Bernard Kipsang Rop,
- , PhD Scholar (MGSK, Reg. Geol., NEMA Expert) Department of Mining, Materials and Petroleum Engineering, Jomo Kenyatta University of Agriculture and Technology Kenya, Nairobi, ,
Abstract
The Olkaria Dome Geothermal Field in the Lake Naivasha Basin is one of Kenya’s principal geothermal resource areas, where fluid circulation and reservoir performance are strongly controlled by geological structures and hydrogeological conditions. This study integrates geological, structural, hydrogeological, mineralogical, and soil-gas data to characterize reservoir permeability and fluid flow pathways. Correlation of lithological units with drilling circulation-loss zones identifies highly fractured formations that enhance geothermal fluid movement. Mineralogical mapping delineates hydrothermal alteration associated with fluid–rock interaction, while soil-gas surveys using radon and carbon dioxide reveal fault-controlled permeable zones and subsurface connectivity within the geothermal system. The results demonstrate that structural controls significantly influence geothermal fluid circulation and reservoir behavior. These findings provide a basis for improved reservoir management, well targeting, and sustainable geothermal resource development in the Olkaria Dome Geothermal Field.
Keywords: Olkaria dome geothermal field, Lake Naivasha basin, geothermal exploration, structural geology, hydrogeology, reservoir permeability, soil-gas geochemistry
[This article belongs to Journal of Geotechnical Engineering ]
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Journal of Geotechnical Engineering
| Volume | 13 | |
| Issue | 02 | |
| Received | 23/06/2026 | |
| Accepted | 02/07/2026 | |
| Published | 12/07/2026 | |
| Publication Time | 19 Days |