While VES2 and VES3 are dense layers so that buildings built in this area will be safer against earthquakes.

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Section: Introductionmentioning

confidence: 99%

Subsurface Layer Investigation Using The Vertical Electrical Sounding (VES) in Muara Batu and Dewantara Sub-districts

Syafrizal

Novita

Muliani

et al. 2023

Proceedings of Malikussaleh International Conference on Multidi

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“…Water is the basic need of living creatures. For humans, it has become the crucial supporter for their social activities, in both private and public sectors [1]. Some areas in Indonesia have an abundant supply of water during the wet season, but some others experience drought during the dry season, i.e.…”

Section: Introductionmentioning

confidence: 99%

Detection of groundwater sources in Lembor village using geoelectrical resistivity method schlumberger configuration

Hasan

Pradiptiya²,

Setiawan³

et al. 2022

IOP Conf. Ser.: Earth Environ. Sci.

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Drought is one of the problems faced by the people of Lembor Village, Lamongan Regency, this problem will be slightly resolved if the area has reserves of groundwater sources. Therefore, this study aims to determine the existence of potential groundwater sources around Lembor Village. The method used is the geoelectrical resistivity method schlumberger configuration. Data acquisition was carried out for 10 measuring points of Vertical Electrical Sounding (VES) with a track length of 310 meters, and a distance between electrodes of 10 meters. The measurement results are then correlated between VES points to produce a 2-dimensional cross-section. The results showed that the measured resistivity value was between 0.03 Ωm to 81.1 Ωm. The structure of the subsurface layer of the study area is dominated by clay and limestone. The indications for the presence of groundwater are found at a depth between 25 to 35 meters at a track distance of 35 to 45 meters, a track distance of 170 to 180 meters, and a track distance of 270 to 280 meters with resistivity values between 0.03 Ωm to 0.32 Ωm. The indications of the presence of groundwater sources need to be investigated in a wider area, to determine the distribution and direction of groundwater flow.

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“…Even the geoelectrical method can also be combined with other methods such as Self Potential (SP) and Ground Penetrating Radar (GPR) [8], [9]. In addition, resistivity data obtained from measurements using the geoelectrical method are also often integrated with borehole data to obtain a better subsurface image [10], [11].…”

Section: Introductionmentioning

confidence: 99%

Identification of the Aquifer Layer using the Geoelectric Method in Teupin Batee Village, Aceh Besar

Idris¹,

Darisma

Pramana

et al. 2022

Bulletin of Comp. Sci. Electr. Eng.

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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 subsurface structures both vertically and horizontally. From the results of the study, it was found that there are four different layers in this research area including, the top soil layer, hard rock, tuffaceous sand and sand layer as aquifer layer. The top soil layer is mixed with tuff, sand and volcanic breccia to a depth of 8 m with a resistivity value of 5-25 ?m. The Hard rock layer is at a depth of 8 m – 30 m with a resistivity value of 45-220 ?m. The tuffaceous sand layer has a resistivity value ranging from 25-55 ?m. While the sand layer or aquifer is at a depth of 10 m – 60 m with a resistivity value of <10 ?m which is separated by a layer of tuffaceous sand between the two aquifer layers.

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Integration of borehole and vertical electrical sounding data to characterise the sedimentation process and groundwater in Krueng Aceh basin, Indonesia

Cited by 21 publications

References 14 publications

Subsurface Layer Investigation Using The Vertical Electrical Sounding (VES) in Muara Batu and Dewantara Sub-districts

Subsurface Layer Investigation Using The Vertical Electrical Sounding (VES) in Muara Batu and Dewantara Sub-districts

Detection of groundwater sources in Lembor village using geoelectrical resistivity method schlumberger configuration

Identification of the Aquifer Layer using the Geoelectric Method in Teupin Batee Village, Aceh Besar

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