Hydrogeologic, hydrogeochemical and stable isotopic study of possible interactions between Lake Naivasha, shallow subsurface and Olkaria geothermal waters, Central Rift Valley, Kenya
AuthorOjiambo, Bwire S
AdvisorLyons, W. Berry
Geological Sciences & Engineering
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Possible interactions between Lake Naivasha and groundwater have been studied. Mixing of deep geothermal waters with shallow groundwaters and Lake Naivasha waters to form the average Olkaria discharge fluids is proposed as the recharge source of the Olkaria geothermal reservoir.
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