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 and Engineering
StatisticsView Usage Statistics
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.
Online access for this thesis was created in part with support from the Institute of Museum and Library Services (IMLS) administered by the Nevada State Library, Archives and Public Records through the Library Services and Technology Act (LSTA). To obtain a high quality image or document please contact the DeLaMare Library at https://unr.libanswers.com/ or call: 775-784-6945.