Changes in the surface water of the Marais de Cygnes River, 1964 to 1998.

dc.advisorDavid Saundersen_US
dc.collegelasen_US
dc.contributor.authorHanson, Kimberly C.
dc.date.accessioned2012-06-21T13:22:23Z
dc.date.available2012-06-21T13:22:23Z
dc.date.created1998en_US
dc.date.issued2012-06-21
dc.departmentphysical sciencesen_US
dc.descriptionvi, 48 leavesen_US
dc.description.abstractAcid precipitation has been moving westward in the past few decades. One way of determiner the extent of acid precipitation IS to evaluate the acidification of surface water. This study compared current with past ratios of alkalinity (HCO,) to hardness (Ca+2 & Mg+l as a measure of the acidification of the Marais de Cygnes River in east-central Kansas. At low to moderate discharge, the ratio showed no significant change, but this study found a decrease at high discharge compared with the data from the 1960s. The ratio was lowest m March, June and November, and highest m August. A site Immediately downstream from Melvern Dam had consistently lower ratios tl1at a site located further downstream m the city of Ottawa.en_US
dc.identifier.urihttp://hdl.handle.net/123456789/1400
dc.language.isoen_USen_US
dc.subjectAcid rain.en_US
dc.subjectAcid precipitation (Meteorology).en_US
dc.subjectCombustion gases-Environmental aspects.en_US
dc.subjectEnvironmental protection-Kansas.en_US
dc.titleChanges in the surface water of the Marais de Cygnes River, 1964 to 1998.en_US
dc.typeThesisen_US

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