4.7 Article

Numerical investigation of successive land reclamation effects on hydrodynamics and water quality in Bohai Bay

Journal

OCEAN ENGINEERING
Volume 268, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.oceaneng.2022.113483

Keywords

Bohai Bay; Hydrodynamics; Water quality; Land reclamation; Residual current

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A coupled hydrodynamics-water quality model was developed to investigate the hydrodynamics and water quality changes in response to land reclamations in Bohai Bay. The simulations show that reclamations significantly impact the residual current fields and tidal prisms. The salinity isolines in the west of the bay have moved towards the open sea after reclamations from 1990 to 2006, leading to a decrease in salinity value. Furthermore, the reclamations in 2022 generate higher salinity concentrations, intensifying salinity intrusion.
The hydrodynamics and water quality evolutions in response to the land reclamations in Bohai Bay were investigated by developing a coupled hydrodynamics-water quality model. Simulated results indicate reclamations considerably change the residual current fields and decrease the tidal prisms. After 1990-2006 reclamations, salinity isolines in the west of the bay obviously move towards open sea, and cause the decrease of salinity value. Compared with the 2006 reclamation scenario, the 2022 reclamation scenario generates larger salinity concentration, thereby intensifying salinity intrusion. Besides, a large amount of dissolved inorganic nitrogen (DIN) is retained in the bay and increases its concentration value due to 1990-2006 reclamations, which almost presents opposite variation in the 2022 reclamation scenario. 1990-2006 reclamations increase phytoplankton carbon concentrations in the most bay areas, with a maximum increased value of 53.37 mu g/L. With the further construction of reclamations (2006-2022), phytoplankton carbon concentrations increase within several estuarine areas, nevertheless the decreases appear in the large areas from estuarine mouths to bay's center. Statistically, the averaged salinity concentration slightly changes in the whole bay, while the averaged DIN and phytoplankton carbon concentrations significantly increase by 14.92% and 13.33% during 1990-2006, then they decrease by 16.02% and 20.68% during 2006-2022, respectively.

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