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dc.creatorCooke, G. Dennisen_US
dc.creatorKennedy, Robert L.en_US
dc.date.accessioned2005-10-01T02:53:42Z
dc.date.available2005-10-01T02:53:42Z
dc.date.issued1970-05en_US
dc.identifier.citationThe Ohio Journal of Science. v70 n3 (May, 1970), 150-161en_US
dc.identifier.issn0030-0950en_US
dc.identifier.urihttp://hdl.handle.net/1811/5538
dc.descriptionAuthor Institution: Institute of Limnology, Department of Biological Sciences, Kent State University, Kent, Ohio 44240en_US
dc.description.abstractDollar Lake in Portage County, Ohio, has a volume of 86,400 cubic meters and an area of 22,212 square meters. The average depth is 3.89 meters, the maximum depth is 7.5 meters. Maximum width of the lake is 140 meters, the maximum length 215 meters. Except for brief periods in spring and fall, deep waters are depleted of dissolved oxygen. Secchi Disc transparency is frequently below one meter. Massive blooms of algae are often observed. The lake stratifies thermally in April, circulates in October, and restratifies in December after ice formation. Spring circulation occurs in March. Dollar Lake is a dimictic, second-class, eutrophic lake.en_US
dc.format.extent804733 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.rightsReproduction of articles for non-commercial educational or research use granted without request if credit to The Ohio State University and The Ohio Academy of Science is given.en_US
dc.titleEutrophication of Northeastern Ohio Lakes. I, Introduction, Morphometry, and Certain Physico-Chemical Data of Dollar Lakeen_US


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