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Mapping Shallow Zones with Potential for Land Subsidence Around Subsurface Water Channels Using 2D Electrical Resistivity Tomography in Bandung
Jurnal Phi : Jurnal Pendidikan Fisika dan Fisika Terapan · Vol. 13 No. 1 (2026) · hlm. 64–77
ISSN 2549-7162, 2460-4348
Terbit 2026-09-08
Penerbit Universitas Islam Negeri Ar-Raniry
Bahasa eng
Abstrak
Recurring ground subsidence around the Cikapayang River, particularly near the Bandung Center for Groundwater and Environmental Geology (PATGTL), indicates ongoing subsurface instability despite previous remediation efforts. This phenomenon is associated with backfill soil, rainwater infiltration, and subsurface drainage structures that can reduce soil bearing capacity and promote the formation of weak zones and voids. This study aims to identify shallow subsurface conditions associated with recurring ground subsidence and potential weak zones around subsurface drainage structures. 2D Electrical Resistivity Tomography (ERT) using the Wenner–Schlumberger configuration was conducted along five survey lines, each 52 m long with a 1 m electrode spacing. The datawere processed using Res2DInv, integrated and visualized in Leapfrog Geo, and validated through synthetic forward modeling using Res2DMod. Resistivity values ranged from 4.86 to 339 Ωm. The low-resistivity zone (4–30 Ωm) was interpreted as a water-saturated clay fill layer with low bearing capacity, while the high-resistivity zone (>101 Ωm) was associated with voids and subsurface drainage structures. Land subsidence zones were identified in four sections in the central area, while potential new land subsidence zones were detected at a depth of approximately 1 m in the outermost section. The results indicate that integrating ERT, synthetic modeling, and line merging is effective inidentifying land subsidence-prone zones and supporting urban risk mitigation.
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Sumatera Institute of Technology Bandung Institute of Technology Pusat Air Tanah dan Geologi Tata Lingkungan
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Metadata asli (oai_dc)
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<dc:title xml:lang="en">Mapping Shallow Zones with Potential for Land Subsidence Around Subsurface Water Channels Using 2D Electrical Resistivity Tomography in Bandung</dc:title>
<dc:creator xml:lang="en">Putra, Rio Restu</dc:creator>
<dc:creator xml:lang="en">Antosia, Risky Martin</dc:creator>
<dc:creator xml:lang="en">Junian, Wahyu Eko</dc:creator>
<dc:creator xml:lang="en">Ruchimat, Acep</dc:creator>
<dc:subject xml:lang="en">Electrical Resistivity Tomography (ERT)</dc:subject>
<dc:subject xml:lang="en">Land Subsidence</dc:subject>
<dc:subject xml:lang="en">Geotechnical Investigation</dc:subject>
<dc:subject xml:lang="en">Geohazard Mitigation</dc:subject>
<dc:subject xml:lang="en">Groundwater Channel</dc:subject>
<dc:subject xml:lang="en">Electrical Resistivity Tomography (ERT)</dc:subject>
<dc:subject xml:lang="en">Land Subsidence</dc:subject>
<dc:subject xml:lang="en">Geohazard Mitigation</dc:subject>
<dc:subject xml:lang="en">Groundwater Channel</dc:subject>
<dc:description xml:lang="en">Recurring ground subsidence around the Cikapayang River, particularly near the Bandung Center for Groundwater and Environmental Geology (PATGTL), indicates ongoing subsurface instability despite previous remediation efforts. This phenomenon is associated with backfill soil, rainwater infiltration, and subsurface drainage structures that can reduce soil bearing capacity and promote the formation of weak zones and voids. This study aims to identify shallow subsurface conditions associated with recurring ground subsidence and potential weak zones around subsurface drainage structures. 2D Electrical Resistivity Tomography (ERT) using the Wenner–Schlumberger configuration was conducted along five survey lines, each 52 m long with a 1 m electrode spacing. The datawere processed using Res2DInv, integrated and visualized in Leapfrog Geo, and validated through synthetic forward modeling using Res2DMod. Resistivity values ranged from 4.86 to 339 Ωm. The low-resistivity zone (4–30 Ωm) was interpreted as a water-saturated clay fill layer with low bearing capacity, while the high-resistivity zone (&gt;101 Ωm) was associated with voids and subsurface drainage structures. Land subsidence zones were identified in four sections in the central area, while potential new land subsidence zones were detected at a depth of approximately 1 m in the outermost section. The results indicate that integrating ERT, synthetic modeling, and line merging is effective inidentifying land subsidence-prone zones and supporting urban risk mitigation.</dc:description>
<dc:publisher xml:lang="en">Universitas Islam Negeri Ar-Raniry</dc:publisher>
<dc:date>2026-09-08</dc:date>
<dc:type>info:eu-repo/semantics/article</dc:type>
<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
<dc:type xml:lang="en">Peer-reviewed Article</dc:type>
<dc:format>application/pdf</dc:format>
<dc:identifier>https://jurnal.ar-raniry.ac.id/index.php/jurnalphi/article/view/34835</dc:identifier>
<dc:identifier>10.22373/p-jpft.v13i1.34835</dc:identifier>
<dc:source xml:lang="en">Jurnal Phi : Jurnal Pendidikan Fisika dan Fisika Terapan; Vol. 13 No. 1 (2027); 64-77</dc:source>
<dc:source xml:lang="id">Jurnal Phi: Kurnal Pendidikan Fisika & Terapan; Vol 13 No 1 (2027); 64-77</dc:source>
<dc:source>2549-7162</dc:source>
<dc:source>2460-4348</dc:source>
<dc:language>eng</dc:language>
<dc:relation>https://jurnal.ar-raniry.ac.id/index.php/jurnalphi/article/view/34835/13444</dc:relation>
<dc:rights xml:lang="en">Copyright (c) 2026 Rio Restu Putra, Risky Martin Antosia, Wahyu Eko Junian, Acep Ruchimat</dc:rights>
<dc:rights xml:lang="en">http://creativecommons.org/licenses/by-nc/4.0</dc:rights>
</oai_dc:dc>
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APA 7
Putra, R. R., Antosia, R. M., Junian, W. E., & Ruchimat, A. (2026). Mapping Shallow Zones with Potential for Land Subsidence Around Subsurface Water Channels Using 2D Electrical Resistivity Tomography in Bandung. Jurnal Phi : Jurnal Pendidikan Fisika dan Fisika Terapan, 13(1), 64–77. https://doi.org/10.22373/p-jpft.v13i1.34835
Salin
IEEE
R. R. Putra, R. M. Antosia, W. E. Junian, and A. Ruchimat, “Mapping Shallow Zones with Potential for Land Subsidence Around Subsurface Water Channels Using 2D Electrical Resistivity Tomography in Bandung,” Jurnal Phi : Jurnal Pendidikan Fisika dan Fisika Terapan, vol. 13, no. 1, pp. 64–77, 2026, doi: 10.22373/p-jpft.v13i1.34835.
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