This analysis identifies aquifers in Kobakma District, defining groundwater depth and distribution patterns, suggesting improved resource management.
Key Points
The study reveals two primary aquifer layers, with depths ranging from 10–60 meters for free aquifers and 100–300 meters for confined aquifers.
Groundwater sources are unevenly distributed within Kobakma District, underscoring the need for targeted extraction strategies and efficient management.
Geoelectric resistivity measurements across 13 test points facilitate the interpretation of subsurface lithology and identify potential aquifer zones.
Findings highlight the influence of fault structures on groundwater movement and the importance of sustainable water resource management in the region.