
Subsurface Geological and Hydrogeological Conditions of the Matale District, Sri Lanka: Inferred from Vertical Electrical Sounding Curves
Abstract
The electrical resistivity method which has important applications in mineral resources and groundwater exploration is used to map variations in the electrical properties of the subsurface. The study area, the District of Matale forms a part of the Central Province of Sri Lanka. The major rock types of the area consist of crystalline limestone, garnet-sillimanite gneiss, charnockitic gneiss and quartzite. Fifteen vertical electrical soundings (VES) were carried out in the Matale District using the Schlumberger configuration. Initially, fifteen apparent resistivity field curves were analyzed manually. Subsequently IPI2WIN open source software was used for computational interpretation. The VES points were located mainly in three lithologies; quartzite, crystalline limestone and gneiss. Electrical conductivity of groundwater in the region was found to be uniform and had no significant salinity-based impact on the resistivity variations. The majority of resistivity layers obtained from the VES correlated with the drill logs of same points indicating a considerable degree of relevance for their application as a tool to investigate subsurface geological and hydrogeological conditions.
DOI: http://dx.doi.org/10.4038/ouslj.v6i0.4116
OUSL Journal (2010) Vol. 6, (pp. 91- 102)
© 2010 CN Nupearachchi, KM Prematilaka, ANB Attanayake, GWAR Fernando, published by Open University of Sri Lanka OUSL
This work is licensed under the Creative Commons License.