Record Display for the EPA National Library Catalog

RECORD NUMBER: 6 OF 8

OLS Field Name OLS Field Data
Main Title Hypolimnetic flow regimes : in lakes and impoundments /
Author Edinger, John Eric. ; Yanagida, Norio ; Cohen., Ira M.
Other Authors
Author Title of a Work
Yanagida, Norio.
Cohen, Ira M.
CORP Author Towne School of Civil and Mechanical Engineering, Philadelphia, Pa.;Office of Water Resources Research, Washington, D.C.;Robert S. Kerr Environmental Research Lab., Ada, Okla.
Publisher Office of Research and Development,
Year Published 1974
Report Number EPA-660/2-74-053; EPA-R-800943; EPA-16080-FVK; W74-11578
Stock Number PB-235 391
OCLC Number 01865934
Subjects Groundwater flow. ; Water, Underground
Additional Subjects Lakes ; Water flow ; Stratification ; Interfaces ; Fluid friction ; Salt water ; Fresh water ; Thermal measurements ; Steady flow ; Computer programs ; Hydraulics ; Flumes ; Nonuniform flow ; Mathematical models ; Hypolimnion ; Stagnant water
Internet Access
Description Access URL
http://nepis.epa.gov/Exe/ZyPDF.cgi?Dockey=9101RIF1.PDF
Holdings
Library Call Number Additional Info Location Last
Modified
Checkout
Status
EJAD  EPA 660/2-74-053 Region 3 Library/Philadelphia, PA 08/02/1996
EJBD ARCHIVE EPA 660-2-74-053 Headquarters Library/Washington,DC 06/17/2013
EJBD  EPA 660-2-74-053 c.1 Headquarters Library/Washington,DC 09/18/2013
EKAM  TC176.E355 Region 4 Library/Atlanta,GA 03/14/1997
ELBD RPS EPA 660-2-74-053 repository copy AWBERC Library/Cincinnati,OH 04/18/2018
EMBD  EPA/660/2-74/053 GWERD Library/Ada,OK 02/17/1995
NTIS  PB-235 391 Most EPA libraries have a fiche copy filed under the call number shown. Check with individual libraries about paper copy. NTIS 01/01/1988
Collation vii, 177 pages : illustrations, diagrams ; 27 cm.
Abstract
The 'hypolimnetic flow' is a two-layered flow with the upper layer stagnant. The report presents the possibility of different flow regimes for the hypolimnetic flow which may be determined from the parameters of slope of channel bottom, flow depth, flowrate, density difference of water in the two layers, and channel roughness. The analysis is limited to the steady-state case of the hypolimnetic flow and the 'upper layer analysis' in which the lower layer is stagnant. Interfacial profile equations which predict possible existence of ten different flow regimes for the hypolimnetic flow and two regimes for the upper layer analysis were obtained from the equations of continuity and momentum for two-layered flow.
Notes
Includes bibliographical references (pages 145-146).