EGU26-22118, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-22118
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Wednesday, 06 May, 17:25–17:35 (CEST)
 
Room L2
Tracking sediment tracer in an Eulerian model
Honghai Li1, Tanya Beck1, Hans Moritz2, Katherine Groth2, Trapier Puckette3, and Jon Marsh4
Honghai Li et al.
  • 1USACE/ERDC, United States of America (honghai.li@usace.army.mil)
  • 2USACE/Portland District, United States of America
  • 3RPS Group Plc., United States of America
  • 4Environmental Tracing, United Kingdom

A field survey program was designed and a numerical hydrodynamic, wave, and sediment transport model was developed to investigate transport of dredged material placed in the nearshore area of an ocean dredged material disposal site (ODMDS) adjacent to the Coos Bay inlet, Oregon. The study focuses on the understanding of coastal hydrodynamic, wave, and sediment transport processes by deploying sediment tracer and simulating the release, movement, and pathways of the tracer under combined influence of wave, current, and wind conditions within and around the immediate vicinity of the inlet.

The measured data and the model results elucidate the magnitude and spatial patterns of ebb and flood currents and capture the tidal flushing of the estuarine system. The sediment mapping feature in the numerical model performs sediment tracer tracking and helps identify sediment transport pathways that corresponds to the specific wave, hydrodynamic, atmospheric, and environmental forcing conditions during the selected simulation period. Sediment tracer tracking by data sampling and model simulation indicates that the released sediment tracer in open ocean area moves towards the inlet entrance at the initial stage of the release. Although a small portion is settled down at the inlet navigation channel, most tracer becomes entrained in the tidal flow, is carried offshore by strong ebb currents, and deposited seaward of the navigation channel. Temporal variations of sediment tracer distributions show that wave and storm conditions drive tracer transport in the open coastal area, whereas sediment pathways are primarily controlled by tidal current inside the Coos Bay and at the inlet entrance. This sediment tracer transport around the inlet system was validated by distal samples collected along the mid-reach of ODMDS.

How to cite: Li, H., Beck, T., Moritz, H., Groth, K., Puckette, T., and Marsh, J.: Tracking sediment tracer in an Eulerian model, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-22118, https://doi.org/10.5194/egusphere-egu26-22118, 2026.