Incorporating both physical and kinetic limitations in quantifying dissolved oxygen flux to aquatic sediments

Journal of Environmental Engineering

Volumn 135, Issue 12, 2009, Pages 1304-1314

  O'connor, Ben L ^a   Hondzo, Miki ^b   Harvey, Judson W ^a  

^a U S GEOLOGICAL SURVEY   (United States)

^b UNIVERSITY OF MINNESOTA   (United States)

Author keywords

Boundary layer flow; Dissolved oxygen; Kinetics; Mass transport; Oxygen demand; Sediment; Surface waters

Indexed keywords

AQUATIC SEDIMENTS; COHERENT MOTION; DO CONCENTRATION; EMPIRICAL MODEL; EXPERIMENTAL EVIDENCE; FINE SEDIMENTS; FLOW CONDITION; FLUME EXPERIMENT; KINETIC LIMITATIONS; LOW VELOCITIES; MASS TRANSFER COEFFICIENT; MASS TRANSPORT; MECHANISTIC MODELS; OXYGEN DEMAND; SEDIMENT SURFACE; SEDIMENT WATER INTERFACE; SURFACE RENEWAL THEORY;

ATMOSPHERIC THERMODYNAMICS; BOUNDARY LAYER FLOW; BOUNDARY LAYERS; DISSOLUTION; DISSOLVED OXYGEN SENSORS; MASS TRANSFER; SEDIMENTOLOGY; SEDIMENTS; SURFACE WATERS; THIN FILM DEVICES;

DISSOLVED OXYGEN;

BOUNDARY LAYER; CHEMICAL OXYGEN DEMAND; DISSOLVED OXYGEN; EMPIRICAL ANALYSIS; FLUID FLOW; MASS TRANSPORT; MICROSTRUCTURE; SEDIMENT CHEMISTRY; SEDIMENT-WATER INTERFACE;

EID: 70450216982     PISSN: 07339372     EISSN: None     Source Type: Journal    
DOI: 10.1061/(ASCE)EE.1943-7870.0000093     Document Type: Article

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