Identifikasi Struktur Akuifer Dangkal Berdasarkan Integrasi Kecepatan Gelombang Seismik dan Resistivitas Listrik: Studi Kasus Kawasan Terintegrasi Kemayoran
DOI:
https://doi.org/10.29303/goescienceed.v7i4.2978Keywords:
Aquifer, MASW, Seismic Refraction, ERT, KemayoranAbstract
Access to clean water in Indonesia still relies heavily on groundwater, making accurate mapping of aquifer structures essential, particularly in densely populated urban areas such as the Kemayoran Integrated Zone. Aquifer interpretation based on a single geophysical method, especially resistivity, has the potential to introduce ambiguity, since resistivity values are influenced by lithology, clay content, and fluid salinity. This study aims to identify shallow aquifer structures at two representative locations, namely Pademangan and Kemayoran, through the integration of shear wave velocity (Vs) and primary wave velocity (Vp) obtained from Multichannel Analysis of Surface Waves (MASW) and Seismic Refraction Tomography, the Vp/Vs ratio, and electrical resistivity from Electrical Resistivity Tomography (ERT) using dipole-dipole and Schlumberger configurations. The data were analyzed qualitatively based on the similarity of patterns, depths, and layer thicknesses. The results show that a shallow unconfined aquifer zone was consistently identified at depths of 15 to 45 meters, with a groundwater table at depths of 5 to 15 meters. Both locations are dominated by water-saturated clay and clayey sand with very low resistivity (<6 Ωm), indicating a possible influence of brackish water or seawater intrusion due to the proximity of the Kemayoran Integrated Zone to Jakarta's coastal area. The integration of seismic and resistivity parameters proved effective in reducing the ambiguity of single-method interpretation and provided a more comprehensive picture of aquifer structure.
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