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contributor authorBernhard H. Schmid
date accessioned2017-05-08T21:24:21Z
date available2017-05-08T21:24:21Z
date copyrightJune 2008
date issued2008
identifier other%28asce%291084-0699%282008%2913%3A6%28505%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/50207
description abstractLongitudinal solute transport modeling requires knowledge of the transport parameters involved. At best, these parameters have been estimated from stream tracer experiments, usually conducted, however, at flow rates different from those characterizing the intended application. Thus, the mathematical simulation of breakthrough curves invariably rests on a transfer of parameters, resulting in errors of an a priori unknown magnitude. In the research reported here, data from nine stream tracer experiments performed on the same channel reach have been used to find out, up to which ratio of respective flow rates transport parameter transfer will still yield acceptable modeling accuracy. The results of the study (obtained with the transient storage model of longitudinal solute transport) suggest that parameter transfer across a range of flow rates not exceeding a ratio of 1:2 will be associated with errors in peak concentrations below the 40% mark.
publisherAmerican Society of Civil Engineers
titleCan Longitudinal Solute Transport Parameters Be Transferred to Different Flow Rates?
typeJournal Paper
journal volume13
journal issue6
journal titleJournal of Hydrologic Engineering
identifier doi10.1061/(ASCE)1084-0699(2008)13:6(505)
treeJournal of Hydrologic Engineering:;2008:;Volume ( 013 ):;issue: 006
contenttypeFulltext


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