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RECORD NUMBER: 34 OF 183

OLS Field Name OLS Field Data
Main Title Diagenetic oxygen equivalents model of sediment oxygen demand /
Author Di Toro, Dominic M. ; DiToro, D. M.
CORP Author Manhattan Coll., Bronx, NY. Environmental Engineering and Science Program.;Environmental Research Lab.-Duluth, MN.
Publisher Environmental Research Laboratory, Office of Research and Development, U.S. Environmental Protection Agency ; reproduced by National Technical Information Service,
Year Published 1984
Report Number EPA-600/D-84-099; EPA-803030; EPA-805229
Stock Number PB84-177369
OCLC Number 13769291
Subjects Sedimentation and deposition--Mathematical models. ; Water quality--Mathematical models.
Additional Subjects Sediments ; Oxygen demand ; Streams ; Water pollution control ; Supply(Economics) ; Phosphorus ; Organic materials ; Algae ; Mathematical models ; Interstices ; Foreign technology ; Sediment oxygen demand ; Sinks ; Nonpoint sources ; Point sources
Internet Access
Description Access URL
http://nepis.epa.gov/Exe/ZyPDF.cgi?Dockey=2000C9YL.PDF
Holdings
Library Call Number Additional Info Location Last
Modified
Checkout
Status
EJBD ARCHIVE EPA 600/D-84-099 Headquarters Library/Washington,DC 03/23/2009
ELDD  EPA-600/D-84-099 3 copies NHEERL/MED Library/Duluth,MN 12/16/2011
NTIS  PB84-177369 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 ii, 61 leaves : ill. ; 28 cm.
Abstract
The consumption of oxygen in the overlying water by sediments is an important component in the oxygen balance of most natural waters. Conventional practice is to specify the magnitude of this sink using direct uptake measurements. Unfortunately, if the management alternative being investigated affects the supply of particulate organic material to the sediment then the use of the existing sediment oxygen demand (SOD) for dissolved oxygen projections may be in error. Examples include the oxygen consequences of phosphorus loading reductions where algal carbon decay in the sediment is a principle DO sink. It is the purpose of this paper to present a model of sediment oxygen demand which attempts to solve the problem in a fashion which ultimately dispenses with the complexity and relates sediment oxygen demand to the flux of the oxygen equivalents of all reduced substances in the interstitial water without specific regard to their identity.
Notes
Cover title. "Prepared for Environmental Research Lab.-Duluth"--Cover. "References": leaves 55-61. EPA grants