WANG Yaping, CHU Yong Shik, LEE Hee Jun, HAN Choong Keun, OH Byung Chul. Estimation of suspended sediment flux from acoustic Doppler current profiling along the Jinhae Bay entrance[J]. Acta Oceanologica Sinica, 2005, (2): 16-27.
Citation:
WANG Yaping, CHU Yong Shik, LEE Hee Jun, HAN Choong Keun, OH Byung Chul. Estimation of suspended sediment flux from acoustic Doppler current profiling along the Jinhae Bay entrance[J]. Acta Oceanologica Sinica, 2005, (2): 16-27.
WANG Yaping, CHU Yong Shik, LEE Hee Jun, HAN Choong Keun, OH Byung Chul. Estimation of suspended sediment flux from acoustic Doppler current profiling along the Jinhae Bay entrance[J]. Acta Oceanologica Sinica, 2005, (2): 16-27.
Citation:
WANG Yaping, CHU Yong Shik, LEE Hee Jun, HAN Choong Keun, OH Byung Chul. Estimation of suspended sediment flux from acoustic Doppler current profiling along the Jinhae Bay entrance[J]. Acta Oceanologica Sinica, 2005, (2): 16-27.
Laboratory of Coast and Island Development of the Ministry of Education, Nanjing University, Nanjing 210097, China;Korea Ocean Research and Development Institute, Ansan, P O Box 29, Seoul 425-600, Korea
2.
Korea Ocean Research and Development Institute, Ansan, P O Box 29, Seoul 425-600, Korea
A Nortek acoustic Doppler current profiler (NDP) was installed on a moving vessel to survey the entrance to the Jinhae Bay on August 22~23, 2001. The current velocity and acoustic backscattering signal were collected along two cross-sections; water samples were also collected during the measurement. The acoustic signals were normalized to compensate for the loss incurred by acoustic beam spreading in the seawater. The in situ calibration shows that a significant relationship is present between suspended sediment concentrations (SSC) and normalized acoustic signals. Two acoustic parameters have been determined to construct an acoustic-concentration model.Using this derived model, the SSC patterns along the surveyed cross-sections were obtained by the conversion of acoustic data. Using the current velocity and SSC data, the flux of suspended sediment was estimated. It indicates that the sediment transport into the bay through the entrance has an order of magnitude of 100 t per tidal cycle.