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dc.contributor.authorOchola, Samuel O
dc.date.accessioned2013-05-09T12:28:10Z
dc.date.available2013-05-09T12:28:10Z
dc.date.issued2003
dc.identifier.citationM.Sc (Environmental Geology Management) Thesis 2003en
dc.identifier.urihttp://erepository.uonbi.ac.ke:8080/xmlui/handle/123456789/20866
dc.descriptionMaster of Science Thesisen
dc.description.abstractLake Nakuru is a small, shallow, alkaline-saline lake located in a closed basin, without surface outlets, in the Eastern Rift Valley, Kenya. It is located at 0° 22'S, and 36° 05'E; 1,759 m above sea level. Its water level fluctuates drastically in response to changes in rainfall and evaporation. Recent concerns on the tropospheric increase of many radiatively important trace gases has led to the need to evaluate the sources and sinks of these gases concerning the relative role of biological and environmental variables in controlling the fluxes between hydrologic, terrestrial ecosystems and the atmosphere.en
dc.description.sponsorshipUniversity of Nairobien
dc.language.isoenen
dc.titleBiogeochemistry of sediment gases in lake Nakuru, Kenyaen
dc.typeThesisen
local.publisherDepartment of Geology, University of Nairobien


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