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dc.contributor.authorMaina, J. W.
dc.contributor.authorGaciri, S.J.
dc.date.accessioned2013-06-28T11:31:59Z
dc.date.available2013-06-28T11:31:59Z
dc.date.issued1983
dc.identifier.citationJournal of African Earth Sciencesen
dc.identifier.urihttp://www.sciencedirect.com/science/article/pii/S0731724784800178
dc.identifier.urihttp://erepository.uonbi.ac.ke:8080/xmlui/handle/123456789/41726
dc.description.abstractThe hydrogeology of the area (800 km2) to the immediate north of the Nairobi Conservation Area, lying between longitudes 36°40′E and 37°00′E and latitudes 1°00′S and 1°15′S has been studied. Water samples were collected from boreholes in this area and analysed for the major mineral constituents namely Na+, K+, Ca2+, Mg2+, SiO2, total iron, F− and Cl−. The pH determinations were carried out. The concentrations of most of these mineral constituents were higher in the discharge than in the recharge area. The concentrations of these minerals relative to water use have been discusseden
dc.language.isoenen
dc.relation.ispartofseriesVolume 2, Issue 3, 1984, Pages 227–232;
dc.titleContributions to the hydrogeochemistry of the area to the immediate north of Nairobi Conservation Area, Kenyaen
dc.typeArticleen
local.publisherGeology Department, University of Nairobi, Kenyaen
local.publisherHydrogeology Section, Water Resources Department, Ministry of Water Development, Kenyaen


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