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Measurement of Tidal Flows in the Sacramento-San Joaquin Delta, California
Richard N. Oltmann and Michael R. Simpson, USGS

Acoustic Technology Being Used to Measure Delta Flows

UVM Station SchematicsUltrasonic Velocity Meter (UVM) station. Channel top and cross-section views.
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A UVM (Laenen, 1985) transmits acoustic pulses back and forth across a channel and precisely measures the travel time of each pulse. The difference in travel time between a pair of back and forth pulses provides an average velocity (Vp) across the channel at the depth of the transducers. The measured velocity (Vp) is not an average cross-sectional velocity and is referred to as an "index velocity" (Vi) that is used when processing the data to determine an average cross-sectional velocity.

ADDMSAcoustic Doppler Discharge Measuring System (ADDMS).
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An ADCP-based portable flow measuring system is used to make fast and accurate flow measurements of a channel for use in calibrating a UVM. Velocity and depth are measured and the flow is computed as the ADCP traverses the channel. Flow measurements of 600-foot wide channels can be made in 2 to 3 minutes with an accuracy of 2% (Simpson and Oltmann, 1993) using only a two-man crew.

A 15-minute interval UVM tidal flow record is computed by multiplying channel cross-sectional area by average channel cross-sectional velocity. Water-surface elevation is measured at the UVM station and converted to channel cross-sectional area by a relation defined from channel geometry surveys. Average channel cross-sectional velocities are determined from ADDMS measurements and are used to define a UVM index-velocity and average channel cross-sectional velocity relation.

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Page Last Modified: Thursday, 13-Dec-2007 12:22:50 PST