Record Display for the EPA National Library Catalog


OLS Field Name OLS Field Data
Main Title Selective withdrawal from a stratified reservoir /
Author Imberger, Jorg.
Other Authors
Author Title of a Work
Fischer, Hugo B.
CORP Author California Univ., Berkeley.
Publisher [Environmental Protection Agency, Water Quality Office],
Year Published 1970
Report Number EPA 15040 EJZ 12/70; EPA-WQO-15040-EJZ; 10750; EPA 810-R-70-043
Stock Number PB-201 726
OCLC Number 00428578
Subjects Fluid mechanics. ; Reservoirs. ; Reservoirs--Mathematical models.
Additional Subjects ( Reservoirs ; Fluid flow) ; ( Water quality ; Mathematical prediction) ; Stratification ; Density ; Model tests ; Boundary layer flow ; Thickness ; Dyes ; Isotopic labeling ; Mathematical models ; Hydraulic gradients ; Density(Mass/Volume) ; Interfaces ; Stratified reservoirs ; Selective withdrawal
Internet Access
Description Access URL
Library Call Number Additional Info Location Last
EJBD ARCHIVE EPA-15040-EJZ-12-70 Headquarters Library/Washington,DC 06/09/2014
EJBD  EPA-15040-EJZ-12-70 Headquarters Library/Washington,DC 06/26/2015
EKAD  15040 EJZ 12/70 Region 4 Library/Atlanta,GA 08/23/2002 DISPERSAL
EKAD  TC167.I4 Region 4 Library/Atlanta,GA 08/23/2002 DISPERSAL
ELBD RPS EPA 810-R-70-043 repository copy AWBERC Library/Cincinnati,OH 11/13/2018
NTIS  PB-201 726 Most EPA libraries have a fiche copy filed under the call number shown. Check with individual libraries about paper copy. 01/01/1988
Collation x, 104 pages : illustrations ; 28 cm.
The study describes both theoretically and experimentally the flow into a line sink in a linearly density stratified reservoir. The geometry of the boundaries is simplified to a parallel walled duct with the line sink at the center of the fluid. The primary focus is on partitioning the flow into distinct flow regimes, and predicting the withdrawal layer thickness as a function of the distance from the sink. Laboratory experiments verified the conclusions reached from the theoretical considerations. The withdrawal layer thicknesses were shown to be closely predicted by the integral solution. Comparison with measurements made by the Tennessee Valley Authority indicates that in a reservoir the withdrawal layers are approximately one and a half times as large as predicted. The difference in thickness is probably explained by the presence of a certain amount of turbulence in the reservoir, and interference by the rear boundary of the reservoir. (WRSIC abstract).
Prepared for the Environmental Protection Agency. "15040 EJZ 12/70." Includes bibliographical references (pages 79-81).