Sabaragamuwa University of Sri Lanka

GROUNDWATER POTENTIAL AND AQUIFER TYPES IN THE PREMISES OF THE SABARAGAMUWA UNIVERSITY OF SRI LANKA

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dc.contributor.author Jayalath, R.D.M.G
dc.contributor.author Wanniarachchi, D.N.S
dc.contributor.author Ranaweera, L.V
dc.date.accessioned 2021-01-06T15:44:09Z
dc.date.available 2021-01-06T15:44:09Z
dc.date.issued 2019-11-14
dc.identifier.uri http://repo.lib.sab.ac.lk:8080/xmlui/handle/123456789/495
dc.description.abstract The gradual development of the Sabaragamuwa University of Sri Lanka (SUSL) and surrounding area introduces new buildings and reforms the natural landscape. The water demand is also increasing as the growth of the community. Therefore understanding of the underlying geological structures and feasibility of the groundwater occurrences are useful in order to overcome the impending water demand as surface water is scare in the area. Topographic and satellite maps were used for preliminary study. Fieldwork was carried out to collect geological and structural data. A detailed geology and structural maps with higher resolution were produce prior to the geophysical surveys. Geo-electrical resistivity surveys were conducted to investigate groundwater conditions of the area. Two types of geo-electrical surveys, vertical electrical sounding (VES) and electrical profiling were conducted using Schlumberger electrode configuration. ArcGIS 10.4 software was used to produce the geological map and the spatial distribution of apparent resistivity values while IPI2win software was used to analyse resistivity data. Out of eighteen VES points, nine locations were identified as possible locations for groundwater abstraction. Groundwater could be located at the depth of 25–60 m. Resistivity data indicate that the aquifers in the area as regolith type aquifers along with deep weathered rock aquifers. The most of the points close to or at valleys prevail deep groundwater aquifers. Considering all the geological, structural, and morphological features, we suggest locations at VES 1, VES 4, VES 5, VES 9 VES 11, VES 13, VES 14, VES 16, and VES 17 as most convincing for test drilling. Moreover, when considering the spatial distribution of apparent resistivity values with the depth high resistivity values could be identified within the University premises. The resistivity data could also be used to interpret subsurface conditions for engineering purposes. en_US
dc.language.iso en_US en_US
dc.publisher Sabaragamuwa University of Sri Lanka en_US
dc.subject Geology map en_US
dc.subject Groundwater en_US
dc.subject Resistivity en_US
dc.subject Sabaragamuwa University of Sri Lanka en_US
dc.title GROUNDWATER POTENTIAL AND AQUIFER TYPES IN THE PREMISES OF THE SABARAGAMUWA UNIVERSITY OF SRI LANKA en_US
dc.type Article en_US


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