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contributor authorRakesh K. Gelda
contributor authorMartin T. Auer
contributor authorSteven W. Effler
contributor authorSteven C. Chapra
contributor authorMichelle L. Storey
date accessioned2017-05-08T21:17:05Z
date available2017-05-08T21:17:05Z
date copyrightApril 1996
date issued1996
identifier other%28asce%290733-9372%281996%29122%3A4%28269%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/45542
description abstractOnondaga Lake, N.Y., experiences a marked annual dissolved oxygen depletion over the entire water column at fall turnover. Depletion occurs as a result of the entrainment of reduced substances that have accumulated in the lake's hypolimnion over the summer. Recovery (return to near-saturated conditions) occurs over a period of 3–4 weeks. Observations of dissolved oxygen (DO) levels during the recovery period of two years are used to calculate the reaeration coefficient (
publisherAmerican Society of Civil Engineers
titleDetermination of Reaeration Coefficients: Whole-Lake Approach
typeJournal Paper
journal volume122
journal issue4
journal titleJournal of Environmental Engineering
identifier doi10.1061/(ASCE)0733-9372(1996)122:4(269)
treeJournal of Environmental Engineering:;1996:;Volume ( 122 ):;issue: 004
contenttypeFulltext


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