Yangtze River ADCP Discharge Measurement Using Multiple External Sensor Inputs

Randy Marsden¹, Chen Shongshen², Ye Dexun³, Wei Jinchun⁴, Hening Huang⁵

¹Inland Product Manager, RD Instruments, 9855 Businesspark Ave., San Diego, CA 92129, USA
²Chief Engineer, Bureau of Hydrology, Changjiang Water Resources Commission,
Wuhan, Hubei, P.R. of China
³Chief Hydrologist, Three Gorges Huangling Temple Station,
Changjiang Water Resources Commission, Yichang, HuBei, P.R. China
⁴Deputy Chief, Scienfitific and Research Institute,
Changjiang Water Resources Commission, Wuhan, Hubei, P.R. of China
⁵Chief Hydraulic Engineer, RD Instruments,
9855 Businesspark Ave., San Diego, CA 92129, USA

During high flow season, the sediment load of the Yangtze River can reach 20 grams per liter. When the sediment load is high, acoustic absorption and scattering interfere with the bottom tracking of ADCPs used to measure discharge on the Yangtze River. In addition, the Changjiang Water Resources Commission (CWRC) uses 30 meter steel hulled vessels to perform discharge measurements on much of the Yangtze River. The steel hull of the vessel prevents using the ADCP’s internal flux-gate compass as a heading reference. We performed tests to determine if accurate discharge measurement could be performed using an ADCP to measure water velocity, a depth sounder for water depth, DGPS to determine vessel speed over ground, and a gyrocompass to provide heading information.

The tests were performed during normal flow conditions when the ADCP bottom tracking is reliable. Using four different ADCPs with the three other external devices, we measured discharge at the CWRC Three Gorges Huangling Temple Hydrology Station. Discharge computed using the external depth sounder, DGPS, and gyrocompass was found to be within 2% of the discharge computed using the ADCP alone. The results of those tests are presented in this paper.