Record Display for the EPA National Library Catalog

RECORD NUMBER: 217 OF 1390

OLS Field Name OLS Field Data
Main Title EFDC1D - A One Dimensional Hydrodynamic and Sediment Transport Model for River and Stream Networks: Model Theory and Users Guide.
Author Hamrick, J. M. ; Hayter, E. J. ;
CORP Author Tetra Tech, Inc., Fairfax, VA.;Environmental Protection Agency, Research Triangle Park, NC. National Exposure Research Lab.
Publisher Sep 2001
Year Published 2001
Report Number EPA-68-C-98-010; EPA/600/R-01/073;
Stock Number PB2004-101171
Additional Subjects Hydrodynamics ; Sediment transport ; User manuals(Computer programs) ; Streams ; Discharge(Water) ; Inflow ; Hydraulics ; Deposition(Sediments) ; EFDC1D computer code ; Stream networks ; EFDC1D(Environmental Fluid Dynamics Code-One Dimensional)
Internet Access
Description Access URL
http://nepis.epa.gov/Exe/ZyPDF.cgi?Dockey=P1000A59.PDF
Holdings
Library Call Number Additional Info Location Last
Modified
Checkout
Status
NTIS  PB2004-101171 Most EPA libraries have a fiche copy filed under the call number shown. Check with individual libraries about paper copy. NTIS 03/15/2004
Collation 100p
Abstract
This technical report describes the new one-dimensional (1D) hydrodynamic and sediment transport model EFDC1D. This model can be applied to stream networks. The model code and two sample data sets are included on the distribution CD. EFDC1D can simulate bi-directional unsteady flows and has the ability to accommodate unsteady inflows and outflows associated with upstream inflows, lateral inflows and withdrawals, groundwater-surface water interaction, evaporation and direct rainfall. The model also includes representation of hydraulic structures such as dams and culverts. For sediment transport, the model includes settling, deposition and resuspension of multiple size classes of cohesive and noncohesive sediments. The bed is represented by multiple layers of mixed sediment classes. A bed consolidation model is implemented to predict time variations of bed depth, void ratio, bulk density and shear strength. The sediment bed representation is dynamically coupled to the cross-sectional area representation to account for area changes due to deposition and resuspension.