The Groundwater Geochemistry in a Semi Arid Fractured Crystalline Basement Area of Dodoma

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dc.contributor.authorNkotagu, Hudson H.
dc.date.accessioned2016-09-21T13:28:12Z
dc.date.available2016-09-21T13:28:12Z
dc.date.issued1996
dc.descriptionFull text can be accessed at http://www.sciencedirect.com/science/article/pii/S0899536297000213en_US
dc.description.abstractThe chemical character of groundwater is generated through processes including the leaching of surficial and near-surface soil salts, cation exchange and mineral dissolution of, in this case, mainly amphiboles and sodic plagioclase. Molar ratios thermodynamic analysis using a NETPATH geochemical model and standard Piper trilinear and Gibbs diagrams have been used to establish these geochemical processes. Though the groundwater is dominantly of NaCl type, it is apparently suitable for general irrigation purposes.en_US
dc.identifier.citationNkotagu, H., 1996. The groundwater geochemistry in a semi-arid, fractured crystalline basement area of Dodoma, Tanzania. Journal of African Earth Sciences, 23(4), pp.593-605.en_US
dc.identifier.doi10.1016/S0899-5362(97)00021-3
dc.identifier.urihttp://hdl.handle.net/20.500.11810/3944
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.titleThe Groundwater Geochemistry in a Semi Arid Fractured Crystalline Basement Area of Dodomaen_US
dc.typeJournal Article, Peer Revieweden_US
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