Towards a Correlation between Long-Term Seawater Intrusion Response and Water Level Fluctuations

Water

AbdelrahmanM. Abdelgawad¹  AshrafA. Ahmed²  Antoifi Abdoulhalik³  G.A. Hamill³ 

[1] Civil Engineering Department, Faculty of Engineering, Assiut University, 71515 Asyut, Egypt;Department of Civil and Environmental Engineering, Brunel University London, Kingston Lane, Uxbridge, Sussex UB8 3PH, UK;School of Natural and Built Environment, Queen’s University, Belfast BT7 1NN, UK;

关键词: sea level rise;    density-driven flow;    transient seawater intrusion;    saltwater intrusion predictions;    SEAWAT;   

DOI  :  10.3390/w13050719

来源: DOAJ

【 摘 要 】

Laboratory and numerical experiments were conducted to provide a quantitative steady-state analysis of the effect of incremental variations of water level on saltwater intrusion. The purpose was to seek mathematical correlations relating both the wedge toe length and the height along the coastline to the boundary head difference. The laboratory experiments were completed in a 2D sand tank where both freshwater and seawater levels were varied. The experiments were conducted for two bead sizes having different hydraulic conductivities. The numerical model SEAWAT was used to validate the results and then to perform sensitivity analysis. The experimental results show that at steady-state conditions, the logarithmic toe length could be expressed as a linear function of the boundary head difference. The linear relationship was recorded in both advancing and receding wedge phases. The linearity of the correlation was also well demonstrated with analytical solutions. Similar relationships were also derived in the scenarios where the sea level fluctuated while the freshwater boundary head was constant. The height of the saltwater wedge along the coastline was also found to be a linear function of the boundary head difference. The sensitivity analysis shows that the regression coefficients were sensitive to the hydraulic conductivity, the dispersivity, and the saltwater density, while the porosity and the rate of boundary head change induced negligible effects. The existence of a linear relationship between the logarithmic toe length and the boundary head difference was also well evidenced in a field-scale aquifer model for all the different hydrogeological aquifer conditions tested. This study is the first attempt in identifying the underlying correlation between the boundary water level variations and the main seawater intrusion (SWI) external metrics under controlled laboratory conditions, which is of great relevance from a water resources management perspective.

【 授权许可】

Unknown