Measurement of Velocity-Concentration Covarianceby Paul S. McQuivey, Res. Hydrol.; U.S. Geological Survey, Bay St. Louis, MO,
Thomas N. Keefer, Res. Hydrol.; U.S. Geological Survey, Bay St. Louis, MO,
Serial Information: Journal of the Hydraulics Division, 1972, Vol. 98, Issue 9, Pg. 1625-1646
Document Type: Journal Paper
A single-electrode conductivity probe in a bridge circuit and a hot-film sensor and anemometer were used to make the first known measurements of the longitudinal velocity-concentration covariance, uc, along a diffusing plume in the flow. The measurements were made in a 3.87-ft (1.18-m) wide flume over three boundary roughnesses. From these measurements the Boussinesq-type mass transfer coefficient was directly evaluated and compared with the longitudinal-diffusion coefficients obtained from a floating-particle study at the water surface. Within experimental accuracy the results show that the Boussinesq-type transfer coefficient is an adequate model for describing the scalar transport process.
Subject Headings: Model accuracy | Flow measurement | Probe instruments | Boussinesq equations | Fluid velocity | Diffusion | Measuring instruments | Bridges
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