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Geoelectrical Resistivity Imaging Survey was conducted in order to profile the resistivity of materials down to a depth 130 m from the surface. In this study five transect lines, perpendicular to the shoreline were constructed. The result indicates the existence of a thick geoelectricallayer with low resistivity « 10 Wm) at the upper portion of the profile. This may be due to saltwater intrusion from the sea, and the aquifer system behaves as semi confined layer(s) that causes the salty water from surface to penetrate downward. The thickness of the low resistivity layer is increasing toward the sea. Electrical conductivity measurement of water samples from boreholes, river and sea is undertaken to support this study. Furthermore, the regional conductivity values of the study area were derived from the geoelectrical imaging profile. Result from utilizing this technique also supports the result of geoelectrical resistivity imaging.

Kaedah keberintangan geoelektrik profil dalam untuk kajian air tanah di lembangan Kuala Langat, Banting, Selangor