Transportation of Sediment and Heavy Metals Resuspended by a Giant Tsunami Based on Coupled Three-Dimensional Tsunami, Ocean, and Particle-Tracking Simulations

Giant tsunamis can disturb marine sediments, leading to muddy water in nearshore areas. Marine sediments can be resuspended and transported by tsunamis, as well as by tidal, wind-forced, and density currents in coastal oceans. Marine sediment in coastal oceans around urban areas contains heavy metals and cysts of harmful algae. The resuspension of marine sediments can induce multiple forms of marine pollution, including harmful red tides and heavy metal contamination. This study evaluated heavy metal pollution caused by transport of resuspended sediment with adsorbed zinc in a pilot sea, Osaka Bay, based on a tsunamigenic earthquake scenario along the Nankai Trough, which is predicted to occur within 30 years with approximately 70% probability. Tsunami and three-dimensional ocean simulations were conducted to calculate sediment transport using a particle-tracking simulation based on tsunami-induced sediment resuspension. The simulation results suggest that particles would upwell vertically from the seabed in sediment resuspension areas that would form locally in nearshore regions, and then be transported southward offshore by estuarine circulation. Sediment transported by tidal and wind currents would gradually migrate to the southern offshore region. The remaining sediment carrying zinc in the bay would decrease to less than half of its initial volume over the 20 days following resuspension.

[1]  Shiho Kobayashi,et al.  High-resolution surface salinity maps in coastal oceans based on geostationary ocean color images: quantitative analysis of river plume dynamics , 2018, Journal of Oceanography.

[2]  E. Kobayashi,et al.  Tsunami-Tide Simulation in a Large Bay Based on the Greatest Earthquake Scenario Along the Nankai Trough , 2016 .

[3]  E. Kobayashi,et al.  Simulation of Heavy Metal Transport Induced by a Giant Tsunami Based on Nankai-Trough Earthquake: Application to Osaka Bay , 2016 .

[4]  E. Kobayashi,et al.  Estimation of the Occurrence Condition of Sediment Resuspension in Osaka Bay by Tsunami , 2015 .

[5]  雅基 佐野,et al.  大阪湾,2013 年の底層環境—主成分分析による水域区分と既往調査との比較— , 2015 .

[6]  S. Mitarai,et al.  Marine Ecosystem Networks in the Seto Inland Sea Analyzed with Coastal Connectivity , 2014 .

[7]  N. Hirose,et al.  Regional data assimilation system extended to the East Asian marginal seas , 2013 .

[8]  N. Hirose,et al.  Green’s function approach for calibrating tides in a circulation model for the East Asian marginal seas , 2012, Journal of Oceanography.

[9]  Takemi Shikata,et al.  Influence of the port facilities by the sediment transport due to tsunami , 2011 .

[10]  N. Imai Investigation of the distribution of elements of the whole of Japan and their applications , 2010 .

[11]  Fumihiko Imamura,et al.  Developing Fragility Functions for Tsunami Damage Estimation Using Numerical Model and Post-Tsunami Data from Banda Aceh, Indonesia , 2009 .

[12]  Sayaka Eguchi,et al.  Relationship between distribution of heavy metals and sedimental condition in the sediment of Osaka Bay , 2004 .

[13]  Changsheng Chen,et al.  An Unstructured Grid, Finite-Volume, Three-Dimensional, Primitive Equations Ocean Model: Application to Coastal Ocean and Estuaries , 2003 .

[14]  H. Nakata,et al.  Tidal-jet and vortex-pair driving of the residual circulation in a tidal estuary , 1994 .

[15]  T. Futawatari,et al.  STUDY ON EROSIONAL PROCESS OF SOFT MUDS , 1988 .