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contributor authorSteven F. Railsback
contributor authorJohn M. Bownds
contributor authorMichael J. Sale
contributor authorMartha M. Stevens
contributor authorGeorge H. Taylor
date accessioned2017-05-08T21:05:23Z
date available2017-05-08T21:05:23Z
date copyrightMarch 1990
date issued1990
identifier other%28asce%290733-9372%281990%29116%3A2%28361%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/38220
description abstractAeration was measured and modeled at 28 navigation dams in the upper Ohio River basin. Dissolved oxygen (DO) deficits upstream and downstream of the dams, water temperatures, and flow rates were measured under a variety of low‐flow, high‐temperature conditions. The DO deficit downstream of each dam was modeled as a linear function of the other variables. The DO deficit upstream was found to be a consistently significant predictor of DO deficits downstream of a dam. Inclusion of temperature and flow rate generally did not significantly improve the statistical aeration models. The field data show that supersaturation can occur at some dams; this means that the reaeration ratio
publisherAmerican Society of Civil Engineers
titleAeration at Ohio River Basin Navigation Dams
typeJournal Paper
journal volume116
journal issue2
journal titleJournal of Environmental Engineering
identifier doi10.1061/(ASCE)0733-9372(1990)116:2(361)
treeJournal of Environmental Engineering:;1990:;Volume ( 116 ):;issue: 002
contenttypeFulltext


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