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040 |aCaOODSP|beng|erda|cCaOODSP
041 |aeng|beng|bfre
0861 |aEn36-539/51-1980E-PDF
1001 |aBeltaos, S., |d1944- |eauthor.
24510|aDispersion in tumbling flow / |cby S. Beltaos.
264 1|aBurlington, Ontario : |bEnvironment Canada, National Water Research Institute = Environnement Canada, Institut national de recherche sur les eaux, |cApril 1980.
300 |a1 online resource (iv, 25 pages, 8 unnumbered pages) : |bcharts.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |a[Unpublished manuscript]
500 |aDigitized edition from print [produced by Environment and Climate Change Canada].
500 |a"This manuscript has been submitted to ASCE, J. of Hydraulics Division for publication and the contents are subject to change."
504 |aIncludes bibliographical references (pages 18-21).
5203 |a"Steep mountain streams are often in the "tumbling" flow regime, that is alternating sub- and super-critical flow with energy dissipation caused mainly by sudden changes in slope and cross section. Though longitudinal dispersion characteristics of tumbling flows are important in time-of-travel, stream gauging, and contaminant spread considerations, very little pertinent information is available. The results of a laboratory study intended to provide preliminary data on tumbling flow dispersion are discussed herein"--Abstract.
546 |aIncludes abstracts in French.
650 0|aStream measurements|xMathematical models.
650 0|aHydraulics|xMathematical models.
650 6|aCours d'eau|xJaugeage|xModèles mathématiques.
650 6|aHydraulique|xModèles mathématiques.
7102 |aNational Water Research Institute (Canada), |eissuing body.
830#0|aUnpublished manuscript (National Water Research Institute (Canada))|w(CaOODSP)9.901451
85640|qPDF|s1.19 MB|uhttps://publications.gc.ca/collections/collection_2021/eccc/en36-539/En36-539-51-1980-eng.pdf