EGU24-2205, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-2205
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Effects of Artificially Reducing Hydraulic Conductivity of Coastal Aquifers on Maximum Sustainable Withdrawal Rate

Jiazhi Sun1, Bo Fan2, and Chunhui Lu1
Jiazhi Sun et al.
  • 1The National Key Laboratory of Water Disaster Prevention, Hohai University, Nanjing, China (jzsun@hhu.edu.cn; clu@hhu.edu.cn)
  • 2Science and Technology Promotion Centre, Ministry of Water Resources, Beijing, China (fanbo@mwr.gov.cn)

Traditional physical barriers for mitigating seawater intrusion are expensive and necessitate complex engineering measures such as excavation or piledriving. An alternative cost-effective method involves artificially reducing the hydraulic conductivity in the upper parts of selected areas (modified zones) using a precipitate. This study presents an analytical solution using the finite Fourier Cosine transform to evaluate the impact of a modified zone on mitigating seawater intrusion and improving the maximum sustainable withdrawal rate in a coastal confined aquifer. Numerical solutions employing the variable density flow code SEAWAT are conducted to validate the proposed analytical solution. Effects of hydraulic conductivity, length, and thickness of the modified zone, along with the well location on the interface toe location and maximum sustainable withdrawal rate are investigated. Additionally, the sensitivities of dimensionless parameters are accessed under various combinations of the length and thickness of the modified zone. Results show that the interface toe shifts inland with an increase in the dimensionless equivalent hydraulic conductivity (κ) and a decrease in the dimensionless length of the modified zone (lD). Consequently, the maximum sustainable withdrawal rate increases as κ decreases and lD increases. The location of the pumping well significantly influences the maximum sustainable withdrawal rate in aquifers with finite domains, considering both inland and lateral boundary conditions. Sensitivities of β = L/W and η = K1H2/(qf L) to the maximum sustainable withdrawal rate are an order of magnitude greater than the sensitivity of αT,D = αT/H, considering aquifer length (L), aquifer width (W), aquifer hydraulic conductivity (K1), aquifer thickness (H), constant inland flux (qf), and transverse dispersivity (αT). These findings offer valuable insights for constructing modified zones to migrate seawater intrusion and for deploying pumping wells in coastal areas.

How to cite: Sun, J., Fan, B., and Lu, C.: Effects of Artificially Reducing Hydraulic Conductivity of Coastal Aquifers on Maximum Sustainable Withdrawal Rate, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-2205, https://doi.org/10.5194/egusphere-egu24-2205, 2024.