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dc.contributor.advisorFaure, Gunteren_US
dc.creatorHicks, Jamesen_US
dc.date.accessioned2014-12-11T21:19:03Z
dc.date.available2014-12-11T21:19:03Z
dc.date.issued1992-06en_US
dc.identifier.urihttp://hdl.handle.net/1811/63113
dc.description.abstractThe principal source of water in the Huron River is groundwater. However, other water types also enter the river at various localities along the course of the river. The water in the Huron River consists of a mixture of two groundwater components as well as waters from other sources whose entry into the river changes the chemical composition of the water of the Huron River along its course. Mixing and dilution occur along the entire course of the river. Initially the two groundwater components mix to form water reflecting both components. In addition, various contaminants enter the river and mix with the pristine water already in the river channel. Meteoric water serves as a diluting agent which decreases the concentrations of the elements dissolved in the water. Contaminants enter the river in the form of sewage effluent and industrial waste discharged either directly or via tributary streams. How and to what extent these influxes of water affect the chemical composition of the river can be determined through the interpretation of chemical analyses of water along the river's course. By treating the water as a series of mixtures, we can determine the natural composition of the water without the effects of contamination.en_US
dc.language.isoen_USen_US
dc.publisherThe Ohio State Universityen_US
dc.relation.ispartofseriesThe Ohio State University. Department of Geological Sciences Senior Theses; 1992en_US
dc.titleA geochemical evaluation of water quality along the course of the Huron River, Northern Ohioen_US
dc.typeThesisen_US
dc.description.embargoNo embargoen_US


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